江南东段平水地区桃红闪长岩：早新元古代洋壳消减的证据

谭清立; 王岳军; 张玉芝; 李庶波; 周永智; 王玉琨

doi:10.3799/dqkx.2017.014

江南东段平水地区桃红闪长岩：早新元古代洋壳消减的证据

doi: 10.3799/dqkx.2017.014

中山大学地球科学与地质工程学院，广东广州 510275

基金项目:

国家自然科学基金项目 41402165

国家自然科学基金项目 41375198

详细信息

作者简介:
谭清立(1987-)，男，博士研究生，从事岩石大地构造研究.ORCID：0000-0003-2346-3641.E-mail: tanqli@mail2.sysu.edu.cn

中图分类号: P588.12;P597.3
计量
- 文章访问数: 4658
- HTML全文浏览量: 2251
- PDF下载量: 38
- 被引次数: 0
出版历程
- 收稿日期: 2016-10-08
- 刊出日期: 2017-02-15

Taohong Diorite from Pingshui Region in Eastern Jiangnan Orogen: Evidence for Early Neoproterozoic Oceanic Crust Subduction

School of Earth Sciences and Geological Engineering, Sun Yat-Sen University, Guangzhou 510275, China

摘要

摘要: 平水一带早新元古代岩浆岩的精细年代学约束及其形成构造背景的厘定是理清华南内部新元古代演化机制的重要突破口.对江南造山带东段平水地区桃红岩体中的闪长岩进行了详细的锆石U-Pb年代学(LA-ICP-MS)、全岩地球化学和Sr-Nd同位素研究，结果显示：闪长岩锆石U-Pb年龄为913±2 Ma和898±2 Ma，代表其形成年龄；去掉挥发分并百分化处理后，SiO₂、Al₂O₃、Na₂O和K₂O含量分别为58.33%~63.36%、15.76%~17.42%、2.62%~3.12%和0.53%~1.53%，属低钾-中钾系列；铝饱和指数(A/CNK) 为0.84~0.92，属偏铝质；轻重稀土分异明显((La/Yb)_N=4.65~6.09)、轻微Eu异常(δEu=0.82~1.01)、高场强元素(Nb、Ta、Ti、P) 强烈亏损、大离子亲石元素(Rb、Ba、K、Sr) 相对富集，具岛弧岩浆亲缘性；具低(⁸⁷Sr/⁸⁶Sr)_i值(0.703 060~0.703 076)、高ε_Nd(t) 值(+6.58~+6.76).综合研究认为桃红闪长岩为扬子与华夏陆块之间的古洋壳南东向俯冲的过程中，被俯冲板片流体和熔体改造的地幔楔橄榄岩部分熔融的产物；双溪坞群及其同期岩浆岩应是扬子与华夏陆块早期拼合阶段的产物，与格林威尔构造事件无关.
- 闪长岩 /
- 洋壳消减 /
- 锆石U-Pb定年 /
- Sr-Nd同位素 /
- 江南造山带 /
- 地球化学
Abstract: The fine chronological constraints and the determination of tectonic setting of the Early Neoproterozoic magmatic rocks in the Pingshui area are important breakthroughs for the Neoproterozoic evolution mechanism in South China. This paper presents a synthesis of zircon U-Pb geochronological, whole rock elementaland Sr-Nd isotopic geochemistry study on the Taohong diorite from Pingshui region along the Eastern Jiangnan Orogen. Two representative samples yielded weighed mean ²⁰⁶Pb/²³⁸U ages of 913±2 Ma and 898±2 Ma, respectively, representing the crystallization ages of the dioritic pluton. In the case of loss on ignition free, the dioritic samples are characterized by SiO₂ of 58.33%-63.36%, Al₂O₃ of 15.76%-17.42%, Na₂O of 2.62%-3.12%, K₂O of 0.53%-1.53% and A/CNK of 0.84-0.92, classified as low to medium-K metaluminous series. Their chondrite-normalized rare earth elements (REEs) patterns exhibit a right-sloping tendency with more enriched light rare earth elements (LREEs) relative to heavy rare earth elements (HREEs) ((La/Yb)_N=4.65-6.09) and slightly Eu abnormality (δEu=0.82-1.01). On the primitive mantle-normalized multi-elements patterns, these samples have strong enrichment in large iron lithophile elements (LILEs) (Rb, Ba, K and Sr) and depletion in high field-strength elements (HFSEs) with marked negative Nb, Ta and Ti, similar to those of typical arc magmatites. The samples show low (⁸⁷Sr/⁸⁶Sr)_i of 0.703 060-0.703 076 ratio and high positive ε_Nd(t) of +6.58 to +6.76 values. It is inferred that the formation of the rocks is attributed to the partial melting of the mantle wedge peridotite, which was modified by the subducted slab-derived fluid and melt during the southeastwards subduction of ancient oceanic crust between the Yangtze and Cathaysia Block. In conjunction with previous studies, it is proposed that the Shuangxiwu Group along Eastern Jiangnan Orogen resulted from suturing of the Yangtze and Cathaysia Block, and is not related to Grenvillian Orogen in petrogenesis.
- diorites /
- subduction of oceanic crust /
- zircon U-Pb Dating /
- Sr-Nd isotope /
- Jiangnan Orogen /
- geochemistry

HTML全文

图 1 华南新元古代地层简图(a) 和江南造山带东段平水地区地质简图(b)

图a据Wang et al.(2013b)；图b据浙江省地质矿产局(1996)

Fig. 1. Simplified geological maps of the Neoproterozoic basement of the Yangtze and Cathaysia Blocks (a) and Pingshui region in eastern Jiangnan Orogen (b)

下载: 全尺寸图片幻灯片

图 2 桃红闪长岩样品13WY-147A (a) 和13WY-147B (b) 显微照片

Bt.黑云母；Pl.斜长石；Qz.石英；Ep.绿帘石；Chl.绿泥石；Spn.榍石

Fig. 2. Photomicrograph of Taohong diorite samples 13WY-147A (a) and 13WY-147B (b)

下载: 全尺寸图片幻灯片

图 3 桃红闪长岩锆石U-Pb年龄谐和图和阴极发光图像(CL)

Fig. 3. Zircon U-PbConcordia diagramand CL images for the Taohong diorite samples

下载: 全尺寸图片幻灯片

图 4 桃红闪长岩样品(a) SiO₂-K₂O图解，(b) A/CNK-A/NK图解，(c) SiO₂-(Na₂O+K₂O) 图解和(d) QAP图解

图a据Middlemost (1985)；图b据Peccerillo and Taylor (1976)；图c据Middlemost (1994)；图d据Baker (1979)

Fig. 4. (a) SiO₂-K₂O, (b) A/CNK-A/NK, (c) SiO₂-(Na₂O+K₂O) and (d) QAP classification diagrams for the Taohong diorite samples

下载: 全尺寸图片幻灯片

图 5 桃红闪长岩哈克图解

图中埃达克型高镁安山岩/闪长岩数据来自Rapp et al.(1999)、Tatsumi (2006)和张玉芝等(2015)

Fig. 5. Hacker diagrams for the Taohong diorite samples

下载: 全尺寸图片幻灯片

图 6 桃红闪长岩球粒陨石标准化稀土元素配分图(a) 和微量元素原始地幔标准化微量元素蛛网图(b)

球粒陨石和原始地幔标准化数据分别引自Taylor and Mclennan (1985)和Sun and McDonough (1989)

