西藏聂荣微陆块奥陶纪和侏罗纪岩浆事件的年龄证据

陆露; 钱程; 赵珍; 吴珍汉; 刘玉双; 周亮; 王岩

doi:10.3799/dqkx.2018.712

西藏聂荣微陆块奥陶纪和侏罗纪岩浆事件的年龄证据

doi: 10.3799/dqkx.2018.712

陆露^1,2,,
钱程³,
赵珍⁴,
吴珍汉⁴,
刘玉双^1,2,
周亮⁵,
王岩¹

1.
沈阳师范大学古生物学院, 辽宁沈阳 110034
2.
国土资源部东北亚古生物演化重点实验室, 辽宁沈阳 110034
3.
沈阳地质矿产研究所, 辽宁沈阳 110000
4.
中国地质科学院, 北京 100081
5.
山东科技大学地球科学与工程学院, 山东青岛 266590

基金项目:

沈阳师范大学博士、引进人才科研项目启动基金项目 BS201705

中国地质调查局项目 DD20160161

国家自然科学基金面上项目 31672332

详细信息

作者简介:
陆露(1985-), 女, 讲师, 博士, 主要从事青藏高原区域地质调查、大陆动力学研究及相关教学工作

中图分类号: P56
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出版历程
- 收稿日期: 2017-12-20
- 刊出日期: 2018-04-15

Geochronological Evidence of Ordovician and Jurassic Magmatic Events in Nyainrong Microcontinent, Tibet

Lu Lu^{1,2
,},
Qian Cheng³,
Zhao Zhen⁴,
Wu Zhenhan⁴,
Liu Yushuang^1,2,
Zhou Liang⁵,
Wang Yan¹

1.
Paleontological College, Shenyang Normal University, Shenyang 110034, China
2.
Key Laboratory of Evolution of Past Life in Northeast Asia, Ministry of Land and Resources, Shenyang 110034, China
3.
Shenyang Institute of Geology and Mineral Resources, Shenyang 110000, China
4.
Chinese Academy of Geological Sciences, Beijing 100081, China
5.
College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China

摘要

摘要: 为了加深对班公湖-怒江缝合带构造演化过程的认识，选择聂荣微陆块内的花岗质片麻岩和花岗闪长质片麻岩中的锆石进行LA-ICP-MS U-Pb定年，结果主要显示两组²⁰⁶Pb/²³⁸U的加权平均年龄：一组为453.7±2.5 Ma; 另一组为176.6±1.1 Ma和178.04±0.8 Ma.花岗质片麻岩中黑云母和花岗闪长质片麻岩中白云母的⁴⁰Ar-³⁹Ar定年结果显示，坪年龄分别为161.8±1.1 Ma和178.9±1.2 Ma.上述年龄结果表明，聂荣微陆块主要经历了晚奥陶世和早侏罗世两期岩浆事件，这两期岩浆事件分别与冈瓦纳大陆北缘早古生代的造山作用和班公湖-怒江洋壳的俯冲闭合存在密切的动力学关系.
- 青藏高原 /
- 聂荣微陆块 /
- 锆石U-Pb年龄 /
- ⁴⁰Ar-³⁹Ar年龄 /
- 班公湖-怒江缝合带 /
- 地质年代学
Abstract: In order to deepen our knowledge and understanding about the tectonic evolution of the Bangonghu-Nujiang suture zone(BNS), zircon U-Pb dating was conducted for granitic gneiss and granodioritic gneiss of Nyainrong microcontinent by LA-ICP-MS in this study. Results show two groups of average zircon U-Pb ages, with one of 453.7±2.5 Ma, and the other of 176.6±1.1 Ma and 178.04±0.8 Ma. ⁴⁰Ar-³⁹Ar dating was conducted for biotite from granitic gneiss and muscovite from granodioritic gneiss in Nyainrong microcontinent.The ⁴⁰Ar-³⁹Ar plateau ages yield 161.8±1.1 Ma and 178.9±1.2 Ma, respectively, showing that the study area experienced the Late Ordovician and the Early Jurassic magmatic events. Combined with field condition and study results, it is suggested that the Ordovician magmatic event was related to the Early Paleozoic orogeny which could be caused by proto-Tethyan oceanic subduction along Gondwana continental margin, and the Jurassic magmatic event was related to the subduction and closure of the Bangong-Nujiang oceanic crust.
- Tibetan plateau /
- Nyainrong microcontinent /
- zircon U-Pb age /
- ⁴⁰Ar-³⁹Ar age /
- Bangonghu-Nujiang suture zone /
- geochronology

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图 1 青藏高原地质简图

MBT.主边界断裂; YZS.雅鲁藏布江缝合带; BNS.班公湖-怒江缝合带; HJS.可可西里-金沙江缝合带; SKS.昆南缝合带; KJF.喀喇昆仑-嘉黎断裂; JSF.金沙江断裂; XSF.鲜水河断裂; EKF.东昆仑断裂.据吴珍汉等(2009)修改

Fig. 1. Geological sketch map of the Tibetan Plateau

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图 2 聂荣微陆块地质简图

据1:25万安多幅(中国地质大学(北京)地质调查研究院, 2005, 1:25万安多幅地质报告)和1:25万那曲幅(西藏自治区地质调查院, 2005, 1:25万那曲幅地质报告)修编

