内蒙古巴林右旗胡都格绍荣岩体的年代学、地球化学、Hf同位素特征及构造背景

李鹏川; 刘正宏; 李世超; 徐仲元; 李刚; 关庆彬

doi:10.3799/dqkx.2016.139

内蒙古巴林右旗胡都格绍荣岩体的年代学、地球化学、Hf同位素特征及构造背景

doi: 10.3799/dqkx.2016.139

吉林大学地球科学学院，吉林长春 130061

基金项目:

国家自然科学基金项目 41340024

内蒙古自治区地质勘查基金项目 NMKD2013-02

中国地质调查局项目 1212011085252

详细信息

作者简介:
李鹏川(1991-)，男，博士研究生，主要从事构造地质学研究.E-mail: lipengchuan@foxmail.com

通讯作者:
刘正宏，E-mail: zhliu@jlu.edu.cn

中图分类号: P581; P597
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出版历程
- 收稿日期: 2016-05-31
- 刊出日期: 2016-12-15

Geochronology, Geochemistry, Zircon Hf Isotopic Characteristics and Tectonic Setting of Hudugeshaorong Pluton in Balinyouqi, Inner Mongolia

College of Earth Sciences, Jilin University, Changchun 130061, China

摘要

摘要: 大兴安岭地区晚中生代的大地构造背景一直存在争议，通过对内蒙古巴林右旗胡都格绍荣岩体进行锆石U-Pb测年、岩石地球化学以及锆石Lu-Hf同位素分析，探讨其形成时代及构造背景.胡都格绍荣岩体主体岩性为似斑状黑云母二长花岗岩，LA-ICP-MS锆石U-Pb测年确定其加权平均年龄为129.9±1.4 Ma(MSWD=0.91)，指示其侵位于早白垩世.花岗岩具有高SiO₂、Na₂O、K₂O含量，低CaO、MgO含量，富集Cs、Rb、K、Th、U、Zr，亏损Ba、Sr、P、Ti，轻稀土富集，具明显Eu负异常(δEu=0.35~0.44)，10 000×[w(Ga)/w(Al)]为2.08~3.05，表明其为典型的A型花岗岩.Hf同位素分析结果显示，锆石具有正的ε_Hf(t)值(2.24~9.41)，Hf两阶段模式年龄为1 030~570 Ma，平均为809 Ma，结合其微量元素特征，认为岩浆来源于新元古代地壳的部分熔融.胡都格绍荣花岗岩指示研究区在早白垩世为伸展构造背景，可能与蒙古-鄂霍茨克洋闭合关系更为密切.
- A型花岗岩 /
- 早白垩世 /
- 大兴安岭 /
- 地质年代学 /
- Hf同位素 /
- 伸展环境 /
- 地球化学
Abstract: The tectonic setting of Da Hinggan Mountains area at the Late Mesozoic has always been controversial, this paper presents zircon U-Pb age, geochemistry and Hf isotopic data of Hudugeshaorong pluton in order to discuss its formation time and tectonic background. Hudugeshaorong pluton is mainly composed of porphyritic biotite monzogranite with LA-ICP-MS zircon U-Pb age of 129.9±1.4 Ma (MSWD=0.91), indicating it was intruded at the Early Cretaceous. This granite pluton is high in SiO₂, Na₂O, K₂O and low in CaO, MgO, enriched in Rb, K, Th, U and Zr, and depleted in Ba, Sr, P and Ti. Rare earth elements show light REE enrichment (LREE/HREE=6.90-9.39) with obvious negative Eu anomalies (δEu=0.35-0.44), the ratio of 10 000×[w(Ga)/w(Al)] is between 2.08 and 3.05, showing that it is typical A-type granite. Hf isotopic analysis results show a positive ε_Hf(t) values (2.24-9.41), two-stage model ages ranging from 1 030 Ma to 570 Ma, with an average age of 809 Ma. Combining with Th/U and Nb/Ta, we suggest that the primary magma was derived from the partial melting of the Neoproterozoic crust. Hudugeshaorong granite indicates that the study area was in an extensional environment during the Early Cretaceous, we suggest it is more likely related to the closure of the Mongol-Okhotsk Ocean.
- A-type granite /
- Early Cretaceous /
- Da Hinggan Mountains /
- geochronology /
- Hf isotope /
- extensional environment /
- geochemistry

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图 1 胡都格绍荣岩体构造位置(a)及地质简图(b)

图a据Xiao et al.(2003)修改

Fig. 1. Tectonic locations (a) and simplified geological sketch (b) of Hudugeshaorong pluton

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图 2 胡都格绍荣花岗岩野外照片(a)和显微镜下照片(b~d)

a.中细粒似斑状黑云母二长花岗岩野外照片；b.黑云母花岗斑岩；c.斜长石发育蠕虫结构；d.石英和钾长石构成文象结构.Pl.斜长石；Kf.钾长石；Mic.微斜长石；Qtz.石英；Bt.黑云母

Fig. 2. Photographs (a) and microphotographs (b-d) for Hudugeshaorong granite

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图 3 胡都格绍荣花岗岩(W18N-1) 部分锆石阴极发光图

