东亚大陆西缘侏罗纪变形——以班公湖-怒江带中段韧性变形为例

施炜; 董树文; 黄兴富; 陈虹; 崔建军

东亚大陆西缘侏罗纪变形——以班公湖-怒江带中段韧性变形为例

1.
中国地质科学院地质力学研究所, 北京 100081
2.
南京大学地球科学与工程学院, 江苏南京 210093

基金项目:

国家重点研发计划项目 2017YFC0601402

中国地质调查局项目 1212011120184

中国地质调查局项目 1212011221111

详细信息

作者简介:
施炜(1971-), 男, 研究员, 主要从事中、新生代构造研究.E-mail:shiweinmg@163.com

中图分类号: P542
计量
- 文章访问数: 308
- HTML全文浏览量: 118
- PDF下载量: 23
- 被引次数: 0
出版历程
- 收稿日期: 2017-03-06
- 刊出日期: 2017-08-01

JURASSIC DEFORMATION AT THE WESTERN MARGIN OF THE EAST ASIA CONTINENT: A CASE STUDY OF DUCTILE DEFORMATION IN THE CENTRAL SEGMENT OF THE BANGONG CO-NUJIANG BELT

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, Jiangsu, China

摘要

摘要: 班公湖-怒江带作为羌塘地块与拉萨地块晚中生代聚合而形成巨型构造带，其形成时代与如何汇聚是构造研究关键所在。本次研究选择班公湖—怒江带中段的安多—聂荣地块发育为研究区，对地块内部基底发育的近东西走向的韧性剪切带，开展了韧性剪切变形分析与同构造年代学研究。剪切带面理和线理测量分析指示北东—南西向构造挤压，其同构造矿物⁴⁰Ar/³⁹Ar的测试分析获得年龄约为167 Ma，表明班公湖-怒江带中段形成于中侏罗世中期北东—南西向汇聚的构造背景下。结合区域构造分析，东亚大陆西缘羌塘地块与拉萨地块在中侏罗世中期以北东—南西向碰撞聚合的构造方式完成大陆拼接，为东亚大陆西缘中侏罗世变形提供了直接构造证据。
- 东亚大陆 /
- 班公湖—怒江带 /
- 安多—聂荣地块 /
- 韧性剪切变形 /
- 侏罗纪
Abstract: The Bangong Co-Nujiang belt resulted from the convergence and collision between the Chiangtang and Lhasa blocks in late Mesozoic. The key issue in this tectonic study is when and how the belt was formed. With the Ando-Nyainrong block of the central segment of the Bangong Co-Nujiang belt as the study area, the ductile shear belts with approximately E-W strike developed in the internal basement of the block are studied based on ductile shear deformation analysis and syntectonic geochronology. The foliation and lineation measurement and analysis of the shear belts indicate tectonic compression with NE-SW strike. Through the test analysis of ⁴⁰Ar/³⁹Ar in syntectonic minerals, the age is worked out as 167 Ma. All the evidence shows that the central segment of the Bangong Co-Nujiang belt was caused under the convergence and collision between the Chiangtang and Lhasa blocks in the middle of Middle Jurassic, which provides direct tectonic evidence for the Jurassic deformation at the western margin of the East Asian continent.
- East Asia continent /
- Bangong Co-Nujiang belt /
- Ando-Nyainrong block /
- ductile shear deformation /
- Jurassic

HTML全文

图 1 青藏高原及其邻区构造纲要图与东亚大陆晚中生代构造简图

F₁—喜马拉雅主冲断层；F₂—雅鲁藏布江缝合带；F₃—班公湖-怒江缝合带；F₄—金沙江缝合带；F₅—昆仑山断裂带；F₆—阿尔金断裂带；F₇—海原-祁连山构造带；F₈—喀喇昆仑断裂带；F₉—龙门山断裂带

Figure 1. Tectonic outline map of the Qinghai-Tibet Plateau and its adjacent areas and simplified tectonic map of the East Asia continent in late Mesozoic

下载: 全尺寸图片幻灯片

图 2 班公湖—怒江缝合带中段地质简图^[70~71]

