吉林省塔东群锆石U-Pb定年、微量元素研究及其地质意义

孟杰; 刘晓旸; 梁一鸿; 秦亚; 句高; 李本仙

doi:10.3799/dqkx.2017.040

吉林省塔东群锆石U-Pb定年、微量元素研究及其地质意义

doi: 10.3799/dqkx.2017.040

孟杰^1,2,,
刘晓旸¹,
梁一鸿¹,
秦亚³,
句高¹,
李本仙^1, ,

1.
吉林大学地球科学学院，吉林长春130061
2.
哈尔滨师范大学地理科学学院，黑龙江哈尔滨150025
3.
桂林理工大学地球科学学院，广西桂林541004

基金项目:

中国地质调查局项目 1212011120329

详细信息

作者简介:
孟杰(1982-)，女，博士研究生，主要从事矿物学、地球化学研究.ORCID:0000-0002-3312-0987.E-mail: mengjie26@126.com

通讯作者:
李本仙，ORCID:0000-0002-6995-4879.E-mail: lbxian@jlu.edu.cn

中图分类号: P597
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出版历程
- 收稿日期: 2016-09-12
- 刊出日期: 2017-04-15

U-Pb Dating and Trance Elements Composition of Tadong Group from Jilin Province and Their Geological Implications

Meng Jie^{1,2
,},
Liu Xiaoyang¹,
Liang Yihong¹,
Qin Ya³,
Ju Gao¹,
Li Benxian^{1
, ,}

1.
College of Earth Sciences, Jilin University, Changchun130061, China
2.
College of Geographical Science, Harbin Normal University, Harbin150025, China
3.
College of Earth Sciences, Guilin University of Technology, Guilin541004, China

摘要

摘要: 吉林省塔东群以含大型磁铁矿床而著称，塔东铁矿是吉黑成矿省内最大的火山喷流沉积-变质改造型铁矿.由于塔东群地质特征复杂，多种地质作用复合叠加，使其形成时代归属一直存在争议.通过LA-ICP-MS锆石定年，确定了吉林省塔东群黑云斜长片麻岩和磁铁透辉斜长变粒岩中锆石年代.黑云斜长片麻岩中锆石呈长柱状，Th/U值为0.17~0.65，²⁰⁶Pb/²³⁸U加权平均年龄为517.6±2.7 Ma，代表了其原岩火山岩形成的年龄.磁铁透辉斜长变粒岩中共有两组锆石年龄，其中一组短柱状，Th/U值介于0.78~1.00，加权平均年龄为249.8±4.0 Ma，代表后期热事件年龄；另一组锆石半自形短柱状晶形，异常高的U、Th, Th最高含量可达17 422 μg/g，²⁰⁶Pb/²³⁸U加权平均年龄为518.3±3.8 Ma，表示热液活动年龄，显示该区518.3 Ma左右经历了一次热液作用，可能与该区的岩浆作用以及塔东铁矿的成矿有关.据此，塔东群内塔东铁矿可能存在一期早寒武世 (±520 Ma) 的成矿作用.
- 塔东群 /
- 岩浆锆石 /
- 热液锆石 /
- U-Pb年龄 /
- 塔东铁矿 /
- 地球化学
Abstract: Tadong Group of Jilin Province is known for large-scale magnetite ore deposit, and Tadong iron deposit is the largest submarine volcano plume-metamorphic-reformation iron deposit in the Jilin-Heilongjiang metallogenic province. Complicated of geological characteristics and geological processes made the ownership of Tadong Group long been controversial. In this paper, the U-Pb zircon ages of the biotite plagioclase gneiss and magnetite diopside plagioclase leptynite are obtained by LA-ICP-MS. Zircons that obtained from biotite plagioclase gneiss are prismatic, and Th/U range between 0.17 and 0.65. U-Pb dating of these zircons record ²⁰⁶Pb/²³⁸U weighted mean age of 517.6±2.7 Ma, indicating the formation age of the vocanic. In the magnetite diopside plagioclase leptynite, there are two kinds of zircons with two age groups, respectively. The first kind of zircons are short columns, and Th/U range between 0.78 and 1.00. U-Pb dating of these zircons record ²⁰⁶Pb/²³⁸U weighted mean age of 249.8±4.0 Ma, indicating the age of thermal disturbance. Another kind of zircons are subhedral short prismatic, and have extremely high U, Th contents, the highest Th contents is 17 422 μg/g, respectively. U-Pb dating of these zircons record ²⁰⁶Pb/²³⁸U weighted mean age of 518.3±3.8 Ma, attributing to the age of hydrothermal event. It is indicated that there is a hydrothermal process at 518.3 Ma or so, which might be related to magmatism. Iron mineralization of Tadong iron deposit of Jilin Province is most likely related with this hydrothermal event. Therefore, one of mineralizations happened in the Early Cambrian Period (±520 Ma) in Tadong iron deposit.
- Tadong Group /
- magmatic zircons /
- hydrothermal zircons /
- U-Pb dating /
- Tadong iron deposit /
- geochemistry