图中锆石之下为U-Pb年龄，锆石内部为Hf两阶段模式年龄和ε_Hf(t)值

Fig. 3. Cathodoluminescence (CL) images of selected zircons from Hudugeshaorong granite (W18N-1)

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图 4 胡都格绍荣花岗岩U-Pb谐和图

Fig. 4. U-Pb concordia diagram for Hudugeshaorong granite

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图 5 胡都格绍荣岩体SiO₂-K₂O图解

据Peccerillo and Taylor(1976)

Fig. 5. SiO₂-K₂O diagram of Hudugeshaorong pluton

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图 6 胡都格绍荣岩体稀土元素球粒陨石标准化配分图解(a)和微量元素原始地幔标准化蛛网图(b)

图a据Boynton(1984)；图b据Sun and McDonough(1989)

Fig. 6. REE chondrite-normalized patterns diagram (a) and trace element primitive mantle-normalized spidergrams (b) of Hudugeshaorong pluton

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图 7 胡都格绍荣花岗岩锆石t-ε_Hf(t)图解

Fig. 7. t-ε_Hf(t) plot for the zircons of Hudugeshaorong granite

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图 8 A型花岗岩判别图

据Whalen et al.(1987)

Fig. 8. A-type granite discrimination diagram

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图 9 胡都格绍荣花岗岩的Y/Nb-Rb/Nb图解(a)和Nb-Y-Ce图解(b)

据Nelson(1992)

Fig. 9. Y/Nb-Rb/Nb diagrams (a) and Nb-Y-Ce diagrams (b) of Hudugeshaorong granite

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表 1 胡都格绍荣岩体LA-ICP-MS锆石U-Pb测年数据

Table 1. LA-ICP-MS zircon U-Pb dating data of Hudugeshaorong pluton

样品	Th/U	同位素比值						锆石年龄(Ma)
样品	Th/U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ
W18N-1	1.40	0.050 76	0.003 66	0.140 30	0.009 19	0.020 41	0.000 41	231.6	166.6	133.3	8.2	130.2	2.6
W18N-2	1.23	0.047 46	0.003 44	0.137 27	0.010 52	0.020 54	0.000 45	72.3	162.9	130.6	9.4	131.1	2.9
W18N-3	1.37	0.050 30	0.004 44	0.132 07	0.010 65	0.019 80	0.000 40	209.3	257.4	126.0	9.6	126.4	2.5
W18N-4	1.38	0.051 87	0.009 70	0.142 97	0.021 79	0.020 99	0.001 18	279.7	379.3	135.7	19.4	133.9	7.4
W18N-5	0.64	0.049 05	0.003 86	0.134 69	0.009 59	0.020 02	0.000 41	150.1	174.0	128.3	8.6	127.8	2.6
W18N-6	1.14	0.050 47	0.008 49	0.146 45	0.018 77	0.021 12	0.000 70	216.7	348.1	138.8	16.6	134.7	4.4
W18N-7	1.16	0.053 70	0.008 34	0.138 18	0.020 98	0.020 41	0.000 94	366.7	309.2	131.4	18.7	130.3	6.0
W18N-9	0.84	0.052 27	0.005 37	0.149 30	0.012 46	0.021 17	0.000 63	298.2	237.0	141.3	11.0	135.0	4.0
W18N-10	0.93	0.050 24	0.004 57	0.140 02	0.011 19	0.020 46	0.000 52	205.6	200.0	133.1	10.0	130.6	3.3
W18N-11	0.48	0.050 15	0.003 70	0.137 14	0.009 15	0.019 77	0.000 45	211.2	172.2	130.5	8.2	126.2	2.9
W18N-13	0.94	0.047 74	0.004 95	0.127 23	0.012 48	0.019 76	0.000 53	87.1	229.6	121.6	11.2	126.1	3.4
W18N-14	0.60	0.051 64	0.003 31	0.142 92	0.007 72	0.020 44	0.000 39	333.4	143.5	135.6	6.9	130.5	2.5
W18N-15	0.65	0.054 38	0.008 26	0.137 93	0.017 70	0.020 86	0.000 73	387.1	148.0	131.2	15.8	133.1	4.6
W18N-16	0.52	0.052 35	0.004 28	0.150 65	0.011 43	0.021 07	0.000 49	301.9	187.0	142.5	10.1	134.4	3.1
W18N-17	0.48	0.054 23	0.006 77	0.130 40	0.012 83	0.019 49	0.000 61	388.9	283.3	124.5	11.5	124.5	3.9
W18N-18	0.58	0.048 01	0.003 71	0.133 18	0.009 05	0.020 25	0.000 37	98.2	174.0	127.0	8.1	129.3	2.4
W18N-19	0.57	0.047 35	0.007 85	0.137 35	0.022 64	0.020 86	0.000 38	77.9	342.6	130.7	20.2	133.1	2.4
W18N-20	0.40	0.049 22	0.003 10	0.135 88	0.007 84	0.020 39	0.000 33	166.8	-50.9	129.4	7.0	130.1	2.1

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表 2 胡都格绍荣岩体主量元素(%)、稀土元素及微量元素(10^-6)分析结果

Table 2. The analysis results of major elements (%), rare elements and trace elements (10^-6) of Hudugeshaorong pluton

