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

张延军; 孙丰月; 许成瀚; 禹禄

doi:10.3799/dqkx.2016.127

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

doi: 10.3799/dqkx.2016.127

吉林大学地球科学学院，吉林长春 130061

基金项目:

中国地质调查局地质调查项目 12120114080801

国家自然科学基金项目 41272093

详细信息

作者简介:
张延军(1976-)，男，博士研究生，主要从事矿床学研究.E-mail：yanjunzhang@yeah.net

通讯作者:
孙丰月, E-mail：sfy@jlu.edu.cn

中图分类号: P581
计量
- 文章访问数: 4479
- HTML全文浏览量: 2453
- PDF下载量: 30
- 被引次数: 0
出版历程
- 收稿日期: 2016-04-25
- 刊出日期: 2016-11-15

Geochronology, Geochemistry and Zircon Hf Isotopes of the Tanjianshan Granite Porphyry Intrusion in Dachaidan Area of the North Margin of Qaidam Basin, NW China

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

摘要

摘要: 为了研究柴北缘大柴旦地区在华力西期构造演化特征，对大柴旦地区滩间山花岗斑岩进行了锆石U-Pb年代学、岩石地球化学以及Hf同位素的研究.花岗斑岩中锆石LA-ICP-MS U-Pb定年结果表明，该岩体形成于晚泥盆世(356.0±2.8 Ma，MSWD=0.53).地球化学分析显示花岗斑岩属于中钾钙碱性-钙碱性系列，A/CNK值为0.97~1.10，属弱过铝质，为I型花岗岩，富集大离子亲石元素(如K、Ba、Rb)和轻稀土元素(LREE)以及Th、U，相对亏损高场强元素(如Ta、Nb、Ti、P).岩石的ε_Hf(t)值和二阶段模式年龄(T_DM2)分别介于±5.43~±8.38和1 017~1 284 Ma之间.上述特征表明，滩间山花岗斑岩的原始岩浆源于中元古代新增生陆壳的部分熔融.综合区域地质演化背景，认为滩间山花岗斑岩形成于柴达木地块与南祁连地块碰撞后伸展构造环境.
- 锆石U-Pb年龄 /
- 锆石Hf同位素 /
- 滩间山 /
- 地球化学 /
- 年代学
Abstract: In order to research the Variscan tectonic evolution features of Dachaidan region in North Qaidam, this paper presents LA-ICP-MS zircon U-Pb dating, geochemical and Hf isotopic data of the granite porphyry from Tanjianshan intrusion in Dachaidan region, with the aim of constraining its formation time, petrogenesis and the regional tectonic setting. The LA-ICP-MS U-Pb dating results of zircons from the granite porphyry indicate that the intrusion formed in the Late Devonian Epoch (356.0±2.8 Ma, MSWD=0.53). Geochemically, these rocks fall into the calc-alkaline to middle-K calc-alkaline series, with an A/CNK ratio of 0.97-1.10, which are weakly peraluminous granites, being of the characteristics of I type granitoids, enriched in LILE(such as K, Ba, Rb), LREE, Th and U, relatively depleted in HFSE (such as Ta, Nb, Ti, P). The ε_Hf(t) values of the granite porphyry vary from ±5.43 to ±8.38, and two-stage model ages (T_DM2) range from 1 017 to 1 284 Ma. These characteristics suggest that the primary magma was derived from the remelting of juvenile crustal materials in Mesoproterozoic. In context of its regional geological background, we conclude the granite porphyry from Tanjianshan intrusion were formed extensional tectonic setting after the collision between Qaidam block and Qilian block.
- zircon U-Pb chronology /
- Zircon Hf isotopes /
- Tanjianshan /
- geochemistry /
- geochronology

HTML全文

图 1 研究区地质简图

1.花岗闪长岩；2.花岗斑岩；3.辉长岩；4.闪长岩；5.第四系；6.中元古代万洞沟群；7.断层；8.取样位置

Fig. 1. Geological sketch map of the study area

下载: 全尺寸图片幻灯片

图 2 花岗斑岩显微照片

花岗斑岩(+)；Bt.黑云母；Or.正长石；Pl.斜长石；Q.石英

Fig. 2. Microphotographs of the granite porphyry in Tanjianshan

下载: 全尺寸图片幻灯片

图 3 花岗班岩锆石CL图像

Fig. 3. CL images of zircons from the granite porphyry

下载: 全尺寸图片幻灯片

图 4 花岗斑岩U-Pb年龄谐和图(a)和加权平均年龄(b)

Fig. 4. Zircon U-Pb concordia diagram (a) and weighted average ages diagram (b) from the granite porphyry

下载: 全尺寸图片幻灯片

图 5 岩石TAS图解(a)和K₂O-SiO₂图解(b)

a.分界线上方为碱性，下方为亚碱性据Irvine and Baragar(1971)；b.据Peccerillo and Taylor(1976)

Fig. 5. TAS diagram (a) and K₂O-SiO₂ (b) diagram of the granite porphyry

下载: 全尺寸图片幻灯片

图 6 A/KNC-A/NK图解

据Maniar and Piccoli(1989)

Fig. 6. A/KNC-A/NK diagram of the granite porphyry

下载: 全尺寸图片幻灯片

图 7 花岗斑岩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)

a.标准化值据Boynton(1984)；b.标准化值据Sun and Mcdonough(1989)

Fig. 7. Chondrite-normalized REE distribution patterns (a) and primitive mantle-normalized trace element spider diagrams of the granite porphyry (b)

下载: 全尺寸图片幻灯片

图 8 岩石的Hf同位素特征

据吴福元等(2007)

Fig. 8. Hf isotopic compositions of the granite porphyry

下载: 全尺寸图片幻灯片

图 9 岩石Hf-Rb/30-3Ta判别图解

据Brown et al.(1984)