Fig. 2. The geological map of Nyainrong microcontinent

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图 3 研究区片麻岩样品野外特征及镜下特征

a.样品B06野外特征; b.样品B06镜下特征; c.样品B65野外特征; d.样品B65镜下特征.Q.石英; Pl.斜长石; Bi.黑云母; Ms.白云母

Fig. 3. Field and microscopic characteristics of gneisses in study area

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图 4 样品B06锆石阴极发光图像

Fig. 4. CL images of zircons from sample B06

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图 5 样品B06锆石U-Pb年龄谐和图

Fig. 5. The zircon U-Pb concordia diagrams of sample B06

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图 6 样品B65锆石阴极发光图像

Fig. 6. CL images of zircons from sample B65

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图 7 样品B65锆石U-Pb年龄谐和图

Fig. 7. The zircon U-Pb concordia diagrams of sample B65

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图 8 聂荣微陆块花岗质片麻岩(B06)黑云母(a~c)和花岗闪长质片麻岩(B65)白云母(d~f)⁴⁰Ar/³⁹Ar坪年龄和等时线年龄

Fig. 8. The ⁴⁰Ar/³⁹Ar age plateaus and isochrones for biotite from granitic gneiss (a-c) and muscovite from granodioritic gneiss (d-f) of Nyainrong microcontinent

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表 1 聂荣微陆块片麻岩LA-ICP-MS锆石U-Pb同位素测年结果

Table 1. LA-ICP-MS data of zircons from gneisses in Nyainrong microcontinent

点号	Th/U	同位素比值						年龄(Ma)
点号	Th/U	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²³⁵U	1σ
花岗质片麻岩(样品B06)
1	0.106 1	0.027 0	0.000 2	0.185 0	0.002 1	0.049 8	0.000 5	171.8	1.2	172.4	1.8
2	2.136 5	0.072 9	0.000 4	0.597 9	0.005 0	0.059 5	0.000 4	453.4	2.6	475.9	3.2
3	5.476 5	0.014 2	0.000 1	0.434 8	0.003 4	0.222 9	0.001 2	90.6	0.6	366.6	2.4
4	1.373 9	0.064 2	0.000 3	0.502 5	0.003 6	0.056 8	0.000 3	400.9	2.0	413.4	2.5
5	0.228 7	0.028 1	0.000 1	0.197 5	0.001 2	0.051 1	0.000 2	178.4	0.8	183.0	1.1
6	1.353 6	0.073 0	0.000 7	0.584 4	0.005 9	0.058 1	0.000 3	454.0	4.2	467.3	3.8
7	0.635 9	0.028 3	0.000 1	0.204 8	0.003 4	0.0525	0.000 9	180.0	0.9	189.2	2.9
8	1.092 7	0.072 6	0.000 4	0.569 2	0.003 6	0.056 9	0.000 2	451.5	2.4	457.5	2.3
9	2.226 1	0.022 4	0.000	0.190 4	0.009 6	0.061 5	0.002 9	143.0	1.6	177.0	8.2
10	0.456 7	0.073 4	0.000 6	0.577 0	0.007 7	0.057 0	0.000 6	456.7	3.5	462.5	5.0
11	1.407 4	0.073 6	0.000 7	0.585 5	0.006 0	0.057 8	0.000 3	457.7	4.2	468.0	3.8
12	0.143 4	0.027 7	0.000 2	0.191 7	0.001 8	0.050 3	0.000 4	176.0	0.9	178.1	1.6
13	6.093 1	0.043 9	0.000 2	0.433 8	0.002 7	0.071 7	0.000 3	276.8	1.2	365.9	1.9
14	0.150 4	0.038 2	0.000 3	0.281 8	0.004 3	0.053 5	0.000 6	241.5	1.8	252.1	3.4
15	0.168 7	0.028 2	0.000 1	0.196 1	0.001 2	0.050 4	0.000 2	179.5	0.8	181.9	1.0
16	0.160 4	0.027 8	0.000 1	0.190 6	0.001 1	0.049 8	0.000 1	176.7	0.9	177.1	0.9
17	0.717 5	0.028 3	0.001 0	0.204 6	0.006 8	0.052 5	0.000 4	179.8	6.6	189.0	5.7
18	0.165 9	0.027 7	0.000 1	0.189 1	0.001 1	0.049 6	0.000 2	175.9	0.7	175.8	0.9
19	0.650 2	0.028 1	0.000 3	0.196 9	0.002 2	0.050 9	0.000 6	178.5	2.1	182.5	1.9
20	1.678 9	0.027 9	0.000 6	0.201 7	0.004 4	0.052 4	0.001 2	177.6	3.7	186.6	3.7
21	0.164 2	0.027 5	0.000 2	0.189 9	0.001 5	0.050 0	0.000 3	175.2	1.0	176.5	1.2
22	1.394 4	0.072 8	0.000 6	0.595 5	0.004 6	0.059 5	0.000 3	453.1	3.6	474.3	2.9
23	5.921 5	0.047 9	0.000 5	0.478 9	0.007 5	0.072 6	0.000 8	301.8	3.3	397.3	5.1
花岗闪长质片麻岩(样品B65)
1	0.290 3	0.066 5	0.000 7	6.080 7	0.057 1	0.663 7	0.002 5	415.0	4.2	1 987.5	8.2
2	1.984 8	0.075 9	0.001 6	6.345 5	0.189 1	0.599 3	0.006 1	471.4	9.8	2 024.8	26.1
3	5.887 7	0.028 2	0.000 5	1.803 3	0.026 0	0.466 4	0.003 4	179.2	3.3	1 046.7	9.4
4	3.381 7	0.028 0	0.000 2	0.198 8	0.002 7	0.051 5	0.000 6	178.2	1.2	184.1	2.3
5	3.136 8	0.029 8	0.000 2	1.361 2	0.012 2	0.331 1	0.002 4	189.4	1.0	872.4	5.3
6	0.433 3	0.028 2	0.000 2	0.202 2	0.002 2	0.052 0	0.000 5	179.5	1.1	187.0	1.9
7	0.701 5	0.081 7	0.000 4	0.656 0	0.004 1	0.058 2	0.000 2	506.2	2.5	512.2	2.5
8	2.606 6	0.059 5	0.000 8	4.638 2	0.062 8	0.565 1	0.001 7	372.7	4.9	1 756.2	11.3
9	0.435 2	0.027 7	0.000 2	0.198 1	0.003 9	0.051 7	0.000 9	176.4	1.1	183.5	3.3
10	2.440 3	0.028 0	0.000 2	1.977 5	0.013 4	0.511 6	0.002 3	178.3	1.2	1 107.9	4.6
11	1.898 1	0.028 1	0.000 1	0.195 6	0.002 2	0.050 5	0.000 5	178.5	0.9	181.4	1.8
12	3.116 1	0.028 2	0.000 3	0.670 7	0.010 1	0.173 3	0.003 0	179.0	1.6	521.2	6.2
13	2.409 7	0.031 6	0.000 5	1.141 4	0.022 6	0.261 4	0.002 3	200.9	3.3	773.2	10.7
14	1.628 7	0.057 7	0.001 8	5.065 0	0.160 7	0.636 9	0.002 4	361.4	11.0	1 830.3	26.9
15	0.508 0	0.027 9	0.000 1	0.201 5	0.001 0	0.052 3	0.000 1	177.6	0.8	186.4	0.8
16	0.038 6	0.027 8	0.000 3	0.190 7	0.002 2	0.049 7	0.000 3	176.9	1.7	177.2	1.9
17	5.200 0	0.032 2	0.000 7	2.626 7	0.038 4	0.595 4	0.005 4	204.2	4.2	1 308.1	10.7
18	2.416 2	0.028 1	0.000 2	0.192 4	0.001 8	0.049 7	0.000 3	178.5	1.2	178.7	1.5
19	1.052 8	0.108 8	0.001 6	5.329 5	0.256 1	0.333 7	0.012 4	665.7	9.5	1 873.6	41.1
20	5.160 5	0.101 0	0.001 5	9.157 6	0.178 8	0.652 4	0.003 7	620.4	9.1	2 353.9	17.9
21	0.428 9	0.025 2	0.001 1	0.933 2	0.055 8	0.480 7	0.214 2	160.7	6.7	669.3	29.3
22	3.723 9	0.040 9	0.009 5	2.533 3	0.110 0	0.594 3	0.014 6	258.2	58.8	1 281.6	31.6