样号	W1YQ-1	W2YQ-1	W3YQ-1	W4YQ-1	W5YQ-1
SiO₂	70.8	71.9	71.5	72.5	71.5
TiO₂	0.31	0.29	0.30	0.28	0.31
Al₂O₃	14.15	14.00	14.05	13.85	14.20
Fe₂O₃	2.69	2.49	2.80	2.41	2.63
MnO	0.05	0.05	0.06	0.05	0.06
MgO	0.59	0.53	0.55	0.49	0.57
CaO	1.81	1.48	1.36	1.44	1.72
Na₂O	4.22	4.27	4.03	4.10	4.09
K₂O	3.86	3.79	4.03	4.11	4.08
P₂O₅	0.10	0.09	0.09	0.08	0.10
烧失量	0.53	0.66	0.62	0.34	0.50
总计	99.26	99.69	99.56	99.80	99.92
Na₂O+K₂O	8.08	8.06	8.06	8.21	8.17
A/CNK	0.98	1.01	1.04	1.00	0.99
Rb	167.0	147.5	162.5	157.5	158.0
Cs	9.59	4.77	9.49	3.71	5.83
Sr	269	261	260	255	318
Ba	495	539	543	517	555
Zr	180	206	193	171	241
Hf	5.7	5.9	5.9	5.4	6.4
U	3.46	2.64	3.56	3.56	4.35
Th	13.65	13.40	13.50	16.55	16.95
Nb	9.5	9.9	9.8	10.5	10.5
Ta	0.9	0.9	0.9	0.9	0.7
Y	30.3	28.1	28.3	32.1	36.0
Cr	30	20	20	30	20
V	104	29	25	20	40
Ga	21.3	21.0	21.4	21.6	21.2
Sn	6	7	4	3	2
Th/U	3.95	5.08	3.79	4.65	3.90
Nb/Ta	10.56	11.00	10.89	11.67	15.00
La	32.6	24.9	26.3	28.2	43.3
Ce	60.4	59.2	59.1	64.0	87.5
Pr	7.51	6.26	6.31	7.15	9.36
Nd	26.7	22.2	23.3	26.7	34.6
Sm	6.05	4.85	5.02	5.76	6.37
Eu	0.67	0.63	0.69	0.64	0.74
Gd	5.34	4.63	4.43	5.20	5.84
Tb	0.88	0.76	0.78	0.85	0.91
Dy	5.00	4.39	4.65	4.97	4.99
Ho	1.02	0.88	0.95	1.07	1.09
Er	2.95	2.65	2.77	3.08	2.94
Tm	0.42	0.38	0.41	0.44	0.48
Yb	2.92	2.63	2.72	3.11	2.59
Lu	0.45	0.41	0.43	0.48	0.53
δEu	0.35	0.40	0.44	0.35	0.36
δCe	0.90	1.11	1.07	1.06	1.00
(La/Yb)_N	7.53	6.38	6.52	6.11	11.27
LREE	133.93	118.04	120.72	132.45	181.87
HREE	18.98	16.73	17.14	19.20	19.37
LREE/HREE	7.06	7.06	7.04	6.90	9.39
∑REE	152.91	134.77	137.86	151.65	201.24

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表 3 胡都格绍荣岩体锆石Lu-Hf同位素数据

Table 3. Zircon Lu-Hf isotope data of Hudugeshaorong pluton

序号	t(Ma)	¹⁷⁶Yb/¹⁷⁷Hf	¹⁷⁶Lu/¹⁷⁷Hf	¹⁷⁶Hf/¹⁷⁷Hf	1σ	ε_Hf(0)	ε_Hf(t)	T_DM1(Ma)	T_DM2(Ma)	f_Lu/Hf
W18N-3	112	0.094 627	0.001 840	0.282 822	5.2	1.77	4.10	623	911	-0.94
W18N-5	112	0.057 225	0.001 103	0.282 864	4.8	3.24	5.62	552	813	-0.97
W18N-6	123	0.096 117	0.001 852	0.282 910	4.4	4.88	7.43	496	705	-0.94
W18N-9	114	0.069 283	0.001 324	0.282 871	2.9	3.49	5.90	545	797	-0.96
W18N-10	113	0.064 391	0.001 314	0.282 783	3.7	0.37	2.76	671	997	-0.96
W18N-11	112	0.061 889	0.001 181	0.282 873	4.7	3.58	5.95	540	792	-0.96
W18N-13	112	0.109 012	0.001 975	0.282 972	3.9	7.09	9.41	407	570	-0.94
W18N-17	115	0.128 320	0.002 883	0.282 770	7.0	-0.06	2.24	719	1031	-0.91
W18N-18	113	0.121 049	0.002 572	0.282 955	4.6	6.47	8.76	439	613	-0.92
W18N-20	117	0.126 951	0.002 943	0.282 847	3.5	2.64	4.99	606	857	-0.91
注：¹⁷⁶Lu衰变常数λ=1.867×10^-11(Söderlund et al., 2004)；球粒陨石的¹⁷⁶Lu/¹⁷⁷Hf、¹⁷⁶Hf/¹⁷⁷Hf分别为0.033 2，0.282 772(Blichert-Toft and Albarède, 1997)；亏损地幔的¹⁷⁶Lu/¹⁷⁷Hf、¹⁷⁶Hf/¹⁷⁷Hf分别为0.038 42、0.283 25(Griffin et al., 2000).