Figure 2. Geological sketch of the middle segment of the Bangong Co-Nujiang suture belt^[70~71]

下载: 全尺寸图片幻灯片

图 3 安多—聂荣地块韧性剪切带北东—南西向构造应力场特征(下半球等角投影(吴氏网))

Figure 3. The characteristics of the NE-SW direction tectonic stress field of the ductile shear belts in the Ando-Nyainrong block

下载: 全尺寸图片幻灯片

图 4 安多—聂荣地块西南缘韧性剪切带(观测点D53)⁴⁰Ar/³⁹Ar坪年龄与等时线年龄

Figure 4. ⁴⁰Ar/³⁹Ar plateau age and isochron age of the ductile shear belts at the southwest margin of the Ando-Nyainrong block(Site D53)

下载: 全尺寸图片幻灯片

图 5 安多—聂荣地块西北缘韧性剪切带(观测点D56)⁴⁰Ar/³⁹Ar坪年龄与等时线年龄

Figure 5. ⁴⁰Ar/³⁹Ar plateau age and isochron age of the ductile shear belts at the northwest margin of the Ando-Nyainrong block(Site D56)

下载: 全尺寸图片幻灯片

表 1 安多—聂荣地块韧性剪切变形测量结果与北东—南西向挤压构造应力场

Table 1. Results of ductile shear deformation analysis and the NE-SW direction compressional tectonic stress field in the Ando-Nyainrong block

点号	经度(E)	纬度(N)	数据量	σ₁(az°/pl°)	σ₂(az°/pl°)	σ₃(az°/pl°)	R
D20	92°20′01″	32°07′16″	19	333/41	085/22	196/39	0.7
D21	92°18′45″	32°07′29″	5	186/34	047/47	292/21	0.7
D22	92°17′44″	32°06′26″	5	153/29	248/08	353/58	0.2
D25	92°12′14″	32°03′23″	4	320/43	111/42	215/15	0.3
D28	92°04′05″	31°47′32″	4	NNE-SSW
D45	93°06′34″	31°50′10″	9	320/18	097/65	225/15	0.1
D53	91°42′06″	31°52′51″	7	244/24	137/33	002/46	0.8
D55	91°41′49″	32°06′05″	4	063/05	157/29	323/59	0.5
D56	91°42′45″	32°07′15″	7	100/17	209/45	355/39	0.5
D70	91°40′56″	32°02′05″	5	030/15	297/11	172/70	0.4
注：σ₁—最大主应力；σ₂—中间主应力；σ₃—最小主应力；az—倾伏向；pl—倾伏角；R=(σ₂-σ₃/σ₁-σ₃)

下载: 导出CSV

表 2 安多—聂荣地块西南缘韧性剪切带(观测点D53)⁴⁰Ar/³⁹Ar坪年龄与等时线年龄

Table 2. ⁴⁰Ar/³⁹Ar plateau age and isochron age of the ductile shear belts at the southwest margin of the Ando-Nyainrong block(Site D53)