Fig. 6. The chondrite-normalized REE pattern (a) and PM-normalized spider diagram (b) for the Taohong diorite samples

下载: 全尺寸图片幻灯片

图 7 桃红闪长岩(⁸⁷Sr/⁸⁶Sr)_i-ε_Nd(t) 关系(a)，SiO₂-Nb/La关系(b)，SiO₂-ε_Nd(t) 关系(c) 和La-La/Sm关系(d)

MORB、BSE数据来自Hawkesworth et al.(1984)、Hart (1988)和Weaver (1991).AFC、FC和部分熔融趋势来自Wang et al.(2013c)和Zhang et al.(2013)

Fig. 7. The relations of (⁸⁷Sr/⁸⁶Sr)_i-ε_Nd(t)(a), SiO₂-Nb/La (b), SiO₂-ε_Nd(t)(c) and La-La/Sm (d) for the Taohong diorite samples

下载: 全尺寸图片幻灯片

图 8 桃红闪长岩SiO₂-Mg^#图解

底图据Cai et al.(2015)；图中1~4 GPa实验变玄武质和榴辉岩熔体的范围来自Rapp and Watson (1995)和Rapp et al.(1999)，0.8~1.6 GPa和1 000~1 050 ℃地壳熔体的范围来自Rapp and Watson (1995)和Sen and Dunn (1994)，0.7 GPa和825~852 ℃地壳熔体的范围来自Springer and Seck (1997)，幔源岩浆结晶分异形成的安山岩/闪长岩的范围来自Tatsumi (2006)，橄榄岩熔体和高镁安山岩/闪长岩范围来自Rapp et al.(1999)、Tatsumi (2006)和张玉芝等(2015)

Fig. 8. SiO₂ versus Mg^# for the Taohong diorite samples

下载: 全尺寸图片幻灯片

图 9 桃红闪长岩Th/Yb-Nd/Yb关系(a) 和Zr/Yb-Nb/Yb关系(b)

据Pearce and Peate (1995)

Fig. 9. The relations of Th/Yb-Nd/Yb (a) and Zr/Yb-Nb/Yb (b) for the Taohong diorite samples