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参考文献(94)

Amelin, Y., Lee, D.C., Halliday, A.N., et al., 1999.Nature of the Earth's Earliest Crust from Hafnium Isotopes in Single Detrital Zircons.Nature, 399(6733):252-255.doi: 10.1038/20426
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
Blichert-Toft, J., Albarède, F., 1997.The Lu-Hf Isotope Geochemistry of Chondrites and the Evolution of the Mantle-Crust System.Earth and Planetary Science Letters, 148(1-2):243-258.doi:10.1016/s0012-821x (97)00040-x
Boynton, W.V., 1984.Cosmochemistry of the Rare Earth Elements:Meteorite Studies.In:Henderson, P., ed., Rare Earth Element Geochemistry:Developments in Geochemistry.Elesevier, Amsterdam, 63-114.
Chen, B., Jahn, B.M., Tian, W., 2009.Evolution of the Solonker Suture Zone:Constraints from Zircon U-Pb Ages, Hf Isotopic Ratios and Whole-Rock Nd-Sr Isotope Compositions of Subduction-and Collision-Related Magmas and Forearc Sediments.Journal of Asian Earth Sciences, 34(3):245-257.doi: 10.1016/j.jseaes.2008.05.007
Fan, W.M., Guo, F., Wang, Y.J., et al., 2003.Late Mesozoic Calc-Alkaline Volcanism of Post-Orogenic Extension in the Northern Da Hinggan Mountains, Northeastern China.Journal of Volcanology and Geothermal Research, 121(1-2):115-135.doi: 10.1016/s0377-0273(02)00415-8
Ge, W.C., Lin, Q., Sun, D.Y., et al., 1999.Geochemical Characteristics of the Mesozoic Basalts in Da Hinggan Ling:Evidence of the Mantle Crust Interaction.Acta Petrologica Sinica, 15(3):396-406(in Chinese with English abstract). https://www.researchgate.net/publication/279540240_Geochemical_characteristics_of_the_Mesozoic_basalts_in_Da_Hinggan_Ling_Evidence_of_the_mantle-crust_interaction
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
Hou, K.J., Li, Y.H., Tian, Y.R., 2009.In Situ U-Pb Zircon Dating Using Laser Ablation-Multi Ion Counting-ICP-MS.Mineral Deposits, 28(4):481-492(in Chinese with English abstract). https://www.researchgate.net/publication/252929356_In_situ_U-Pb_zircon_dating_using_laser_ablation-multi_ion_couting-ICP-MS
Hou, K.J., Li, Y.H., Zou, T.R., et al., 2007.Laser Ablation-MC-ICP-MS Technique for Hf Isotope Microanalysis of Zircon and Its Geological Applications.Acta Petrologica Sinica, 23(10):2595-2604(in Chinese with English abstract). http://www.oalib.com/paper/1472292
Kravchinsky, V.A., Cogné, J.P., Harbert, W.P., et al., 2002.Evolution of the Mongol-Okhotsk Ocean as Constrained by New Palaeomagnetic Data from the Mongol-Okhotsk Suture Zone, Siberia.Geophysical Journal International, 148(1):34-57.doi: 10.1046/j.1365-246x.2002.01557.x
Kuang, H.W., Liu, Y.Q., Liu, Y.X., et al., 2013.Stratigraphy and Depositional Palaeogeography of the Early Cretaceous Basins in Da Hinggan Mountains-Mongolia Orogenic Belt and Its Neighboring Areas.Geological Bulletin of China, 32(7):1063-1084(in Chinese with English abstract). https://www.researchgate.net/publication/286673825_Stratigraphy_and_depositional_palaeogeography_of_the_Early_Cretaceous_basins_in_Da_Hinggan_Mountains-Mongolia_orogenic_belt_and_its_neighboring_areas
Li, B.L., Sun, Y.G., Chen, G.J., et al., 2016.Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Composition and Its Geological Implication of the Fine-Grained Syenogranite in Dong'an Goldfield from the Lesser Xing'an Mountains.Earth Science, 41(1):1-16(in Chinese with English abstract).
Li, J.Y., 2006.Permian Geodynamic Setting of Northeast China and Adjacent Regions:Closure of the Paleo-Asian Ocean and Subduction of the Paleo-Pacific Plate.Journal of Asian Earth Sciences, 26(3-4):207-224.doi: 10.1016/j.jseaes.2005.09.001
Li, J.Y., Mo, S.G., He, Z.J., et al., 2004.The Timing of Crustal Sinistral Strike-Slip Movement in the Northern Great Khing'an Ranges and Its Constraint on Reconstruction of the Crustal Tectonic Evolution of NE China and Adjacent Areas since the Mesozoic.Earth Science Frontiers, 11(3):157-168(in Chinese with English abstract). doi: 10.1007/s00126-010-0320-9
Li, Y.L., Zhou, H.W., Zhong, Z.Q., et al., 2009.Collision Processes of North China and Siberian Plates:Evidence from LA-ICP-MS Zircon U-Pb Age on Deformed Granite in Xar Moron Suture Zone.Earth Science, 34(6):931-938(in Chinese with English abstract).