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表 2 聂荣微陆块花岗质片麻岩黑云母和花岗闪长质片麻岩白云母常规⁴⁰Ar/³⁹Ar测年结果

Table 2. Conventionally ⁴⁰Ar/³⁹Ar isotopic age analyses of biotite and muscovite

T(℃)	(⁴⁰Ar/³⁹Ar)_m	(³⁶Ar/³⁹Ar)_m	(³⁷Ar/³⁹Ar)_m	(³⁸Ar/³⁹Ar)_m	⁴⁰Ar(%)	F	³⁹Ar(10^-14 mol)	³⁹Ar(Cum.)(%)	Age(Ma)	±1(Ma)
样品B06(花岗质片麻岩)黑云母W=28.03 mg J=0.004 267
700	56.020 7	0.151 9	8.741 9	0.043 7	20.96	11.8233	0.19	0.49	88.8	2.8
750	26.404 5	0.016 4	0.269 1	0.016 0	81.69	21.574 1	3.33	9.06	158.9	1.5
790	23.095 3	0.002 7	0.154 6	0.013 3	96.55	22.300 6	6.08	24.73	164.0	1.6
830	22.700 9	0.001 3	0.276 4	0.013 0	98.32	22.323 5	6.21	40.73	164.1	1.6
870	22.721 8	0.001 6	0.181 9	0.013 1	97.95	22.259 1	2.84	48.04	163.7	1.6
910	22.990 2	0.003 9	0.858 4	0.013 4	95.21	21.903 0	1.64	52.27	161.2	1.6
950	22.954 2	0.004 7	0.658 3	0.013 4	94.15	21.622 3	1.47	56.05	159.2	1.6
1 000	22.579 1	0.002 9	0.373 0	0.013 6	96.28	21.746 7	3.13	64.13	160.1	1.5
1 050	22.627 6	0.001 5	0.237 2	0.013 1	98.04	22.188 1	5.89	79.31	163.2	1.6
1 080	26.087 2	0.014 8	0.254 4	0.015 2	83.24	21.718 6	3.37	87.99	159.9	1.5
1 120	23.158 5	0.003 1	0.181 3	0.013 2	96.13	22.265 0	3.91	98.07	163.7	1.6
1 400	126.013 0	0.410 7	1.920 1	0.084 4	3.79	4.789 6	0.75	100.00	36.5	1.1
样品B665(花岗闪长质片麻岩)白云母W=27.40 mg J=0.004 301
700	20.958 2	0.015 6	6.004 6	0.015 3	80.03	16.853 6	0.22	0.56	126.2	2.9
750	22.734 0	0.004 2	1.643 3	0.013 2	95.02	21.630 0	0.71	2.39	160.5	1.7
800	23.079 3	0.002 2	1.306 9	0.012 8	97.62	22.554 9	1.43	6.07	167.0	1.6
850	23.584 9	0.001 6	0.723 0	0.012 7	98.24	23.183 9	2.40	12.27	171.5	1.7
890	24.330 9	0.001 6	0.235 4	0.012 8	98.05	23.861 3	4.47	23.79	176.2	1.7
930	24.430 3	0.000 7	0.082 3	0.012 6	99.17	24.229 6	4.82	36.21	178.8	1.7
970	24.757 4	0.001 1	0.345 5	0.012 6	98.81	24.470 2	4.77	48.52	180.5	1.7
1 010	24.624 2	0.001 1	0.156 1	0.012 6	98.69	24.304 2	2.68	55.42	179.4	1.7
1 050	24.713 4	0.001 4	0.376 0	0.012 8	98.43	24.332 2	4.11	66.03	179.6	1.7
1 090	24.616 5	0.001 2	0.253 1	0.012 7	98.60	24.276 7	6.55	82.92	179.2	1.7
1 130	24.592 5	0.000 8	0.234 4	0.012 5	99.11	24.379 0	6.16	98.81	179.9	1.7
1 180	26.853 2	0.010 5	3.263 8	0.012 7	89.30	24.044 0	0.39	99.81	177.5	2.0
1 400	75.442 2	0.210 9	24.901 3	0.050 8	19.74	15.195 3	0.07	100.00	114.2	7.0
注：W.实验参数; J.照射参数.

