云开地块印支期变质-深熔作用:混合岩、片麻岩锆石U-Pb年代学和Hf同位素证据

柯贤忠; 周岱; 龙文国; 王晶; 徐德明; 田洋; 金巍

doi:10.3799/dqkx.2018.574

云开地块印支期变质-深熔作用:混合岩、片麻岩锆石U-Pb年代学和Hf同位素证据

doi: 10.3799/dqkx.2018.574

中国地质调查局武汉地质调查中心, 湖北武汉 430205

基金项目:

中国地质调查局项目 DD20160031

中国地质调查局项目 12120114039201

中国地质调查局项目 12120113066400

中国地质调查局项目 DD20160035

详细信息

作者简介:
柯贤忠(1984-), 男, 助理研究员, 博士, 主要从事区域地质调查及研究工作

中图分类号: P597
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出版历程
- 收稿日期: 2017-10-16
- 刊出日期: 2018-07-15

Indosinian Metamorphism and Anatexis in Yunkai Massif: Evidences from Zircon Geochronology and Hf Isotopes of Migmatites and Gneisses

Wuhan Center of China Geological Survey, Wuhan 430205, China

摘要

摘要: 云开地块中生代构造演化是华南地区的研究热点之一.通过对云开地块变质基底中的混合岩、片麻岩（5个样品）和花岗岩（1个样品）开展锆石LA-ICP-MS U-Pb定年，获得440.3±3.3 Ma、230.2±2.9 Ma、230.7±1.3 Ma、459.5±2.7 Ma、431.5±4.3 Ma、229.2±5.4 Ma、229.7±2.7 Ma 7组变质（深熔）或岩浆年龄和2组（样品1432-1和ID7-3）碎屑锆石年龄，碎屑锆石年龄范围均为太古代-新元古代，且具有~1.0 Ga年龄主峰，与天堂山岩群和云开群碎屑锆石年龄谱相似.区域资料表明云开地块天堂山岩群和云开群具有相似的物质组成，均形成于早古生代-新元古代，存在变质程度和物质面貌的差异；在加里东期构造-热事件的基础上，广泛叠加了印支期区域变质（深熔）-构造-流体作用影响.4个样品中（1431-1、1432-1、D116-3和ID7-3）锆石原位Lu-Hf同位素组成显示，加里东期变质和深熔锆石Lu/Hf同位素组成基本一致，应继承了原岩的同位素组成特征.印支期变质和深熔锆石Lu/Hf同位素组成不同，可能主要由变质作用和深熔作用的差异所致.以古-中元古代为主的地壳物质参与了加里东期和印支期变质-深熔作用，在加里东期和印支期深熔作用过程中，均有少量幔源物质的加入，印支期幔源物质的贡献相对显著.
- 锆石U-Pb年代学 /
- Hf同位素 /
- 变质-深熔作用 /
- 印支期 /
- 云开地块 /
- 地球化学
Abstract: The Mesozoic tectonic evolution in Yunkai massif has always been one of hot topics in South China. Zircons from five metamorphic rocks including migmatite and gneiss and one granite from the metamorphic basement in Yunkai massif were measured by the LA-ICP-MS U-Pb dating method, yielding 7 metamorphic (anatectic) or magmatic ages (440.3±3.3 Ma, 230.2±2.9 Ma, 230.7±1.3 Ma, 459.5±2.7 Ma, 431.5±4.3 Ma, 229.2±5.4 Ma, 229.7±2.7 Ma) and 2 groups of detrital ages. Both the detrital zircons showed Archaean-Neoproterozoic age range with~1.0 Ga age peaks, which were similar with those of the Tiantangshan Group and the Yunkai Group. Together with the regional data, it was concluded that the Tiantangshan Group and the Yunkai Group, which were analogous in provenance and formed in Early Palaeozoic-Neoproterozoic, were broadly overprinted by the Indosinian metamorphism (anatexis)-deformation-fluid activities after the Caledonian tectonic-thermal events, resulting in differences in metamorphic grade and appearance. In situ zircon Lu-Hf isotopic analysis from four samples show that both the isotopic compositions of Caledonian metamorphic and anatectic zircons were similar with each other, which was ascribed to inheriting the compositions of provenance rocks, whereas the different isotopic compositions of Indosinian metamorphic and anatectic zircons could have been caused by individual mechanism of metamorphic and anatectic processes. It was inferred that the dominant Paleo-Mesoproterozoic crustal material played important role in the metamorphism and anatexis processes in Caledonian and Indosinian, and a few mantle-derived material was added in the anatectic processes in Caledonian and Indosinian with relatively remarkable contribution of mantle-derived material in Indosinian.
- zircon U-Pb geochronology /
- Hf isotopes /
- metamorphism-anatexis /
- Indosinian /
- Yunkai massif /
- geochemistry

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图 1 云开地区地质简图及采样位置

图a据Wang et al.(2013b)；图b据邱元禧等(2006)；Chen et al.(2017)

Fig. 1. Simplified geological map of the Yunkai region and the sampling localities

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图 2 变质岩宏观和微观照片

a, f.眼球状混合片麻岩(1431-1)；b, g.条带状混合片麻岩(1432-1)；c, h.混合岩(D116-3)；d.花岗质片麻岩(15BR04)；e.条带状混合岩(ID7-3)、花岗岩脉(ID7-5)；i.条带状混合岩(ID7-3)；j.花岗岩脉(ID7-5)；Qz.石英；Pl.斜长石；Kfs.钾长石；Mic.微斜长石；Bt.黑云母；Mus.白云母

Fig. 2. Macro- and micro-photographs of the metamorphic rocks in Yunkai massif

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图 3 云开地块变质岩典型锆石阴极发光(CL)图像

Fig. 3. Cathodoluminescence (CL) images of representative zircons from the metamorphic rocks in Yunkai massif

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图 4 云开地块变质岩锆石U-Pb谐和图

Fig. 4. Concordia diagrams of zircon U-Pb data for the metamorphic rocks in Yunkai massif

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图 5 样品D116-3变质锆石与深熔锆石Th/U值(a)和稀土配分曲线(b)

Fig. 5. Th/U ratios and REE distribution pattern of the metamorphic and anatectic zircons from sample D116-3

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图 6 云开地区变质岩锆石Hf同位素图解

a.t-ε_Hf图解；b. ¹⁷⁶Lu/¹⁷⁷Hf-¹⁷⁶Hf/¹⁷⁷Hf图解；c.ε_Hf和T_DM2分布直方图

Fig. 6. Hf isotopic diagrams of zircon from metamorphic rocks in Yunkai region

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图 7 云开地区印支期不同类型变质年龄分布直方图

Fig. 7. Histograms of differetnt types of Indosinian metamorphic age in Yunkai region

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表 1 云开地块变质岩LA-ICP-MS锆石U-Th-Pb同位素分析结果

Table 1. Zircon U-Th-Pb isotopic compositions of metamorphic rocks in Yunkai massif