下载: 全尺寸图片幻灯片

表 1 桃红闪长岩样品LA-ICP-MS锆石U-Pb分析结果

Table 1. Zircon LA-ICP-MS dating results for the Taohong diorite samples

分析点	Th (10^-6)	U (10^-6)	Th/U	同位素比值						年龄(Ma)
分析点	Th (10^-6)	U (10^-6)	Th/U	²⁰⁷Pb/²⁰⁶Pb	1 σ	²⁰⁷Pb/²³⁵U	1 σ	²⁰⁶Pb/²³⁸U	1 σ	²⁰⁷Pb/²⁰⁶Pb	1 σ	²⁰⁷Pb/²³⁵U	1 σ	²⁰⁶Pb/²³⁸U	1 σ
13WY-147A-01	188	383	0.49	0.069 55	0.000 24	1.459 58	0.015 05	0.152 26	0.001 57	917	6	914	6	914	9
13WY-147A-02	247	332	0.75	0.069 47	0.000 22	1.455 78	0.015 22	0.152 02	0.001 60	922	7	912	6	912	9
13WY-147A-03	207	305	0.68	0.069 57	0.000 28	1.459 93	0.014 71	0.152 24	0.001 48	917	8	914	6	913	8
13WY-147A-04	200	311	0.64	0.069 61	0.000 28	1.465 37	0.014 21	0.152 66	0.001 40	917	7	916	6	916	8
13WY-147A-05	203	432	0.47	0.069 63	0.000 27	1.459 93	0.014 79	0.152 25	0.001 58	917	8	914	6	914	9
13WY-147A-06	269	304	0.89	0.069 30	0.000 26	1.443 74	0.011 56	0.151 08	0.001 14	909	8	907	5	907	6
13WY-147A-07	206	361	0.57	0.069 43	0.000 25	1.450 39	0.013 86	0.151 61	0.001 45	922	7	910	6	910	8
13WY-147A-08	180	322	0.56	0.070 27	0.000 33	1.512 31	0.016 14	0.155 92	0.001 46	936	9	935	7	934	8
13WY-147A-09	167	321	0.52	0.069 68	0.000 33	1.472 76	0.014 41	0.153 26	0.001 35	920	9	919	6	919	8
13WY-147A-10	249	307	0.81	0.069 32	0.000 23	1.443 61	0.013 61	0.151 10	0.001 43	909	7	907	6	907	8
13WY-147A-11	196	322	0.61	0.069 57	0.000 28	1.463 21	0.012 71	0.152 53	0.001 23	917	8	915	5	915	7
13WY-147A-12	251	350	0.72	0.069 38	0.000 22	1.451 30	0.012 76	0.151 69	0.001 29	909	7	910	5	910	7
13WY-147A-13	193	286	0.67	0.069 57	0.000 36	1.462 24	0.014 13	0.152 56	0.001 38	917	11	915	6	915	8
13WY-147A-14	213	301	0.71	0.069 75	0.000 30	1.467 11	0.013 56	0.152 53	0.001 30	920	5	917	6	915	7
13WY-147A-15	213	326	0.65	0.074 30	0.000 61	1.546 91	0.016 76	0.151 71	0.001 62	1050	17	949	7	911	9
13WY-147A-16	283	302	0.94	0.069 49	0.000 21	1.458 56	0.013 95	0.152 18	0.001 42	922	7	913	6	913	8
13WY-147A-17	204	307	0.67	0.069 83	0.000 33	1.467 88	0.016 25	0.152 38	0.001 55	924	5	917	7	914	9
13WY-147A-18	212	318	0.67	0.069 39	0.000 31	1.449 13	0.014 61	0.151 54	0.001 46	909	9	910	6	910	8
13WY-147A-19	253	313	0.81	0.069 68	0.000 25	1.467 94	0.014 47	0.152 79	0.001 45	920	3	917	6	917	8
13WY-147A-20	169	341	0.50	0.070 01	0.000 29	1.471 25	0.013 24	0.152 44	0.001 28	928	9	919	5	915	7
13WY-147A-21	184	334	0.55	0.070 27	0.000 25	1.477 62	0.016 71	0.152 37	0.001 61	936	7	921	7	914	9
13WY-147A-22	257	294	0.87	0.069 60	0.000 27	1.461 50	0.011 52	0.152 34	0.001 14	917	7	915	5	914	6
13WY-147A-23	197	344	0.57	0.069 46	0.000 26	1.452 83	0.014 04	0.151 78	0.001 43	922	7	911	6	911	8
13WY-147A-24	161	367	0.44	0.069 89	0.000 26	1.479 24	0.014 60	0.153 64	0.001 52	924	8	922	6	921	8
13WY-147A-25	143	327	0.44	0.069 60	0.000 25	1.462 88	0.013 36	0.152 42	0.001 32	917	7	915	6	915	7
13WY-147A-26	166	393	0.42	0.069 58	0.000 18	1.462 00	0.014 64	0.152 41	0.001 52	917	5	915	6	914	9
13WY-147A-27	200	302	0.66	0.069 66	0.000 24	1.466 48	0.013 63	0.152 75	0.001 40	918	2	917	6	916	8
13WY-147A-28	184	323	0.57	0.071 97	0.000 47	1.491 23	0.016 70	0.150 71	0.001 65	985	13	927	7	905	9
13WY-147A-29	184	322	0.57	0.069 59	0.000 26	1.459 23	0.014 70	0.152 21	0.001 51	917	7	914	6	913	8
13WY-147A-30	185	273	0.68	0.069 61	0.000 31	1.457 74	0.013 81	0.152 05	0.001 41	917	9	913	6	912	8
13WY-147A-31	248	292	0.85	0.069 72	0.000 25	1.467 05	0.012 09	0.152 71	0.001 26	920	3	917	5	916	7
13WY-147A-32	243	369	0.66	0.069 84	0.000 27	1.478 29	0.013 60	0.153 60	0.001 38	924	7	922	6	921	8
13WY-147A-33	190	316	0.60	0.069 61	0.000 29	1.427 10	0.011 70	0.148 68	0.001 09	917	8	900	5	894	6
13WY-147A-34	267	340	0.79	0.06948	0.000 19	1.452 05	0.013 25	0.151 58	0.001 37	922	6	911	5	910	8
13WY-147A-35	248	308	0.81	0.069 62	0.000 25	1.460 84	0.015 56	0.152 31	0.001 58	917	7	914	6	914	9
13WY-147A-36	260	246	1.06	0.069 26	0.000 24	1.440 74	0.013 93	0.150 84	0.001 39	906	12	906	6	906	8
13WY-147A-37	294	309	0.95	0.069 99	0.000 27	1.495 67	0.012 69	0.154 93	0.001 18	928	40	929	5	929	7
13WY-147A-38	249	286	0.87	0.069 60	0.000 25	1.463 65	0.013 04	0.152 51	0.001 28	917	7	916	5	915	7
13WY-147A-39	243	303	0.80	0.069 52	0.000 23	1.460 27	0.013 46	0.152 32	0.001 34	915	6	914	6	914	8
13WY-147A-40	264	258	1.02	0.069 41	0.000 22	1.452 41	0.013 66	0.151 71	0.001 36	911	6	911	6	911	8
13wy-147B-01	177	263	0.67	0.068 51	0.000 23	1.412 70	0.013 19	0.149 00	0.001 35	883	12	894	6	895	8
13wy-147B-02	192	255	0.75	0.068 36	0.000 27	1.399 58	0.011 27	0.148 09	0.001 13	880	7	889	5	890	6
13wy-147B-03	162	270	0.60	0.069 06	0.000 28	1.435 39	0.013 30	0.150 40	0.001 30	902	8	904	6	903	7
13wy-147B-04	126	295	0.43	0.069 00	0.000 20	1.432 85	0.013 24	0.150 33	0.001 34	898	6	903	6	903	7
13wy-147B-05	155	277	0.56	0.068 93	0.000 24	1.424 66	0.012 93	0.149 68	0.001 27	898	3	899	5	899	7
13wy-147B-06	189	253	0.75	0.068 64	0.000 28	1.410 08	0.012 25	0.148 80	0.001 16	887	9	893	5	894	7
13wy-147B-08	176	264	0.67	0.068 77	0.000 21	1.411 82	0.014 46	0.148 72	0.001 48	900	6	894	6	894	8
13wy-147B-09	186	259	0.72	0.068 79	0.000 26	1.417 62	0.013 94	0.149 16	0.001 32	892	9	896	6	896	7
13wy-147B-10	194	249	0.78	0.068 83	0.000 30	1.423 23	0.014 87	0.149 68	0.001 41	894	8	899	6	899	8
13wy-147B-11	143	280	0.51	0.068 74	0.000 31	1.414 90	0.014 51	0.149 12	0.001 44	900	10	895	6	896	8
13wy-147B-12	189	253	0.75	0.068 37	0.000 21	1.421 34	0.011 02	0.150 50	0.001 11	880	7	898	5	904	6
13wy-147B-13	172	264	0.65	0.068 29	0.000 26	1.399 51	0.010 45	0.148 37	0.001 02	877	4	889	4	892	6
13wy-147B-14	168	266	0.63	0.068 68	0.000 35	1.405 31	0.014 44	0.148 17	0.001 40	900	10	891	6	891	8
13wy-147B-15	220	231	0.95	0.068 49	0.000 33	1.428 76	0.010 14	0.150 96	0.000 84	883	10	901	4	906	5
13wy-147B-16	170	262	0.65	0.067 45	0.000 33	1.400 89	0.009 87	0.150 31	0.000 86	852	9	889	4	903	5
13wy-147B-17	189	251	0.75	0.067 95	0.000 28	1.411 09	0.010 53	0.150 27	0.001 01	878	9	894	4	902	6
13wy-147B-18	159	268	0.59	0.067 72	0.000 37	1.402 92	0.010 52	0.149 92	0.000 90	861	11	890	4	901	5
13wy-147B-19	153	274	0.56	0.067 36	0.000 36	1.387 22	0.011 40	0.148 98	0.001 01	850	11	884	5	895	6
13wy-147B-20	193	248	0.78	0.067 38	0.000 31	1.388 81	0.009 68	0.149 14	0.000 94	850	9	884	4	896	5
13wy-147B-21	118	295	0.40	0.067 50	0.000 31	1.399 18	0.011 59	0.149 93	0.001 13	854	11	889	5	901	6
13wy-147B-22	126	293	0.43	0.067 24	0.000 32	1.374 70	0.011 63	0.147 93	0.001 16	856	10	878	5	889	7
13wy-147B-23	136	284	0.48	0.067 25	0.000 36	1.380 57	0.010 14	0.148 59	0.000 96	856	11	881	4	893	5
13wy-147B-24	175	259	0.67	0.066 87	0.000 44	1.369 95	0.011 95	0.148 16	0.000 97	835	18	876	5	891	5
注：采样点GPS坐标为29°51.4966′N 120°34.3332′E，地点为浙江绍兴平水镇桃红村红兵线与船外线交界处.

下载: 导出CSV

表 2 桃红闪长岩样品主量元素(%) 和微量元素(10^-6) 分析结果

Table 2. Major elements (%) and trace elements (10^-6) results for the Taohong diorite samples