T/℃	(⁴⁰Ar/ ³⁹Ar) _m	⁽³⁶Ar/ ³⁹Ar) _m	(³⁷Ar ₀/ ³⁹Ar) _m	(³⁸Ar/ ³⁹Ar) _m	⁴⁰Ar/%	F	³⁹Ar/10 ^-14mol	³⁹Ar(Cum.)/%	Age/Ma	±1σ/Ma
D53-1钾长石 W=27.71 mg J=0.002684 Total age=161.0Ma
700	165.8118	0.1561	0.7508	0.0540	72.22	119.8151	0.06	0.33	503.0	5.9
800	31.5490	0.0041	0.0206	0.0137	96.14	30.3332	1.28	6.84	141.2	1.4
860	28.0541	0.0010	0.0474	0.0129	98.90	27.7466	0.80	10.93	129.6	1.3
920	28.3819	0.0031	0.1538	0.0141	96.81	27.4801	0.62	14.06	128.4	1.3
980	28.7767	0.0015	0.1156	0.0130	98.46	28.3349	0.35	15.83	132.2	1.4
1040	30.5556	0.0048	0.0293	0.0139	95.30	29.1211	0.64	19.07	135.8	1.4
1100	34.8159	0.0072	0.0410	0.0148	93.85	32.6757	1.03	24.32	151.6	1.5
1160	37.8379	0.0090	0.0237	0.0147	92.95	35.1694	1.65	32.70	162.7	1.6
1210	38.8774	0.0080	0.0170	0.0147	93.90	36.5066	3.23	49.13	168.6	1.6
1260	38.2769	0.0067	0.0052	0.0142	94.83	36.2989	6.82	83.80	167.7	1.6
1290	37.4411	0.0059	0.0204	0.0141	95.33	35.6945	2.62	97.10	165.0	1.6
1330	37.8766	0.0080	0.1179	0.0146	93.74	35.5089	0.43	99.27	164.2	1.7
1400	40.3533	0.0196	0.3614	0.0165	85.72	34.5995	0.14	100.00	160.2	2.4
D56-1黑云母 W=33.07 mg J=0.002735 Total age=165.6Ma
700	56.7666	0.1419	1.2378	0.0440	26.28	14.9359	0.06	0.37	72.2	5.2
760	36.0626	0.0190	0.1219	0.0169	84.48	30.4678	1.00	6.30	144.4	1.4
800	36.3997	0.0037	0.0783	0.0139	96.99	35.3058	1.61	15.86	166.3	1.6
840	36.1519	0.0021	0.0000	0.0133	98.24	35.5169	1.64	25.62	167.3	1.6
880	36.0022	0.0024	0.1252	0.0138	98.05	35.3049	1.15	32.45	166.3	1.6
920	36.0515	0.0017	0.0771	0.0134	98.59	35.5449	1.15	39.31	167.4	1.6
960	36.0165	0.0019	0.1006	0.0134	98.47	35.4710	1.13	46.01	167.0	1.6
1000	36.2395	0.0019	0.0167	0.0131	98.46	35.6825	1.13	52.75	168.0	1.6
1040	35.9673	0.0014	0.0470	0.0134	98.82	35.5425	2.20	65.84	167.4	1.6
1080	36.0125	0.0015	0.0312	0.0133	98.78	35.5726	2.63	81.46	167.5	1.6
1200	36.1565	0.0014	0.0076	0.0130	98.88	35.7507	2.96	99.05	168.3	1.6
1400	39.5904	0.0179	0.7467	0.0179	86.78	34.3776	0.16	100.00	162.1	2.3
注：表中下标m代表样品中测定的同位素比值，F=⁴⁰Ar^*/³⁹Ar, is the ratio of radiogenic Argon40 and Argon39

下载: 导出CSV

参考文献(80)