点号	位置	Th (10^-6)	U (10^-6)	Th/ U	同位素比值						表面年龄(Ma)						谐和度 (%)
点号	位置	Th (10^-6)	U (10^-6)	Th/ U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	谐和度 (%)
1431-1(眼球状混合片麻岩)，核-边结构为主，少量核-幔-边结构
1	m	80	286	0.28	0.055 7	0.002 4	0.554 5	0.024 6	0.071 9	0.000 9	443	129	448	16.1	448	5.3	99
2	c	152	271	0.56	0.057 7	0.002 5	0.556 1	0.023 3	0.069 6	0.000 7	517	94.4	449	15.2	434	4.2	96
3	c	89	347	0.26	0.057 4	0.002 2	0.569 8	0.021 5	0.071 5	0.000 7	506	83.3	458	13.9	445	4.3	97
4	c	172	335	0.51	0.058 1	0.002 5	0.582 9	0.024 5	0.072 3	0.000 9	532	99.1	466	15.7	450	5.3	96
5	c	59	313	0.19	0.057 2	0.002 2	0.565 2	0.021 8	0.070 9	0.000 7	502	85.2	455	14.1	442	4.5	97
6	c	49	305	0.16	0.056 2	0.002 4	0.534 1	0.022 9	0.068 8	0.000 9	461	96.3	435	15.2	429	5.4	98
7	c	93	368	0.25	0.058 3	0.002 1	0.553 4	0.020 0	0.068 5	0.000 7	543	77.8	447	13.1	427	4.2	95
8	c	115	218	0.53	0.056 2	0.002 5	0.551 3	0.024 7	0.071 3	0.000 9	461	100.0	446	16.1	444	5.5	99
9	c	882	606	1.45	0.059 1	0.002 2	0.582 2	0.021 4	0.071 3	0.000 9	572	81.5	466	13.7	444	5.3	95
10	c	60	304	0.20	0.056 4	0.002 9	0.541 1	0.027 7	0.069 3	0.001 0	478	119	439	18.3	432	5.8	98
11	c	76	181	0.42	0.060 8	0.003 4	0.584 5	0.032 9	0.070 7	0.001 2	632	119	467	21.1	440	7.3	94
12	c	65	200	0.33	0.052 9	0.002 9	0.494 7	0.026 4	0.068 0	0.000 8	324	124	408	17.9	424	5.0	96
13	c	61	573	0.11	0.057 1	0.002 2	0.553 3	0.021 3	0.069 9	0.000 8	494	83.3	447	13.9	436	4.6	97
14	c	61	330	0.19	0.057 5	0.002 2	0.570 4	0.022 2	0.071 6	0.000 8	509	78.7	458	14.4	446	4.9	97
15	c	91	428	0.21	0.057 3	0.001 8	0.559 6	0.017 7	0.070 5	0.000 7	502	70.4	451	11.5	439	4.2	97
16	r	20	237	0.08	0.058 3	0.002 7	0.581 1	0.027 1	0.071 9	0.000 8	539	101	465	17.4	448	5.1	96
17	c	125	237	0.53	0.071 5	0.003 6	0.679 6	0.035 0	0.068 4	0.000 8	972	103	527	21.2	426	4.9	79
18	c	44	220	0.20	0.058 8	0.003 0	0.573 5	0.029 8	0.070 2	0.000 9	561	139	460	19.2	438	5.6	94
19	c	59	374	0.16	0.060 0	0.002 5	0.595 3	0.025 4	0.071 4	0.000 8	611	95.4	474	16.2	445	4.9	93
20	c	54	274	0.20	0.055 2	0.002 5	0.553 4	0.024 7	0.072 3	0.000 8	420	102	447	16.1	450	4.5	99
21	c	84	472	0.18	0.055 2	0.002 0	0.540 1	0.019 6	0.070 5	0.000 7	420	81.5	439	12.9	439	4.2	99
22	r	0	12.6	0.01	0.000 0	0.000 0	0.376 6	0.223 2	0.040 2	0.002 4			325	165	254	15	75
23	c	54	262	0.20	0.058 5	0.002 6	0.564 8	0.024 7	0.069 9	0.000 8	550	96.3	455	16.0	436	4.6	95
24	c	69	255	0.27	0.055 2	0.002 5	0.553 4	0.025 5	0.072 5	0.000 8	420	102	447	16.7	451	5.0	99
25	c	72	344	0.21	0.055 7	0.002 3	0.550 6	0.022 7	0.071 7	0.000 8	439	92.6	445	14.9	446	4.6	99
26	r	59	97	0.61	0.075 0	0.004 9	0.730 1	0.047 6	0.071 2	0.001 1	1 069	132	557	27.9	443	6.8	77
1432-1(条带状混合片麻岩)，核-幔-边结构为主
1	r	6	642	0.01	0.051 5	0.001 8	0.256 0	0.008 5	0.036 0	0.000 4	265	79.6	231	6.9	228	2.5	98
2	c	182	354	0.51	0.101 2	0.001 7	3.895 3	0.067 7	0.277 5	0.002 2	1 656	31.8	1 613	14.1	1 579	10.9	97
3	c	142	229	0.62	0.078 1	0.001 8	1.856 4	0.041 0	0.171 8	0.001 5	1 150	44.4	1 066	14.6	1 022	8.1	95
4	m	4	421	0.01	0.051 7	0.002 1	0.265 1	0.011 0	0.037 0	0.000 4	272	96.3	239	8.8	234	2.3	98
5	r	176	290	0.61	0.147 1	0.002 7	8.255 9	0.146 3	0.404 6	0.003 0	2 313	31.2	2 259	16.1	2 190	14.0	96
6	c	514	2 784	0.18	0.093 4	0.001 7	1.865 4	0.040 4	0.143 3	0.001 7	1 496	35.2	1 069	14.3	863	9.3	78
7	c	567	629	0.90	0.074 3	0.001 6	1.779 9	0.038 4	0.172 4	0.001 5	1 050	47.2	1 038	14.0	1 025	8.2	98
8	r	62	646	0.10	0.078 0	0.001 9	1.741 4	0.044 1	0.160 5	0.001 8	1 147	48.1	1 024	16.3	960	10.0	93
9	r	2	272	0.01	0.058 1	0.003 2	0.287 2	0.015 4	0.035 9	0.000 4	532	122	256	12.2	227	2.7	88
10	c	557	894	0.62	0.133 7	0.002 6	6.623 6	0.124 6	0.356 1	0.002 5	2 147	33.3	2 062	16.6	1 964	12.1	95
11	c	328	1 292	0.25	0.069 6	0.001 3	1.428 1	0.027 3	0.147 5	0.001 1	917	38.9	901	11.4	887	6.3	98
12	r	2.46	322	0.01	0.045 7	0.002 5	0.227 2	0.012 2	0.036 3	0.000 4			208	10.1	230	2.7	89
13	c	69	563	0.12	0.140 1	0.002 5	7.334 8	0.131 9	0.375 9	0.003 0	2 228	30.1	2 153	16.1	2 057	13.9	95
14	r	3	332	0.01	0.046 3	0.002 5	0.228 4	0.012 0	0.036 0	0.000 4	16.8	125.915	209	9.9	228	2.3	91
15	r	15	384	0.04	0.055 5	0.002 0	0.504 9	0.023 7	0.064 8	0.002 1	432	81.5	415	16.0	405	12.9	97
16	c	74	70	1.06	0.200 1	0.004 7	14.352 1	0.332 2	0.516 8	0.005 2	2 827	38.9	2 773	22.1	2 685	22.3	96
17	c	362	800	0.45	0.060 0	0.001 5	0.830 1	0.020 8	0.099 3	0.000 9	606	53.7	614	11.6	610	5.1	99
18	r	70	289	0.24	0.068 1	0.002 9	0.939 3	0.035 8	0.100 6	0.001 2	872	91.7	673	18.8	618	7.1	91
19	c	145	257	0.57	0.067 6	0.001 6	1.433 0	0.033 8	0.152 8	0.0014	857	50.5	903	14.1	917	7.6	98
20	r	102	401	0.25	0.067 3	0.001 5	1.231 6	0.027 9	0.132 0	0.001 4	856	46.3	815	12.7	799	7.9	98
21	c	76	323	0.23	0.066 5	0.001 4	1.469 4	0.031 1	0.159 2	0.001 2	833	44.4	918	12.8	953	6.9	96
22	c	629	439	1.43	0.067 3	0.001 4	1.549 2	0.032 1	0.166 1	0.001 3	856	-156.5	950	12.8	991	7.3	95
23	r	19	455	0.04	0.053 1	0.002 0	0.371 4	0.013 6	0.050 7	0.000 5	332	87.0	321	10.1	319	3.3	99
24	r	5	383	0.01	0.052 4	0.002 1	0.352 8	0.014 3	0.048 8	0.000 6	302	90.7	307	10.7	307	3.8	99
25	c	176	265	0.66	0.052 9	0.001 7	0.730 7	0.023 5	0.099 9	0.001 0	324	74.1	557	13.8	614	6.0	90
26	c	64	112	0.57	0.068 8	0.002 3	1.608 6	0.053 4	0.169 4	0.001 7	894	63.9	974	20.8	1 009	9.2	96
27	c	47	501	0.09	0.055 3	0.001 8	0.485 7	0.016 1	0.063 6	0.000 7	433	72.2	402	11.0	397	4.2	98
28	c	125	221	0.57	0.072 3	0.002 1	1.691 7	0.050 0	0.168 0	0.001 4	994	25.0	1 005	18.9	1 001	8.0	99
29	c	666	611	1.09	0.072 2	0.001 7	1.632 9	0.038 2	0.162 6	0.001 4	991	47.1	983	14.7	971	7.5	98
30	r	4	568	0.01	0.052 6	0.002 1	0.267 1	0.010 9	0.036 6	0.000 4	322	125.0	240	8.7	232	2.4	96
D116-3(混合岩)，核-边或核-幔-边结构
1	r	152	289	0.52	0.052 2	0.003 0	0.259 8	0.013 7	0.036 4	0.000 4	295	127	235	11.0	230	2.6	98
2	r	370	454	0.81	0.071 0	0.001 4	1.681 3	0.033 9	0.170 5	0.001 6	967	40.7	1 001	12.8	1 015	8.7	98
3	r	153	250	0.61	0.050 1	0.002 5	0.255 2	0.012 8	0.036 6	0.000 5	211	121	231	10.4	232	2.8	99
4	c	68	103	0.66	0.060 4	0.005 3	0.308 6	0.027 3	0.038 0	0.000 6	617	189	273	21.2	240	3.7	87
5	c	213	499	0.43	0.099 4	0.002 0	3.976 5	0.076 1	0.288 1	0.002 1	1 613	37.0	1 629	15.6	1 632	10.4	99
6	r	200	290	0.69	0.051 4	0.002 6	0.260 2	0.012 8	0.036 9	0.000 4	257	117	235	10.3	234	2.7	99
7	r	167	239	0.70	0.054 8	0.003 3	0.293 9	0.017 0	0.039 1	0.0004	467	133	262	13.3	247	2.7	94
8	r	100	235	0.42	0.054 0	0.002 9	0.269 2	0.014 0	0.036 8	0.000 5	372	129	242	11.2	233	3.0	96
9	r	55	334	0.16	0.050 4	0.002 5	0.250 1	0.012 2	0.035 9	0.000 4	213	114	227	10.0	227	2.4	99
10	r	71	199	0.36	0.193 9	0.007 0	1.430 0	0.057 2	0.052 9	0.000 7	2 776	59.3	902	23.9	332	4.5	7
11	c	197	862	0.23	0.050 8	0.001 5	0.257 2	0.007 5	0.036 6	0.000 3	235	70.4	232	6.1	232	1.9	99
12	r	7	821	0.01	0.0506	0.001 7	0.254 7	0.008 3	0.036 6	0.000 4	233	77.8	230	6.7	232	2.3	99
13	c	1 470	583	2.52	0.070 5	0.001 5	1.518 5	0.032 3	0.155 2	0.001 2	943	43.7	938	13.0	930	6.9	99
14	m	46	72.5	0.63	0.083 6	0.009 9	0.431 6	0.049 6	0.038 5	0.000 9	1 283	233	364	35.2	244	5.5	60
15	r	6	991	0.01	0.051 0	0.001 9	0.254 1	0.008 9	0.036 1	0.000 3	239	83.3	230	7.2	228	1.8	99
16	r	65	587	0.11	0.051 9	0.002 3	0.260 1	0.011 0	0.036 7	0.0004	280	106.5	235	8.8	232	2.7	98
17	r	6	918	0.01	0.051 5	0.001 8	0.256 0	0.008 6	0.036 1	0.000 3	261	75.0	231	7.0	228	2.2	98
18	c	33	574	0.06	0.069 5	0.001 7	1.282 5	0.030 1	0.133 0	0.001 1	922	48.9	838	13.4	805	6.0	96
19	r	29	902	0.03	0.054 8	0.001 7	0.290 0	0.010 2	0.037 9	0.000 5	467	70.4	259	8.1	240	3.2	92
20	c	133	214	0.62	0.073 8	0.002 0	1.644 9	0.044 4	0.160 7	0.001 4	1 035	59.7	988	17.1	961	7.8	97
21	c	353	46 083	0.01	0.297 0	0.010 3	1.835 1	0.057 6	0.045 2	0.000 7	3 455	54.7	1 058	20.7	285	4.2	-16
22	c	65	163	0.40	0.052 2	0.004 7	0.255 6	0.021 6	0.036 9	0.000 6	300	207	231	17.4	234	3.6	98
23	r	82	125	0.66	0.130 0	0.003 1	6.633 2	0.159 3	0.367 3	0.003 3	2 098	42.3	2 064	21.2	2 017	15.8	97
24	r	180	780	0.23	0.056 5	0.003 5	0.266 1	0.016 5	0.034 0	0.000 4	472	137	240	13.2	215	2.7	89
25	c	220	276	0.80	0.049 0	0.003 8	0.250 0	0.017 2	0.035 9	0.000 5	146	170	227	14.0	228	2.9	99
26	r	19	589	0.03	0.071 2	0.003 5	0.470 9	0.032 6	0.045 3	0.0014	965	100	392	22.5	286	8.5	68
27	r	194	306	0.63	0.050 6	0.003 2	0.252 6	0.015 4	0.036 6	0.000 5	233	144	229	12.5	232	3.1	98
28	r	72	150	0.48	0.050 2	0.005 4	0.251 3	0.025 9	0.036 2	0.000 6	211	224	228	21.0	229	3.6	99
29	r	10	1 038	0.01	0.111 5	0.004 6	0.556 1	0.024 4	0.035 7	0.000 4	1 824	75.2	449	15.9	226	2.3	33