Lin, Q., Ge, W.C., Sun, D.Y., et al., 1998.Tectonic Significance of Mesozoic Volcanic Rocks in Northeastern China.Scientia Geologica Sinica, 33(2):129-138(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX802.000.htm
Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010.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
Ludwing, K.R., 2001.Users Manual for Isoplot/EX (Rev.2.49):A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication, Berkeley, 1-55.
Meng, Q.R., 2003.What Drove Late Mesozoic Extension of the Northern China-Mongolia Tract?Tectonophysics, 369(3-4):155-174.doi: 10.1016/s0040-1951(03)00195-1
Metelkin, D.V., Vernikovsky, V.A., Kazansky, A.Y., et al., 2010.Late Mesozoic Tectonics of Central Asia Based on Paleomagnetic Evidence.Gondwana Research, 18(2-3):400-419.doi: 10.1016/j.gr.2009.12.008
Nelson, G.E., 1992.Chemical Subdivision of the A-Type Granitoids:Petrogenetic and Tectonic Implications.Geology, 20(7):641-644.doi:10.1130/0091-7613(1992)020<0641:csotat>2.3.co;2
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
Rudnick, R.L., 2000.Rutile-Bearing Refractory Eclogites:Missing Link between Continents and Depleted Mantle.Science, 287(5451):278-281.doi: 10.1126/science.287.5451.278
Scherer, E.E., Cameron, K.L., Blichert-Toft, J., 2000.Lu-Hf Garnet Geochronology:Closure Temperature Relative to the Sm-Nd System and the Effects of Trace Mineral Inclusions.Geochimica et Cosmochimica Acta, 64(19):3413-3432.doi: 10.1016/s0016-7037(00)00440-3
Sengör, A.M.C., Natalin, B.A., 1996.Paleotectonics of Asia:Fragments of a Synthesis.Translated by Yin, A., Harrison, M., Cambridge University Press, London, 486-640.
Shao, J.A., Liu, F.T., Chen, H., 2000.Seismic Tomography of the Northwest Pacific and Its Geodynamic Implications.Progress in Natural Science, 11(1):46-49. https://www.researchgate.net/publication/297284294_Seismic_tomography_of_the_northwest_Pacific_and_its_geodynamic_implications
Shao, J.A., Liu, F.T., Chen, H., et al., 2001.Relationship between Mesozoic Magmatism and Subduction in Da Hinggan-Yanshan Area.Acta Geologica Sinica, 75(1):56-63(in Chinese with English abstract). https://www.researchgate.net/publication/229926265_Relationship_between_Mesozoic_Magmatism_and_Subduction_in_the_Da_Hinggan-Yanshan_Area
Shao, J., Zhang, L.Q., Mu, B.L., 1998.Tectono-Thermal Evolution of Middle-South Section of the Da Hinggan Mountains.Science in China (Series D), 41(6):570-579.doi: 10.1007/bf02878738
Shao, J.A., Zhang, L.Q., Xiao, Q.H., et al., 2005.Rising of Da Hinggan Mts.in Mesozoic:A Possible Mechanism of Intracontinental Orogeny.Acta Petrologica Sinica, 21(3):789-794(in Chinese with English abstract). https://www.researchgate.net/publication/282285871_Rising_of_Da_Hinggan_Mts_in_Mesozoic_A_possible_mechanism_of_intracontinental_orogeny
Söderlund, U., Patchett, P.J., Vervoort, J.D., et al., 2004.The ¹⁷⁶Lu Decay Constant Determined by Lu-Hf and U-Pb Isotope Systematics of Precambrian Mafic Intrusions.Earth and Planetary Science Letters, 219(3-4):311-324.doi:10.1016/s0012-821x (04)00012-3
Sorokin, A.A., Yarmolyuk, V.V., Kotov, A.B., et al., 2004.Geochronology of Triassic-Jurassic Granitoids in the Southern Framing of the Mongol-Okhotsk Foldbelt and the Problem of Early Mesozoic Granite Formation in Central and Eastern Asia.Doklady Earth Sciences, 399(8):1091-1094.
Su, Y.P., Tang, H.F., 2005.Trace Element Geochemistry of A-Type Granites.Bulletin of Mineralogy, Petrology and Geochemistry, 24(3):245-251(in Chinese with English abstract). https://www.researchgate.net/publication/291978400_Trace_element_geochemistry_of_A-type_granites
Sun, D.Y., Gou, J., Ren, Y.S., et al., 2011.Zircon U-Pb Dating and Study on Geochemistry of Volcanic Rocks in Manitu Formation from Southern Manchuria, Inner Mongolia.Acta Petrologica Sinica, 27(10):3083-3094(in Chinese with English abstract). https://www.researchgate.net/publication/279714834_Zircon_U-Pb_dating_and_study_on_geochemistry_of_volcanic_rocks_in_Manitu_Formation_from_southern_Manchuria_Inner_Mongolia