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图 1 吉林塔东群地质

Fig. 1. Geological sketch of Jilin Tadong Group

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图 2 岩石薄片显微照片

a.TD11；b.TDFE；Bi.黑云母；Pl.斜长石；Q.石英；Di.透辉石；Mt.磁铁矿

Fig. 2. Photomicrographs of the samples

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图 3 锆石阴极发光 (CL) 图像及测试位置

a.TD11锆石CL图像及测试位置；b.TDFE锆石CL图像及测试位置

Fig. 3. Cathodoluminescence (CL) images of zircons and their test locations

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图 4 吉林塔东群锆石U-Pb谐和图

a.样品TD11中锆石U-Pb谐和图；b.样品TDFE中锆石U-Pb谐和图

Fig. 4. Concordia diagrams of zircon U-Pb date from Jilin Tadong Group

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图 5 吉林塔东群锆石REE球粒陨石标准化分配模式

a.TD11中锆石REE球粒陨石标准化分配模式；b.TDFE 518.3±3.8 Ma锆石REE球粒陨石标准化分配模式

Fig. 5. Chondrite normalized REE patterns of zircon grains from Tadong Group, Jilin Province

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图 6 样品TD11和TDFE中锆石δ(Ce)/[w(Sm)/w(La)]_N图解

Fig. 6. Pattern of δ(Ce)/[w(Sm)/w(La)]_N of zircon grains in sample TD11 and TDFE

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表 1 塔东群沿革

Table 1. The evolution of Tadong group

地调单位	时间	地点	地层
沈阳局大黑山队	1957	敦化	Ar
沈阳局大黑山队	1957	敦化	五台系
吉林区调队三分队	1960	敦化	太古界
延边地质综合队	1974	塔东	志留系-泥盆系
黑龙江局一队	1977	镜泊湖	二合营群 (S)
黑龙江局一队	1977	镜泊湖	红光组
吉林区调队一分队	1978	塔东	S-D
吉林区调队一分队	1978	塔东	青龙村群
吉林局六所一分队	1988	塔东	二合营群 (S)
吉林局六所一分队	1988	塔东	红光组
吉林省区调六所	1988	塔东	O-∈
吉林省区调六所	1988	塔东	黄莺屯组	西保安组
李东津等	1997	塔东	塔东 (岩) 群
李东津等	1997	塔东	朱敦店组	拉拉沟组

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表 2 吉林塔东群LA-ICP-MS锆石U-Pb同位素测试结果

Table 2. Zircon U-Pb isotopic date obtained by LA-ICP-MS for Tadong Group, Jilin Province