[1]	Wong W H. The Mesozoic orogenic movement in eastern China[J]. Bulletin of the Geological Society of China, 1929, 8(1): 33~44. doi: 10.1111/j.1755-6724.1929.mp8001004.x/pdf
[2]	Jahn B M, Chen P Y, Yen T P. Rb-Sr ages of granitic rocks in southeastern China and their tectonic significance[J]. GSA Bulletin, 1976, 87(5): 763~776. doi: 10.1130/0016-7606(1976)87<763:RAOGRI>2.0.CO;2
[3]	Zhao X X, Coe R S, Zhou Y X, et al. New paleomagnetic results from northern China: collision and suturing with Siberia and Kazakhstan[J]. Tectonophysics, 1990, 181(1/4): 43~81. http://adsabs.harvard.edu/abs/1990Tectp.181...43X
[4]	赵越, 杨振宇, 马醒华.东亚大地构造发展的重要转折[J].地质科学, 1994, 29(2): 105~119. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX402.000.htm ZHAO Yue, YANG Zhenyu, MA Xinghua. Geotectonic transition from Paleoasian system and Paleotethyan system to Paleopacific active continental margin in eastern Asia[J]. Scientia Geologica Sinica, 1994, 29(2): 105~119. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX402.000.htm
[5]	Davis G A, Darby B J, Zheng Y D, et al. Geometric and temporal evolution of an extensional detachment fault, Hohhot metamorphic core complex, Inner Mongolia, China[J]. Geology, 2002, 30(11): 1003~1006. doi: 10.1130/0091-7613(2002)030<1003:GATEOA>2.0.CO;2
[6]	Yin A, Nie S Y. A Phanerozoic palinspastic reconstruction of China and its neighbouring regions[A]. Yin A, Harrison T M. The Tectonic Evolution of Asia[M].Cambridge: Cambridge University Press, 1996, 442~485.
[7]	董树文, 吴锡浩, 吴珍汉, 等.论东亚大陆的构造翘变——燕山运动的全球意义[J].地质论评, 2000, 46(1): 8~13. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200001001.htm DONG Shuwen, WU Xihao, WU Zhenhan, et al. On tectonic seesawing of the East Asia continent-global implication of the Yanshanian Movement[J]. Geological Review, 2000, 46(1): 8~13. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200001001.htm
[8]	董树文, 张岳桥, 陈宣华, 等.晚侏罗世东亚多向汇聚构造体系的形成与变形特征[J].地球学报, 2008, 29(3): 306~317. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200803006.htm DONG Shuwen, ZHANG Yueqiao, CHEN Xuanhua, et al. The formation and deformational characteristics of East Asia multi-direction convergent tectonic system in Late Jurassic[J]. Acta Geoscientica Sinica, 2008, 29(3): 306~317. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200803006.htm
[9]	董树文, 张岳桥, 龙长兴, 等.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报, 2007, 81(11): 1449~1461. doi: 10.3321/j.issn:0001-5717.2007.11.001 DONG Shuwen, ZHANG Yueqiao, LONG Changxing, et al. Jurassic tectonic revolution in china and new interpretation of the Yanshan Movement[J]. Acta Geologica Sinica, 2007, 81(11): 1449~1461. doi: 10.3321/j.issn:0001-5717.2007.11.001
[10]	Deng J F, Su S G, Mo X X, et al. The sequence of magmatic-tectonic events and orogenic processes of the Yanshan belt, North China[J]. Acta Geologica Sinica (English Edition), 2004, 78(1): 260~266. doi: 10.1111/j.1755-6724.2004.tb00698.x/full
[11]	张宏仁, 张永康, 蔡向民, 等.燕山运动的"绪动"——燕山事件[J].地质学报, 2013, 87(12): 1779~1790. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201312001.htm ZHANG Hongren, ZHANG Yongkang, CAI Xiangmin, et al. The triggering of Yanshan Movement: Yanshan event[J]. Acta Geologica Sinica, 2013, 87(12): 1779~1790. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201312001.htm
[12]	Dong S W, Zhang Y Q, Zhang F Q, et al. Late Jurassic-Early Cretaceous continental convergence and intracontinental orogenesis in East Asia: a synthesis of the Yanshan Revolution[J]. Journal of Asian Earth Sciences, 2015, 114: 750~770. doi: 10.1016/j.jseaes.2015.08.011