Sun, D.Y., Wu, F.Y., Gao, S., et al., 2005.Confirmation of Two Episodes of A-Type Granite Emplacement during Late Triassic and Early Jurassic in the Central Jilin Province, and Their Constraints on the Structural Pattern of Eastern Jilin-Heilongjiang Area, China.Earth Science Frontiers, 12(2):263-275(in Chinese with English abstract). doi: 10.1080/00206814.2014.956818?scroll=top&needAccess=true
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
Tan, J., Wei, J.H., Li, S.R., et al., 2008.Geochemical Characteristics and Tectonic Significance of Kunlunguan A-Type Granite, Guangxi.Earth Science, 33(6):743-754(in Chinese with English abstract). https://www.researchgate.net/publication/281510397_Geochemical_characteristics_and_tectonic_significance_of_Kunlunguan_A-type_granite_Guangxi
Vervoort, J.D., Patchett, P.J., Gehrels, G.E., et al., 1996.Constraints on Early Earth Differentiation from Hafnium and Neodymium Isotopes.Nature, 379(6566):624-627.doi: 10.1038/379624a0
Wang, F., Zhou, X.H., Zhang, L.C., et al., 2006.Late Mesozoic Volcanism in the Great Xing'an Range (NE China):Timing and Implications for the Dynamic Setting of NE Asia.Earth and Planetary Science Letters, 251(1-2):179-198.doi: 10.1016/j.epsl.2006.09.007
Wang, T., Zheng, Y.D., Zhang, J.J., et al., 2011.Pattern and Kinematic Polarity of Late Mesozoic Extension in Continental NE Asia:Perspectives from Metamorphic Core Complexes.Tectonics, 30(6):148-151.doi: 10.1029/2011tc002896
Wang, X.X., Wang, T., Happala, I., et al., 2005.Genesis of Mafic Enclaves from Rapakivi-Textured Granites in the Qinling and Its Petrological Significance:Evidence of Elements and Nd, Sr Isotopes.Acta Petrologica Sinica, 21(3):935-946(in Chinese with English abstract). https://www.researchgate.net/publication/286792005_Genesis_of_mafic_enclaves_from_rapakivi-textured_granites_in_the_Qinling_and_its_petrological_significance_Evidence_of_elements_and_Nd_Sr_isotopes
Wang, Y.B., Han, J., Li, J.B., et al., 2010.Age, Petrogenesis and Geological Significance of the Deformed Granitoids in the Louzidian Metamorphic Core Complex, Southern Chifeng, Inner Mongolia:Evidence from Zircon U-Pb Dates and Hf Isotopes.Acta Petrologica et Mineralogica, 29(6):763-778(in Chinese with English abstract).
Whalen, J.B., Currie, K.L., Chappell, B.W., 1987.A-Type Granites:Geochemical Characteristics, Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology, 95(4):407-419.doi: 10.1007/bf00402202
Wu, F.Y., Li, X.H., Yang, J.H., et al., 2007a.Discussions on the Petrogenesis of Granites.Acta Petrologica Sinica, 23(6):1217-1238(in Chinese with English abstract).
Wu, F.Y., Li, X.H., Zheng, Y.F., et al., 2007b.Lu-Hf Isotopic Systematics and Their Applications in Petrology.Acta Petrologica Sinica, 23(2):185-220(in Chinese with English abstract). https://www.researchgate.net/publication/305531916_Lu-Hf_isotopic_systematics_and_thier_applications_in_petrology
Xiao, W.J., Windley, B.F., Hao, J., et al., 2003.Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China:Termination of the Central Asian Orogenic Belt.Tectonics, 22(6):8-1-8-20.doi: 10.1029/2002tc001484
Xu, W.L., Wang, F., Pei, F.P., et al., 2013.Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations.Acta Petrologica Sinica, 29(2):339-353(in Chinese with English abstract). https://www.researchgate.net/publication/282382991_Mesozoic_tectonic_regimes_and_regional_ore-forming_background_in_NE_China_Constraints_from_spatial_and_temporal_variations_of_Mesozoic_volcanic_rock_associations_Acta_Petrologica_Sinica_292
Yang, D.B., Xu, W.L., Pei, F.P., et al., 2009.Petrogenesis of the Paleoproterozoic K-Feldspar Granites in Bengbu Uplift:Constraints from Petro-Geochemistry, Zircon U-Pb Dating and Hf Isotope.Earth Science, 34(1):148-164(in Chinese with English abstract). doi: 10.1111/1755-6724.13197/full
Yang, D.B., Xu, W.L., Wang, Q.H., et al., 2007.Petrogenesis of the Mesozoic Granite in Bengbu Uplift:Constraints from Zircon Hf Isotope.Acta Petrologica Sinica, 23(2):381-392(in Chinese with English abstract). https://www.researchgate.net/publication/279623970_Petrogenesis_of_the_Mesozoic_granite_in_Bengbu_uplift_Constraints_from_zircon_Hf_isotope