30	c	82	228	0.36	0.160 9	0.003 1	10.185 5	0.199 1	0.456 7	0.003 6	2 466	32.4	2 452	18.2	2 425	15.8	98
31	r	132	265	0.50	0.052 7	0.003 3	0.262 8	0.016 0	0.037 1	0.000 5	322	143	237	12.9	235	3.1	99
15BR04(花岗质片麻岩)，核-边结构为主，少量核-幔-边结构
01	r	217	7 930	0.03	0.051 8	0.001 2	0.276 9	0.006 6	0.038 5	0.000 3	276	53.7	248	5.3	244	1.8	98
02	c	516	792	0.65	0.055 7	0.002 0	0.581 1	0.021 0	0.075 2	0.000 7	443	76.8	465	13.5	467	4.1	99
03	r	1 582	18 896	0.08	0.083 2	0.001 6	0.420 3	0.008 2	0.036 4	0.000 3	1 273	37.5	356	5.9	231	1.9	57
04	c	723	907	0.80	0.055 8	0.001 9	0.571 1	0.019 6	0.073 8	0.000 7	443	74.1	459	12.7	459	4.3	99
05	c	592	880	0.67	0.054 7	0.002 2	0.560 3	0.022 8	0.074 1	0.000 8	398	90.7	452	14.8	461	4.9	98
06	r	1 090	11 359	0.10	0.060 3	0.001 4	0.360 3	0.008 1	0.043 1	0.000 3	613	50.0	312	6.1	272	2.0	86
07	c	683	1 261	0.54	0.055 8	0.001 7	0.575 5	0.018 2	0.074 3	0.000 9	456	66.7	462	11.7	462	5.4	99
08	c	530	1 007	0.53	0.055 8	0.001 9	0.579 8	0.020 1	0.075 1	0.000 8	456	75.9	464	12.9	467	4.6	99
09	r	1 652	15 414	0.11	0.061 7	0.001 8	0.311 1	0.009 4	0.036 4	0.0004	665	63.0	275	7.3	230	2.2	82
10	c	523	1 152	0.45	0.073 1	0.002 5	0.675 9	0.023 8	0.066 9	0.000 9	1 017	68.5	524	14.4	417	5.5	77
11	c	512	1 060	0.48	0.058 3	0.002 0	0.684 5	0.023 0	0.085 0	0.000 8	543	74.1	529	13.8	526	4.7	99
12	c	356	889	0.40	0.057 3	0.001 8	0.579 2	0.018 1	0.073 1	0.000 8	502	66.7	464	11.7	455	4.7	97
13	c	1 092	1 519	0.72	0.055 2	0.001 4	0.562 0	0.014 9	0.073 5	0.000 6	420	57.4	453	9.7	457	3.5	99
14	c	661	930	0.71	0.055 0	0.001 6	0.557 0	0.016 2	0.073 2	0.000 7	413	64.8	450	10.6	455	4.0	98
15	c	344	519	0.66	0.053 5	0.002 0	0.539 8	0.020 1	0.073 4	0.0009	350	85.2	438	13.2	457	5.2	95
16	r	1 060	10 099	0.10	0.060 7	0.001 5	0.304 0	0.006 7	0.036 3	0.000 3	628	51.8	269	5.3	230	1.9	84
17	r	3 416	15 123	0.23	0.075 0	0.002 1	0.381 7	0.010 1	0.036 8	0.000 3	1 133	54.5	328	7.5	233	2.1	65
18	r	97	5 303	0.02	0.052 8	0.001 4	0.313 9	0.008 7	0.042 9	0.000 5	320	65.7	277	6.7	271	3.4	97
19	r	296	16 710	0.02	0.057 6	0.001 3	0.288 7	0.007 0	0.036 0	0.000 4	517	50.0	258	5.5	228	2.3	87
20	r	381	9 853	0.04	0.055 4	0.001 3	0.321 7	0.007 3	0.041 9	0.000 4	428	51.8	283	5.6	264	2.2	93
21	r	602	19 102	0.03	0.211 9	0.004 8	1.597 8	0.041 1	0.053 9	0.000 6	2 920	41.8	969	16.1	339	3.4	3
22	r	1 797	26 530	0.07	0.072 1	0.001 5	0.293 1	0.006 0	0.029 2	0.000 2	991	41.8	261	4.7	186	1.5	66
23	c	1 819	2 348	0.77	0.057 3	0.001 4	0.585 5	0.014 5	0.073 4	0.000 7	506	58.3	468	9.3	457	4.3	97
24	r	1 162	26 617	0.04	0.071 3	0.001 5	0.261 4	0.005 6	0.026 5	0.000 3	966	42.6	236	4.5	169	2.2	66
ID7-3(条带状混合岩)，核-边或核-幔-边结构
1	r	115	297	0.39	0.175 6	0.006 0	9.480 6	0.315 5	0.383 9	0.004 0	2 613	90	2 386	31	2 095	19	87
2	c	235	491	0.48	0.177 9	0.005 1	9.188 3	0.265 6	0.367 6	0.003 8	2 635	48	2 357	27	2 018	18	84
3	r	13	1 102	0.01	0.053 3	0.002 0	0.274 7	0.009 9	0.037 1	0.000 4	339	92	246	8	235	2	95
4	r	131	2 373	0.06	0.051 5	0.001 5	0.494 6	0.014 7	0.068 6	0.000 7	265	69	408	10	427	4	95
5	c	30	1 662	0.02	0.050 4	0.001 8	0.259 2	0.009 3	0.036 7	0.000 4	217	85	234	8	233	3	99
6	r	67	1 375	0.05	0.059 3	0.001 7	0.856 5	0.030 1	0.102 3	0.002 0	589	58	628	16	628	12	99
7	r	130	222	0.59	0.066 7	0.002 6	1.046 6	0.042 0	0.112 0	0.001 6	828	80	727	21	684	9	93
8	r	214	1 045	0.21	0.054 8	0.001 7	0.526 2	0.015 4	0.068 7	0.000 6	467	73	429	10	428	3	99
9	r	176	461	0.38	0.050 4	0.002 0	0.489 5	0.019 7	0.069 4	0.000 8	213	91	405	13	433	5	93
10	r	45	1 042	0.04	0.116 4	0.003 0	4.951 6	0.139 6	0.301 4	0.003 5	1 902	47	1 811	24	1 698	17	93
11	r	287	463	0.62	0.053 9	0.002 3	0.512 1	0.021 1	0.068 5	0.000 7	369	64	420	14	427	4	98
12	r	177	206	0.86	0.059 7	0.003 4	0.566 3	0.031 9	0.068 8	0.000 9	591	131	456	21	429	6	93
13	c	93	254	0.37	0.054 5	0.003 2	0.565 9	0.032 9	0.074 4	0.000 9	394	133	455	21	462	5	98
14	r	36	2 519	0.01	0.052 2	0.001 7	0.254 5	0.008 0	0.034 8	0.000 3	300	74	230	6	221	2	95
15	r	103	218	0.47	0.053 7	0.003 4	0.5383	0.035 4	0.071 7	0.001 3	367	143	437	23	446	8	97
16	c	381	1 148	0.33	0.074 6	0.001 8	1.815 9	0.043 9	0.173 6	0.001 4	1 057	49	1 051	16	1 032	8	98
17	c	118	271	0.44	0.057 6	0.003 1	0.566 3	0.030 6	0.070 6	0.000 9	522	121	456	20	440	6	96
18	r	449	607	0.74	0.059 8	0.002 2	0.576 6	0.020 6	0.069 3	0.000 7	594	77	462	13	432	4	93
19	c	156	484	0.32	0.070 9	0.002 2	1.602 9	0.048 3	0.161 4	0.001 7	955	62	971	19	965	9	99
20	r	276	645	0.43	0.096 1	0.002 9	3.545 5	0.103 1	0.263 6	0.002 3	1 550	57	1 537	23	1 508	12	98
21	c	10	670	0.02	0.055 2	0.003 2	0.283 5	0.018 0	0.036 7	0.000 9	420	130	253	14	232	5	91
22	r	31	2 248	0.01	0.052 3	0.001 7	0.263 0	0.008 5	0.036 0	0.000 3	298	69	237	7	228	2	96
23	r	91	506	0.18	0.072 6	0.002 1	1.468 1	0.040 6	0.145 2	0.001 2	1 011	58	917	17	874	7	95
24	c	217	265	0.82	0.092 4	0.002 6	3.341 2	0.092 6	0.259 1	0.002 3	1 476	53	1 491	22	1 485	12	99
25	r	23	2 020	0.01	0.048 6	0.0014	0.251 0	0.007 3	0.037 0	0.000 3	128	67	227	6	234	2	97
26	c	197	521	0.38	0.074 0	0.002 0	1.675 0	0.044 4	0.162 6	0.001 7	1 043	54	999	17	971	9	97
27	r	418	1 465	0.29	0.052 5	0.001 4	0.550 6	0.015 6	0.075 3	0.000 8	306	63	445	10	468	5	95
28	r	111	116	0.96	0.057 4	0.003 5	0.976 4	0.059 0	0.124 3	0.001 8	509	137	692	30	755	10	91
29	r	215	566	0.38	0.052 4	0.002 1	0.496 4	0.020 2	0.067 7	0.000 7	306	89	409	14	422	4	96
30	c	326	461	0.71	0.069 1	0.002 0	1.524 3	0.043 9	0.158 3	0.001 4	903	59	940	18	947	8	99
31	r	88	2 692	0.03	0.053 5	0.001 4	0.507 9	0.012 8	0.068 2	0.000 6	350	53	417	9	425	3	98
32	m	23	592	0.04	0.057 9	0.001 9	0.762 7	0.025 1	0.094 7	0.000 9	528	74	576	14	583	5	98
33	r	89	2 138	0.04	0.055 9	0.001 4	0.520 0	0.013 4	0.066 8	0.000 6	456	56	425	9	417	3	97
34	r	7	618	0.01	0.056 1	0.002 8	0.325 3	0.016 2	0.041 9	0.000 7	454	109	286	12	264	4	92
35	c	443	523	0.85	0.056 7	0.002 1	0.541 3	0.020 0	0.069 0	0.000 7	480	83	439	13	430	4	97
36	r	89	1 464	0.06	0.058 1	0.001 9	0.558 2	0.018 6	0.069 0	0.000 6	532	75	450	12	430	4	95
37	r	102	212	0.48	0.062 6	0.002 9	1.005 9	0.047 5	0.116 1	0.001 5	694	100	707	24	708	9	99
38	c	173	203	0.85	0.070 2	0.002 8	1.595 8	0.061 8	0.165 2	0.001 8	1 000	82	969	24	986	10	98
39	r	186	328	0.57	0.061 9	0.002 7	0.600 1	0.026 9	0.069 9	0.000 8	733	94	477	17	436	5	90
40	r	10	1 245	0.01	0.053 5	0.001 7	0.487 4	0.015 3	0.065 6	0.000 5	350	70	403	10	409	3	98
41	c	190	295	0.64	0.060 4	0.0028	0.588 3	0.026 6	0.071 1	0.000 8	620	100	470	17	443	5	94
42	r	5	416	0.01	0.055 4	0.003 2	0.275 0	0.015 2	0.036 4	0.000 4	428	126	247	12	231	3	93
ID7-5(花岗岩脉)，核-边结构
1	r	92	1 103	0.08	0.050 4	0.001 8	0.255 8	0.008 8	0.036 6	0.000 4	213	86.1	231	7	232	2	99
2	c	78	1 323	0.06	0.067 3	0.001 8	1.130 8	0.030 2	0.120 6	0.001 2	856	55.6	768	14	734	7	95
3	r	41	668	0.06	0.056 1	0.001 9	0.545 1	0.020 3	0.069 6	0.001 1	454	69.4	442	13	434	7	98
4	r	23.5	973	0.02	0.050 0	0.002 0	0.248 2	0.009 6	0.035 8	0.000 3	195	92.6	225	8	227	2	99
5	r	140	436	0.32	0.064 3	0.002 5	0.624 4	0.027 9	0.069 2	0.001 8	750	83.3	493	17	431	11	86
6	r	102	1 068	0.10	0.050 2	0.0018	0.261 5	0.009 6	0.037 4	0.000 4	211	85.2	236	8	237	2	99
7	r	295	1 157	0.26	0.050 0	0.001 8	0.244 0	0.008 6	0.035 1	0.000 3	195	83.3	222	7	222	2	99
8	r	415	833	0.50	0.050 8	0.002 1	0.252 8	0.010 5	0.035 8	0.000 4	232	98.1	229	9	227	2	99
9	r	340	1 456	0.23	0.050 3	0.001 8	0.248 1	0.008 4	0.035 6	0.000 4	209	81.5	225	7	225	2	99
10	r	305	1 450	0.21	0.050 6	0.001 8	0.255 7	0.009 1	0.036 3	0.000 3	220	50.9	231	7	230	2	99
11	c	433	1 140	0.38	0.056 0	0.002 0	0.273 8	0.009 6	0.035 4	0.000 3	450	79.6	246	8	224	2	90
12	r	212	6 335	0.03	0.054 1	0.001 7	0.264 5	0.009 1	0.035 2	0.000 5	376	76.8	238	7	223	3	93
13	r	298	653	0.46	0.056 2	0.002 7	0.289 8	0.013 9	0.037 4	0.000 4	461	106	258	11	237	3	91
14	r	229	524	0.44	0.052 8	0.003 0	0.263 5	0.015 0	0.036 3	0.000 4	320	134	238	12	230	3	96
15	r	235	611	0.38	0.052 0	0.002 7	0.262 6	0.014 0	0.036 6	0.000 4	283	150	237	11	232	3	97
16	r	932	3 530	0.26	0.053 2	0.002 2	0.271 3	0.011 7	0.036 9	0.000 4	339	94.4	244	9	233	2	95
17	r	256	580	0.44	0.053 9	0.003 0	0.276 6	0.015 9	0.037 3	0.000 5	369	132	248	13	236	3	95
18	r	108	851	0.13	0.062 9	0.002 3	0.614 4	0.024 9	0.070 7	0.001 4	706	75.0	486	16	440	8	90
19	r	239	606	0.39	0.049 1	0.002 4	0.255 0	0.012 5	0.037 5	0.000 4	154	115	231	10	237	3	97
20	r	147	308	0.48	0.051 0	0.003 8	0.257 5	0.018 9	0.036 5	0.000 5	239	203	233	15	231	3	99
注：c.锆石核部；m.锆石幔部；r.锆石边部.