Fig. 9. Hf-Rb/30-3Ta diagram of the granite porphyry

下载: 全尺寸图片幻灯片

表 1 花岗斑岩中锆石U-Pb同位素分析结果

Table 1. Zircon U-Pb analyses of the granite porphyry

样品	Th U		Th/U	²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U		²⁰⁶Pb/²³⁸U
样品	10^-6		Th/U	比值	1σ	比值	1σ	比值	1σ	年龄(Ma)	1σ
XJG-N1	408	1023	0.40	0.073 385	0.002 213	0.421 631	0.017 651	0.056 094	0.000 712	352	4
XJG-N2	202	451	0.45	0.064 487	0.002 807	0.414 923	0.021 425	0.056 369	0.000 752	354	4
XJG-N3	189	426	0.44	0.055 518	0.003 134	0.425 024	0.021 744	0.056 384	0.000 857	354	6
XJG-N4	41	88	0.47	0.064 909	0.005 129	0.424 216	0.014 781	0.056 387	0.000 653	354	7
XJG-N5	203	403	0.50	0.076 04	0.002 895	0.415 678	0.019 986	0.056 414	0.000 656	354	4
XJG-N6	198	444	0.45	0.052 461	0.002 33	0.407 076	0.017 546	0.056 626	0.000 838	355	5
XJG-N7	209	504	0.41	0.051 271	0.002 702	0.402 974	0.021 623	0.056 732	0.000 757	356	4
XJG-N8	205	493	0.42	0.055 962	0.001 978	0.408 925	0.014 645	0.056 826	0.000 588	356	3
XJG-N9	335	804	0.42	0.056 416	0.001 648	0.414 312	0.012 994	0.057 268	0.000 740	359	4
XJG-N10	246	565	0.44	0.057 981	0.002 648	0.414 513	0.021 865	0.057 832	0.000 747	362	4
XJG-N11	102	245	0.42	0.059 846	0.003 280	0.425 621	0.025 976	0.057 889	0.000 785	363	6

下载: 导出CSV

表 2 滩间山花岗斑岩主量元素、稀土元素和微量元素含量及有关参数

Table 2. Major, REE and trace element content and parameter of the granite porphyry in Tanjianshan

样品	XJG-Y1-1	XJG-Y1-2	XJG-Y1-3	XJG-Y1-4	XJG-Y1-5	XJG-Y1-6	XJG-Y1-7	XJG-Y1-8
SiO₂	68.64	71.61	70.08	68.72	71.72	69.52	69.27	71.05
TiO₂	0.29	0.32	0.30	0.31	0.32	0.31	0.30	0.31
Al₂O₃	14.55	15.39	14.53	14.72	15.10	14.85	14.62	15.08
Fe₂O₃	0.82	0.86	0.93	0.94	1.12	0.96	1.02	0.95
FeO	1.43	1.33	1.23	1.25	1.06	1.23	1.31	1.33
MnO	0.07	0.06	0.07	0.07	0.04	0.06	0.08	0.07
MgO	0.83	0.73	0.73	0.80	0.66	0.82	0.85	0.74
CaO	3.27	2.98	2.59	2.91	2.88	2.37	2.64	2.68
Na₂O	4.30	4.32	4.51	4.21	4.28	4.24	4.20	4.63
K₂O	1.85	2.08	1.77	2.02	2.10	1.98	1.99	1.90
P₂O₅	0.08	0.08	0.08	0.08	0.09	0.08	0.08	0.08
LOI	3.77	2.11	3.02	3.61	2.05	3.11	3.38	2.23
Total	99.91	101.86	99.83	99.65	101.43	99.53	99.73	101.04
ALK	6.15	6.39	6.29	6.24	6.39	6.22	6.19	6.52
Na₂O/K₂O	2.33	2.08	2.54	2.08	2.04	2.14	2.12	2.44
A/CNK	0.97	1.04	1.03	1.02	1.04	1.10	1.05	1.04
Mg^#	42.09	39.70	40.13	41.89	37.58	42.60	41.95	39.04
La	11.28	6.63	10.42	12.38	13.11	13.97	12.20	11.14
Ce	25.00	16.35	22.24	26.85	27.14	28.96	25.76	24.26
Pr	2.70	1.83	2.58	2.95	3.05	3.27	3.02	2.68
Nd	11.09	7.65	10.62	11.02	12.32	12.98	12.23	9.06
Sm	2.13	1.41	2.16	2.30	2.41	2.43	2.35	2.07
Eu	0.60	0.34	0.54	0.59	0.53	0.67	0.63	0.51
Gd	1.77	1.05	1.75	1.77	2.05	1.98	2.04	1.72
Tb	0.28	0.17	0.28	0.25	0.30	0.28	0.31	0.24
Dy	1.54	0.97	1.59	1.41	1.74	1.64	1.66	1.33
Ho	0.23	0.15	0.23	0.21	0.25	0.24	0.26	0.20
Er	0.72	0.49	0.73	0.62	0.80	0.72	0.77	0.61
Tm	0.09	0.06	0.10	0.08	0.09	0.10	0.10	0.07
Yb	0.59	0.43	0.67	0.61	0.68	0.65	0.66	0.55
Lu	0.08	0.06	0.10	0.08	0.09	0.09	0.10	0.07
Y	7.12	3.04	7.31	6.15	7.53	7.65	8.11	4.89
ΣREE	58.10	37.59	54.01	61.12	64.56	67.98	62.09	54.51
LREE	52.80	34.21	48.56	56.09	58.56	62.28	56.19	49.72
HREE	5.30	3.38	5.45	5.03	6.00	5.70	5.90	4.79
LREE/HREE	9.96	10.12	8.91	11.15	9.76	10.93	9.52	10.38
La_N/Yb_N	12.89	10.40	10.49	13.68	13.00	14.49	12.46	13.66
δEu	0.92	0.82	0.82	0.86	0.71	0.91	0.86	0.80
δCe	1.06	1.11	1.01	1.04	1.00	1.00	0.99	1.04
Rb	87.58	92.35	94.15	96.31	88.98	94.12	98.78	101.12
Ba	207.90	228.20	195.30	325.20	277.80	241.80	249.30	221.30
Th	5.97	2.40	5.78	6.46	6.81	7.17	6.62	6.22
U	1.76	1.74	2.24	1.84	2.65	2.33	2.15	2.13
Nb	2.57	2.62	2.63	2.54	2.74	2.69	2.67	2.60
Ta	0.68	0.71	0.72	0.76	0.69	0.56	0.69	0.74
Sr	215.10	137.00	180.40	174.10	174.50	195.60	217.10	173.00
Nd	11.09	7.65	10.62	11.02	12.32	12.98	12.23	9.06
Zr	55.47	62.07	107.90	48.97	99.63	67.24	95.57	49.55
Hf	1.57	1.79	2.86	1.46	2.54	1.87	2.50	1.54
Nb/Ta	3.78	3.69	3.65	3.34	3.97	4.80	3.87	3.51
Rb/Sr	0.41	0.67	0.52	0.55	0.51	0.48	0.45	0.58
Hf/Th	0.26	0.75	0.50	0.23	0.37	0.26	0.38	0.25
La/Nb	4.40	2.53	3.96	4.88	4.78	5.19	4.57	4.29
注：主量元素单位为10^-2；微量、稀土元素单位为10^-6.