样品	13WY-147A	13WY-147B	13WY-147C	13WY-147D	13WY-147E	13WY-147F	Ye et al.(2007)
SiO₂	56.82	57.17	56.80	62.18	57.43	56.88	56.72~66.57
TiO₂	0.57	0.60	0.59	0.53	0.56	0.60	0.62~0.64
Al₂O₃	16.94	16.81	16.94	15.46	16.33	16.77	14.46~16.99
Fe₂O₃t	8.25	7.93	7.95	6.48	7.78	8.04	4.52~8.24
MgO	3.62	3.56	3.59	2.68	3.57	3.69	1.82~3.68
MnO	0.16	0.15	0.15	0.13	0.15	0.15	0.07~0.19
CaO	7.43	7.18	7.46	5.78	7.86	7.32	4.10~8.47
K₂O	0.59	0.51	0.61	1.50	0.81	0.71	0.60~2.69
Na₂O	2.59	3.04	2.86	2.99	2.55	2.61	2.84~3.49
P₂O₅	0.18	0.18	0.19	0.16	0.16	0.18	0.09~0.19
LOI	2.71	2.64	2.62	1.87	2.56	2.82	1.76~3.23
Total	99.88	99.76	99.76	99.76	99.76	99.78	99.65~100.51
A/CNK	0.92	0.90	0.90	0.91	0.84	0.91	0.78~1.02
Mg^#	51	51	51	49	52	52	44~51
K₂O/Na₂O	4.36	5.92	4.65	2.00	3.14	3.70
V	243	227	173	253	244	198	79.3~184
Cr	33.5	28.1	28.2	25.3	35.1	32.1
Co	20.9	23.1	23.1	16.7	21.8	23.0
Ni	13.2	14.6	15.4	10.7	16.4	17.4
Zn	99.6	82.3	92.7	79.3	88.8	88.4
Ga	16.4	17.2	17.3	15.8	16.7	17.7	12.1~16.2
Rb	10.1	11.5	13.2	34.1	16.8	15.7	13.9~38.9
Sr	502	580	600	518	614	607	369~541
Y	15.20	15.70	13.90	18.70	15.90	15.70	12.50~19.90
Zr	52.60	50.00	62.20	80.30	59.20	44.20	28.00~99.10
Nb	1.90	1.89	1.85	2.40	1.90	1.81	1.87~3.23
Cs	0.62	0.31	0.27	0.75	0.22	0.38
Ba	285	253	312	466	360	366	262~635
La	11.80	11.40	12.10	16.10	12.50	12.00	9.84~20.70
Ce	22.9	27.2	28.0	37.0	29.4	28.1	20.6~42.6
Pr	3.50	3.35	3.33	4.36	3.54	3.39	2.58~5.63
Nd	14.7	14.8	14.3	18.8	15.3	14.9	11.2~24.0
Sm	3.04	3.59	3.12	4.16	3.58	3.37	2.06~5.10
Eu	0.99	1.01	0.96	1.02	1.00	1.02	0.71~1.14
Gd	2.90	3.01	2.81	3.46	2.77	3.07	1.73~4.77
Tb	0.42	0.48	0.42	0.52	0.45	0.45	0.25~0.66
Dy	2.43	2.74	2.47	3.07	2.57	2.64	1.45~3.91
Ho	0.51	0.57	0.49	0.63	0.55	0.55	0.31~0.82
Er	1.44	1.58	1.45	1.83	1.63	1.60	0.88~2.30
Tm	0.22	0.24	0.19	0.27	0.25	0.22	0.12~0.35
Yb	1.41	1.65	1.34	1.89	1.55	1.56	0.88~2.31
Lu	0.23	0.22	0.20	0.26	0.21	0.20	0.15~0.35
Hf	1.49	1.31	1.41	2.04	1.62	1.25	0.63~2.62
Ta	0.33	0.16	0.14	0.22	0.15	0.15	0.11~0.21
Pb	2.93	2.01	2.23	3.28	2.50	2.24
Th	1.23	0.92	1.05	2.94	1.38	1.03	0.45~7.10
U	0.37	0.31	0.33	1.06	0.39	0.34	0.16~3.79
δEu	1.01	0.94	0.99	0.82	0.97	0.97	0.71~1.15
(La/Yb)_N	5.64	4.65	6.09	5.76	5.43	5.18	4.68~7.58
Sr/Y	33	37	43	28	39	39	19~48

下载: 导出CSV

表 3 桃红闪长岩样品Sr-Nd同位素分析结果

Table 3. Sr-Nd isotopic results for Taohong diorite samples

样品	13WY-147A	13WY-147C	13WY-147F	Li et al.(2009)
⁸⁷Rb/⁸⁶Sr	0.058 19	0.063 63	0.074 81	-
⁸⁷Sr/⁸⁶Sr	0.703 817	0.703 898	0.704 049	-
1σ	7	6	7	-
(⁸⁷Sr/⁸⁶Sr)_i	0.703 060	0.703 070	0.703 076	-
¹⁴⁷Sm/¹⁴⁴Nd	0.125 022	0.132 072	0.136 573	0.116~0.135
¹⁴³Nd/¹⁴⁴Nd	0.512 547	0.512 598	0.512 623	0.512 552~0.512 635
1σ	6	5	5
(¹⁴³Nd/¹⁴⁴Nd)_i	0.511 801	0.511 810	0.511 808	0.511 821~0.511 912
t_DM(Ga)	1.04	1.03	1.04	0.86~1.02
ε_Nd(t)	+6.58	+6.76	+6.72	+6.74~+8.50

下载: 导出CSV

参考文献(111)