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表 2 云开地块变质岩锆石Lu-Hf同位素分析结果

Table 2. Zircon Lu-Hf isotopic compositions of metamorphic rocks in Yunkai massif

点号	年龄(Ma)	¹⁷⁶Hf/¹⁷⁷Hf	2σ	¹⁷⁶Lu/¹⁷⁷Hf	¹⁷⁶Yb/¹⁷⁷Hf	ε_Hf(t)	T_DM1(Ma)	T_DM2(Ma)	f_Lu/Hf
1431-1(眼球状混合片麻岩)
01	448	0.282 468	0.000 015	0.001 753	0.046 160	-1.4	1 132	1 520	-0.95
02	434	0.282 294	0.000 018	0.001 041	0.026 061	-7.7	1 355	1 905	-0.97
03	445	0.282 437	0.000 020	0.001 418	0.037 749	-2.5	1 167	1 585	-0.96
04	450	0.282 624	0.000 016	0.002 280	0.059 929	4.0	921	1 178	-0.93
05	442	0.282 428	0.000 015	0.001 235	0.031 850	-2.8	1 173	1 603	-0.96
06	429	0.282 437	0.000 016	0.001 495	0.038 807	-2.8	1 168	1 594	-0.95
07	427	0.282 591	0.000 017	0.002 563	0.068 942	2.3	977	1 268	-0.92
08	444	0.282 320	0.000 015	0.000 879	0.022 018	-6.5	1 313	1 837	-0.97
09	444	0.282 639	0.000 032	0.002 762	0.072 882	4.2	912	1 157	-0.92
10	432	0.282 499	0.000 015	0.001 887	0.048 346	-0.7	1 091	1 461	-0.94
11	440	0.282 342	0.000 013	0.000 860	0.021 631	-5.8	1 282	1 790	-0.97
12	424	0.282 478	0.000 012	0.001 527	0.039 823	-1.5	1 111	1 507	-0.95
13	436	0.282 563	0.000 016	0.002 470	0.062 280	1.5	1 016	1 326	-0.93
14	446	0.282 588	0.000 017	0.002 427	0.063 446	2.6	978	1 264	-0.93
15	439	0.282 566	0.000 022	0.002 209	0.057 846	1.7	1 003	1 312	-0.93
16	448	0.282 472	0.000 014	0.001 320	0.032 147	-1.2	1 113	1 502	-0.96
17	426	0.282 350	0.000 016	0.001 316	0.033 605	-5.9	1 286	1 789	-0.96
18	438	0.282 485	0.000 015	0.001 825	0.048 092	-1.1	1 110	1 488	-0.95
19	445	0.282 417	0.000 017	0.001 223	0.031 860	-3.1	1 188	1 625	-0.96
20	450	0.282 496	0.000 015	0.002 040	0.053 560	-0.5	1 101	1 461	-0.94
21	439	0.282 416	0.000 021	0.001 765	0.046 068	-3.4	1 207	1 641	-0.95
23	436	0.282 439	0.000 015	0.001 318	0.034 035	-2.6	1 160	1 583	-0.96
24	451	0.282 492	0.000 014	0.001 525	0.039 717	-0.4	1 091	1 460	-0.95
25	446	0.282 521	0.000 015	0.001 872	0.049 339	0.4	1 059	1 403	-0.94
26	443	0.282 448	0.000 014	0.001 409	0.037 540	-2.1	1 150	1 560	-0.96
1432-1(条带状混合片麻岩)
01	228	0.281 936	0.000 048	0.000 262	0.006 999	-24.6	1 816	2 816	-0.99
02	1 656	0.281 558	0.000 014	0.000 564	0.014 335	-6.8	2 346	2 772	-0.98
03	1 150	0.281 836	0.000 014	0.000 407	0.009 754	-8.0	1 960	2 464	-0.99
04	234	0.282 257	0.000 018	0.000 224	0.006 124	-13.1	1 377	2 098	-0.99
05	2 313	0.281 723	0.000 016	0.002 010	0.049 768	11.6	2 203	2 143	-0.94
06	863	0.281 635	0.000 012	0.001 300	0.034 471	-21.9	2 285	3 117	-0.96
07	1 050	0.282 242	0.000 022	0.001 906	0.050 251	3.1	1 461	1 692	-0.94
08	960	0.282 154	0.000 016	0.000 704	0.018 665	-1.1	1 537	1 890	-0.98
09	227	0.282 011	0.000 028	0.000 268	0.006 986	-22.0	1 715	2 652	-0.99
12	230	0.282 312	0.000 015	0.000 143	0.003 990	-11.3	1 299	1 978	-1.00
13	2 228	0.281 222	0.000 011	0.000 296	0.008 632	-5.5	2 781	3 128	-0.99
14	228	0.282 298	0.000 012	0.000 514	0.013 413	-11.8	1 330	2 012	-0.98
15	405	0.282 260	0.000 015	0.000 405	0.009 098	-9.3	1 379	1 987	-0.99
16	2 827	0.280 883	0.000 032	0.000 268	0.007 300	-3.8	3 229	3 482	-0.99
17	610	0.282 382	0.000 016	0.000 797	0.021 576	-0.7	1 223	1 595	-0.98
19	917	0.282 145	0.000 024	0.001 189	0.031 299	-2.7	1 569	1 955	-0.96
21	953	0.282 619	0.000 016	0.001 040	0.025 766	15.0	898	866	-0.97
22	991	0.281 988	0.000 013	0.000 902	0.023 044	-6.5	1 775	2 248	-0.97
25	614	0.282 390	0.000 022	0.000 594	0.014 459	-0.2	1 206	1 571	-0.98
26	1 009	0.282 023	0.000 016	0.000 779	0.020 820	-4.7	1 720	2 153	-0.98
27	397	0.282 409	0.000 015	0.000 778	0.021 401	-4.3	1 185	1 663	-0.98
28	1 001	0.282 178	0.000 014	0.000 746	0.019 867	0.6	1 505	1 812	-0.98
29	971	0.282 690	0.000 020	0.003 444	0.094 073	16.4	852	793	-0.90
30	232	0.282 251	0.000 017	0.000 115	0.003 486	-13.3	1 381	2 111	-1.00
D116-3(混合岩)
01	230	0.282 818	0.000 017	0.001 068	0.027 294	6.5	616	847	-0.97
02	1 015	0.282 234	0.000 013	0.001 093	0.030 814	2.7	1 441	1 694	-0.97
03	232	0.282 753	0.000 021	0.001 374	0.035 760	4.2	715	996	-0.96
05	1 612	0.281 877	0.000 017	0.000 671	0.017 897	3.5	1 917	2 103	-0.98
06	234	0.282 923	0.000 016	0.001 621	0.042 230	10.2	474	612	-0.95
07	247	0.282 619	0.000 011	0.000 416	0.010 888	-0.1	884	1 281	-0.99
08	233	0.282 542	0.000 012	0.000 229	0.006 513	-3.0	985	1 459	-0.99
09	227	0.282 537	0.000 017	0.000 726	0.016 422	-3.4	1 005	1 480	-0.98
11	232	0.282 571	0.000 030	0.001 173	0.028 255	-2.2	969	1 404	-0.96
12	232	0.282 420	0.000 014	0.000 977	0.023 338	-7.5	1 177	1 743	-0.97
15	228	0.282 401	0.000 035	0.001 627	0.038 922	-8.4	1 224	1 793	-0.95
17	228	0.282 330	0.000 027	0.001 035	0.026 165	-10.8	1 304	1 946	-0.97
20	961	0.282 257	0.000 015	0.000 612	0.015 639	2.6	1 391	1 655	-0.98
22	234	0.282 516	0.000 011	0.000 128	0.003 789	-4.0	1 019	1 518	-1.00
27	232	0.282 683	0.000 010	0.000 806	0.022 699	1.8	803	1 150	-0.98
28	229	0.282 432	0.000 020	0.000 132	0.003 970	-7.0	1 135	1 710	-1.00
31	235	0.282 617	0.000 018	0.000 565	0.016 434	-0.4	890	1 295	-0.98
ID7-3(条带状混合岩)
01	2613	0.281 283	0.000 013	0.001 097	0.024 874	4.1	2 755	2 839	-0.97
03	235	0.282 155	0.000 011	0.000 090	0.002 561	-16.7	1 511	2 324	-1.00
04	427	0.282 397	0.000 014	0.001 344	0.035 268	-4.3	1 221	1 684	-0.96
05	233	0.282 212	0.000 010	0.000 016	0.000 532	-14.7	1 431	2 198	-1.00
08	428	0.282 513	0.000 009	0.002 136	0.050 505	-0.4	1 079	1 437	-0.94
09	433	0.282 375	0.000 008	0.000 956	0.023 856	-4.8	1 239	1 723	-0.97
11	427	0.282 341	0.000 012	0.000 791	0.019 131	-6.1	1 280	1 798	-0.98
12	429	0.282 325	0.000 011	0.000 962	0.023 720	-6.6	1 308	1 836	-0.97
14	221	0.282 190	0.000 024	0.000 275	0.006 514	-15.8	1 471	2 257	-0.99
15	446	0.282 399	0.000 010	0.001 095	0.026 459	-3.7	1 210	1 664	-0.97
17	440	0.282 392	0.000 010	0.001 256	0.029 347	-4.1	1 224	1 685	-0.96
21	232	0.281 691	0.000 030	0.000 452	0.011 587	-33.2	2 158	3 356	-0.99
22	228	0.282 128	0.000 008	0.000 161	0.004 703	-17.8	1 551	2 389	-1.00
25	234	0.282 216	0.000 021	0.000 147	0.004 027	-14.5	1 430	2 189	-1.00
27	468	0.282 392	0.000 011	0.001 212	0.030 833	-3.5	1 223	1 668	-0.96
29	422	0.282 360	0.000 013	0.001 060	0.025729	-5.6	1 263	1 764	-0.97
33	417	0.282 310	0.000 013	0.001 162	0.027 958	-7.5	1 337	1 881	-0.96
35	430	0.282 490	0.000 014	0.002 036	0.049 664	-1.1	1 109	1 485	-0.94
36	430	0.282 201	0.000 012	0.000 822	0.020 732	-11.0	1 477	2 111	-0.98
39	436	0.282 402	0.000 012	0.001 227	0.029 842	-3.9	1 210	1 665	-0.96
40	409	0.282 271	0.000 010	0.000 735	0.019 771	-8.9	1 376	1 965	-0.98
41	443	0.282 361	0.000 011	0.001 050	0.025 305	-5.1	1 261	1 749	-0.97
42	231	0.282 238	0.000 033	0.000 022	0.000 762	-13.8	1 395	2 140	-1.00