下载: 导出CSV

表 3 滩间山花岗斑岩锆石Hf同位素分析结果

Table 3. LA-ICPMS zircon U-Pb analyses of the granite porphyry in Tanjianshan

样品	年龄(Ma)	¹⁷⁶Yb/¹⁷⁷Hf	¹⁷⁶Lu/¹⁷⁷Hf	¹⁷⁶Hf/¹⁷⁷Hf	1σ	ε_Hf(t)	T_DM1(Hf)(Ma)	T_DM2(Hf)(Ma)	f_Lu/Hf
XJG-N1-01	352	0.054 353	0.001 117	0.282 797	0.000 026	8.38	647	1 017	-0.97
XJG-N1-02	354	0.020 430	0.000 414	0.282 783	0.000 024	8.08	655	1 044	-0.99
XJG-N1-03	354	0.034 401	0.000 712	0.282 710	0.000 021	5.43	762	1 284	-0.98
XJG-N1-04	354	0.025 633	0.000 574	0.282 710	0.000 036	5.46	759	1 281	-0.98
XJG-N1-05	354	0.038 097	0.000 767	0.282 781	0.000 018	7.91	664	1 060	-0.98
XJG-N1-06	355	0.033 948	0.000 720	0.282 755	0.000 022	7.05	699	1 139	-0.98
XJG-N1-07	356	0.033 248	0.000 728	0.282 763	0.000 019	7.32	689	1 115	-0.98
XJG-N1-08	356	0.048 840	0.001 110	0.282 745	0.000 017	6.60	722	1 180	-0.97
XJG-N1-09	359	0.028 541	0.000 880	0.282 754	0.000 018	7.05	704	1 142	-0.97
XJG-N1-10	362	0.031 018	0.000 780	0.282 764	0.000 044	7.51	688	1 102	-0.98
XJG-N1-11	363	0.042 696	0.001 172	0.282 775	0.000 018	7.82	679	1 075	-0.96

下载: 导出CSV

参考文献(131)