Baker, F., 1979.Trondhjemite:Definition, Environment and Hypotheses of Origin.In:Baker, F., ed., Trondhjemites, Dacites and Related Rocks.Elsevier, Amsterdam, 1-12.
Bureau of Geology and Mineral Resource of Zhejiang Province, 1996.Stractigraphy (Lithostratic) of Zhejiang Province.China University of Geosciences Press, Wuhan (in Chinese).
Cai, Y.F., Wang, Y.J., Cawood, P.A., et al., 2015.Neoproterozoic Crustal Growth of the Southern Yangtze Block:Geochemical and Zircon U-Pb Geochronological and Lu-Hf Isotopic Evidence of Neoproterozoic Diorite from the Ailaoshan Zone.Precambrian Research, 266:137-149. doi: 10.1016/j.precamres.2015.05.008
Carmichael, I.S., 2002.The Andesite Aqueduct:Perspectives on the Evolution of Intermediate Magmatism in West-Central (105°-99°W) Mexico.Contributions to Mineralogy and Petrology, 143(6):641-663.doi: 10.1007/s00410-002-0370-9
Chen, H., Ni, P., Chen, R.Y., et al., 2016.Chronology and Geological Significance of Spillite-Keratophyre in Pingshui Formation, Northwest Zhejiang Province.Geology in China, 43(2):410-418(in Chinese with English abstract).
Chen Z.H., Guo K.Y., Dong Y.G., et al., 2009a.Possible Early Neoproterozoic Magmatism Associated with Slab Window in the Pingshui Segment of the Jiangshan-Shaoxing Suture Zone:Evidence from Zircon LA-ICP-MS U-Pb Geochronology and Geochemistry.Science in China (Series D), 39(7):994-1008 (in Chinese). http://www.cnki.com.cn/Article/CJFDTOTAL-JDXG200907005.htm
Chen, Z.H., Xing, G.F., Guo, K.Y., et al., 2009b.Petrogenesis of Keratophyes in the Pingshui Group, Zhejiang:Constraints from Zircon U-Pb Ages and Hf Isotopes.Chinese Science Bulletin, 54(5):610-617(in Chinese with English abstract). http://d.scholar.cnki.net/detail/SSJD_U/SSJD00003493407
Class, C., Miller, D.M., Goldstein, S.L., et al., 2000.Distinguishing Melt and Fluid Subduction Components in Umnak Volcanics, Aleutian Arc.Geochemistry, Geophysics, Geosystems, 1(6):1-28.doi: 10.1029/1999gc000010
Elliott, T., Plank, T., Zindler, A., et al., 1997.Element Transport from Slab to Volcanic Front at the Mariana Arc.Journal of Geophysical Research, 102(B7):14991-15019.doi: 10.1029/97jb00788
van de Flierdt, T., Hoernes, S., Jung, S., et al., 2003.Lower Crustal Melting and the Role of Open-System Processes in the Genesis of Syn-Orogenic Quartz Diorite-granite-leucogranite Associations:Constraints from Sr-Nd-O Isotopes from the Bandombaai Complex, Namibia.Lithos, 67(3-4):205-226.doi: 10.1016/s0024-4937(03)00016-1
Gao, L.Z., Dai, C.G., Liu, Y.X., et al., 2010.Zircon SHRIMP U-Pb Dating of the Tuffaceous Bed of Xiajiang Group in Guizhou Province and Its Stratigraphic Implication.Geology in China, 37(4):1071-1080(in Chinese with English abstract). https://www.researchgate.net/publication/280018736_Zircon_SHRIMP_U-Pb_dating_of_the_tuffaceous_bed_of_xiajiang_group_in_guizhou_province_and_its_stratigraphic_implication
Gao, L.Z., Huang, Z.Z., Ding, X.Z., et al., 2012a.Zircon SHRIMP U-Pb Dating of Xiushui and Majianqiao Formations in Northwestern Jiangxi Province.Geological Bulletin of China, 31(7):1086-1093(in Chinese with English abstract). https://www.researchgate.net/publication/291105009_Zircon_SHRIMP_U-Pb_dating_of_Xiushui_and_Majianqiao_Formations_in_northwestern_Jiangxi_Province?_sg=IIPoB0xzZJanCTwM8MyzZRJl4_xQ-mB9TSwyWYgkUTp1mkx__wIwYedYr3XjLmz7XLnR3O5mnRVxpVf3IRpHCg
Gao, L.Z., Liu, Y.X., Ding, X.Z., et al., 2012b.SHRIMP Dating of Cangshuipu Group in the Middle Part of the Jiangnan Orogen and its Implications for Tectonic Evolutions.Geology in China, 39(1):12-20(in Chinese with English abstract).
Gao L.Z., Zhang C.L., Liu P.J., et al., 2009.Recognition of Meso-and Neoproterozoic Stratigraphic Framework in North and South China.Acta Geoscientica Sinica, 30(4):433-446(in Chinese with English abstract). http://www.oalib.com/paper/1557866
Grove, T.L., Elkins-Tanton, L.T., Parman, S.W., et al., 2003.Fractional Crystallization and Mantle-Melting Controls on Calc-Alkaline Differentiation Trends.Contributions to Mineralogy and Petrology, 145(5):515-533.doi: 10.1007/s00410-003-0448-z
Hart, S.R., 1988.Heterogeneous Mantle Domains:Signatures, Genesis and Mixing Chronologies.Earth and Planetary Science Letters, 90(3):273-296.doi: 10.1016/0012-821x(88)90131-8
Hawkesworth, C.J., Rogers, N.W., van Calsteren, P.W.C., et al., 1984.Mantle Enrichment Processes.Nature, 311:331-335.doi: 10.1038/311331a0
Jung, S., Hoernes, S., Mezger, K., 2002.Synorogenic Melting of Mafic Lower Crust:Constraints from Geochronology, Petrology and Sr, Nd, Pb and O Isotope Geochemistry of Quartz Diorites (Damara Orogen, Namibia).Contributions to Mineralogy and Petrology, 143(5):551-566.doi: 10.1007/s00410-002-0366-5
Kelemen, P.B., Yogodzinski, G.M., Scholl, D.W., 2003.Along-Strike Variation in the Aleutian Island Arc:Genesis of High Mg^# Andesite and Implications for Continental Crust.In:Eiler, J., ed., Inside the Subduction Factory.American Geophysical Union Geophysical Monograph, 138:223-276.doi: 10.1029/138gm11
Keppie, J.D., Dostal, J., Cameron, K.L., et al., 2003.Geochronology and Geochemistry of Grenvillian Igneous Suites in the Northern Oaxacan Complex, Southern Mexico:Tectonic Implications.Precambrian Research, 120(3-4):365-389.doi: 10.1016/s0301-9268(02)00166-3
le Bas M.J., 2000.IUGS Reclassification of the High-Mg and Picritic Volcanic Rocks.Journal of Petrology, 41(10):1467-1470.doi: 10.1093/petrology/41.10.1467
Li, X.H., Li, W.X., He, B., 2012.Building of the South China Block and its Relevance to Assembly and Breakup of Rodinia Supercontinent:Observations, Interpretations and Tests.Bulletin of Mineralogy, Petrology and Geochemistry, 31(6):543-559(in Chinese with English abstract). https://www.researchgate.net/publication/286123654_Building_of_the_South_China_Block_and_its_relevance_to_assembly_and_breakup_of_Rodinia_supercontinent_Observations_interpretations_and_tests
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, W.X., Li, Z.X., et al., 2009.Amalgamation between the Yangtze and Cathaysia Blocks in South China:Constraints from SHRIMP U-Pb Zircon Ages, Geochemistry and Nd-Hf Isotopes of the Shuangxiwu Volcanic Rocks.Precambrian Research, 174(1-2):117-128.doi: 10.1016/j.precamres.2009.07.004
Li, X.H., Liu, D.Y., Sun, M., et al., 2004.Precise Sm-Nd and U-Pb Isotopic Dating of the Supergiant Shizhuyuan Polymetallic Deposit and Its host Granite, SE China.Geological Magazine, 141(2):225-231.doi: 10.1017/s0016756803008823
Li, X.H., Liu, Y., Tu, X.L., et al., 2002.Precise Determination of Chemical Compositions in Silicate Rocks Using Icp Aesand Icp Ms:A Comparative Study of Sample Digestion Techniquesof Alkali Fusion and Acid Dissolution.Geochimica, 31(3):289-294 (in Chinese with English abstract).
Liang, X.R., Wei, G.J., Li, X.H., et al., 2003.Precise Measurement of ¹⁴³Nd/¹⁴⁴Nd and Sm/Nd Ratios Using Multiple Collectors Inductively Coupled Plasma Mass Spectrometer (MC-ICP-MS).Geochimica, 32(1):91-96(in Chinese with English abstract).
Liu, Y.S., Gao, S., Hu, Z.C., et al., 2010.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 from Mantle Xenoliths.Journal of Petrology, 51(1-2):537-571.doi: 10.1093/petrology/egp082
Li, Z.X., Li, X.H., Kinny, P.D., et al., 1999.The Breakup of Rodinia:Did it Start with a Mantle Plume beneath South China? Earth and Planetary Science Letters, 173(3):171-181.doi: 10.1016/s0012-821x(99)00240-x
Li, Z.X., Li, X.H., Zhou, H.W., et al., 2002.Grenvillian Continental Collision in South China:New SHRIMP U-Pb Zircon Results and Implications for the Configuration of Rodinia.Geoglogy, 30(2):163-166.doi:10.1130/0091-7613(2002)030 < 0163:gccisc>2.0.co; 2.
Ludwig, K.R., 2001.Users Manual for Isoplot/Ex Rev.2.49:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronological Center Special Publication, Berkeley.
Middlemost, E.A.K., 1985.Magmas and Magmatic Rocks.Longman, London.
Middlemost, E.A.K., 1994.Naming Materials in the Magma/igneous Rock System.Earth-Science Reviews, 37(3-4):215-224.doi: 10.1016/0012-8252(94)90029-9