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表 3 云开地区印支期变质年龄统计表

Table 3. Summary of Indosinian metamorphic ages in Yunkai region

样号	岩性	采样位置	数据来源	定年方法	年龄(Ma)	成因分类
1432-1	混合片麻岩	信宜			230.2±2.9	区域变质
D116-3	混合岩	罗定			229.6±2.1	(或深熔)
D116-3	混合岩	罗定	本文	LA-ICPMS锆石U-Pb	231.3±1.6	作用
ID7-3	条带状混合岩	高州			229.2±5.4	流体活动
15BR04	花岗质片麻岩	北流炳荣			244.0±1.8
GD-131	基性麻粒岩	钦州那蒙			238.0±8.0
GD-132	基性麻粒岩	钦州大寺		SHRIMP锆石U-Pb	244.0±7.0
GD-4	含石榴子石角闪岩	高州谢鸡	Wang et al., 2012	SHRIMP锆石U-Pb	230.0±6.0
YK-13	斜长角闪岩	容县黎村			248.0±6.0
YK-9A	混合岩化角闪岩	信宜金垌			221.0±4.0
09YK-8B	正片麻岩	信宜	Wang et al., 2011	LA-ICPMS锆石U-Pb	203.0±10.0
09YK-12	正片麻岩	容县黎村	Wang et al., 2011		239.0±6.0
02YK-42	正片麻岩	电白	Wang et al., 2007d	SHRIMP锆石U-Pb	236.0±3.0
L114	矽线石榴堇青片麻岩	云开	Wan et al., 2010	SHRIMP锆石U-Pb	242.0±8.0
GZ-0307	片麻状混合岩	高州云炉	Wang et al., 2013b	LA-ICPMS锆石U-Pb	241.0±3.0
GZ-08	正片麻岩	高州云炉		LA-ICPMS锆石U-Pb	238.0±4.0
GZ-03	紫苏花岗岩	高州云炉	Chen et al., 2012	电子探针独居石U-Th-Pb	231.0±9.0
23GX-11	副片麻岩	高州云炉		电子探针独居石U-Th-Pb	237.0±13.0
23GX04	黑云母片麻岩	高州	Chen et al., 2017	LA-ICPMS锆石U-Pb	229.0±10.0	区域变质
11GD04	黑云母片麻岩	高州	Chen et al., 2017	LA-ICPMS锆石U-Pb	245.0±5.0	(或深熔)
11GD01	片麻状花岗岩	高州			233.0±4.0	作用
11GDGZA1	片麻状花岗岩	高州			233.0±5.0
23GX04	黑云母片麻岩	高州			237.0±3.0
23GX05-2	黑云母片麻岩	高州			234.0±5.0
23GX15	二云母片麻岩	高州			236.0±4.0
11GD06	二云母片麻岩	高州	Chen et al., 2017	电子探针独居石U-Th-Pb	240.0±4.0
11GD07	片麻状花岗岩	高州	Chen et al., 2017	电子探针独居石U-Th-Pb	233.0±11.0
23GX13-2	黑云母片麻岩	高州			~240.0
23GX14	石榴石电气石片岩	高州			236.0±8.0
11GD03	石榴石电气石片岩	高州			244.0±11.0
11GD04	黑云母片麻岩	高州			236.0±5.0
11GD05	黑云母片麻岩	高州			239.0±6.0
--	泥质麻粒岩	钦州旧州	赵亮等，2010	LA-ICPMS锆石U-Pb	253.0±3.0
hdt-2	基性麻粒岩	钦州大龟山	彭松柏等，2004	SHRIMP锆石U-Pb	248.0±6.0
Datong 1	糜棱岩	合浦			213.0±4.0
Datong 2	糜棱岩	合浦	Zhang and Cai, 2009	白云母Ar-Ar	212.0±3.0
Hetai 1	糜棱岩	北流	Zhang and Cai, 2009	白云母Ar-Ar	199.0±1.0
Hetai 2	糜棱岩	北流			195.0±1.0
02YK-27	糜棱状花岗岩	信宜			230.0±1.0
02YK-30	花岗质糜棱岩	信宜白石			225.0±1.0
02YK-38	糜棱状片麻岩	高州			222.0±1.0
02YK-74	糜棱状副片麻岩	信宜			228.0±1.0
02YK-39	糜棱状混合岩	高州谢鸡			225.0±1.0
02YK-09	糜棱状片麻岩	阳春			208.0±1.0
02YK-12	糜棱状片麻岩	阳春	Wang et al., 2007c	黑云母Ar-Ar	209.0±1.0
02YK-15	糜棱岩	阳春永宁			212.0±1.0	构造变形
02YK-56	花岗质糜棱岩	博白			219.0±1.0
02YK-64	糜棱岩	容县黎村			211.0±1.0
02YK-80	糜棱状花岗岩	罗定榃滨			209.0±1.0
02YK-26	糜棱状片麻岩	信宜钱排			214.0±1.0
02YK-31	糜棱状花岗岩	信宜白石			217.0±1.0
G13Y1	片岩	罗定泗纶	彭少梅等，1996	白云母Ar-Ar	249.0±3.0
G03Y1	片理化片麻状花岗岩	阳春	彭少梅等，1996	白云母Ar-Ar	229.0±2.0
G13Y1	混合岩	罗定泗纶			250.0±3.0
G12Y2	石英片岩质糜棱岩	分界	邵建国等，1995	白云母Ar-Ar	255.0±3.0
G03Y1	糜棱状花岗岩	永宁			229.0±3.0
Jiangshan1	绢云母千糜岩	防城江山	丁汝鑫等，2015	绢云母Ar-Ar	244.8±0.6
Jiangshan2	绢云母千糜岩				203.9±1.7
14HT060	糜棱岩	河台金矿	焦骞骞等，2017	LA-ICPMS锆石U-Pb	240.1±4.1	流体活动
14HT111	糜棱岩	河台金矿	焦骞骞等，2017	LA-ICPMS锆石U-Pb	204.1±4.3

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参考文献(136)