样号	²³²Th (10^-6)	²³⁸U (10^-6)	Th/U	Pb (10^-6)	同位素比值						年龄 (Ma)
样号	²³²Th (10^-6)	²³⁸U (10^-6)	Th/U	Pb (10^-6)	²⁰⁷Pb/²⁰⁶Pb	±σ%	²⁰⁷Pb/²³⁵U	±σ%	²⁰⁶Pb/²³⁸U	±σ%	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁶Pb/²³⁸U	1σ
TD11
TD1101	386	2 211	0.17	286	0.057 5	0.19	0.654 4	2.05	0.082 5	0.09	512	75	513	6
TD1103	1 851	4 581	0.40	941	0.057 1	0.13	0.660 6	1.57	0.083 0	0.06	496	39	514	4
TD1105	327	1 806	0.18	229	0.056 1	0.19	0.659 5	2.17	0.084 5	0.10	456	53	523	6
TD1106	691	3 630	0.26	401	0.056 3	0.18	0.654 5	2.04	0.083 2	0.08	463	51	515	5
TD1108	1 063	2 146	0.50	515	0.052 8	0.15	0.619 6	1.76	0.084 2	0.10	320	43	521	6
TD1109	1 004	3 499	0.29	598	0.055 8	0.15	0.653 7	1.75	0.083 9	0.10	445	39	519	6
TD1110	378	1 828	0.21	270	0.057 6	0.19	0.676 3	2.30	0.084 0	0.13	516	48	520	8
TD1111	2 686	4 793	0.56	1 211	0.055 2	0.16	0.641 5	1.78	0.083 3	0.09	419	43	516	5
TD1112	464	1 851	0.25	282	0.056 0	0.19	0.646 6	2.21	0.083 0	0.10	450	55	514	6
TD1113	614	2 860	0.21	397	0.056 6	0.16	0.664 8	1.79	0.084 4	0.09	477	40	522	5
TD1114	743	2 782	0.27	449	0.056 6	0.16	0.655 2	1.89	0.083 3	0.10	475	42	516	6
TD1115	2 096	4 752	0.44	1 075	0.060 9	0.18	0.704 5	2.06	0.083 2	0.09	637	43	515	6
TD1116	4 482	7 407	0.61	1 985	0.058 1	0.16	0.679 8	1.86	0.084 3	0.10	534	39	522	6
TD1117	1 036	2 274	0.46	473	0.057 3	0.18	0.663 0	2.02	0.083 5	0.09	502	49	517	5
TD1118	5 701	8 827	0.65	2 558	0.057 1	0.13	0.666 1	1.56	0.083 9	0.08	495	34	519	5
TDFE
TDFE01	557	711	0.78	103	0.053 1	0.29	0.283 7	1.51	0.039 0	0.06	333	93	246	4
TDFE02	889	921	0.96	162	0.051 4	0.25	0.285 3	1.34	0.040 5	0.05	260	84	256	3
TDFE03	461	554	0.83	92	0.058 1	0.46	0.310 7	2.42	0.039 2	0.14	533	110	248	8
TDFE04	446	544	0.82	85	0.053 8	0.31	0.299 2	1.70	0.040 3	0.07	364	99	255	4
TDFE05	739	888	0.83	138	0.051 1	0.27	0.277 8	1.38	0.039 8	0.06	246	85	252	4
TDFE06	6 290	3 038	2.07	2 073	0.057 4	0.16	0.663 9	1.77	0.083 4	0.08	507	41	516	5
TDFE10	3 597	2 455	1.46	1 293	0.057 6	0.16	0.671 5	1.94	0.084 0	0.09	513	45	520	5
TDFE11	10 971	3 418	3.21	2 537	0.059 6	0.17	0.688 0	1.96	0.083 2	0.08	590	45	515	5
TDFE12	4 999	2 550	1.96	1 749	0.059 2	0.16	0.691 2	1.82	0.084 2	0.08	575	41	521	5
TDFE13	9 863	3 662	2.69	2 164	0.059 0	0.13	0.687 5	1.72	0.083 9	0.10	565	34	519	6
TDFE15	17 422	4 169	4.18	3 254	0.057 9	0.15	0.672 8	1.81	0.083 6	0.09	527	40	517	5
TDFE16	929	933	1.00	173	0.052 6	0.26	0.288 5	1.46	0.039 6	0.06	310	88	251	4
TDFE17	909	1 040	0.87	164	0.049 2	0.27	0.261 1	1.42	0.038 9	0.06	157	95	246	4
TDFE18	16 206	3 989	4.06	2 389	0.057 8	0.14	0.673 2	1.58	0.084 0	0.08	523	34	520	5