Parman, S.W., Grove, T.L., 2004.Harzburgite Melting with and without H₂O:Experimental Data and Predictive Modeling.Journal of Geophysical Research, 109(B2):1-20.doi: 10.1029/2003jb002566
Pearce, J.A., Peate, D.W., 1995.Tectonic Implications of the Composition of Volcanic Arc Magmas.Annual Review of Earth & Planetary Sciences, 23:251-285. https://www.researchgate.net/publication/234148960_Tectonic_Implications_of_the_Composition_of_Volcanic_ARC_Magmas
Peccerillo, A., Taylor, S.R., 1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey.Contributions to Mineralogy and Petrology, 58(1):63-81.doi: 10.1007/bf00384745
Peng, S.B., Liu, S.F., Lin, M.S., et al., 2016.Early Paleozoic Subduction in Cathaysia (Ⅱ):New Evidence from the Dashuang High Magnesian-Magnesian Andesite.Earth Science, 41(6):931-947. https://www.researchgate.net/publication/305417476_Early_Paleozoic_subduction_in_Cathaysia_II_New_evidence_from_the_Dashuang_high_magnesian-magnesian_andesite
Petrone, C.M., Francalanci, L., Carlson, R.W., et al., 2003.Unusual Coexistence of Subduction-Related and Intraplate-Type Magmatism:Sr, Nd and Pb Isotope and Trace Element Data from the Magmatism of the San Pedro-Ceboruco Graben (Nayarit, Mexico).Chemical Geology, 193(1-2):1-24.doi: 10.1016/s0009-2541(02)00229-2
Qi, L., Hu, J., 2000.Determination of Trace Elements in Granites by Inductively Coupled Plasma Mass Spectrometry.Guangxi Chemical Industry, (S1):140-142 (in Chinese with English abstract).
Rapp, R.P., Watson, E.B., 1995.Dehydration Melting of Metabasalt at 8-32 Kbar:Implications for Continental Growth and Crust-Mantle Recycling.Journal of Petrology, 36(4):891-931.doi: 10.1093/petrology/36.4.891
Rapp, R.P., Shimizu, N., Norman, M.D., et al., 1999.Reaction between Slab-Derived Melts and Peridotite in the Mantle Wedge:Experimental Constraints at 3.8 GPa.Chemical Geology, 160(4):335-356.doi: 10.1016/s0009-2541(99)00106-0
Rivers, T., 1997.Lithotectonic Elements of the Grenville Province:Review and Tectonic Implications.Precambrian Research, 86(3-4):117-154.doi: 10.1016/s0301-9268(97)00038-7
Sen, C., Dunn, T., 1994.Dehydration Melting of a Basaltic Composition Amphibolite at 1.5 and 2.0 GPa:Implications for the Origin of Adakites.Contributions to Mineralogy and Petrology, 117(4):394-409.doi: 10.1007/bf00307273
Shaw, A., Downes, H., Thirlwall, M.F., 1993.The Quartz-Diorites of Limousin:Elemental and Isotopic Evidence for Devono-Carboniferous Subduction in the Hercynian Belt of the French Massif Central.Chemical Geology, 107(1-2):1-18.doi: 10.1016/0009-2541(93)90098-4
Shu, L.S., 2012.An Analysis of Principal Features of Tectonic Evolution in South China Block.Geological Bulletin of China, 31(7):1035-1053(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201207004.htm
Shu, L.S., Faure, M., Yu, J.H., et al., 2011.Geochronological and Geochemical Features of the Cathaysia Block (South China):New Evidence for the Neoproterozoic Breakup of Rodinia.Precambrian Research, 187(3-4):263-276.doi: 10.1016/j.precamres.2011.03.003
Springer, W., Seck, H.A., 1997.Partial Fusion of Basic Granulites at 5 to 15 Kbar:Implications for the Origin of TTG Magmas.Contributions to Mineralogy and Petrology, 127(1-2):30-45.doi: 10.1007/s004100050263
Su, J.B., Zhang, Y.Q., Dong, S.W., et al., 2014.Geochronology and Hf Isotopes of Granite Gravel from Fanjingshan, South China:Implication for the Precambrian Tectonic Evolution of Western Jiangnan Orogen.Journal of Earth Science, 25(4):619-629.doi: 10.1007/s12583-014-0469-8
Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society, London, Special Publications, 42(1):313-345.doi: 10.1144/gsl.sp.1989.042.01.19
Tatsumi, Y., 1982.Origin of High-Magnesian Andesites in the Setouchi Volcanic Belt, Southwest Japan, Ⅱ.Melting Phase Relations at High Pressures.Earth and Planetary Science Letters, 60(2):305-317.doi: 10.1016/0012-821x(82)90009-7
Tatsumi, Y., 2001.Geochemical Modeling of Partial Melting of Subducting Sediments and Subsequent Melt-Mantle Interaction:Generation of High-Mg Andesites in the Setouchi Volcanic Belt, Southwest Japan.Geology, 29(4):323-326.doi:10.1130/0091-7613(2001)029 < 0323:gmopmo>2.0.co; 2.
Tatsumi, Y., 2006.High-Mg Andesites in the Setouchi Volcanic Belt, Southwestern Japan:Analogy to Archean Magmatism and Continental Crust Formation? Annual Review of Earth and Planetary Sciences, 34(1):467-499.doi: 10.1146/annurev.earth.34.031405.125014
Taylor, S.R., Mclennan, S.M., 1985.The Continental Crust:Its Composition and Evolution.Oxford Press, Oxford.
Wang, D., Wang, X.L., Zhou, J.C., et al., 2013a.Unraveling the Precambrian Crustal Evolution by Neoproterozoic Conglomerates, Jiangnan Orogen:U-Pb and Hf Isotopes of Detrital Zircons.Precambrian Research, 233:223-236.doi: 10.1016/j.precamres.2013.05.005
Wang, Y.J., Fan, W.M., Zhang, G.W., et al., 2013b.Phanerozoic Tectonics of the South China Block:Key Observations and Controversies.Gondwana Research, 23(4):1273-1305.doi: 10.1016/j.gr.2012.02.019
Wang, Y.J., Zhang, A.M., Cawood, P.A., et al., 2013c.Geochronological, Geochemical and Nd-Hf-Os Isotopic Fingerprinting of an Early Neoproterozoic Arc-Back-Arc System in South China and Its Accretionary Assembly along the Margin of Rodinia.Precambrian Research, 231:343-371.doi: 10.1016/j.precamres.2013.03.020
Wang, Q., 2005.Petrogenesis of Adakitic Porphyries in an Extensional Tectonic Setting, Dexing, South China:Implications for the Genesis of Porphyry Copper Mineralization.Journal of Petrology, 47(1):119-144.doi: 10.1093/petrology/egi070
Wang, Q., Xu, J.F., Zhao, Z.H., 2001.The Summary and Comment on Research on a New Kind of Igneous Rock-Adakite.Advance in Earth Sciences, 16(2):201-208(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXJZ200102009.htm
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, X.L., Zhou, J.C., Griffin, W.L., et al., 2007b.Detrital Zircon Geochronology of Precambrian Basement Sequences in the Jiangnan Orogen:Dating the Assembly of the Yangtze and Cathaysia Blocks.Precambrian Research, 159(1-2):117-131.doi: 10.1016/j.precamres.2007.06.005
Wang, X.L., Zhao, G.C., Zhou, J.C., et al., 2008.Geochronology and Hf Isotopes of Zircon from Volcanic Rocks of the Shuangqiaoshan Group, South China:Implications for the Neoproterozoic Tectonic Evolution of the Eastern Jiangnan Orogen.Gondwana Research, 14(3):355-367.doi: 10.1016/j.gr.2008.03.001
Wang, X.L., Zhou, J.C., Griffin, W.L., et al., 2014a.Geochemical Zonation across a Neoproterozoic Orogenic Belt:Isotopic Evidence from Granitoids and Metasedimentary Rocks of the Jiangnan Orogen, China.Precambrian Research, 242:154-171.doi: 10.1016/j.precamres.2013.12.023
Wang, Y.J., Zhang, Y.Z., Fan, W.M., et al., 2014b.Early Neoproterozoic Accretionary Assemblage in the Cathaysia Block:Geochronological, Lu-Hf Isotopic and Geochemical Evidence from Granitoid Gneisses.Precambrian Research, 249:144-161.doi: 10.1016/j.precamres.2014.05.003
Weaver, B.L., 1991.The Origin of Ocean Island Basalt End-Member Compositions:Trace Element and Isotopic Constraints.Earth and Planetary Science Letters, 104(2-4):381-397.doi: 10.1016/0012-821x(91)90217-6
Xia, X.P., Sun, M., Geng, H.Y., et al., 2011.Quasi-Simultaneous Determination of U-Pb and Hf Isotope Compositions of Zircon by Excimer Laser-Ablation Multiple-Collector ICPMS.Journal of Analytical Atomic Spectrometry, 26(9):1868-1871.doi: 10.1039/c1ja10116a
Xue, H.M., Ma, F., Song, Y.Q., et al., 2010.Geochronology and Geochemisty of the Neoproterozoic Granitoid Association from Eastern Segment of the Jiangnan Orogen, China:Constraints on the Timing and Process of Amalgamation between the Yangtze and Cathaysia Blocks.Acta Petrologica Sinica, 26(11):3215-3244 (in Chinese with English abstract). https://www.researchgate.net/publication/279629265_Geochronology_and_geochemisty_of_the_Neoproterozoic_granitoid_association_from_eastern_segment_of_the_Jiangnan_orogen_China_Constraints_on_the_timing_and_process_of_amalgamation_between_the_Yangtze_an