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
Amelin, Y., Lee, D.C., Halliday, A, N., 2000.Early-Middle Archean Crustal Evolution Deduced from Lu-Hf and U-Pb Isotope Studies of Single Zircon Grains.Geochimica Cosmochimica Acta, 64(24):4205-4225.doi: 10.1016/S0016-7037(00)00493-2
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
Boynton, W.V., 1984.Geochemistry of the Rare Earth Elements:Meteorite Studies, In:Henderson, P., ed., Rare Earth Elements Geochemistry.Elsevier, Amsterdam, 63-114.
Brown, G.C., Thorpe, R.S., Webb, P.C., 1984.The Geochemical Characteristics of Granitoids in Constrasting Arcs and Comments on Magma Sources.Journal of the Geological Society, 141: 411-426. doi: 10.1144/gsjgs.141.3.0413
Chen, N.S., Wang, X.Y., Zhang, H.F., et al., 2007.Geochemistry and Nd-Sr-Pb Isotopic Compositions of Granitoids from Qaidam and Oulongbuluke Micro-Blocks, NW China:Constraints on Basement Nature and Tectonic Affinity.Earth Science, 32(1):7-15 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX200701001.htm
Defant, M.J., Drummond, M.S., 1990.Derivation of some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature, 347(6294):662-665.doi: 10.1038/347662a0
Defant, M.J., Xu, J.F., Kepezhinskas, P., et al., 2002.Adakites:Some Variations on a Theme.Acta Petrologica Sinica, (18):129-142. http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200202000.htm
Dong, Z.C., Gu, P.Y., Chen, R.M., et al., 2015.Geochronology, Geochemistry, and Hf Isotope of YanchangbeishanAdamellite of Lenghu Area in Qinghai.Earth Science, 40(1):130-144 (in Chinese with English abstract).doi: 10.3799/dqkx.2015.009
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
Guillot, S., Mahéo, G., de Sigoyer, J., et al., 2008.Tethyan and Indian Subduction Viewed from the Himalayan High-to Ultrahigh-Pressure Metamorphic Rocks.Tectonophysics, 451(1-4):225-241.doi: 10.1016/j.tecto.2007.11.059
Hao, G.J., Lu, S.N., Wang, H.C., et al., 2004.The Pre-Devonian Tectonic Framework in the Northern Margin of Qaidam Basin and Geological Evolution of Olongbuluck Palaeo-Block.Earth Science Frontiers, 11(3):115-122 (in Chinese with English abstract).
Hu, Z.C., Liu, Y.S., Gao, S., et al., 2012.Improved In-Situ Hf Isotope Ratio Analysis of Zircon Using Newly Designed X Skimmer Cone and Jet Sample Cone in Combination with the Addition of Nitrogen by Laser Ablation Multiple Collector ICP-MS.Journal of Analytical Atomic Spectrometry, 27(9):1391.doi: 10.1039/c2ja30078h
Hugh, R.R., John, T., 2005.Adakites—The Key to Understanding LILE Depletion in Granulites.Lithos, (79):61-81. http://www.sciencedirect.com/science/article/pii/S0024493704002695
Irvine, T.N., Baragar, W.R.A., 1971.A Guide to the Chemical Classification of the Common Volcanic Rocks.Canadian Journal of Earth Sciences, 8(5):523-548.doi: 10.1139/e71-055
Knudsen, T.L., Griffin, W., Hartz, E., et al., 2001.In-Situ Hafnium and Lead Isotope Analyses of Detrital Zircons from the Devonian Sedimentary Basin of NE Greenland:A Record of Repeated Crustal Reworking.Contributions to Mineralogy and Petrology, 141(1):83-94.doi: 10.1007/s004100000220
Kou, X.H., Zhang, K.X., Lin, Q.X., et al., 2007.The Distribution of Permian Sedimentary Sequences in the Adjacent Area of Qinglin-Qilian-Kunlun.Earth Science, 32(5):681-690 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200705013.htm
Lai, S.C., Deng, F.J., Zhao, H.L., 1996.Volcanism and Tectonic Setting during Ordovician Period on North Margin of Qaidam.Journal of Xi an College of Geology, 18(3):8-14 (in Chinese with English abstract). https://www.researchgate.net/publication/292712058_Volcanism_and_tectonic_setting_during_Ordovician_period_on_north_margin_of_Qaidam
Leake, B.E., 1990.Granite Magmas:Their Sources, Initiation and Consequences of Emplacement.Journal of the Geological Society, 147(4):579-589.doi: 10.1144/gsjgs.147.4.0579
Li, C., Zhai, Q.G., Dong, Y.S., et al., 2006.Discovery of Eclogite and Its Geological Significance in Qiangtang Area, Central Tibet.Chinese Science Bulletin, 51(9):1095-1100.doi: 10.1007/s11434-006-1095-3
Li, D.F., Lun, Z.Q., Guo, J.Y., et al., 1991.Regional Geology of Qinghai Province.Geological Publishing House, Beijing, 662 (in Chinese). https://www.researchgate.net/publication/288858553_Qinghai_Bureau_of_Geology_and_Mineral_Resources
Li, H.K., Lu, S.N., Wang, H.C., et al., 2003.Neopropterozoic the Geological Record of Supercontinent in North Qaidam Qinghai-Quanji Group.Geological Survey and Research, 26(1):27-37 (in Chinese). https://www.researchgate.net/publication/281999808_Quanji_Group-the_geological_record_of_the_Rodinia_Supercontinent_breakup_in_the_early_Neoproterozoic_preserved_in_the_north_Qaidam_margin_Qinghai_Northwest_China
Ling, J.L., Zhao, Y.F., Kang, Z., 2014.Petrogenesis and Mineralization of Niubiziliang Mafic-Ultramafic Intrusion in the Northern Margin of Qaidam Block, NW China.Acta Petrologica Sinica, 30(6):1628-1646 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201406008.htm
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
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
Lu, S.N., Chen, Z.H., Li, H.K., et al., 2004.Late Mesoproterozoic-Early Neoproterozoic Evolution of the Qinling Orogen.Geological Bulletin of China, 23(2):107-112 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200402001.htm