[13]	李三忠, 张国伟, 周立宏, 等.中、新生代超级汇聚背景下的陆内差异变形:华北伸展裂解和华南挤压逆冲[J].地学前缘, 2011, 18(3): 79~107. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201103012.htm LI Sanzhong, ZHANG Guowei, ZHOU Lihong, et al. The opposite Meso-Cenozoic intracontinental deformations under the superconvergence: rifting and extension in the North China Craton and shortening and thrusting in the South China Craton[J]. Earth Science Frontiers, 2011, 18(3): 79~107. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201103012.htm
[14]	张长厚, 吴淦国, 徐德斌, 等.燕山板内造山带中段中生代构造格局与构造演化[J].地质通报, 2004, 23(9): 864~875. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2004Z2006.htm ZHANG Changhou, WU Ganguo, XU Debin, et al. Mesozoic tectonic framework and evolution in the central segment of the intraplate Yanshan orogenic belt[J]. Geological Bulletin of China, 2004, 23(9): 864~875. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2004Z2006.htm
[15]	崔盛芹, 马寅生, 吴珍汉, 等.燕山陆内造山带造山过程及动力机制[M].北京:地震出版社, 2006, 1~280. CUI Shengqin, MA Yinsheng, WU Zhenhan, et al. Orogenic process and dynamic mechanism of the Yanshan intracontinental orogenic belt[M]. Beijing: Seismological Press, 2006, 1~280.
[16]	董树文, 胡健民, 施炜, 等.大巴山侏罗纪叠加褶皱与侏罗纪前陆[J].地球学报, 2006, 27(5): 403~410. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200605003.htm DONG Shuwen, HU Jianmin, SHI Wei, et al. Jurassic superposed folding and Jurassic foreland in the Daba mountain, Central China[J]. Acta Geoscientia Sinica, 2006, 27(5): 403~410. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200605003.htm
[17]	Dong S W, Gao R, Yin A, et al. What drove continued continent-continent convergence after ocean closure? Insights from high-resolution seismic-reflection profiling across the Daba Shan in central China[J]. Geology, 2013, 41(6): 671~674. doi: 10.1130/G34161.1
[18]	张岳桥, 董树文, 赵越, 等.华北侏罗纪大地构造:综评与新认识[J].地质学报, 2007, 81(11): 1462~1480. doi: 10.3321/j.issn:0001-5717.2007.11.002 ZHANG Yueqiao, DONG Shuwen, ZHAO Yue, et al. Jurassic tectonics of North China: a synthetic view[J]. Acta Geologica Sinica, 2007, 81(11): 1462~1480. doi: 10.3321/j.issn:0001-5717.2007.11.002
[19]	张岳桥, 廖昌珍, 施炜, 等.论鄂尔多斯盆地及其周缘侏罗纪变形[J].地学前缘, 2007, 14(2): 182~196. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200702014.htm ZHANG Yueqiao, LIAO Changzhen, SHI Wei, et al. On the Jurassic deformation in and around the Ordos Basin, North China[J]. Earth Science Frontiers, 2007, 14(2): 182~196. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200702014.htm
[20]	张岳桥, 董树文, 李建华, 等.中生代多向挤压构造作用与四川盆地的形成和改造[J].中国地质, 2011, 38(2): 233~250. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201102002.htm ZHANG Yueqiao, DONG Shuwen, LI Jianhua, et al. Mesozoic multi-directional compressional tectonics and formation-reformation of Sichuan basin[J]. Geology in China, 2011, 38(2): 233~250. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201102002.htm
[21]	Shi W, Zhang Y Q, Dong S W, et al. Intra-continental Dabashan orocline, southwestern Qinling, Central China[J]. Journal of Asian Earth Sciences, 2012, 46: 20~38. doi: 10.1016/j.jseaes.2011.10.005
[22]	Shi W, Dong S W, Li J H, et al. Formation of the Moping dome in the Xuefengshan orocline, central China and its tectonic significance[J]. Acta Geologica Sinica (English Edition), 2013, 87(3): 720~729. doi: 10.1111/acgs.2013.87.issue-3
[23]	Shi W, Dong S W, Ratschbacher L, et al. Meso-Cenozoic tectonic evolution of the Dangyang Basin, north-central Yangtze craton, central China[J]. International Geology Review, 2013, 55(3): 382~396. doi: 10.1080/00206814.2012.715732