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参考文献(96)

Cawood, P.A., Buchan, C., 2007.Linking Accretionary Orogenesis with Supercontinent Assembly.Earth-Science Reviews, 82(3-4):217-256. https://doi.org/10.1016/j.earscirev.2007.03.003
Chang, C.F., Zheng, X.L., 1973.The Geological Structure Characteristics of Everest in Southern of Tibet and the Formation of the East-West Striking Mountains in Tibet Plateau, China.Science in China, (2):190-201 (in Chinese).
Chen, G.R., Liu, H.F., Jiang, G.W., et al., 2004.Discovery of the Shamuluo Formation in the Central Segment of the Bangong Co-Nujiang River Suture Zone, Tibet.Geological Bulletin of China, 23(2):193-194 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD200402015.htm
Chen, W., Zhang, Y., Zhang, Y.Q., et al., 2006.Late Cenozoic Episodic Uplifting in Southeastern Part of the Tibetan Plateau—Evidence from Ar-Ar Thermochronology.Acta Petrologica Sinica, 22(4):867-872 (in Chinese with English abstract). http://adsabs.harvard.edu/abs/2009gecas..73r1512z
Chen, Y., Zhu, D.C., Zhao, Z.D., et al., 2014.Slab Break off Triggered ca.113 Ma Magmatism around Xainza Area of the Lhasa Terrane, Tibet.Gondwana Research, 26(2):449-463. https://doi.org/10.1016/j.gr.2013.06.005
Ding, S., Tang, J.X., Zheng, W.B., et al., 2017.Geochronology and Geochemistry of Naruo Porphyry Cu(Au) Deposit in Duolong Ore-Concentrated Area, Tibet, and Their Geological Significance.Earth Science, 42(1):1-23 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DQKX201701001.htm
Dong, M.L., Dong, G.C., Mo, X.X., et al., 2012.Geochronology and Geochemistry of the Early Palaeozoic Granitoids in Baoshan Block, Western Yunnan and Their Implications.Acta Petrologica Sinica, 28 (5):1453-1464 (in Chinese with English abstract). http://www.oalib.com/paper/1475754
Du, D.D., Qu, X.M., Wang, G.H., et al., 2011.Bidirectional Subduction of the Middle Tethys Oceanic Basin in the West Segment of Bangonghu-Nujiang Suture, Tibet:Evidence from Zircon U-Pb LA-ICP-MS Dating and Petrogeochemistry of Arc Granites.Acta Petrologica Sinica, 27(7):1993-2002 (in Chinese with English abstract).
Gu, P.Y., Li, R.S., He, S.P., et al., 2012.The Amphibolite from Nyainrong Rock Group in Northern Nagqu:Geological Records of Break-up of the Supercontinent Rodinia.Acta Petrologica et Mineralogica, 31(2):145-154 (in Chinese with English abstract). doi: 10.1080/00206814.2015.1065207
Guynn, J.H., Kapp, P., Gehrels, G.E., et al., 2012.U-Pb Geochronology of Basement Rocks in Central Tibet and Paleogeographic Implications.Journal of Asian Earth Sciences, 43(1):23-50. https://doi.org/10.1016/j.jseaes.2011.09.003
Guynn, J.H., Kapp, P., Pullen, A., et al., 2006.Tibetan Basement Rocks near Amdo Reveal "Missing" Mesozoic Tectonism along the Bangong Suture, Central Tibet.Geology, 34(6):505-508. doi: 10.1130/G22453.1
Hu, J., Wan, Y.W., Tao, Z., et al., 2014.New Geochemistry and Geochronology Evidences Related to Southward Subduction of Tethys Ocean Basin in West Segment of Bangonghu-Nujiang Suture Belt.Journal of Chengdu University of Technology (Science & Technology Edition), 41(4):505-515 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-CDLG201404014.htm
Hu, P.Y., Li, C., Su, L., et al., 2010.Zircon U-Pb Dating of Granitic Gneiss in Wugong Mountain Area, Central Qiangtang, Qinghai-Tibet Plateau:Age Records of Pan-African Movement and Indo-China Movement.Geology in China, 37(4):1050-1061 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dizi201004021.htm
Huang J.J., 2001.Tectonic Characteristics and Evolution of the Qiangtang Basin.Regional Geology of China, 20(2):178-186 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD200102010.htm
Jager, E., 1979. Introduction to Geochronology. In: Jager, E., Hunziker, J. C., eds., Lectures in Isotope Geology. Springer-Verlag, Berlin, 1-12.
Kapp, P., Murphy, M.A., Yin, A., et al., 2003.Mesozoic and Cenozoic Tectonic Evolution of the Shiquanhe Area of Western Tibet.Tectonics, 22(4):1-24. https://doi.org/10.1029/2001tc001332