Lu, S.N., Wang, H.C., Li, H.K., et al., 2002.Redefinition of the "DakendabanGroup" on the Northern Margin of the Qaidam Basin.Geological Bulletin of China, 21(1):19-23 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200201003.htm
Lu, X.X., Sun, Y, G., Zhang, X.T., et.al., 2007.The SHRIMP Age of Tatalin Rapakivi Granite at the North Margin of Qaidam Basin.Acta Geologica Sinica, 81(5):626-634 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dzxe200705005.htm
Ludwig, K.R., 2003.User s Manual for Isoplot 3.00:A Geochronological Toolkit for Microsoft Execl.No.4.Berkeley Geochronology Center Special Publication, U.S.A..
Martin, H., 1986.Effect of Steeper Archean Geothermal Gradient on Geochemistry of Subduction-Zone Magmas.Geology, S14(9):753.doi:10.1130/0091-7613(1986)14<753:eosagg>2.0.co;2
Maniar, P.D., Piccoli, P.M., 1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin, 101(5):635-643.doi:10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
Meng, F.C., Zhang, J.X., Yang, J.S., 2005.Teetono-Thermal Event of Post-HP/UHP Metamorphism in the Xitieshan Area of the North Qaidam Mounatins, Western China:Isotopic and Geochemical Evidence of Granite and Gneiss.Acate Petrologica Sinica, 21(l):45-56 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB200501005.htm
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
Patchett, P.J., Kouvo, O., Hedge, C.E., et al., 1982.Evolution of Continental Crust and Mantle Heterogeneity:Evidence from Hf Isotopes.Contributions to Mineralogy and Petrology, 78(3):279-297.doi: 10.1007/bf00398923
Peacock, S.A., 1990.Fluid Processes in Subduction Zones.Science, 248(4953):329-337.doi: 10.1126/science.248.4953.329
Qiu, J.X., Yang, W.R., Xia, W.H., 1998.Early Paleozoic Marine Volcanic Rocks, Metallogenic Conditions and Prospecting Directions of the Associated Copper and Polymetallic Deposits in the South Qilian Massif.In:Xia, L.Q., ed., Volcanism and Mineralization in the Qilian Mountain and Its Adjacent.Geologycal Publishing House, Beijing, 111-163 (in Chinese).
Royden, L.H., Burchfiel, B.C., van der Hilst, R.D., 2008.The Geological Evolution of the Tibetan Plateau.Science, 321(5892):1054-1058.doi: 10.1126/science.1155371
Shi, R.D., Yang, J.S., Wu, C.L., 2003.The Discovery of Adakitic Dacite in Early Palaeozoic Island Arc Volcanic Rocks on the Northern Margin of Qaidam Basin and Its Geological Significance.Acta Petrologica et Mineralogica, 22(3):229-236 (in Chinese with English abstract).
Shi, R.D., Yang, J.S., Wu, C.L., et al., 2004.Island Arc Volcanic Rocks in the North Qaidam UHP Metamorphic Belt.Acta Geologica Sinica, 78(1):52-64 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200401007.htm
Song, S.G., Niu, Y.L., Su, L., et al., 2014a.Continental Orogenesis from Ocean Subduction, Continent Collision/subduction, to Orogen Collapse, and Orogen Recycling:The Example of the North Qaidam UHPM Belt, NW China.Earth-Science Reviews, (129):59-84.doi: 10.1016/j.earscirev.2013.11.010
Song, S.G., Niu, Y.L., Su, L., et al., 2014b.Adakitic (Tonalitic-Trondhjemitic) Magmas Resulting from Eclogite Decompression and Dehydration Melting during Exhumation in Response to Continental Collision.Geochimica et Cosmochimica Acta, (130):42-62.doi: 10.1016/j.gca.2014.01.008
Song, S.G., Niu, Y.L., Zhang, L.F., et al., 2009.Time Constraints on Orogenesis from Oceanic Subduction to Continental Subduction, Collision, and Exhumation:An Example from North Qilian and North Qaidam HP-UHP Belts.Acta Petrologica Sinica, 25(9):2067-2077 (in Chinese with English abstract). http://www.oalib.com/paper/1472497
Song, S.G., Yang, J.S., 2001.Sanidine Quartz Inclusions in Dulan Eclogites:Evidence for UHP Metamorphism on the North Margin of the Qaidam Basin, NW China.Acta Geologica Sinica, 75(2):180-185 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200102005.htm
Song, S.G., Yang, J.S., Liou, J.G., et al., 2003a.Petrology, Geochemistry and Isotopic Ages of Eclogites from the Dulan UHPM Terrane, the North Qaidam, NW China.Lithos, 70(3-4):195-211.doi: 10.1016/s0024-4937(03)00099-9
Song, S.G., Yang, J.S., Xu, Z.Q., et al., 2003b.Metamorphic Evolution of the Coesite-Bearing Ultrahigh-Pressure Terrane in the North Qaidam, Northern Tibet, NW China.Journal of Metamorphic Geology, 21(6):631-644.doi: 10.1046/j.1525-1314.2003.00469.x
Song, S.G., Zhang, L.F., Niu, Y.L., 2004.Ultra-Deep Origin of Garnet Peridotite from the North Qaidam Ultrahigh-Pressure Belt, Northern Tibetan Plateau, NW China.American Mineralogist, 89(8-9):1330-1336.doi: 10.2138/am-2004-8-922
Song, S.G., Zhang, L.F., Chen, J., et al., 2015a.Sodic Amphibole Exsolutions in Garnet from Garnet-Peridotite, North Qaidam UHPM Belt, NW China:Implications for Ultradeep-Origin and Hydroxyl Defects in Mantle Garnets.American Mineralogist, 90(5-6):814-820.doi: 10.2138/am.2005.1684
Song, S.G., Wang, M.J., Wang, C., et al., 2015b.Magmatism during Continental Collision, Subduction, Exhumation and Mountain Collapse in Collisional Orogenic Belts and Continental Net Growth:A Perspective.Science China:Earth Sciences, (58):1284-1304 (in Chinese). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxg201508005&dbname=CJFD&dbcode=CJFQ
Song, S.G., Zhang, L., Niu, Y., et al., 2005a.Geochronology of Diamond-Bearing Zircons from Garnet Peridotite in the North Qaidam UHPM Belt, Northern Tibetan Plateau:A Record of Complex Histories from Oceanic Lithosphere Subduction to Continental Collision.Earth and Planetary Science Letters, 234(1-2):99-118.doi: 10.1016/j.epsl.2005.02.036