[24]	Shi W, Dong S W, Zhang Y Q, et al. The typical large-scale superposed folds in the central South China: implications for Mesozoic intracontinental deformation of the South China Block[J]. Tectonophysics, 2015, 664: 50~66. doi: 10.1016/j.tecto.2015.08.039
[25]	Huang X F, Shi W, Chen P, et al. Superposed deformation in the Helanshan Structural Belt: implications for Mesozoic intracontinental deformation of the North China Plate[J]. Journal of Asian Earth Sciences, 2015, 114: 140~154. doi: 10.1016/j.jseaes.2015.05.027
[26]	Scotese C R. Jurassic and Cretaceous plate tectonic reconstructions[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1991, 87(1/4): 493~501. http://cat.inist.fr/?aModele=afficheN&cpsidt=5542144
[27]	Delvaux D, Moeys R, Stapel G, et al. Palaeostress reconstructions and geodynamics of the Baikal region, Central Asia, Part I. Palaeozoic and Mesozoic pre-rift evolution[J]. Tectonophysics, 1995, 252(1/4): 61~101.
[28]	Kravchinsky V A, Cogné J P, Harbert W P, et al. Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia[J]. Geophysical Journal International, 2002, 148(1): 34~57. doi: 10.1046/j.1365-246x.2002.01557.x
[29]	Tomurtogoo O, Windley B F, Kröner A, et al. Zircon age and occurrence of the Adaatsag ophiolite and Muron shear zone, central Mongolia: constraints on the evolution of the Mongol-Okhotsk Ocean, suture and orogen[J]. Journal of the Geological Society, 2005, 162(1): 125~134. doi: 10.1144/0016-764903-146
[30]	Xiao W J, Kusky T. Geodynamic processes and metallogenesis of the Central Asian and related orogenic belts: introduction[J]. Gondwana Research, 2009, 16(2): 167~169. doi: 10.1016/j.gr.2009.05.001
[31]	Zorin Y A. Geodynamics of the western part of the Mongolia-Okhotsk collisional belt, Trans-Baikal region (Russia) and Mongolia[J]. Tectonophysics, 1999, 306(1): 33~56. doi: 10.1016/S0040-1951(99)00042-6
[32]	Parfenov L M, Popeko L I, Tomurtogoo O. Problems of tectonics of the Mongol-Okhotsk orogenic belt[J]. Geology of the Pacific Ocean, 2001, 16(5): 797~830. https://www.intechopen.com/books/statistics/updates-in-volcanology-a-comprehensive-approach-to-volcanological-problems/bimodal-volcano-plutonic-complexes-in-the-frame-of-eastern-member-of-mongol-okhotsk-orogenic-belt-as
[33]	Sun D Y, Gou J, Wang T H, et al. Geochronological and geochemical constraints on the Erguna massif basement, NE China-subduction history of the Mongo-Okhotsk oceanic crust[J]. International Geology Review, 2013, 55(14): 1801~1816. doi: 10.1080/00206814.2013.804664
[34]	Cogné J P, Kravchinsky V A, Halim N, et al. Late Jurassic-Early Cretaceous closure of the Mongol-Okhotsk ocean demonstrated by new Mesozoic palaeomagnetic results from the Trans-Baïkal area (SE Siberia)[J]. Geophysical Journal International, 2005, 163(2): 813~832. doi: 10.1111/gji.2005.163.issue-2
[35]	Metelkin D V, Vernikovsky V A, Kazansky A Y, et al. Late Mesozoic tectonics of Central Asia based on paleomagnetic evidence[J]. Gondwana Research, 2010, 18(2/3): 400~419.
[36]	Pei J L, Sun Z M, Liu J, et al. A paleomagnetic study from the Late Jurassic volcanics (155 Ma), North China: implications for the width of Mongol-Okhotsk Ocean[J]. Tectonophysics, 2011, 510(3/4): 370~380. http://adsabs.harvard.edu/abs/2011Tectp.510..370J
[37]	马寅生.燕山东段—下辽河地区中新生代盆山构造演化[J].地质力学学报, 2001, 7(1): 79~91. http://www.cnki.com.cn/Article/CJFDTotal-DZLX200101011.htm MA Yinsheng. The evolution of Mesozoic-Cenozoic basin-mountain structure in the east Yanshan area and Xialiaohe basin[J]. Journal of Geomechanics, 2001, 7(1): 79~91. http://www.cnki.com.cn/Article/CJFDTotal-DZLX200101011.htm