Andersen, T., 2002.Correction of Common Lead in U-Pb Analyses that do not Report ²⁰⁴Pb.Chemical Geology, 192(1-2):59-79.doi: 10.1016/s0009-2541(02)00195-x
Cai, J.X., 2012.Hetai Dextral Ductile Shear Zone, Western Guangdong, and Its Controlling on Formation of Gold Deposit.Geological Review, 58(6):1069-1080 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP201206009.htm
Chen, C.H., Hsieh, P.S., Lee, C.Y., et al., 2011.Two Episodes of the Indosinian Thermal Event on the South China Block:Constraints from LA-ICPMS U-Pb Zircon and Electron Microprobe Monazite Ages of the Darongshan S-Type Granitic Suite.Gondwana Research, 19(4):1008-1023.doi: 10.1016/j.gr.2010.10.009
Chen, C.H., Liu, Y.H., Lee, C.Y., et al., 2012.Geochronology of Granulite, Charnockite and Gneiss in the Poly-Metamorphosed Gaozhou Complex (Yunkai Massif), South China:Emphasis on the In-Situ EMP Monazite Dating.Lithos, 144-145:109-129.doi: 10.1016/j.lithos.2012.04.009
Chen, C.H., Liu, Y.H., Lee, C.Y., et al., 2017.The Triassic Reworking of the Yunkai Massif (South China):EMP Monazite and U-Pb Zircon Geochronologic Evidence.Tectonophysics, 694:1-22.doi: 10.13039/501100001868
Chen, D.G., Ni, T., Xie, L.W., 2007.Zircon Lu-Hf Isotopic Compositions of Ultra-High Pressure Metamorphic Rocks from Dabie Terrain, China.Acta Petrologica Sinica, 23(2):331-342 (in Chinese with English abstract).doi: 10.3969/j.issn.1000-0569.2007.02.013
Chen, H.D., Hou, M.C., Xu, X.S., et al., 2006.Tectonic Evolution and Sequence Stratigraphic Framework in South China during Caledonian.Journal of Chengdu University of Technology, 33(1):1-8 (in Chinese with English abstract).doi: 10.3969/j.issn.1671-9727.2006.01.001
Chen, W.F., Chen, P.R., Huang, H.Y., et al., 2007.Chronological and Geochemical Studies of Granite and Enclave in Baimashan Pluton, Hunan, South China.Science in China (Series D), 37(7):873-893.doi: 10.1007/s11430-007-0073-1
Chu, M.F., Chung, S.L., Song, B., et al., 2006.Zircon U-Pb and Hf Isotope Constraints on the Mesozoic Tectonics and Crustal Evolution of Southern Tibet.Geology, 34(9):745.doi: 10.1130/g22725.1
Deng, X.G., Chen, Z.G., Li, X.H., et al., 2004.SHRIMP U-Pb Zircon Dating of the Darongshan-Shiwandashan.Geological Review, 50(4):426-432.doi: 10.16509/j.georeview.2004.04.017 (in Chinese with English abstract).
Ding, R.X., Zou, H.P., Lao, M.J., et al., 2015.Indosinian Activity Records of Ductile Shear Zones in Southern segment of Qin-Hang Combined Belt:A case Study of Fangcheng-Lingshan Fault Zone.Earth Science Frontiers, 22(2):79-85.doi: 10.13745/j.esf.2015.02.007 (in Chinese with English abstract).
Ding, X., Zhou, X.M., Sun, T., 2005.The Episodic Growth of the Continental Crustal Basement in South China:Single Zircon LA-ICPMS U-Pb Dating of Guzhai Granodiorite in Guangdong.Geological Review, 51 (4):382-392.doi: 10.16509/j.georeview.2005.04.004 (in Chinese with English abstract).
Dong, C.Y., Liu, D.Y., Wan, Y.S., et al., 2009.Hf Isotope Composition and REE Pattern of Zircons from Early Precambrian Metamorphic Rocks in the Daqing Mountains, Inner Mongolia.Geological Review, 55 (4):509-520.doi: 10.16509/j.georeview.2009.04.007 (in Chinese with English abstract).
Dong, C.Y., Zhao, K.D., Jiang, S.Y., et al., 2010.Zircon Geochronology, Geochemistry and Petrogenesis of Granite from the Baimianshi Uranium Ore District in the Southern Jiangxi Province.Geological Journal of China Universities, 16 (2):149-160.doi: 10.3969/j.issn.1006-7493.2010.02.003 (in Chinese with English abstract).
Gong, G.L., Chen, G.H., Lin, G., et al., 2010.Tectonic Stress Field Evolution and Structural Ore Controlling Model of Hetai Gold Deposit, Guangdong.Mineral Deposits, 29(Suppl.2):16-26 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ199302005.htm
Griffin, W.L., Pearson, N.J., Belousova, E., et al., 2000.The Hf Isotope Composition of Cratonic Mantle:LAM-MC-ICPMS Analysis of Zircon Megacrysts in Kimberlites.Geochimica et Cosmochimica Acta, 64(1):133-147.doi: 10.1016/s0016-7037(99)00343-9
Griffin, W.L., Wang, X., Jackson, S.E., et al., 2002.Zircon Chemistry and Magma Mixing, SE China:In-Situ Analysis of Hf Isotopes, Tonglu and Pingtan Igneous Complexes.Lithos, 61(3-4):237-269.doi: 10.1016/s0024-4937(02)00082-8
Han, K.Y., Xu, K.J., Gao, L.Z., et al., 2017.U-Pb Age and Lu-Hf Isotope of Detrital Zircons from the Meta-Sedimentary Rocks in the Yunkai Region and Their Geological Significance.Acta Petrologica Sinica, 33 (9):2939-2956 (in Chinese with English abstract).
He, Z.Y., Xu, X.S., Niu, Y.L., 2010.Petrogenesis and Tectonic Significance of a Mesozoic Granite-Syenite-Gabbro Association from Inland South China.Lithos, 119(3-4):621-641.doi: 10.1016/j.lithos.2010.08.016
Jiao, Q.Q., Xu, D.R., Chen, G.W., et al., 2017.Zircon LA-ICP-MS U-Pb Age of Mylonite in the Hetai Gold Field, Guangdong Province of South China and the Geological Implication.Acta Petrologica Sinica, 33(6):1755-1774 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20170609
Jiao, S.J., Guo, J.H., Peng, S.B., 2013.Petrogenesis of Garnet in the Darongshan-Shiwandashan Granitic Suite of the South China Block and the Metamorphism of the Granulite Enclave.Acta Petrologica Sinica, 29(5):1740-1758 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20130520
Lei, W.Y., Shi, G.H., Liu, Y.X., 2013.Research Progress on Trace Element Characteristics of Zircons of Different Origins.Earth Science Frontiers, 20(4):273-284 (in Chinese with English abstract). https://www.researchgate.net/publication/279571372_Research_progress_on_trace_element_characteristics_of_zircons_of_different_origins
Li, W.W., Wang, G., Chen, W.F., et al., 2010.Geochemical Characteristic and Geological Implications of Xiangcaoping Granite Pluton in Miaoershan Area.Uranium Geology, 26(4):215-227.doi: 10.3969/j.issn.1000-0658.2010.04.004 (in Chinese with English abstract).
Li, X.H., Li, W.X., Li, Z.X., et al., 2008.850-790 Ma Bimodal Volcanic and Intrusive Rocks in Northern Zhejiang, South China:A Major Episode of Continental Rift Magmatism during the Breakup of Rodinia.Lithos, 102(1-2):341-357.doi: 10.1016/j.lithos.2007.04.007
Li, X.H., Li, Z.X., Li, W.X., 2014.Detrital Zircon U-Pb Age and Hf Isotope Constrains on the Generation and Reworking of Precambrian Continental Crust in the Cathaysia Block, South China:A Synthesis.Gondwana Research, 25(3):1202-1215.doi: 10.1016/j.gr.2014.01.003
Li, X.H., Li, Z.X., Li, W.X., et al., 2007.U-Pb Zircon, Geochemical and Sr-Nd-Hf Isotopic Constraints on Age and Origin of Jurassic I-and A-Type Granites from Central Guangdong, SE China:A Major Igneous Event in Response to Foundering of a Subducted Flat-Slab?Lithos, 96(1-2):186-204.doi: 10.1016/j.lithos.2006.09.018
Li, Z.X., Li, X.H., Wartho, J.A., et al., 2010.Magmatic and Metamorphic Events during the Early Paleozoic Wuyi-Yunkai Orogeny, Southeastern South China:New Age Constraints and Pressure-Temperature Conditions.Geological Society of America Bulletin, 122(5-6):772-793.doi: 10.1130/b30021.1
Ling, H.F., Shen, W.Z., Deng, P., et al., 2005.Study of Geochemistry and Petrogenesis of the Maofeng Granite, Northern Guangdong Province.Acta Petrologica Sinica, 21(3):677-687.doi: 10.3969/j.issn.1000-0569.2005.03.009 (in Chinese with English abstract).
Liu, Y.S., Gao, S., Hu, Z.C., et al., 2010a.Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons of Mantle Xenoliths.Journal of Petrology, 51(1-2):537-571.doi: 10.1093/petrology/egp082
Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology, 257(1-2):34-43.doi: 10.1016/j.chemgeo.2008.08.004
Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010b.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS.Chinese Science Bulletin, 55(15):1535-1546.doi: 10.1007/s11434-010-3052-4
Long, W.G., Xu, D.M., Wang, L., et al., 2012.Formation Age of Hypometamorphic Rocks in Basement of Yunkai Area, South China.Geology and Mineral Resources of South China, 28(4):290-297 (in Chinese with English abstract).doi: 10.3969/j.issn.1007-3701.2012.04.002
Ludwig, K. R., 2008. User's Manual for ISOPLOT 3. 00: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Centre, Berkeley, 1-76.
Luo, Z.G., Wang, Y.J., Zhang, F.F., et al., 2010.LA-ICPMS Zircon U-Pb Dating for Baimashan and Jintan Indosinian Granitic Plutons and Its Petrogenetic Implications.Geotectonica et Metallogenia, 34(2):282-290 (in Chinese with English abstract).doi: 10.16539/j.ddgzyckx.2010.02.009
Ma, T.Q., Bai, D.Y., Kuang, J., et al., 2005.Zircon SHRIMP Dating of the Xitian Granite Pluton, Chaling, Southeastern Hunan.Geological Bulletin of China, 24(5):415-419 (in Chinese with English abstract).doi: 10.3969/j.issn.1671-2552.2005.05.004
Mojzsis, S.J., Harrison, T.M., 2002.Establishment of a 3.83 Ga Magmatic Age for the Akilia Tonalite (southern West Greenland).Earth and Planetary Science Letters, 202(3-4):563-576.doi: 10.1016/s0012-821x(02)00825-7
Peng, B.X., Wang, Y.J., Fan, W.M., et al., 2006.LA-ICPMS Zircon U-Pb Dating for Three Indosinian Granitic Plutons from Central Hunan and Western Guangdong Provinces and its Petrogenetic Implications.Acta Geologica Sinica, 80(5):660-669.doi: 10.1111/j.1755-6724.2006.tb00290.x
Peng, S.M., Fu, L.F., Zhou, G.Q., 1996.Shearing Anatectic Mechanism of Gneissic granitic Rocks and Their Implications for Tectonic Evolution in Yunkai Massif.China University of Geosciences Press, Wuhan (in Chinese).
Qi, C.S., Deng, X.G., Li, W.X., et al., 2007.Origin of the Darongshan-Shiwandashan S-type Granitoid Belt from Southeastern Guangxi:Geochemical and Sr-Nd-Hf Isotopic Constraints.Acta Petrologica Sinica, 23(2):403-412 (in Chinese with English abstract). http://www.oalib.com/paper/1472011