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表 3 锆石微量元素分析结果 (μg/g)

Table 3. Trace elements analyses of zircon (μg/g)

样号	La	Ce	Pr	Nd	Sm	Eu	Gd	Tb	Dy	Ho	Er	Tm	Yb	Lu
TD11
TD1101	1.720	44.9	0.810	7.14	11.20	2.21	68.3	31.9	503	212	1 063	254	2 692	460
TD1103	1.310	103.0	0.910	7.50	14.50	4.60	117.0	49.0	659	259	1 256	276	2 833	457
TD1105	0.190	35.1	0.052	2.11	5.67	2.29	56.5	28.4	422	182	916	216	2 364	385
TD1106	0.030	53.7	0.078	1.03	6.73	3.23	70.3	29.4	442	180	884	202	2 147	355
TD1107	3.820	97.1	2.290	20.50	38.80	5.20	217.0	77.8	998	385	1 748	386	4 123	651
TD1108	1.360	54.7	0.810	8.07	11.50	4.67	85.0	34.1	463	176	830	187	1 974	305
TD1109	0.078	67.6	0.089	2.03	12.20	3.32	90.4	38.4	566	224	1132	259	2 860	441
TD11010	0.011	41.2	0.037	1.92	5.84	2.31	56.4	27.2	398	163	838	2 029	2 216	348
TD11011	1.460	127.0	0.750	8.04	19.90	7.03	161.0	60.9	832	319	1 478	328	3 376	525
TD11012	0.026	39.1	0.097	2.74	8.18	3.25	92.0	39.4	583	244	1 247	286	3 082	501
TD11013	0.023	67.4	0.098	3.25	9.28	3.88	107.0	49.1	736	299	1 477	340	3 618	564
TD11014	0.023	74.1	0.054	2.47	9.63	3.88	101.0	44.1	662	275	1 395	327	3 507	552
TD11015	10.200	113.0	5.580	39.40	32.70	7.47	140.0	48.5	630	231	1 087	241	2 538	399
TD11016	1.230	166.0	1.030	11.90	29.10	8.63	194.0	71.7	943	344	1 597	346	3 507	529
TD11017	0.086	69.3	0.190	3.89	15.40	4.79	116.0	45.3	624	236	1 121	253	2 638	410
TD11018	6.030	226.0	3.810	26.10	43.00	13.20	245.0	85.9	1120	405	1 817	396	3 998	593
TDFE
TDFE01	3.140	112.0	0.94	6.39	7.31	3.65	45.0	15.1	165	64.8	313	71.4	770	140
TDFE02	3.330	138.0	1.06	17.60	28.70	9.73	118.0	33.8	362	128.0	579	122.0	1 244	233
TDFE03	0.067	47.3	0.25	3.01	7.03	2.88	40.3	12.1	138	51.8	254	58.1	663	127
TDFE04	0.050	65.4	0.40	6.87	11.50	4.22	52.8	16.8	189	71.2	347	80.7	854	167
TDFE05	2.720	107.0	0.97	6.14	8.44	3.77	39.0	13.3	155	60.5	298	69.9	749	152
TDFE06	4.370	93.8	2.82	17.20	11.20	2.87	46.6	14.6	200	88.7	507	136.0	1 673	343
TDFE10	6.810	73.6	3.49	20.50	12.80	3.18	45.4	14.3	199	91.1	531	144.0	1 756	376
TDFE11	59.400	321.0	38.30	215.00	71.10	8.83	69.6	14.7	162	65.5	365	97.7	1 163	245
TDFE12	57.400	254.0	30.30	154.00	58.20	7.39	72.9	14.9	158	67.5	376	98.4	1 197	261
TDFE13	22.600	190.0	15.40	88.30	33.10	5.60	76.3	23.5	303	138.0	784	210.0	2 578	541
TDFE15	56.100	347.0	35.60	200.00	74.60	10.40	98.6	24.7	281	115.00	631	168.0	2 004	412
TDFE16	4.130	149.0	1.64	13.10	15.40	6.11	83.0	24.6	278	106.0	481	107.0	1 092	202
TDFE17	0.370	115.0	0.34	5.93	10.50	4.69	59.1	17.9	217	79.0	367	83.6	911	177
TDFE18	38.850	251.0	25.30	139.00	53.90	7.78	89.2	20.9	263	116.0	648	173.0	2 110	447
TDFE19	8.560	136.0	3.28	21.70	21.30	8.40	92.8	26.0	281	99.3	449	100.0	1 024	189