Ye, M.F., Li, X.H., Li, W.X., et al., 2007.SHRIMP Zircon U-Pb Geochronological and Whole-Rock Geochemical Evidence for an Early Neoproterozoic Sibaoan Magmatic Arc along the Southeastern Margin of the Yangtze Block.Gondwana Research, 12(1-2):144-156.doi: 10.1016/j.gr.2006.09.001
Zhang, G.W., Guo, A.L., Wang, Y.J., et al., 2013.Tectonics of South China Continent and Its Implications.Science in China (Series D), 43(10):1553-1582 (in Chinese). doi: 10.1007/s11430-013-4679-1
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, B.T., Ling, H.F., Shen, W.Z., 1992.Sm-Nd Isochronic Age of Spilite-Keratophyre of Shuangxiwu Group and Sm-Nd System of Orthomeamphibolite of Chencai Group in Shaoxing, Zhejiang Province.Advance in Earth Sciences, 7(4):94 (in Chinese).
Zhang, Y.Z., Wang, Y.J., 2016.Early Neoproterozoic (?840 Ma) Arc Magmatism:Geochronological and Geochemical Constraints on the Metabasites in the Central Jiangnan Orogen.Precambrian Research, 275:1-17.doi: 10.1016/j.precamres.2015.11.006
Zhang, Y.Z., Wang, Y.J., Geng, H.Y., et al., 2013.Early Neoproterozoic (?850 Ma) Back-Arc Basin in the Central Jiangnan Orogen (Eastern South China):Geochronological and Petrogenetic Constraints from Meta-Basalts.Precambrian Research, 231:325-342.doi: 10.1016/j.precamres.2013.03.016
Zhang, Y.Z., Wang, Y.J., Guo, X.F., et al., 2015.Geochronology and Geochemistry of Cihua Neoproterozoic High-Mg Andesites in Jiangnan Orogen and their Tectonic Implications.Earth Science, 40(11):1781-1795 (in Chinese with English abstract). https://www.researchgate.net/publication/289545541_Geochronology_and_geochemistry_of_Cihua_neoproterozoic_High-Mg_andesites_in_Jiangnan_orogen_and_their_tectonic_implications
Zhang, Y.Z., Wang, Y.J., Zhang, Y.H., et al., 2015.Neoproterozoic Assembly of the Yangtze and Cathaysia Blocks:Evidence from the Cangshuipu Group and Associated Rocks along the Central Jiangnan Orogen, South China.Precambrian Research, 269:18-30.doi: 10.1016/j.precamres.2015.08.003
Zhao, G.C., Guo, J.H., 2012.Precambrian Geology of China:Preface.Precambrian Research, 222-223:1-12.doi: 10.1016/j.precamres.2012.09.018
Zhao G.C., 2015.Jiangnan Orogen in South China:Developing from Divergent Double Subduction.Gondwana Research, 27(3):1173-1180.doi: 10.1016/j.gr.2014.09.004
Zhao, J.H., Zhou, M.F., Yan, D.P., et al., 2011.Reappraisal of the Ages of Neoproterozoic Strata in South China:No Connection with the Grenvillian Orogeny.Geology, 39(4):299-302.doi: 10.1130/g31701.1
Zhao, S.Q., Fu, L.B., Wei, J.H., et al., 2015.Petrogenesis and Geodynamic Setting of Late Triassic Quartz Diorites in Zhiduo Area, Qinghai Province.Earth Science, 40(1):61-76(in Chinese with English abstract). https://www.researchgate.net/publication/281940790_Petrogenesis_and_geodynamic_setting_of_late_Triassic_quartz_diorites_in_Zhiduo_area_Qinghai_Province
Zheng, Y.F., Zhang, S.B., Zhao, Z.F., et al., 2007.Contrasting Zircon Hf and O Isotopes in the Two Episodes of Neoproterozoic Granitoids in South China:Implications for Growth and Reworking of Continental Crust.Lithos, 96(1-2):127-150.doi: 10.1016/j.lithos.2006.10.003
Zheng, Y.F., Wu, R.X., Wu, Y.B., et al., 2008.Rift Melting of Juvenile Arc-Derived Crust:Geochemical Evidence from Neoproterozoic Volcanic and Granitic Rocks in the Jiangnan Orogen, South China.Precambrian Research, 163(3-4):351-383.doi: 10.1016/j.precamres.2008.01.004
Zhong, Y.F., Ma, C.Q., She, Z.B., et al., 2005.Shrimp U-Pb Zircon Geochronology of the Jiuling Granitic Complex Batholith in Jiangxi Province.Earth Science, 30(6):685-691 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200506004.htm
Zhou, H.W., Li, X.H., Wang, H.R., et al., 2002.U-Pb Zircon Geochronology of Basic Volcanic Rocks of the Yingyangguan Group in Hezhou, Guangxi, and Its Tectonic Implications.Geological Review, 48(S1):22-25 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP2002S1005.htm
Zhou, J.B., Li, X.H., Ge, W.C., et al., 2007.Age and Origin of Middle Neoproterozoic Mafic Magmatism in Southern Yangtze Block and Relevance to the Break-Up of Rodinia.Gondwana Research, 12(1-2):184-197.doi: 10.1016/j.gr.2006.10.011
Zhou, J.C., Wang, X.L., Qiu, J.S., 2008.Is the Jiangnan Orogenic Belt a Grenvillian Orogenic Belt:Some Problems about the Precambrian Geology of South China.Geological Journal of China Universities, 14(1):64-72(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-GXDX200801009.htm
Zhou, J.C., Wang, X.L.and Qiu, J.S., 2009.Geochronology of Neoproterozoic Mafic Rocks and Sandstones from Northeastern Guizhou, South China:Coeval Arc Magmatism and Sedimentation.Precambrian Research, 170(1-2):27-42. doi: 10.1016/j.precamres.2008.11.002
Zhou, J.C., Wang, X.L., Qiu, J.S., 2014.Neoproterozoic Tectonic-Magmatic Evolution of Jiangnan Orogen.Science Pressing, Beijing (in Chinese).
Zhou, J.C., Wang, X.L., Qiu, J.S., et al., 2004.Geochemistry of Meso-and Neoproterozoic Mafic-Ultramafic Rocks from Northern Guangxi, China:Arc or Plume Magmatism? Geochemical Journal, 38(2):139-152.doi: 10.2343/geochemj.38.139
陈辉, 倪培, 陈仁义, 等, 2016.浙西北平水铜矿细碧角斑岩成岩年龄及其地质意义.中国地质, 43(2): 410-418. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201602004.htm
陈志洪, 郭坤一, 董永观, 等, 2009a.江山-绍兴拼合带平水段可能存在新元古代早期板片窗岩浆活动:来自锆石LA-ICP-MS年代学和地球化学的证据.中国科学(D辑), 39(7): 994-1008. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200907011.htm
陈志洪, 邢光福, 郭坤一, 等, 2009b.浙江平水群角斑岩的成因:锆石U-Pb年龄和Hf同位素制约.科学通报, 54(5): 610-617. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200905012.htm
高林志, 戴传固, 刘燕学, 等, 2010.黔东地区下江群凝灰岩锆石SHRIMP U-Pb年龄及其地层意义.中国地质, 37(4), 1071-1080. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201004023.htm
高林志, 黄志忠, 丁孝忠, 等, 2012a.赣西北新元古代修水组和马涧桥组SHRIMP锆石U-Pb年龄.地质通报, 31(7): 1086-1093. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201207009.htm
高林志, 刘燕学, 丁孝忠, 等, 2012b.江南古陆中段沧水铺群锆石U-Pb年龄和构造演化意义, 中国地质, 39(1): 12-20. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201201003.htm
高林志, 张传恒, 刘鹏举, 等, 2009.华北-江南地区中、新元古代地层格架的再认识.地球学报, 30(4), 433-446. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DQXB200908001005.htm
李献华, 李武显, 何斌, 2012.华南陆块的形成与Rodinia超大陆聚合-裂解--观察、解释与检验.矿物岩石地球化学通报, 31(6): 543-559. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201206001.htm
李献华, 刘颖, 涂湘林, 等, 2002.硅酸盐岩石化学组成的ICP-AES和ICP-MS准确测定:酸溶与碱熔分解样品方法的对比.地球化学, 31(3): 289-294. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200203009.htm
梁细荣, 韦刚健, 李献华, 等, 2003.利用MC-ICP-MS精确测定¹⁴³Nd/¹⁴⁴Nd和Sm/Nd比值.地球化学, 32(1): 91-96.
彭松柏, 刘松峰, 林木森, 等, 2016.华夏早古生代俯冲作用(Ⅱ):大爽高镁-镁质安山岩新证据.地球科学, 41(6): 931-947. http://www.earth-science.net/WebPage/Article.aspx?id=3309
漆亮, 胡静, 2000.电感耦合等离子体质谱法测定花岗岩、沉积物中的微量元素.广西化工, (S1): 140-142. http://www.cnki.com.cn/Article/CJFDTOTAL-GXHG2000S1062.htm
舒良树, 2012.华南构造演化的基本特征.地质通报, 31(7): 1035-1053. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201207004.htm
王强, 许继锋, 赵振华, 2001.一种新的火成岩--埃达克岩的研究综述.地球科学进展, 16 (2): 201-208. http://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ200102009.htm
薛怀民, 马芳, 宋永勤, 等, 2010.江南造山带东段新元古代花岗岩组合的年代学和地球化学:对扬子与华夏地块拼合时间与过程的约束.岩石学报, 26(11): 3215-3244. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201011006.htm
章邦桐, 凌洪飞, 沈渭洲, 1992.浙江绍兴双溪坞群Sm-Nd同位素年龄的确定和Sm-Nd体系在陈蔡群正斜长角闪岩中重置现象的发现.地球科学进展, 7(4): 94. http://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ199204025.htm
张国伟, 郭安林, 王岳军, 等, 2013.中国华南大陆构造与问题.中国科学(D辑), 43(10): 1553-1582. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201310003.htm
张玉芝, 王岳军, 郭小飞, 等, 2015.江南中段慈化地区新元古代高镁安山岩的厘定及其构造意义.地球科学, 40(11): 1781-1795. http://www.earth-science.net/WebPage/Article.aspx?id=3185
赵少卿, 付乐兵, 魏俊浩, 等, 2015.青海治多地区晚三叠世石英闪长岩地球化学特征及成岩动力学背景.地球科学, 40(1): 61-76. http://www.earth-science.net/WebPage/Article.aspx?id=3025
浙江省地质矿产局, 1996.浙江岩石地层.武汉:中国地质大学出版社.
钟玉芳, 马昌前, 佘振兵, 等, 2005.江西九岭花岗岩类复式岩基锆石SHRIMP U-Pb年代学.地球科学, 30(6): 685-691. http://www.earth-science.net/WebPage/Article.aspx?id=1522
周汉文, 李献华, 王汉荣, 等, 2002.广西鹰扬关群基性火山岩的锆石U-Pb年龄及其地质意义.地质论评, 48(增刊1), 22-25. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP2002S1005.htm
周金城, 王孝磊, 邱检生, 2008.江南造山带是否格林威尔期造山带--关于华南前寒武纪地质的几个问题.高校地质学报, 14(1): 64-72. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200801009.htm
周金城, 王孝磊, 邱检生, 2014.江南造山带新元古代构造-岩浆演化.北京:科学出版社.