Song, S.G., Zhang, L.F., Niu, Y.L., 2005b.Evolution from Oceanic Subduction to Continental Collision:A Case Study from the Northern Tibetan Plateau Based on Geochemical and Geochronological Data.Journal of Petrology, 47(3):435-455.doi: 10.1093/petrology/egi080
Song, S.G., Zhang, L.F., Niu, Y.L., et al., 2007.Two Types of Peridotite in Continental Orogenic Belts—A Case Study from the North Qaidam UHP Metamorphic Belt.Earth Science Frontiers, 14(2):129-138 (in Chinese with English abstract). http://www.researchgate.net/publication/260835246_two_types_of_peridotite_in_continental_orogenic_belts_-_a_case_study_from_the_north_qaidam_uhp_metamorphic_belt
Sun, Y.G., Zhang, G.W., Wang, J., et al., 2004.⁴⁰Ar/³⁹Ar Age of the Basic Sill Swarms of Two Period in the Junction Area of Qinling and Kunlun and Its Tectonic Significance.Acta Geologica Sinica, 78(1):65-71 (in Chinese with English abstract). https://www.researchgate.net/publication/284799480_40Ar39Ar_age_of_the_basic_sill_swarms_of_two_periods_in_the_junctions_area_of_Qinling_and_Kunlun_and_its_tectonic_significance
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
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, H.Q., Zhu, Y.H., Lin, Q.X., et al., 2010.LA-ICP-MS Zircon U-Ph Dating of the Gabbro from Longwu Gorge Ophiolite, Jianzha-Tongren Area, Qinghai, China and Its Geological Significance.Geological Bulletin of China, 29(1):86-92(in Chinese with English abstract).
Wang, M.J., Song, S.G., Niu, Y.L., et al., 2014.Post-Collisional Magmatism:Consequences of UHPM Terrane Exhumation and Orogen Collapse, N.Qaidam UHPM Belt, NW China.Lithos, 210-211:181-198.doi: 10.1016/j.lithos.2014.10.006
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
Wu, C.L., Gao, Y.H., Li, Z.L., et al., 2014.Zircon SHRIMP U-Pb Dating of Granites from Dulan and the Chronological Framework of the North Qaidam UHP Belt, NW China.Science China:Earth Sciences, 44(10):2142-2159 (in Chinese with English abstract). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxg201412009&dbname=CJFD&dbcode=CJFQ
Wu, C.L., Gao, Y.H., Wu, S.P., et al., 2007.Zircon SHRIMP U-Pb Dating of Granites from the Da Qaidam Area in the North Margin of Qaidam Basin, NW China.Acta Petrologica Sinica, 23(8):1861-1875 (in Chinese with English abstract). http://www.oalib.com/paper/1491384
Wu, C.L., Wooden, J.L., Yang, J.S., et al., 2006.Granitic Magmatism in the North Qaidam Early Paleozoic Ultrahigh-Pressure Metamorphic Belt, Northwest China.International Geology Review, 48(3):223-240.doi: 10.2747/0020-6814.48.3.223
Wu, C.L., Yang, J.S., Li, H.B., et al., 2001a.Zircon SHRIMP Ages of Aolaoshan Granite from the South Margin of Qilianshan and Its Geological Significance.Acta Petrologica Sinica, 17(2):215-221 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200102004.htm
Wu, C.L., Yang, J.S., Wooden, J.L., 2001b.Zircon SHRIMP Dating of Qaidamshan.Chinese Science Bulletin, 46(20):1743-1747 (in Chinese). https://www.researchgate.net/publication/284468788_SHRIMP_zircon_dating_from_granite_in_Qaidam_mountain
Wu, C.L., Yang, J.S., Wooden, J.L., 2004.Zircon SHRIMP Dating of Yematan Granite from the North Margin of Qaidam.Chinese Science Bulletin, 49(16):1667-1672 (in Chinese). doi: 10.1007/BF03184297
Wu, F.Y., Li, X.H., Zheng, Y.F., et al., 2007.Lu-Hf Isotopic Systematics and Their Applications in Petrology.Acta Pertrologica Sinica, 23(2):185-220(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB200702002.htm
Xiao, Q.H., Lu, X.X., Wang, F., et al., 2003.Geochronology of Rapakiwi Granite of the Yingfeng in the North Margin of the Qadam Basin and Its Geological Significance.Science China:Earth Sciences, 33(12):1193-1200.
Xin, H.T., Hao, G.J., Wang, H.C., et al., 2002.New Idea on Presinian Strata in the Northern Margin of Qaidam Massif.Progress in Precambrian Reserch, 25(2):113-119 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ200202007.htm
Xu, Z.Q., Yang, J.S., Wu, C.L., et al., 2003.Timing and Machanism of Formation and Exhumation of the Qaidam Ultra-Pressure Metamorphic Belt.Acta Geologica Sinica, 77(2):163-176 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200302006.htm
Xu, Z.Q., Yang, J.S., Wu, C.L., et al., 2006.Timing and Mechanism of Formation and Exhumation of the Northern Qaidam Ultrahigh-Pressure Metamorphic Belt.Journal of Asian Earth Sciences, 28(2-3):160-173.doi: 10.1016/j.jseaes.2005.09.016
Yang, J.S., Liu, F.L., Wu, C.L., et al., 2003.Two Ultrahigh Pressure Metamorphic Events Recognized in the CectralOrogenic Belt of China:Evidence from the U-Pb Dating of Coesite-Bearing Zircons.Acta Geologica Sinica, 77(4):463-477(in Chinese with English abstract). doi: 10.2747/0020-6814.47.4.327
Yang, J.S., Xu, Z.Q., Li, H.B., et al., 1998.Discovery of Eclogite at Northern Margin of Qaidam Basin, NW China.Chinese Science Bulletin, 43(14):1544-1549 (in Chinese). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jxtw199820016&dbname=CJFD&dbcode=CJFQ
Yang, J.S., Xu, Z.Q.Song, S.G., et al., 2000.Discovery of Eclogite in Dulan, Qinghai Province and Its Significance for Studying the HP-UHP Metamorphic Belt along the Entral Rogenic Bel t of China.Acta Geologica Sinica, 74(2):156-168 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200002006.htm