Knenedy, W. Q., 1964. The Structural Differentiation of Africa in the Pan-African (500 m. y. ) Tectonic Episode. Research Institute African Geology University Leeds 8th Ann, Report, 48. http://www.researchgate.net/publication/285376314_The_structural_differentiation_of_Africa_in_the_Pan-African_500_my_tectonic_episode
Li, Z.H., Lin, S.L., Cong, F., et al., 2012.U-Pb Ages of Zircon from Metamorphic Rocks of the Gaoligongshan Group in Western Yunnan and Its Tectonic Significance.Acta Petrologica Sinica, 28(5):1529-1541 (in Chinese with English abstract). http://www.oalib.com/paper/1476386
Liu, D.L., Huang, Q.S., Fan, S.Q., et al., 2014.Subduction of the Bangong-Nujiang Ocean:Constraints from Granites in the Bangong Co Area, Tibet.Geological Journal, 49(2):188-206. https://doi.org/10.1002/gj.2510
Liu, D.L., Shi, R.D., Ding, L., et al., 2017.Zircon U-Pb Age and Hf Isotopic Compositions of Mesozoic Granitoids in Southern Qiangtang, Tibet:Implications for the Subduction of the Bangong-Nujiang Tethyan Ocean.Gondwana Research, 41:157-172. https://doi.org/org/10.1016/j.gr.2015.04.007
Liu, M., Zhao Z.D., Guan, Q., et al., 2011.Tracing Magma Mixing Genesis of the Middle Early-Jurassic Host Granites and Enclaves in Nyainrong Microcontinent, Tibet from Zircon LA-ICP-MS U-Pb Dating and Hf Isotopes.Acta Petrologica Sinica, 27(7):1931-1937 (in Chinese with English abstract). http://npd.nsfc.gov.cn/OutComeSearch!searchById.action?id=1061034&typeId=010
Liu, M., Zhu, D.C., Zhao Z.D., et al., 2010.Magma Mixing of Late Early Jurassic Age from Nyainrong, Northern Tibet and Its Tectonic Significance.Acta Petrologica Sinica, 26(10):3117-3130 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201010023.htm
Lu, L., Wu, Z.H., Zhao, Z., et al., 2014.Zircon SHRIMP U-Pb Dating, Geochemical Characteristics and Tectonic Significance of Granitic Gneisses in Amdo, Tibet.Journal of Earth Science, 25(3):473-485. https://doi.org/10.1007/s12583-014-0448-0
Ludwig, K. R., 2001. Squid 1. 02: A User Manual. Berkeley Geochronological Center Special Publication, Berkeley, 2: 19.
Mi, W.T., Zhu, L.D., Yang, W.G., et al., 2017.Provenance of the Niubao Formation and Its Geological Implications in the North Depression of the Nima Basin in the Tibet.Earth Science, 42(2):240-257 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DQKX201702006.htm
Mo, X.X., Dong, G.C., Zhao, Z.D., et al., 2005.Spatial and Temporal Distribution and Characteristics of Granitoids in the Gangdese, Tibet and Implication for Crustal Growth and Evolution.Geological Journal of China Universities, 11(3):281-290 (in Chinese with English abstract). http://npd.nsfc.gov.cn/projectDetail.action?pid=40821061
Pan, G.T., Mo, X.X., Hou, Z.Q., et al., 2006.Spatial-Temporal Framework of the Gangdese Orogenic Belt and Its Evolution.Acta Petrologica Sinica, 22(3):521-533 (in Chinese with English abstract). http://www.oalib.com/paper/1472080
Pan, G.T., Wang, L.Q., Zhu, D.C., 2004.Thoughts on Some Important Scientific Problems in Regional Geological Survey of the Qinghai-Tibet Plateau.Geological Bulletin of China, 23(1):12-19 (in Chinese with English abstract). http://www.nsfc.gov.cn/publish/portal1/tab284/info24555.htm
Qu, X.M., Wang, R.J., Xin, H.B., et al., 2009.Geochronology and Geochemistry of Igneous Rocks Related to the Subduction of the Tethys Oceanic Plate along the Bangong Lake Arc Zone, the Western Tibetan Plateau.Geochimica, 38(6):523-535 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQHX200906005.htm
Qu, X.M., Wang, R.J., Xin, H.B., et al., 2012.Age and Petrogenesis of A-Type Granites in the Middle Segment of the Bangonghu-Nujiang Suture, Tibetan Plateau.Lithos, 146-147:264-275. https://doi.org/10.1016/j.lithos.2012.05.006
Shi, R.D., William, L.G., Suzanne, Y.O., et al., 2012.Melt/Mantle Mixing Produces Podiform Chromite Deposits in Ophiolites:Implications of Re-Os Systematics in the Dongqiao Neo-Tethyan Ophiolite, Northern Tibet.Gondwana Research, 21:194-206. https://doi.org/10.1016/j.gr.2011.05.011
Shi, R.D., Yang, J.S., Xu, Z.Q., et al., 2008.The Bangong Lake Ophiolite (NW Tibet) and Its Bearing on the Tectonic Evolution of the Bangong-Nujiang Suture Zone.Journal of Asian Earth Sciences, 32(5-6):438-457. https://doi.org/10.1016/j.jseaes.2007.11.011