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参考文献(37)

Belousova, E.A., Griffin, W.L., O'Reilly, S.Y., et al., 2002.Igneous Zircon:Trace Element Composition as an Indicator of Source Rock Type.Contributions to Mineralogy and Petrology, 143:602-622.doi: 10.1007/s00410-002-0364-7
Corfu, F., Hanchar, J.M., Hoskin, P.W.O., et al., 2003.Altas of Zircon Textures.Reviews in Mineralogy and Geochemistry, 53:469-500.doi: 10.2113/0530469
Geisler, T., Rashwan, A.A., Rahn, M.K.W., et al., 2003.Low-Temperature Hydrothermal Alteration of Natural Metamict Zircons from the Eastern Desert, Egypt.Mineralogical Magazine, 67(3):485-508.doi: 10.1180/0026461036730112
Hoskin, P.W.O., 2005.Trace-Element Composition of Hydrothermal Zircon and the Alteration of Hadean Zircon from the Jack Hills, Australia.Geochimica et Cosmochimica Acta, 69(3):637-648.doi: 10.1016/j.gca.2004.07.006
Hoskin, P.W.O., Schaltegger, U., 2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Reviews in Mineralogy and Geochemistry, 53(1):27-62.doi: 10.2113/0530027
Hoskin, P.W.O., Ireland, T.R., 2000.Rare Earth Element Chemistry of Zircon and Its Use as a Provenance Indicator.Geology, 28(7):627-630.doi:10.1130/0091-7613(2000)28<627:REECOZ>2.0.CO; 2
Hu, Z.C., Gao, S., Liu, Y.S., et al., 2008.Signal Enhancement in Laser Ablation ICP-MS by Addition of Nitrogen in the Central Channel Gas.Journal of Analytical Atomic Spectrometry, 23(8):1093-1101.doi: 10.1039/b804760j
Koschek G., 1993.Origin and Significance of the SEM Cathodoluminescence from Zircon.Microscopy, 171:223-232.doi: 10.1111/j.1365-2818.1993.tb03379.x
Kou, L.L., Zhang, S., Lü, J.C., et al., 2013.Geochemical Characteristics and Tectonic Implication of the Iron Ore Formation in Tadong Area, Jilin Province.Geology and Resources, 22(4): 289-295 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GJSD201304006.htm
Li, Q.W., Zhang, B., Zhang, H.H., et al., 2010.A New Understanding of Metallogenic Regularity of the Tadong Iron Deposit.Jilin Geology, 29(4):59-61 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JLDZ201004014.htm
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., Gao, S., Hu, Z., 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 of Mantle Xenoliths.Journal of Petrology, 51(1-2):537-571.doi: 10.1093/petrology/egp082
Ludwig, K.R., 2003.ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center, Berkeley. https://www.researchgate.net/publication/306157481_Isoplot_v_30_a_geochronological_toolkit_for_Microsoft_Excel
Li, D.J., Wan, Q.H., Xu, L.J., et al., 1997.Petrology and Stratum of Jilin Province.China University of Geoscience Press, Wuhan, 10-11 (in Chinese).
Peng, Y.J., Wang, Z.F., 1995.Determination of A-type Granite Zone in the Central Part of Jilin Province and Its Significance in Tectonics.Jilin Geology, 14(3):31-43 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JLDZ503.002.htm
Peng, Y.J., Zhao, C.B., 2001.The Evolution of the Paleo Jihei Orogenic Belt and Accretion of Continental Crust.Jilin Geology, 20(2):1-9 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JLDZ200102000.htm
Rubatto, D., Gebauer, D., 2000.Use of Cathodoluminescence for U-Pb Zircon Dating by ION Microprobe:Some Examples from the Western Alps.Cathodoluminescence in Geoscience, Springer-Verlag Berlin Heidelberg, New York, 373-400. https://www.researchgate.net/publication/230814801_Use_of_Cathodoluminescence_for_U-Pb_Zircon_Dating_by_Ion_Microprobe_Some_Examples_from_the_Western_Alps
Rubatto, D., Hermann, J., 2003.Zircon Formation During Fluid Circulation in Eclcgites (Monviso, Western Alps):Implications for Zr and Hf Budget in Subduction Zones.Geochimica et Cosmochimica Acta, 67(12):2173-2187.doi: 10.1016/S0016-7037(02)01321-2