施引文献

资源附件(0)

访问统计

点击查看大图

图(9) / 表(3)

计量

文章访问数: 4658
HTML全文浏览量: 2251
PDF下载量: 38
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

江南东段平水地区桃红闪长岩：早新元古代洋壳消减的证据

doi: 10.3799/dqkx.2017.014

作者简介:
谭清立(1987-)，男，博士研究生，从事岩石大地构造研究.ORCID：0000-0003-2346-3641.E-mail: tanqli@mail2.sysu.edu.cn

计量

Taohong Diorite from Pingshui Region in Eastern Jiangnan Orogen: Evidence for Early Neoproterozoic Oceanic Crust Subduction

计量

目录

留言板

江南东段平水地区桃红闪长岩：早新元古代洋壳消减的证据

doi: 10.3799/dqkx.2017.014

作者简介: 谭清立(1987-)，男，博士研究生，从事岩石大地构造研究.ORCID：0000-0003-2346-3641.E-mail: tanqli@mail2.sysu.edu.cn

计量

出版历程

Taohong Diorite from Pingshui Region in Eastern Jiangnan Orogen: Evidence for Early Neoproterozoic Oceanic Crust Subduction

计量

出版历程

目录

作者简介:
谭清立(1987-)，男，博士研究生，从事岩石大地构造研究.ORCID：0000-0003-2346-3641.E-mail: tanqli@mail2.sysu.edu.cn