Sui, Q.L., Wang, Q., Zhu, D.C., et al., 2013.Compositional Diversity of ca.110 Ma Magmatism in the Northern Lhasa Terrane, Tibet:Implications for the Magmatic Origin and Crustal Growth in a Continent-Continent Collision Zone.Lithos, 168-169:144-159. https://doi.org/10.1016/j.lithos.2013.01.012
Wang, M., Li, C., Xie, C.M., et al., 2012.LA-ICP-MS U-Pb Dating of Zircon from Granitic Gneiss of the Nierong Microcontinent:The Discovery of the Neoproterozoic Basement Rock and Its Significance.Acta Petrologica Sinica, 28(12):4101-4108 (in Chinese with English abstract). http://www.oalib.com/paper/1474698
Wang, W.L., Aitchison, J.C., Lo, C.H., et al., 2008.Geochemistry and Geochronology of the Amphibolite Blocks in Ophiolitic Mélanges along Bangong-Nujiang Suture, Central Tibet.Journal of Asian Earth Sciences, 33(1-2):122-138. https://doi.org/10.1016/j.jseaes.2007.10.022
Wang, X.X., Zhang, J.J., Yang, X.Y., et al., 2011.Zircon SHRIMP U-Pb Ages, Hf Isotopic Features and Their Geological Significance of the Greater Himalayan Crystalline Complex Augen Gneiss in Gyirong Area, South Tibet.Earth Science Frontiers, 18(2):127-139 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY201102014.htm
Wei, S.G., Tang, J.X., Song, Y., et al., 2017.Early Cretaceous Bimodal Volcanism in the Duolong Cu Mining District, Western Tibet:Record of Slab Break off That Triggered ca.108-113 Ma Magmatism in the Western Qiangtang Terrane.Journal of Asian Earth Sciences, 138:588-607. https://doi.org/10.1016/j.jseaes.2016.12.010
Wu, Z.H., Wu, Z.H., Hu, D.G., et al., 2009.Uplift and Tectonic Evolution of the Cenozoic in the Tibetan Plateau.Geological Publishing House, Beijing (in Chinese).
Xia, B., Xu, L.F., Wei, Z.Q., et al., 2008.SHRIMP Zircon Dating of Gabbro from the Donqiao Ophiolite in Tibet and Its Geological Implications.Acta Geologica Sinica, 82(4):528-531 (in Chinese with English abstract). http://www.researchgate.net/publication/279556448_SHRIMP_zircon_dating_of_gabbro_from_the_Donqiao_ophiolite_in_Tibet_and_its_geological_implications
Xiao, X.C., Li, T.D., 2000.The Tectonic Evolution and Uplift of the Tibet Plateau.Guangdong Science and Technology Press, Guangzhou, 239-268 (in Chinese).
Xie, C. M., 2013. Tectonic Evolution of the Nyainrong Microcontinent, Tibet—Constraints from Geochronology and Geochemistry (Dissertation). Jilin University, Changchun (in Chinese with English abstract).
Xie, C.M., Li, C., Su, L., et al., 2010.LA-ICP-MS U-Pb Dating of Zircon from Granite-Gneiss in the Amdo Area, Northern Tibet, China.Geological Bulletin of China, 29(12):1737-1744 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD201012003.htm
Xie, C.M., Li, C., Wu, Y.W., et al., 2014.⁴⁰Ar/³⁹Ar Thermochronology Constraints on Jurassic Tectonothermal Event of Nyainrong Microcontinent.Journal of Earth Science, 25(1):98-108. https://doi.org/10.1007/s12583-014-0403-0
Xu, R.H., Schärer, U., Allègre, C.J., 1985.Magmatism and Metamorphism in the Lhasa Block (Tibet):A Geochronological Study.The Journal of Geology, 93(1):41-57. https://doi.org/10.1086/628918
Xu, Z.Q., Yang, J.S, Liang, F.H., et al., 2005.Pan-African and Early Paleozoic Orogenic Events in the Himalaya Terrane:Inference from SHRIMP U-Pb Zircon Ages.Acta Petrologica Sinica, 21(1):1-12 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200501001.htm
Yang, H., Liu, F.L., Liu, P.H., et al., 2013.⁴⁰Ar-³⁹Ar Dating for Muscovite in Garnet Muscovite-Felsic Schists of the Dahongshan Group in Southwestern Yangtze Block and Its Geological Significance.Acta Petrologica Sinica, 29(6):2161-2170 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201306022.htm
Ye, P.S., Wu, Z.H., Hu, D.G., et al., 2004.Geochemical Characteristics and Tectonic Setting of Ophiolite of Dongqiao, Tibet.Geoscience, 18(3):309-315 (in Chinese with English abstract). http://www.researchgate.net/publication/284938968_Geochemical_characteristics_and_tectonic_setting_of_ophiolite_of_Dongqiao_Tibet
Yin, A., Harrison, T.M., 2000.Geologic Evolution of the Himalayan-Tibetan Orogen.Annual Review of Earth and Planetary Sciences, 28(1):211-280. https://doi.org/10.1146/annurev.earth.28.1.211