Yang, J.S., Song, S.G., Xu, Z.Q., et al., 2001.Discovery of Coesite in the North Qaidam Early Paleozoic Ultrahigh-High Pressure(UHP-HP) Metamorphic Belt, NW China.Acta Geologica Sinica, 75(2):175-179 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZXE200102004.htm
Yang, J.S., Xu, Z.Q., Zhang, J.X., et al., 2002.Early Palaeozoic North Qaidam UHP Metamorphic Belt on the North-Eastern Tibetan Plateau and a Paired Subduction Model.Terra Nova, 14(5):397-404.doi: 10.1046/j.1365-3121.2002.00438.x
Yin, A., Dang, Y.Q., Wang, L.C., et al., 2008a.Cenozoic Tectonic Evolution of Qaidam Basin and its Surrounding Regions (Part 1):The Southern Qilian Shan-Nan Shan Thrust Belt and Northern Qaidam Basin.Geological Society of America Bulletin, 120(7-8):813-846.doi: 10.1130/b26180.1
Yin, A., Dang, Y.Q., Zhang, M., et al., 2008b.Cenozoic Tectonic Evolution of the Qaidam Basin and its Surrounding Regions (Part 3):Structural Geology, Sedimentation, and Regional Tectonic Reconstruction.Geological Society of America Bulletin, 120(7-8):847-876.doi: 10.1130/b26232.1
Yu, S.Y., Zhang, J.X., Li, H.K., et al., 2013.Geochemistry, Zircon U-Pb Geochronology and Lu-Hf Isotopic Composition of Eclogites and Their Host Gneisses in the Dulan Area, North Qaidam UHP Terrane:New Evidence for Deep Continental Subduction.Gondwana Research, 23(3):901-919.doi: 10.1016/j.gr.2012.07.018
Yu, S.Y., Zhang, J.X., Mattinson, C.G., et al., 2014.Paleozoic HP Granulite-Facies Metamorphism and Anatexis in the Dulan Area of the North Qaidam UHP Terrane, Western China:Constraints from Petrology, Zircon U-Pb and Amphibole Ar-Ar Geochronology.Lithos, (198-199):58-76.doi: 10.1016/j.lithos.2014.03.016
Yu, S.Y., Zhang, J.X., Real, P.G.D., 2012.Geochemistry and Zircon U-Pb Ages of Adakitic Rocks from the Dulan Area of the North Qaidam UHP Terrane, North Tibet:Constraints on the Timing and Nature of Regional Tectonothermal Events Associated with Collisional Orogeny.Gondwana Research, 21(1):167-179.doi: 10.1016/j.gr.2011.07.024
Yu, S.Y., Zhang, J.X., Sun, D.Y., et al., 2015.Petrology, Geochemistry, Zircon U-Pb Dating and Lu-Hf Isotope of Granitic Leucosomes within Felsic Gneiss from the North Qaidam UHP Terrane:Constraints on the Timing and Nature of Partial Melting.Lithos, (218-219):1-21.doi: 10.1016/j.lithos.2015.01.008
Yuan, G.B., Wang, H.C., Li, H.M., et al., 2002.Zircon U-Pb Age of the Gabbros in Luliangshan Area on the Northern Margin of Qaidam Basin and Its Geological Implication.Progress in Precambrian Research, 25(1):36-40 (in Chinese with English abstract). https://www.researchgate.net/publication/248613875_Geological_factors_associated_with_unsuccessful_exploration_wells_in_the_northern_margin_of_the_Qaidam_basin
Yuan, H.L., Gao, S., Liu, X.M., et al., 2004.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research, 28(3):353-370.doi: 10.1111/j.1751-908x.2004.tb00755.x
Zha, X.F., Gu, P.Y., Dong, Z.C., et al., 2016.Geological Record of Tectono-Thermal Event at Early Paleozoic and Its Tectonic Setting in West Segment of the North Qaidam.Earth Science, 41 (4):586-604 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201604003.htm
Zhai, Q.G., Zhang, R.Y., Jahn, B.M., et al., 2011.Triassic Eclogites from Central Qiangtang, Northern Tibet, China:Petrology, Geochronology and Metamorphic P-T Path.Lithos, 125(1-2):173-189.doi: 10.1016/j.lithos.2011.02.004
Zhang, J.X., Mattinson, C.G., Meng, F.C., et al., 2008.Polyphase Tectonothermal History Recorded in Granulitized Gneisses from the North Qaidam HP/UHP Metamorphic Terrane, Western China:Evidence from Zircon U-Pb Geochronology.Geological Society of America Bulletin, 120(5-6):732-749.doi: 10.1130/b26093.1
Zhang, J.X., Meng, F.C., Li, J.P., et al., 2009.Coesite in Eclogite from the North Qaidam Mountains and Its Implications.Chinese Science Bulletin, 54(5):618-623 (in Chinese). http://www.oalib.com/paper/1684047
Zhang, J.X., Yang, J.S., Xu, Z.Q., et al., 2000.Peak and Retrograde Age of Eclogites at the Northern Margin of Qaidam Basin Northern China:Evidence from U-Pb and Ar-Ar Dates.Geochimica, 29(3):217-222 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX200003001.htm
Zhang, Q., Wang, Y., Pan, G.Q., et al., 2008.Sourees of Granites:Some Crucial Questions on Granite Study(4).Acta Petrologica Sinica, 24(6):1193-1204 (in Chinese with English abstract). https://www.researchgate.net/publication/285897167_Sources_of_granites_Some_crucial_questions_on_granite_study_4
Zhou, B., Zhen, Y.Y., Xu, R.K., et al., 2013.LA-ICP-MS Zircon U-Pb Dating and Hf Isotope Geochemical Characteristics of Qaidamshan Intrusive Body.Geological Bulletin of China, 32(7):1027-1034 (in Chinese with English abstract). https://www.researchgate.net/publication/288672687_LA-ICP-MS_zircon_U-Pb_dating_and_Hf_isotope_geochemical_characteristics_of_Qaidamshan_intrusive_body
Zhu, X.H., Chen, D.L., Liu, L., et al., 2013.Geochemistry, Geochronology and Hf Isotopic Compositions of the Tuanyushan Pluton from the Western Segment of the Northern Qaidam.Geological Journal of China Universities, 19(2):233-244 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX201302008.htm
陈能松, 王新宇, 张宏飞, 等, 2007.柴-欧微陆地块花岗岩地球化学和Nd-Sr-Pb同位素组成:基地性质和构造属性启示.地球科学, 32(1):7-15. http://earth-science.net/WebPage/Article.aspx?id=1657
董增产, 辜平阳, 陈锐明, 等, 2015.柴北缘西端盐场北山二长花岗岩年代学、地球化学及其Hf同位素特征.地球科学, 40(1):130-144. http://earth-science.net/WebPage/Article.aspx?id=3013