Yang, G.X., Li, Y.J., Si, G.H., et al., 2010.Trace Elements Geochemistry Feature and Tectonic Significance of the Beilekuduke Aluminous A-Type Granite in East Junggar.Journal of Earch Sciences and Environment, 32(1):34-39(in Chinese with English abstract). https://www.researchgate.net/publication/261701431_Geochemistry_of_A-type_granites_in_the_Huangshaping_polymetallic_deposit_South_Hunan_China_Implications_for_granite_evolution_and_associated_mineralization
Zhang, K.X., Pan, G.T., He, W.H., et al., 2015.New Division of Tectonic-Strata Superregion in China.Earth Science, 40(2):206-233(in Chinese with English abstract). https://www.researchgate.net/publication/281911273_New_division_of_tectonic-strata_superregion_in_China
Zhang, L.C., Chen, Z.G., Zhou, X.H., et al., 2007.Characteristics of Deep Sources and Tectonic-Magmatic Evolution of the Early Cretaceous Volcanics in Genhe Area, Da-Hinggan Mountains:Constraints of Sr-Nd-Pb-Hf Isotopic Geochemistries.Acta Petrologica Sinica, 23(11):2823-2835(in Chinese with English abstract).
Zhang, Q., Jin, W.J., Li, C.D., et al., 2009.Yanshanian Large-Scale Magmatism and Lithosphere Thinning in Eastern China:Relation to Large Igneous Province.Earth Science Frontiers, 16(2):21-51(in Chinese with English abstract). https://www.researchgate.net/publication/284562276_Yanshanian_large-scale_magmatism_and_lithosphere_thinning_in_Eastern_China_relation_to_large_igneous_province
Zhang, Q., Ran, H., Li, C.D., 2012.A-Type Granite:What is the Essence?Acta Petrologica et Mineralogica, 31(4):621-626(in Chinese with English abstract). http://www.iep.utm.edu/aq-meta/
Zhao, G.L., Yang, G.L., Wang, Z., 1989.Mesozoic Volcanic Rocks in Southern-Central Da Hinggan Mountains.Beijing Science and Technology Press, Beijing (in Chinese).
Zhao, H.L., Deng, J.F., Chen, F.J., et al., 1998.Petrology of the Mesozoic Volcanic Rocks and the Basin Formation in the Northeast China.Geoscience, 12(1):56-62(in Chinese with English abstract).
Zhao, Y., Yang, Z.Y., Ma, X.H., 1994.Geotectonic Transition from Paleoasian System and Paleotethyan System to Paleo-Pacific Active Continental Margin in Eastern Asia.Scientia Geologica Sinica, 29(2):105-119(in Chinese with English abstract). https://www.researchgate.net/publication/287537111_Late_Mesozoic_sedimentary_basin_evolution_and_tectonic_implication_in_Huangling_area_northern_of_Yangtze_block
Zhao, Z.H., Xiong, X.L., Wang, Q., et al., 2008.Some Aspects on Geochemistry of Nb and Ta.Geochimica, 37(4):304-320(in Chinese with English abstract). https://www.researchgate.net/publication/285505066_Some_aspects_on_geochemistry_of_Nb_and_Ta
Zheng, Y.D., 2005.Kinematics and Dynamics of the Mesozoic Orogeny and Late-Orogenic Extensional Collapse in the Sino-Mongolian Border Areas.Science in China (Series D), 48(7):849-862.doi: 10.1360/03yd0552
Zheng, Y.D., Davis, G.A.Wang, C., et al., 2000.Major Mesozoic Tectonic Events in the Yanshan Belt and the Plate Tectonic Setting.Acta Geologica Sinica, 74(4):289-302(in Chinese with English abstract). https://www.researchgate.net/publication/284596167_Major_Mesozoic_tectonic_events_in_the_Yanshan_belt_and_the_plate_tectonic_setting
Zheng, Y.F., Chen, R.X., Zhang, S.B., et al., 2007.Zircon Lu-Hf Isotope Study of Ultrahigh-Pressure Eclogite and Granitic Gneiss in the Dabie Orogen.Acta Petrologica Sinica, 23(2):317-330(in Chinese with English abstract). https://www.researchgate.net/publication/279702417_Zircon_Lu-HF_isotope_study_of_ultrahigh-pressure_eclogite_and_granitic_gneiss_in_the_Dabie_orogen
Zorin, Y.A., 1999.Geodynamics of the Western Part of the Mongolia-Okhotsk Collisional Belt, Trans-Baikal Region (Russia) and Mongolia.Tectonophysics, 306(1):33-56.doi: 10.1016/s0040-1951(99)00042-6
葛文春, 林强, 孙德有, 等, 1999.大兴安岭中生代玄武岩的地球化学特征:壳幔相互作用的证据.岩石学报, 15(3):396-406. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB199903007.htm