Zeitler, P.K., 1985.Cooling History of the NW Himalaya, Pakistan.Tectonics, 4(1):127-151. https://doi.org/10.1029/tc004i001p00127
Zhang, X.R., Shi, R.D., Huang, Q.S., et al., 2010.Finding of High-Pressure Mafic Granulites in the Amdo Basement, Central Tibet.Chinese Science Bulletin, 55(27-28):2702-2711 (in Chinese). doi: 10.1007/s11434-010-4127-y
Zhang, X.R., Shi, R.D., Huang, Q.S., et al., 2014.Early Jurassic High-Pressure Metamorphism of the Amdo Terrane, Tibet:Constraints from Zircon U-Pb Geochronology of Mafic Granulites.Gondwana Research, 26(3-4):975-985. https://doi.org/10.1016/j.gr.2013.08.003
Zhang, X.Z., Dong, Y.S., Xie, C.M., et al., 2010.Identification and Significance of High-Pressure Granulite in Anduo Area, Tibetan Plateau.Acta Petrologica Sinica, 26(7):2106-2112 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201007013.htm
Zhang, Y., Chen, W., Chen, K.L., et al., 2006.Study on the Ar-Ar Age Spectrum of Diagenetic I/S and the Mechanism of ³⁹Ar Recoil Loss—Examples from the Clay Minerals of P-T Boundary in Changxing, Zhejiang Province.Geological Review, 52(4):556-561 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/004019519290128S
Zhu, D.C., Li, S.M., Cawood, P.A., et al., 2016.Assembly of the Lhasa and Qiangtang Terranes in Central Tibet by Divergent Double Subduction.Lithos, 245:7-17. https://doi.org/10.1016/j.lithos.2015.06.023
Zhu, D.C., Mo, X.X, Niu, Y.L, et al., 2009.Geochemical Investigation of Early Cretaceous Igneous Rocks along an East-West Traverse throughout the Central Lhasa Terrane, Tibet.Chemical Geology, 268(3):298-312. http://npd.nsfc.gov.cn/projectDetail.action?pid=40830317
Zhu, D.C., Pan, G.T., Wang, L.Q., et al., 2008a.Spatial-Temporal Distribution and Tectonic Setting of Jurassic Magmatism in the Gangdise Belt, Tibet, China.Geological Bulletin of China, 27(4):458-468 (in Chinese with English abstract). http://www.researchgate.net/publication/287635476_Spatial-temporal_distribution_and_tectonic_setting_of_Jurassic_magmatism_in_the_Gangdise_belt_Tibet
Zhu, D.C., Pan, G.T., Wang, L.Q., et al., 2008b.Tempo-Spatial Variations of Mesozoic Magmatic Rocks in the Gangdise Belt, Tibet, China, with a Discussion of Geodynamic Setting-Related Issues.Geological Bulletin of China, 27(9):1535-1536 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200809015.htm
Zhu, D.C., Pan, G.T., Mo, X.X., et al., 2006.Late Jurassic-Early Cretaceous Geodynamic Setting in Middle-northern Gangdese:New Insights from Volcanic Rocks.Acta Petrologica Sinica, 22(3):534-546 (in Chinese with English abstract). http://www.oalib.com/paper/1472180
Zhu, D.C., Zhao, Z.D., Niu, Y.L., et al., 2011.The Lhasa Terrane:Record of a Microcontinent and Its Histories of Drift and Growth.Earth and Planetary Science Letters, 301(1-2):241-255. https://doi.org/10.1016/j.epsl.2010.11.005
Zhu, D.C., Zhao, Z.D., Niu, Y.L., et al., 2012.Cambrian Bimodal Volcanism in the Lhasa Terrane, Southern Tibet:Record of an Early Paleozoic Andean-Type Magmatic Arc in the Australian Proto-Tethyan Margin.Chemical Geology, 328:290-308. https://doi.org/10.1016/j.chemgeo.2011.12.024
Zhu, D.C., Zhao, Z.D., Niu, Y.L., et al., 2012.Origin and Paleozoic Tectonic Evolution of the Lhasa Terrane.Geological Journal of China Universities, 18(1):1-15 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-GXDX201201003.htm
常承法, 郑锡澜, 1973.中国西藏南部珠穆朗玛地区地质构造特征以及青藏高原东西向诸山系形成的探讨.中国科学, (2): 190-201. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jaxk197302006&dbname=CJFD&dbcode=CJFQ
陈国荣, 刘鸿飞, 蒋光武, 等, 2004.西藏班公湖-怒江结合带中段沙木罗组的发现.地质通报, 23(2): 193-194. http://d.old.wanfangdata.com.cn/Periodical/zgqydz200402015
陈文, 张彦, 张岳桥, 等, 2006.青藏高原东南缘晚新生代幕式抬升作用的Ar-Ar热年代学证据.岩石学报, 22(4): 867-872. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20060492&journal_id=ysxb
丁帅, 唐菊兴, 郑文宝, 等, 2017.西藏拿若斑岩型铜(金)矿含矿岩体年代学、地球化学及地质意义.地球科学, 42(1): 1-23. http://www.earth-science.net/WebPage/Article.aspx?id=3409
董美玲, 董国臣, 莫宣学, 等, 2012.滇西保山地块早古生代花岗岩类的年代学、地球化学及意义.岩石学报, 28(5): 1453-1464. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20120509