Qian, J.H., Yang, X.Q., Liu, L., et al., 2013.Zircon U-Pb Dating, Mineral Inclusions, Lu-Hf Isotopic Data and Their Geological Significance of Garnet Amphibolite from Songshugou, North Qinling.Acta Petrologica Sinica, 29(9):3087-3098 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201309011.htm
Qiu, J.S., Mcinnes, B.I.A., Xu, X.S., et al., 2004.Zircon ELA-ICP-MS Dating for Wuliting Pluton Dajishan, Southern Jiangxi and New Recognition about Its Relation to Tungsten Mineralization.Geological Review, 50 (2):125-133 (in Chinese with English abstract).
Qiu, J.S., Wang, D.Z., McInnes, B.I.A., et al., 2004.Two Subgroups of A-Type Granites in the Coastal Area of Zhejiang and Fujian Provinces, SE China:Age and Geochemical Constraints on Their Petrogenesis.Transactions of the Royal Society of Edinburgh:Earth Sciences, 95(1-2):227-236.doi: 10.1017/s0263593300001036
Qiu, X.F., Yang, H.M., Zhao, X.M., et al., 2016.Early Triassic Gneissoid Granites in the Gaozhou Area (Yunkai Massif), South China:Implications for the Amalgamation of the Indochina and South China Blocks.The Journal of Geology, 124(3):395-409.doi: 10.1086/685765
Qiu, Y.X., Liang, X.Q., 2006.Evolution of Basin-Range Coupling in the Yunkai Dashan-Shiwan Dashan area, Guangdong and Guangxi:with A Discussion of Several Tectonic Problems of South China.Geological Bulletin of China, 25(3):340-347 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200603004.htm
Qiu, Z.L., Wu, F.Y., Yang, S.F., et al., 2008.Age and Genesis of the Myanmar Jadeite:Constraints from U-Pb Ages and Hf Isotopes of Zircon Inclusions.Chinese Science Bulletin, 53(24):3104-3114 (in Chinese).doi: 10.1007/s11434-008-0490-3
Rowley, D.B., Xue, F., Tucker, R.D., et al., 1997.Ages of Ultrahigh Pressure Metamorphism and Protolith Orthogneisses from the Eastern Dabie Shan:U/Pb Zircon Geochronology.Earth and Planetary Science Letters, 151(3-4):191-203.doi: 10.1016/s0012-821x(97)81848-1
Shao, J.G., Peng, S.M., Peng, S.B., 1995.⁴⁰Ar/³⁶Ar-³⁹Ar/³⁶Ar Isochron Dating for Peripheral Faults of Yunkai Massif.Guangdong Geology, 10(2):34-40 (in Chinese with English abstract). https://www.researchgate.net/publication/311175543_40Ar36Ar-39Ar36Ar_isochron_dating_for_peripheral_faults_of_Yunkai_massif
Sun, T., 2005.Strongly Peraluminous Granites of Mesozoic in Eastern Nanling Range, Southern China:Petrogenesis and Implications for Tectonics.Science in China (Series D), 48(2):165.doi: 10.1360/03yd0042
Tan, X.F., Pan, Y.M., Li, J., et al., 2006.Zircon SHRIMP U-Pb Geochrondogy of the Yunkai Metamorphic Complex in Southeastern Guangxi China.Geological Bulletin of China, 25(5):553-559.
Wan, Y.S., Liu, D.Y., Wilde, S.A., et al., 2010.Evolution of the Yunkai Terrane, South China:Evidence from SHRIMP Zircon U-Pb Dating, Geochemistry and Nd Isotope.Journal of Asian Earth Sciences, 37(2):140-153.doi: 10.1016/j.jseaes.2009.08.002
Wang, J., 2003.History of Neoproterozoic Rift Basins in South China:Implications for Rodinia Break-Up.Precambrian Research, 122(1-4):141-158.doi: 10.1016/s0301-9268(02)00209-7
Wang, L., Long, W.G., Xu, D.M., et al., 2015.Zircon U-Pb Geochronology of Metamorphic Basement in Yunkai Area and Its Implications on the Grenvillian Event in the Cathaysia Block.Earth Science Frontiers, 22 (2):25-40.doi: 10.13745/j.esf.2015.02.003 (in Chinese with English abstract).
Wang, L., Long, W.G., Zhou, D., et al., 2016.Late Triassic Zircon U-Pb Ages and Sr-Nd-Hf Isotopes of Darongshan Granites in Southeastern Guangxi and Their Geological Implications.Geological Bulletin of China, 35(8):1291-1303 (in Chinese with English abstract).doi: 10.3969/j.issn.1671-2552.2016.08.010
Wang, X.C., Li, X.H., Li, W.X., et al., 2007a.Ca.825 Ma Komatiitic Basalts in South China:First Evidence for >1 500℃ Mantle Melts by a Rodinian Mantle Plume.Geology, 35(12):1103.doi: 10.1130/g23878a.1
Wang, Y.J., Fan, W.M., Sun, M., et al., 2007b.Geochronological, Geochemical and Geothermal Constraints on Petrogenesis of the Indosinian Peraluminous Granites in the South China Block:A Case Study in the Hunan Province.Lithos, 96(3-4):475-502.doi: 10.1016/j.lithos.2006.11.010
Wang, Y.J., Fan, W.M., Cawood, P.A., et al., 2007c.Indosinian High-Strain Deformation for the Yunkaidashan Tectonic Belt, South China:Kinematics and ⁴⁰Ar/³⁹Ar Geochronological Constraints.Tectonics, 26(6):TC6008.doi: 10.1029/2007tc002099
Wang, Y.J., Fan, W.M., Zhao, G.C., et al., 2007d.Zircon U-Pb Geochronology of Gneissic Rocks in the Yunkai Massif and Its Implications on the Caledonian Event in the South China Block.Gondwana Research, 12(4):404-416.doi: 10.1016/j.gr.2006.10.003
Wang, Y.B., Wang, D.H., Han, J., et al., 2010.U-Pb Dating and Hf Isotopic Characteristics of Zircons and Re-Os Dating of Molybdenite from Gao'aobei Tungsten-Molybdenum Deposit, Southern Hunan Province.Geological Review, 56(6):820-830 (in Chinese with English abstract).doi: 10.16509/j.georeview.2010.06.016
Wang, Y.J., Fan, W.M., Zhang, G.W., et al., 2013a.Phanerozoic Tectonics of the South China Block:Key Observations and Controversies.Gondwana Research, 23(4):1273-1305.doi: 10.13039/501100002367
Wang, D., Zheng, J.P., Ma, Q., et al., 2013b.Early Paleozoic Crustal Anatexis in the Intraplate Wuyi-Yunkai Orogen, South China.Lithos, 175-176:124-145.doi: 10.13039/501100001809
Wang, Y.J., Zhang, A.M., Fan, W.M., et al., 2013c.Origin of Paleosubduction-Modified Mantle for Silurian Gabbro in the Cathaysia Block:Geochronological and Geochemical Evidence.Lithos, 160-161:37-54.doi: 10.1016/j.lithos.2012.11.004
Wang, Y.J., Wu, C.M., Zhang, A.M., et al., 2012.Kwangsian and Indosinian Reworking of the Eastern South China Block:Constraints on Zircon U-Pb Geochronology and Metamorphism of Amphibolites and Granulites.Lithos, 150:227-242.doi: 10.1016/j.lithos.2012.04.022
Wang, Y.J., Zhang, A.M., Fan, W.M., et al., 2011.Kwangsian Crustal Anatexis within the Eastern South China Block:Geochemical, Zircon U-Pb Geochronological and Hf Isotopic Fingerprints from the Gneissoid Granites of Wugong and Wuyi-Yunkai Domains.Lithos, 127(1-2):239-260.doi: 10.13039/501100001809
Wu, F.Y., Yang, J.H., Liu, X.M., et al., 2005.Hf Isotopes of the 3.8 Ga Zircons in Eastern Hebei Province, China:Implications for Early Crustal Evolution of the North China Craton.Chinese Science Bulletin, 50(18):1996-2003 (in Chinese).doi: 10.1360/982005-629
Wu, F.Y., Li, X.H., Zheng, Y.F., et al., 2007.Lu-Hf Isotopic Systematics and Their Applications in Petrology.Acta Petrologica Sinica, 23(2):185-220 (in Chinese with English abstract).doi: 10.3969/j.issn.1000-0569.2007.02.001
Wu, J., Liang, H.Y., Huang, W.T., et al., 2012.Indosinian Isotope Ages of Plutons and Deposits in Southwestern Miaoershan-Yuechengling, Northeastern Guangxi and Implications on Indosinian Mineralization in South China.Chinese Science Bulletin, 57(13):1126-1136 (in Chinese).doi: 10.1007/s11434-011-4968-z
Wu, Y.B., Zheng, Y.F., 2004.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age.Chinese Science Bulletin, 49(16):1589-1604 (in Chinese).doi: 10.1007/bf03184122
Wu, Y.B., Zheng, Y.F., Zhao, Z.F., et al., 2006.U-Pb, Hf and O Isotope Evidence for Two Episodes of Fluid-Assisted Zircon Growth in Marble-Hosted Eclogites from the Dabie Orogen.Geochimica et Cosmochimica Acta, 70(14):3743-3761.doi: 10.1016/j.gca.2006.05.011
Xie, X.H., Chen, W.F., Zhao, K.D., et al., 2008.Geochemical Characteristics and Geochronology of the Douzhashan Granite, Northeastern Guangxi Province, China.Acta Petrologica Sinica, 24 (6):1302-1312 (in Chinese with English abstract). http://www.oalib.com/paper/1472474
Xu, X.B., Zhang, Y.Q., Jia, D., et al., 2009.Early Mesozoic Geotectonic Processes in South China.Geology in China, 36(3):573-593 (in Chinese with English abstract).doi: 10.3969/j.issn.1000-3657.2009.03.007
Xu, X.S., Deng, P., O'Reilly, S.Y., et al., 2003.Single Zircon LAM-ICPMS U-Pb Dating of Guidong Complex (SE China) and Its Petrogenetic Significance.Chinese Science Bulletin, 48(17):1892-1899.doi: 10.1007/bf03184074
Yin, X.Y., Zhou, H.Y., Liu, D.Y., et al., 2015.Ancient Material Records in the North China Craton:SHRIMP U-Pb Dating and LA-MC-ICPMS Hf Anaysis of Zircons from Archean Metamorphic Rocks in the Jiaozuo Area, Henan.Geological Review, 61 (1):183-194 (in Chinese with English abstract).doi: 10.16509/j.georeview.2015.01.018
Yu, J.H., O'Reilly, S.Y., Wang, L.J., et al., 2010.Components and Episodic Growth of Precambrian Crust in the Cathaysia Block, South China:Evidence from U-Pb Ages and Hf Isotopes of Zircons in Neoproterozoic Sediments.Precambrian Research, 181(1-4):97-114.doi: 10.1016/j.precamres.2010.05.016
Yu, J.H., Wang, L, J., Wei, Z.Y., et al., 2007a.Phanerozoic Metamorphic Episodes and Charaeteristics of Cathaysia Block.Gedogical Journal of China Universities, 13(3):474-483 (in Chinese with English abstract).
Yu, J.H., Wang, L.J., Wang, X.L., et al., 2007b.Geochemistry and Geochronology of the Fucheng Complex in the Southeastern Jiangxi Province, China.Acta Petrologica Sinica, 23 (6):1441-1456 (in Chinese with English abstract).doi: 10.3969/j.issn.1000-0569.2007.06.020
Yu, J.H., Zhou, X.M., O'Reilly, Y.S., et al., 2005.Formation History and Protolith Characteristics of Granulite Facies Metamorphic Rock in Central Cathaysia Deduced from U-Pb and Lu-Hf Isotopic Studies of Single Zircon Grains.Chinese Science Bulletin, 50(16):1758-1767 (in Chinese with English abstract).doi: 10.1007/bf03322805