Rubatto, D., 2002.Zircon Trace Element Geochemistry:Partitioning with Garnet and the Link between U-Pb Ages and Metamorphism.Chemical Geology, 84(1-2):123-138.doi: 10.1016/S0009-2541(01)00355-2
Shao, J.B., Zhang, X.Y., Wang, H.T., et al., 2014.Geochemistry and Pyrite Re-Os Dating of the Tadong Iron Deposit in Jilin Province.Acta Geologoca Sinica, 88(1):83-98 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201401008.htm
Sinha, A.K., Wayne, D.M., Hewitt, D.A., 1992.The Hydrothermal Stability of Zircon:Preliminary Experimental and Isotopic Studies.Geochimica et Cosmochimica Acta, 56(9):3551-3560.doi: 10.1016/0016-7037(92)90398-3
Wang, F., Xu, W.L., Gao, F.H., et al., 2014.Precambrian Terrane within the Songnen-Zhangguangcai Range Massif, NE China:Evidence from U-Pb Ages of Detrital Zircons from the Dongfengshan and Tadong Groups.Gondwana Research, 26(1):402-413.doi: 10.1016/j.gr.2013.06017
Watson, E.B., Cherniak, D.J., Hanchar, J.M., et al., 1997.The Incorporation of Pb into Zircon.Chemical Geology, 141:19-31.doi: 10.1016/S0009-2541(97)00054-5
Wiedenbeck, M., Alle, P., Corfu, F., et al., 1995.Three Natural Zircon Standards for U-Th-Pb, Lu-Hf, Trace Element and REE Analyses.Geostandards and Geoanalytical Research, 19(1):1-23.doi: 10.1111/j.1751-908X.1995.tb00147.x
Wu, Y.B., Zheng, Y.F., 2004.Genesis of Zircons and Its Constraints on Interpretation of U-Pb Age.Chinese Science Bulletin, 49(15):1554-1569 (in Chinese). doi: 10.1007/BF03184122
Yu, J.J., Hou, X.G., Ge, W.C., et al., 2013.Magma Mixing Genesis of the Early Permian Liulian Pluton at the Northeastern Margin of the Jiamusi Massif in NE China:Evidences from Petrography, Geochronology and Geochemistry.Acta Petrologica Sinica, 29(9):2971-2986 (in Chinese with English abstract). https://www.researchgate.net/publication/282383157_Magma_mixing_genesis_of_the_Early_Permian_Liulian_pluton_at_the_northeastern_margin_of_the_Jiamusi_massif_in_NE_China_Evidences_from_petrography_geochronology_and_geochemistry
Zhang, Y.J., Sun, F.Y., Xu, C.H., et al., 2016.Geochronology, Geochemistry and Zircon Hf Isotopes of the Tanjianshan Granite Porphyry Intrusion in Dachaidan Area of the North Margin of Qaidam Basin, NW China.Earth Science, 41(11):1830-1844 (in Chinese with English abstract). https://www.researchgate.net/profile/Huaikun_Li/citations?sorting=recent&page=1
Zhang, Y.Q., 2012.Study on the Laser-Raman Spectroscopy Analysis and CL Images:Implications for Metamictized Zircons and U-Pb Ages.Geological Survey and Research, 35(3):224-228 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ201203013.htm
寇林林, 张森, 吕俊超, 等, 2013.吉林塔东铁矿赋矿建造地球化学特征及其地质构造意义.地质与资源, 22(4): 289-295. http://www.cnki.com.cn/Article/CJFDTOTAL-GJSD201304006.htm
李东津, 万清海, 许良久等, 1997.吉林省岩石地层.武汉:中国地质大学出版社, 10-11.
李庆武, 张斌, 张红红, 等, 2010.塔东铁矿床成矿规律新认识.吉林地质, 29(4): 59-61. http://www.cnki.com.cn/Article/CJFDTOTAL-JLDZ201004014.htm
彭玉鲸, 王占福, 1995.吉林省中部A型花岗岩带的确定及其构造意义.吉林地质, 14(3): 31-43. http://www.cnki.com.cn/Article/CJFDTOTAL-JLDZ503.002.htm
彭玉鲸, 赵成弼, 2001.古吉黑造山带的演化与陆壳的增生.吉林地质, 20(2): 1-9. http://www.cnki.com.cn/Article/CJFDTOTAL-JLDZ200102000.htm
邵建波, 张希友, 王洪涛, 等, 2014.吉林省塔东大型铁矿地球化学特征及黄铁矿Re-Os同位素定年.地质学报, 88(1): 83-98. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201401008.htm
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
张延军, 孙丰月, 许成瀚, 等, 2016.柴北缘大柴旦滩间山花岗斑岩体锆石U-Pb年代学、地球化学及Hf同位素.地球科学, 41(11): 1830-1844. http://www.earth-science.net/WebPage/Article.aspx?id=3382
张永清, 2012.激光拉曼、阴极荧光研究对蜕晶化锆石及其U-Pb年龄解释的指示意义.地质调查与研究, 35(3): 224-228. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ201203013.htm