杜德道, 曲晓明, 王根厚, 等, 2011.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据.岩石学报, 27(7): 1993-2002. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201107009&dbname=CJFD&dbcode=CJFQ
辜平阳, 李荣社, 何世平, 等, 2012.西藏那曲县北聂荣微地块聂荣岩群中斜长角闪岩——Rodinia超大陆裂解的地质纪录.岩石矿物学杂志, 31(2): 145-154. http://d.old.wanfangdata.com.cn/Periodical/yskwxzz201202003
胡隽, 万永文, 陶专, 等, 2014.班公湖-怒江缝合带西段特提斯洋盆南向俯冲的地球化学和年代学证据.成都理工大学学报(自然科学版), 41(4): 505-515. http://d.wanfangdata.com.cn/Periodical_cdlgxyxb201404014.aspx
胡培远, 李才, 苏犁, 等, 2010.青藏高原羌塘中部蜈蚣山花岗片麻岩锆石U-Pb定年——泛非与印支事件的年代学记录.中国地质, 37(4): 1050-1061. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201004019
黄继钧, 2001.藏北羌塘盆地构造特征及演化.中国区域地质, 20(2): 178-186. http://www.cqvip.com/qk/95894X/200102/5234128.html
李再会, 林仕良, 丛峰, 等, 2012.滇西高黎贡山群变质岩的锆石年龄及其构造意义.岩石学报, 28(5): 1529-1541. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20120515
刘敏, 赵志丹, 管琪, 等, 2011.西藏聂荣微陆块早侏罗世中期花岗岩及其包体的岩浆混合成因:锆石LA-ICP-MS U-Pb定年和Hf同位素证据.岩石学报, 27(7): 1931-1937. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201107002
刘敏, 朱弟成, 赵志丹, 等, 2010.藏北聂荣地区早侏罗世末期的岩浆混合作用及构造意义.岩石学报, 26(10): 3117-3130. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201010023.htm
密文天, 朱利东, 杨文光, 等, 2017.西藏尼玛盆地北部古近系牛堡组物源及地质意义.地球科学, 42(2): 240-257. http://www.earth-science.net/WebPage/Article.aspx?id=3429
莫宣学, 董国臣, 赵志丹, 等, 2005.西藏冈底斯带花岗岩的时空分布特征及地壳生长演化信息.高校地质学报, 11(3): 281-290. http://d.old.wanfangdata.com.cn/Periodical/gxdzxb200503001
潘桂棠, 莫宣学, 侯增谦, 等, 2006.冈底斯造山带的时空结构及演化.岩石学报, 22(3): 521-533. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200603001
潘桂棠, 王立全, 朱弟成, 2004.青藏高原区域地质调查中几个重大科学问题的思考.地质通报, 23(1): 12-19. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200401003.htm
曲晓明, 王瑞江, 辛洪波, 等, 2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学.地球化学, 38(6): 523-535. http://d.old.wanfangdata.com.cn/Periodical/dqhx200906002
王明, 李才, 解超明, 等, 2012.聂荣微陆块花岗片麻岩锆石LA-ICP-MS U-Pb定年——新元古代基底岩石的发现及其意义.岩石学报, 28(12): 4101-4108. http://www.oalib.com/paper/1474698
王晓先, 张进江, 杨雄英, 等, 2011.藏南吉隆地区早古生代大喜马拉雅片麻岩锆石SHRIMP U-Pb年龄、Hf同位素特征及其地质意义.地学前缘, 18(2): 127-139. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201102011
吴珍汉, 吴中海, 胡道功, 等, 2009.青藏高原新生代构造演化与隆升过程.北京:地质出版社.
夏斌, 徐力峰, 韦振权, 等, 2008.西藏东巧蛇绿岩中辉长岩锆石SHRIMP定年及其地质意义.地质学报, 82(4): 528-531. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200804010
肖序常, 李廷栋, 2000.青藏高原的构造演化与隆升机制.广州:广东科技出版社, 239-268.
解超明, 李才, 苏黎, 等, 2010.藏北安多地区花岗片麻岩锆石LA-ICP-MS U-Pb定年.地质通报, 29(12): 1737-1744. doi: 10.3969/j.issn.1671-2552.2010.12.002
解超明, 2013. 青藏高原聂荣微陆块构造演化——年代学与地球化学制约. 长春: 吉林大学.
许志琴, 杨经绥, 梁凤华, 等, 2005.喜马拉雅地体的泛非-早古生代造山事件年龄记录.岩石学报, 21(1): 1-12. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200501001
杨红, 刘福来, 刘平华, 等, 2013.扬子地块西南缘大红山群石榴白云母-长石石英片岩的白云母⁴⁰Ar-³⁹Ar定年及其地质意义.岩石学报, 29(6): 2161-2170. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201306021
叶培盛, 吴珍汉, 胡道功, 等, 2004.西藏东巧蛇绿岩的地球化学特征及其形成的构造环境.现代地质, 18(3): 309-315. http://d.old.wanfangdata.com.cn/Periodical/xddz200403007
张晓冉, 史仁灯, 黄启帅, 等, 2010.青藏高原安多高压基性麻粒岩的发现及其地质意义.科学通报, 55(27-28): 2702-2711. https://www.researchgate.net/profile/Xiaoran_Zhang3/publication/267439734_qingcanggaoyuananduogaoyajixingmaliyandefaxianjiqidezhiyiyi/links/544f6c760cf26dda08906120/qingcanggaoyuananduogaoyajixingmaliyandefaxianjiqidezhiyiyi.pdf
张修政, 董永胜, 解超明, 等, 2010.安多地区高压麻粒岩的发现及其意义.岩石学报, 26(7): 2106-2112. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201007012
张彦, 陈文, 陈克龙, 等, 2006.成岩混层(I/S)Ar-Ar年龄谱型及.³⁹Ar核反冲丢失机理研究——以浙江长兴地区P-T界线粘土岩为例.地质论评, 52(4): 556-561. http://www.oalib.com/paper/4573945
朱弟成, 潘桂棠, 莫宣学, 等, 2006.冈底斯中北部晚侏罗世-早白垩世地球动力学环境:火山岩约束.岩石学报, 22(3): 534-546. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200603002.htm
朱弟成, 潘桂棠, 王立全, 等, 2008a.西藏冈底斯带侏罗纪岩浆作用的时空分布及构造环境.地质通报, 27(4): 458-468. http://d.old.wanfangdata.com.cn/Periodical/zgqydz200804003
朱弟成, 潘桂棠, 王立全, 等, 2008b.西藏冈底斯带中生代岩浆岩的时空分布和相关问题的讨论.地质通报, 27(9): 1535-1536. http://d.old.wanfangdata.com.cn/Periodical/zgqydz200809013
朱弟成, 赵志丹, 牛耀龄, 等, 2012.拉萨地体的起源和古生代构造演化.高校地质学报, 18(1): 1-15. https://www.researchgate.net/profile/Yaoling_Niu/publication/260835521_Origin_and_Paleozoic_Tectonic_Evolution_of_the_Lhasa_Terrane/links/54c645600cf219bbe4f79a90.pdf?origin=publication_detail