侯可军, 李延河, 田有荣, 2009.LA-MC-ICP-MS锆石微区原位U-Pb定年技术.矿床地质, 28(4):481-492. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200904009.htm
侯可军, 李延河, 邹天人, 等, 2007.LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报, 23(10):2595-2604. doi: 10.3969/j.issn.1000-0569.2007.10.025
旷红伟, 柳永清, 刘燕学, 等, 2013.兴蒙造山区及邻区早白垩世盆地岩石地层格架与沉积古地理演化.地质通报, 32(7):1063-1084. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201307010.htm
李碧乐, 孙永刚, 陈广俊, 等, 2016.小兴安岭东安金矿区细粒正长花岗岩U-Pb年龄、岩石地球化学、Hf同位素组成及地质意义.地球科学, 41(1):1-16. doi: 10.11764/j.issn.1672-1926.2016.01.0001
李锦轶, 莫申国, 和政军, 等, 2004.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约.地学前缘, 11(3):157-168. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200403022.htm
李益龙, 周汉文, 钟增球, 等, 2009.华北与西伯利亚板块的对接过程:来自西拉木伦缝合带变形花岗岩锆石LA-ICP-MS U-Pb年龄证据.地球科学, 34(6):931-938. http://earth-science.net/WebPage/Article.aspx?id=1908
林强, 葛文春, 孙德有, 等, 1998.中国东北地区中生代火山岩的大地构造意义.地质科学, 33(2):129-138. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX802.000.htm
邵济安, 刘福田, 陈辉, 等, 2001.大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系.地质学报, 75(1):56-63. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200101010.htm
邵济安, 张履桥, 肖庆辉, 等, 2005.中生代大兴安岭的隆起-一种可能的陆内造山机制.岩石学报, 21(3):789-794. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503019.htm
苏玉平, 唐红峰, 2005.A型花岗岩的微量元素地球化学.矿物岩石地球化学通报, 24(3):245-251. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH200503012.htm
孙德有, 苟军, 任云生, 等, 2011.满洲里南部玛尼吐组火山岩锆石U-Pb年龄与地球化学研究.岩石学报, 27(10):3083-3094. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201110024.htm
孙德有, 吴福元, 高山, 等, 2005.吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约.地学前缘, 12(2):263-275. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY20050200Z.htm
谭俊, 魏俊浩, 李水如, 等, 2008.广西昆仑关A型花岗岩地球化学特征及构造意义.地球科学, 33(6):743-754. http://earth-science.net/WebPage/Article.aspx?id=1765
王晓霞, 王涛, Happala, I., 等, 2005.秦岭环斑结构花岗岩中暗色包体的岩浆混合成因及岩石学意义--元素和Nd、Sr同位素地球化学证据.岩石学报, 21(3):935-946. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503032.htm
王彦斌, 韩娟, 李建波, 等, 2010.内蒙赤峰楼子店拆离断层带下盘变形花岗质岩石的时代、成因及其地质意义--锆石U-Pb年龄和Hf同位素证据.岩石矿物学杂志, 29(6):763-778. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201006013.htm
吴福元, 李献华, 杨进辉, 等, 2007a.花岗岩成因研究的若干问题.岩石学报, 23(6):1217-1238. http://www.cnki.com.cn/Article/CJFDTOTAL-HBDK199001002.htm
吴福元, 李献华, 郑永飞, 等, 2007b.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
许文良, 王枫, 裴福萍, 等, 2013.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约.岩石学报, 29(2):339-353. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201302002.htm
杨德彬, 许文良, 裴福萍, 等, 2009.蚌埠隆起区古元古代钾长花岗岩的成因:岩石地球化学、锆石U-Pb年代学与Hf同位素的制约.地球科学, 34(1):148-164. http://earth-science.net/WebPage/Article.aspx?id=1794
杨德彬, 许文良, 王清海, 等, 2007.蚌埠隆起区中生代花岗岩的岩石成因:锆石Hf同位素的证据.岩石学报, 23(2):381-392. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200702018.htm
杨高学, 李永军, 司国辉, 等, 2010.东准噶尔贝勒库都克铝质A型花岗岩微量元素地球化学特征及地质意义.地球科学与环境学报, 32(1):34-39. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX201001008.htm
张克信, 潘桂棠, 何卫红, 等, 2015.中国构造-地层大区划分新方案.地球科学, 40(2):206-233. http://earth-science.net/WebPage/Article.aspx?id=3179
张连昌, 陈志广, 周新华, 等, 2007.大兴安岭根河地区早白垩世火山岩深部源区与构造-岩浆演化:Sr-Nd-Pb-Hf同位素地球化学制约.岩石学报, 23(11):2823-2835. doi: 10.3969/j.issn.1000-0569.2007.11.013
张旗, 金惟俊, 李承东, 等, 2009.中国东部燕山期大规模岩浆活动与岩石圈减薄:与大火成岩省的关系.地学前缘, 16(2):21-51. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200902003.htm
张旗, 冉皞, 李承东, 2012.A型花岗岩的实质是什么?岩石矿物学杂志, 31(4):621-626. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ201401010038.htm
赵国龙, 杨桂林, 王忠, 1989.大兴安岭中南部中生代火山岩.北京:北京科学技术出版社.
赵海玲, 邓晋福, 陈发景, 等, 1998.中国东北地区中生代火山岩岩石学特征与盆地形成.现代地质, 12(1):56-62. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ801.006.htm
赵越, 杨振宇, 马醒华, 1994.东亚大地构造发展的重要转折.地质科学, 29(2):105-119. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX402.000.htm
赵振华, 熊小林, 王强, 等, 2008.铌与钽的某些地球化学问题.地球化学, 37(4):304-320. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200804004.htm
郑亚东, Davis, G.A., 王琮, 等, 2000.燕山带中生代主要构造事件与板块构造背景问题.地质学报, 74(4):289-302. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200004000.htm
郑永飞, 陈仁旭, 张少兵, 等, 2007.大别山超高压榴辉岩和花岗片麻岩中锆石Lu-Hf同位素研究.岩石学报, 23(2):317-330. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200702013.htm