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吉林省塔东群锆石U-Pb定年、微量元素研究及其地质意义

doi: 10.3799/dqkx.2017.040

作者简介:
孟杰(1982-)，女，博士研究生，主要从事矿物学、地球化学研究.ORCID:0000-0002-3312-0987.E-mail: mengjie26@126.com

通讯作者:
李本仙，ORCID:0000-0002-6995-4879.E-mail: lbxian@jlu.edu.cn

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U-Pb Dating and Trance Elements Composition of Tadong Group from Jilin Province and Their Geological Implications

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留言板

吉林省塔东群锆石U-Pb定年、微量元素研究及其地质意义

doi: 10.3799/dqkx.2017.040

作者简介: 孟杰(1982-)，女，博士研究生，主要从事矿物学、地球化学研究.ORCID:0000-0002-3312-0987.E-mail: mengjie26@126.com

通讯作者: 李本仙，ORCID:0000-0002-6995-4879.E-mail: lbxian@jlu.edu.cn

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U-Pb Dating and Trance Elements Composition of Tadong Group from Jilin Province and Their Geological Implications

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出版历程

目录

作者简介:
孟杰(1982-)，女，博士研究生，主要从事矿物学、地球化学研究.ORCID:0000-0002-3312-0987.E-mail: mengjie26@126.com

通讯作者:
李本仙，ORCID:0000-0002-6995-4879.E-mail: lbxian@jlu.edu.cn