Yuan, H.L., Gao, S., Dai, M.N., et al., 2008.Simultaneous Determinations of U-Pb Age, Hf Isotopes and Trace Element Compositions of Zircon by Excimer Laser-Ablation Quadrupole and Multiple-Collector ICP-MS.Chemical Geology, 247(1-2):100-118.doi: 10.1016/j.chemgeo.2007.10.003
Zhang, A.M., Wang, Y.J., Fan, W.M., et al., 2012.Earliest Neoproterozoic (ca.1.0 Ga) Arc-Back-Arc Basin Nature along the Northern Yunkai Domain of the Cathaysia Block:Geochronological and Geochemical Evidence from the Metabasite.Precambrian Research, 220-221:217-233.doi: 10.1016/j.precamres.2012.08.003
Zhang, K.J., Cai, J.X., 2009.NE-SW-Trending Hepu-Hetai Dextral Shear Zone in Southern China:Penetration of the Yunkai Promontory of South China into Indochina.Journal of Structural Geology, 31(7):737-748.doi: 10.1016/j.jsg.2009.04.012
Zhang, M., Chen, P.R., Huang, G.L., et al., 2006.Single Zircon LA-ICP-MS Ages of the Longyuanba Pluton in the Eastern Nanling Region and Geological Implication.Acta Geologica Sinica, 80 (7):984-994 (in Chinese with English abstract).doi: 10.3321/j.issn:0001-5717.2006.07.005
Zhang, W.L., Hua, R.M., Wang, R.C., et al., 2004.Single Zircon U-Pb Isotopic Age of the Wuliting Granite in Dajishan Area of Jiangxi, and Its Geological Implication.Acta Geologica Sinica, 78(3):352-358 (in Chinese with English abstract).doi: 10.3321/j.issn:0001-5717.2004.03.008
Zhao, G.Y., Qin, X.F., Wang, Z.Q., 2016.Geochronology, Geochemistry and Geological Significance of Gabbros from Xindi-Anping Area, Southeastern Guangxi.Acta Petrologica et Mineralogica, 35 (5):791-803 (in Chinese with English abstract).doi: 10.3969/j.issn.1000-6524.2016.05.004
Zhao, L., Guo, F., Fan, W.M., et al., 2010.Crustal Evolution of the Shiwandashan Area in South China:Zircon U-Pb-Hf Isotopic Records from Granulite Enclaves in Indo-Sinian Granites.Chinese Science Bulletin, 55(15):1489-1498.doi: 10.1007/s11434-010-3225-1
Zheng, Y.F., Wu, Y.B., Zhao, Z.F., et al., 2005.Metamorphic Effect on Zircon Lu-Hf and U-Pb Isotope Systems in Ultrahigh-Pressure Eclogite-Facies Metagranite and Metabasite.Earth and Planetary Science Letters, 240(2):378-400.doi: 10.1016/j.epsl.2005.09.025
Zheng, Y.F., Zhao, Z.F., Wu, Y.B., et al., 2006.Zircon U-Pb Age, Hf and O Isotope Constraints on Protolith Origin of Ultrahigh-Pressure Eclogite and Gneiss in the Dabie Orogen.Chemical Geology, 231(1-2):135-158.doi: 10.1016/j.chemgeo.2006.01.005
Zhou, D., Long, W.G., Ke, X.Z., et al., 2017a.Petrogenesis of the Tectonic Melange on the Northern Margin of the Yunkai Terrane, South China.Acta Petrologica Sinica, 33(3):810-830 (in Chinese with English abstract).
Zhou, D., Long, W.G., Wang, L., et al., 2017b.Geochronology and Lu-Hf Isotope of Early Paleozoic Zhuya-Shiban Gabbros in Yunkai Terrane, South China.Geological Bulletin of China, 36(5):726-737 (in Chinese with English abstract).doi: 10.3969/j.issn.1671-2552.2017.05.005
Zhou, X.Y., Yu, J.H., Wang, L.J., et al., 2015.Compositions and Formation of the Basement Metamorphic Rocks in Yunkai Terrane, Western Guangdong Province, South China.Acta Petrologica Sinica, 31(3):855-882 (in Chinese with English abstract). https://www.researchgate.net/publication/281729048_Compositions_and_formation_of_the_basement_metamorphic_rocks_in_Yunkai_terrane_western_Guangdong_Province_South_China
蔡建新, 2012.广东河台右旋韧性剪切带及其对金矿的控制.地质论评, 58(6):1069-1080. http://www.cqvip.com/QK/91067X/201206/44159662.html
陈道公, 倪涛, 谢烈文, 2007.大别地体超高压变质岩石锆石Lu-Hf同位素研究.岩石学报, 23(2):331-342. http://www.cnki.com.cn/Article/CJFDTotal-YSXB200702014.htm
陈洪德, 侯明才, 许效松, 等, 2006.加里东期华南的盆地演化与层序格架.成都理工大学学报(自然科学版), 33(1):1-8. http://www.cnki.com.cn/Article/CJFDTotal-TRQG201403004.htm
陈卫锋, 陈培荣, 黄宏业, 等, 2007.湖南白马山岩体花岗岩及其包体的年代学和地球化学研究.中国科学(D辑), 37(7):873-893. http://www.cqvip.com/QK/98491X/200707/25024317.html
邓希光, 陈志刚, 李献华, 等, 2004.桂东南地区大容山-十万大山花岗岩带SHRIMP锆石U-Pb定年.地质论评, 50(4):426-432. http://www.oalib.com/paper/4898375
丁汝鑫, 邹和平, 劳妙姬, 等, 2015.钦-杭结合带南段韧性剪切带印支期活动记录:以防城-灵山断裂带为例.地学前缘, 22(2):79-85. http://www.cnki.com.cn/Article/CJFDTotal-DXQY201502008.htm
丁兴, 周新民, 孙涛, 2005.华南陆壳基底的幕式生长——来自广东古寨花岗闪长岩中锆石LA-ICPMS定年的信息.地质论评, 51(4):382-392. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGKD200504001131.htm
董晨阳, 赵葵东, 蒋少涌, 等, 2010.赣南白面石铀矿区花岗岩的锆石年代学、地球化学及成因研究.高校地质学报, 16(2):149-160. http://edu.wanfangdata.com.cn/Periodical/Detail/qgsj201224100
董春艳, 刘敦一, 万渝生, 等, 2009.内蒙古大青山地区早前寒武纪变质岩的锆石Hf同位素组成和稀土模式.地质论评, 55(4):509-520. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20130211&journal_id=ysxb&year_id=2013
龚贵伦, 陈广浩, 林舸, 等, 2010.广东河台金矿构造应力场演化及构造控矿模式.矿床地质, 29(S2):16-26. http://www.oalib.com/paper/4573147
韩坤英, 许可娟, 高林志, 等, 2017.云开地区变质沉积岩碎屑锆石U-Pb年龄、Lu-Hf同位素特征及其地质意义.岩石学报, 33(9):2939-2956. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201310005.htm
焦骞骞, 许德如, 陈根文, 等, 2017.广东省河台金矿区糜棱岩锆石LA-ICP-MS U-Pb年龄及其地质意义.岩石学报, 33(6):1755-1774. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ199704000.htm
焦淑娟, 郭敬辉, 彭松柏, 2013.华南大容山-十万大山花岗岩体中石榴石成因以及麻粒岩包体变质作用研究.岩石学报, 29(5):1740-1758. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201305020
雷玮琰, 施光海, 刘迎新, 2013.不同成因锆石的微量元素特征研究进展.地学前缘, 20(4):273-284. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH200503012.htm
李妩巍, 王敢, 陈卫锋, 等, 2010.香草坪花岗岩体年代学和地球化学特征.铀矿地质, 26(4):215-221, 227. http://www.cqvip.com/qk/91728X/201004/34412901.html
凌洪飞, 沈渭洲, 邓平, 等, 2005.粤北帽峰花岗岩体地球化学特征及成因研究.岩石学报, 21(3):677-687. https://www.cnki.com.cn/qikan-YSXB200503010.html
龙文国, 徐德明, 王磊, 等, 2012.两广云开地区基底深变质岩的形成时代.华南地质与矿产, 28(4):290-297. http://mall.cnki.net/magazine/Article/SDDI198902002.htm
罗志高, 王岳军, 张菲菲, 等, 2010.金滩和白马山印支期花岗岩体LA-ICPMS锆石U-Pb定年及其成岩启示.大地构造与成矿学, 34(2):282-290. http://d.old.wanfangdata.com.cn/Periodical/ddgzyckx201002015
马铁球, 柏道远, 邝军, 等, 2005.湘东南茶陵地区锡田岩体锆石SHRIMP定年及其地质意义.地质通报, 24(5):415-419. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200416013.htm
彭少梅, 符力奋, 周国强, 1996.云开地块构造演化及片麻状花岗质岩石的剪切深熔成因.武汉:中国地质大学出版社.
彭松柏, 付建明, 刘云华, 2004.大容山-十万大山花岗岩带中A型紫苏花岗岩、麻粒岩包体的发现及意义.科学技术与工程, 4(10):832-834. doi: 10.3969/j.issn.1671-1815.2004.10.006
祁昌实, 邓希光, 李武显, 等, 2007.桂东南大容山-十万大山S型花岗岩带的成因:地球化学及Sr-Nd-Hf同位素制约.岩石学报, 23(2):403-412. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200702019
钱加慧, 杨秀清, 刘良, 等, 2013.北秦岭松树沟榴闪岩锆石U-Pb定年、矿物包裹体和Lu-Hf同位素特征及其地质意义.岩石学报, 29(9):3087-3098. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB502.000.htm
邱检生, McInnes, B. I. A., 徐夕生, 等, 2004.赣南大吉山五里亭岩体的锆石ELA-ICP-MS定年及其与钨成矿关系的新认识.地质论评, 50(2):125-133. http://d.old.wanfangdata.com.cn/Periodical/dzlp200402003
丘元禧, 梁新权, 2006.两广云开大山-十万大山地区盆山耦合构造演化——兼论华南若干区域构造问题.地质通报, 25(3):340-347. http://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ200511021.htm
丘志力, 吴福元, 杨树锋, 等, 2008.缅甸翡翠形成时代和成因的锆石U-Pb年龄与Hf同位素制约.科学通报, 53(24):3104-3114. doi: 10.3321/j.issn:0023-074X.2008.24.019
邵建国, 彭少梅, 彭松柏, 1995.云开地块周边断裂带⁴⁰Ar/³⁶Ar-³⁹Ar/³⁶Ar等时线定年.广东地质, 10(2):34-40.
覃小锋, 潘元明, 李江, 等, 2006.桂东南云开地区变质杂岩锆石SHRIMP U-Pb年代学.地质通报, 25(5):553-559. http://mall.cnki.net/magazine/Article/ZQYD200605004.htm
王磊, 龙文国, 徐德明, 等, 2015.云开地区变质基底锆石U-Pb年代学及对华夏地块Grenvillian事件的指示.地学前缘, 22(2):25-40. http://www.doc88.com/p-9147652412188.html
王磊, 龙文国, 周岱, 等, 2016.桂东南大容山晚二叠世花岗岩锆石U-Pb年龄和Sr-Nd-Hf同位素特征及其地质意义.地质通报, 35(8):1291-1303. http://www.cqvip.com/QK/95894A/201608
王彦斌, 王登红, 韩娟, 等, 2010.汝城高坳背钨-钼矿区花岗岩锆石U-Pb年龄、Hf同位素及矿石辉钼矿Re-Os年龄.地质论评, 56(6):820-830. https://www.wenkuxiazai.com/doc/ef838fe4284ac850ad02428c.html
吴福元, 李献华, 郑永飞, 等, 2007.Lu-Hf同位素体系及其岩石学应用.岩石学报, 23(2):185-220. http://www.cnki.com.cn/Article/CJFDTotal-YSXB200702002.htm
吴福元, 杨进辉, 柳小明, 等, 2005.冀东3.8 Ga锆石Hf同位素特征与华北克拉通早期地壳时代.科学通报, 50(18):1996-2003. doi: 10.3321/j.issn:0023-074X.2005.18.013
吴元保, 郑永飞, 2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报, 49(16):1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002
伍静, 梁华英, 黄文婷, 等, 2012.桂东北苗儿山-越城岭南西部岩体和矿床同位素年龄及华南印支期成矿分析.科学通报, 57(13):1126-1136. http://www.cnki.com.cn/Article/CJFDTotal-DXQY201502003.htm
谢晓华, 陈卫锋, 赵葵东, 等, 2008.桂东北豆乍山花岗岩年代学与地球化学特征.岩石学报, 24 (6):1302-1312. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200806014.htm
徐先兵, 张岳桥, 贾东, 等, 2009.华南早中生代大地构造过程.中国地质, 36(3):573-593. https://www.researchgate.net/profile/Xianbing_Xu2/publication/282543455_Early_Mesozoic_geotectonic_processes_in_South_China/links/56392ef808ae2da875c7a289/Early-Mesozoic-geotectonic-processes-in-South-China.pdf
殷小艳, 周红英, 刘敦一, 等, 2015.华北克拉通古老物质记录——焦作地区太古宙变质岩的锆石SHRIMP U-Pb定年和LA-MC-ICPMS Hf同位素分析.地质论评, 61(1):183-194. http://www.cnki.com.cn/Article/CJFDTotal-DZLP201501021.htm
于津海, 王丽娟, 魏震洋, 等, 2007a.华夏地块显生宙的变质作用期次和特征.高校地质学报, 13(3):474-483. http://www.cqvip.com/QK/90539X/200703/25509795.html
于津海, 王丽娟, 王孝磊, 等, 2007b.赣东南富城杂岩体的地球化学和年代学研究.岩石学报, 23(6):1441-1456. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=200706137
于津海, 周新民, O, Reilly, Y.S., 等, 2005.南岭东段基底麻粒岩相变质岩的形成时代和原岩性质:锆石的U-Pb-Hf同位素研究.科学通报, 50(16):1758-1767. doi: 10.3321/j.issn:0023-074X.2005.16.015
张敏, 陈培荣, 黄国龙, 等, 2006.南岭东段龙源坝复式岩体LA-ICP-MS锆石U-Pb年龄及其地质意义.地质学报, 80(7):984-994. http://www.cnki.com.cn/Article/CJFDTotal-DQKX201401003.htm
张文兰, 华仁民, 王汝成, 等, 2004.江西大吉山五里亭花岗岩单颗粒锆石U-Pb同位素年龄及其地质意义探讨.地质学报, 78(3):352-358. http://cdmd.cnki.com.cn/Article/CDMD-10405-1015990409.htm
赵国英, 覃小锋, 王宗起, 等, 2016.桂东南新地-安平地区辉长岩的年代学、地球化学特征及其地质意义.岩石矿物学杂志, 35(5):791-803. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197702002.htm
赵亮, 郭锋, 范蔚茗, 等, 2010.广西十万大山地壳演化:来自印支期花岗岩中麻粒岩包体锆石U-Pb年代学及Hf同位素记录.科学通报, 55(15):1489-1498. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb201015012&dbname=CJFD&dbcode=CJFQ
周岱, 龙文国, 柯贤忠, 等, 2017a.云开地块北缘构造混杂岩的岩石成因探讨.岩石学报, 33(3):810-830. http://cdmd.cnki.com.cn/Article/CDMD-10697-2007129676.htm
周岱, 龙文国, 王磊, 等, 2017b.云开地区早古生代竹雅-石板辉长岩锆石U-Pb定年与Lu-Hf同位素特征.地质通报, 36(5):726-737. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201705005
周雪瑶, 于津海, 王丽娟, 等, 2015.粤西云开地区基底变质岩的组成和形成.岩石学报, 31(3):855-882. http://www.cnki.com.cn/Article/CJFDTOTAL-HNKC201204017.htm