郝国杰, 陆松年, 王惠初, 等, 2004.柴达木盆地北缘前泥盆纪构造格架及欧龙布鲁克古陆块地质演化.地学前缘, 11(3):115-122. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200403016.htm
寇晓虎, 张克信, 林启祥, 等, 2007.秦祁昆接合部二叠纪沉积建造时空分布.地球科学, 32(5):681-690. http://earth-science.net/WebPage/Article.aspx?id=3528
赖绍聪, 邓晋福, 赵海玲, 1996.柴达木北缘奥陶纪火山作用与构造机制, 西安地质学院学报, 18(3):8-14. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX603.001.htm
李德发, 伦志强, 郭家玉, 等, 1991.青海省区域地质志.北京:地质出版社, 662.
李怀坤, 陆松年, 王惠初, 等, 2003.青海柴北缘新元古代超大陆裂解的地质记录——全吉群.地质调查与研究, 26(1):27-37. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200301005.htm
凌锦兰, 赵彦峰, 康珍, 等, 2014.柴达木地块北缘牛鼻子梁镁铁质-超镁铁质岩体岩石成因与成矿条件.岩石学报, 30(6):1628-1646. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201406008.htm
陆松年, 王惠初, 李怀坤, 等, 2002.柴达木盆地北缘"达肯大坂群"的再厘定.地质通报, (21):19-23. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200201003.htm
陆松年, 陈志宏, 李怀坤, 2004.秦岭造山带中-新元古代(早期)地质演化.地质通报, (2):107-112. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200402001.htm
卢欣祥, 孙延贵, 张雪亭, 等, 2007.柴达木盆地北缘塔塔楞环斑花岗岩的SHRIMP年龄.地质学报, 81(5):626-634. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200705005.htm
孟繁聪, 张建新, 杨经绥, 2005.柴北缘锡铁山早古生代HP/UHP变质作用后的构造热事件-花岗岩和片麻岩的同位素与岩石地球化学证据.岩石学报, 21(1):45-56. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200501005.htm
邱家骧, 杨巍然, 夏卫华, 1998.南祁连早古生代海相火山岩及铜、多金属矿床成矿条件及找矿方向.祁连山及邻区火山作用与成矿.北京:地质出版社, 111-163.
史仁灯, 杨经绥, 吴才来, 2003.柴北缘早古生代岛弧火山岩中埃达克质英安岩的发现及其地质意义.岩石矿物学杂志, 22(3):229-236. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200303004.htm
史仁灯, 杨经绥, 吴才来, 等, 2004.柴达木北缘超高压变质带中的岛弧火山岩.地质学报, 78(1):52-64. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200401007.htm
宋述光, 杨经绥, 2001.柴达木盆地北缘都兰地区榴辉岩中透长石+石英包裹体:超高压变质作用的证据.地质学报, 75(2):180-185. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200102005.htm
宋述光, 张立飞, 牛耀龄, 等, 2007.大陆碰撞造山带的两类橄榄岩——以柴北缘超高压变质带为例.地学前缘, 14(2):129-138. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200702009.htm
宋述光, 牛耀龄, 张立飞, 等, 2009.大陆造山运动:从大洋俯冲到大陆俯冲、碰撞、折返的时限——以北祁连山、柴北缘为例.岩石学报, 25(9):2067-2077. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200909003.htm
宋述光, 王梦珏, 王潮, 等, 2015b.大陆造山带碰撞-俯冲-折返-垮塌过程的岩浆作用及大陆地壳净生长.中国科学:地球科学, 45(7):916-940. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201507003.htm
孙延贵, 张国伟, 王瑾, 等, 2004.秦-昆结合区两期基性岩墙群⁴⁰Ar/³⁹Ar定年及其构造意义.地质学报, 78(1):65-71. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200401008.htm
吴才来, 郜源红, 李兆丽, 等, 2014.都兰花岗岩锆石SHRIMP定年及柴北缘超高压带花岗岩年代学格架.中国科学:地球科学, 44(10):2142-2159. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201410004.htm
吴才来, 郜源红, 吴锁平, 等, 2007.柴北缘大柴旦地区古生代花岗岩锆石SHRIMP定年.岩石学报, 23(8):1861-1875. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200708007.htm
吴才来, 郜源红, 吴锁平, 等, 2008.柴北缘西段花岗岩锆石SHRIMP U-Pb定年及其岩石地球化学特征.中国科学:地球科学, 38(8):930-949. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200808002.htm
吴才来, 杨经绥, 李海兵, 等, 2001a.祁连南缘嗷唠山花岗岩SHRIMP锆石年龄及其地质意义.岩石学报, 17(2):215-221. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200102004.htm
吴才来, 杨经绥, Wooden, J.L., 等, 2001b.柴达木山花岗岩锆石SHRIMP定年.科学通报, 46(20):1743-1747. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200120017.htm
吴才来, 杨经绥, Wooden, J.L., 等, 2004.柴达木北缘都兰野马滩花岗岩锆石SHRIMP定年.科学通报, 49(16):1667-1672. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200416013.htm
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
王绘清, 朱云海, 林启祥, 等, 2010.青海尖扎-同仁地区隆务峡蛇绿岩的形成时代及意义——来自辉长岩锆石LA-ICP-MS U-Pb年龄的证据.地质通报, 29(1):86-92. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201001011.htm
肖庆辉, 卢欣祥, 王菲, 等, 2003.柴达木北缘鹰峰环斑花岗岩的时代及地质意义.中国科学:地球科学, 33(12):1193-1200. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200312007.htm
辛后田, 郝国杰, 王惠初, 等, 2002.柴北缘前震旦纪地层系统的新认识.前寒武纪研究进展, 25(2):113-119. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200202007.htm
许志琴, 杨经绥, 吴才来, 等, 2003.柴达木北缘超高压变质带形成与折返的时限及机制.地质学报, 77(2):163-176. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200302006.htm
杨经绥, 刘福来, 吴才来, 等, 2003.中央碰撞造山带中两期超高压变质作用——来自含柯石英锆石的定年证据.地质学报, 77(4):463-477. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200304002.htm
杨经绥, 宋述光, 许志琴, 等, 2001.柴北缘早古生代高压-超高压变质带中发现典型的超高压矿物——柯石英.地质学报, 75(2):175-179. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200102004.htm
杨经绥, 许志琴, 李海兵, 等, 1998.我国西部柴达木北缘地区发现榴辉岩.科学通报, 43(14), 1544-1549. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199814022.htm
杨经绥, 许志琴, 宋述光, 等, 2000.青海都兰榴辉岩的发现及对中国中央造山带内高压-超高压变质带研究的意义.地质学报, 74(2):156-168. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200002006.htm
袁桂邦, 王惠初, 李惠民, 等, 2002.柴北缘绿梁山地区辉长岩的锆石U-Pb年龄及意义.前寒武纪研究进展, 25(1):36-40. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200201004.htm
査显锋, 牟平阳, 董增产, 等, 2016.柴北缘西段早古生代构造-热事件及其构造环境.地球科学, 41(4):586-604. http://earth-science.net/WebPage/Article.aspx?id=3276
张建新, 杨经绥, 许志琴, 等, 2000.柴北缘榴辉岩的峰期和退变质年龄:来自U-Pb及Ar-Ar同位素测定的证据.地球化学, 29(3):217-222. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200003001.htm
张建新, 孟繁聪, 李金平, 等, 2009.柴达木北缘榴辉岩中的柯石英及其意义.科学通报, 54(5):618-623. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200905013.htm
张旗, 王焰, 潘国强, 等, 2008.花岗岩源岩问题——关于花岗岩研究的思考之四.岩石学报, 24(6):1193-1204. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200806004.htm
周宾, 郑有业, 许荣科, 等, 2013.青海柴达木山岩体LA-ICP-MS锆石U-Pb定年及Hf同位素特征.地质通报, 32(7):1027-1034. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201307007.htm
朱小辉, 陈丹玲, 刘良, 等, 2013.柴北缘西段团鱼山岩体的地球化学、年代学及Hf同位素示踪.高校地质学报, 19(2):233-244. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201302008.htm