[38]	崔盛芹, 吴珍汉, 马寅生, 等.北京地区中新生代陆内造山过程——以十三陵—龙庆峡—八达岭路线观察为基础[J].地质力学学报, 2003, 9(3): 201~219. http://mall.cnki.net/magazine/Article/DZLX200303002.htm CUI Shengqin, WU Zhenhan, MA YinSheng, et al. Meso-Cenozoic intracontinental orogenic process in the Beijing area-a case study based on geological observations from the Ming tombs to Badaling mountain[J]. Journal of Geomechanics, 2003, 9(3): 201~219. http://mall.cnki.net/magazine/Article/DZLX200303002.htm
[39]	Daoudene Y, Ruffet G, Cocherie A, et al. Timing of exhumation of the Ereendavaa metamorphic core complex (north-eastern Mongolia)-U-Pb and ⁴⁰Ar/³⁹Ar constraints[J]. Journal of Asian Earth Sciences, 2013, 62: 98~116. doi: 10.1016/j.jseaes.2011.04.009
[40]	Berzina A P, Berzina A N, Gimon V O. Geochemical and Sr-Pb-Nd isotopic characteristics of the Shakhtama porphyry Mo-Cu system (Eastern Transbaikalia, Russia)[J]. Journal of Asian Earth Sciences, 2014, 79: 655~665. doi: 10.1016/j.jseaes.2013.07.028
[41]	Isozaki Y. Jurassic accretion tectonics of Japan[J]. Island Arc, 1997, 6(1): 25~51. doi: 10.1111/iar.1997.6.issue-1
[42]	Zhou X M, Li W X. Origin of Late Mesozoic igneous rocks in Southeastern China: implications for lithosphere subduction and underplating of mafic magmas[J]. Tectonophysics, 2000, 326(3/4): 269~287. http://adsabs.harvard.edu/abs/2000Tectp.326..269Z
[43]	Li X H, Li Z X, Li W X, et al. U-Pb zircon, geochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I-and A-type granites from central Guangdong, SE China: a major igneous event in response to foundering of a subducted flat-slab?[J]. Lithos, 2007, 96(1/2): 186~204.
[44]	Cui J J, Zhang Y Q, Dong S W, et al. Zircon U-Pb geochronology of the Mesozoic metamorphic rocks and granitoids in the coastal tectonic zone of SE China: constraints on the timing of Late Mesozoic orogeny[J]. Journal of Asian Earth Sciences, 2013, 62: 237~252. doi: 10.1016/j.jseaes.2012.09.014
[45]	Safonova I Y, Santosh M. Accretionary complexes in the Asia-Pacific region: tracing archives of ocean plate stratigraphy and tracking mantle plumes[J]. Gondwana Research, 2014, 25(1): 126~158. doi: 10.1016/j.gr.2012.10.008
[46]	Maruyama S. Pacific-type orogeny revisited: Miyashiro-type orogeny proposed[J]. Island Arc, 1997, 6(1): 91~120. doi: 10.1111/iar.1997.6.issue-1
[47]	Wu F Y, Han R H, Yang J H, et al. Initial constraints on the timing of granitic magmatism in North Korea using U-Pb zircon geochronology[J]. Chemical Geology, 2007, 238(3/4): 232~248.
[48]	Wu F Y, Lin J Q, Wilde S A, et al. Nature and significance of the Early Cretaceous giant igneous event in eastern China[J]. Earth and Planetary Science Letters, 2005, 233(1/2): 103~119.
[49]	Wu F Y, Yang J H, Wilde S A, et al. Geochronology, petrogenesis and tectonic implications of Jurassic granites in the Liaodong Peninsula, NE China[J]. Chemical Geology, 2005, 221(1/2): 127~156.
[50]	Lim C, Cho M. Two-phase contractional deformation of the Jurassic Daebo Orogeny, Chungnam Basin, Korea, and its correlation with the early Yanshanian movement of China[J]. Tectonics, 2012, 31(1): TC1004.
[51]	Li J H, Zhang Y Q, Dong S W, et al. Cretaceous tectonic evolution of South China: a preliminary synthesis[J]. Earth-Science Reviews, 2014, 134: 98~136. doi: 10.1016/j.earscirev.2014.03.008
[52]	李海龙, 张宏仁, 渠洪杰, 等.燕山运动"绪动/A幕"的本意及其锆石U-Pb年代学制约[J].地质论评, 2014, 60(5): 1026~1042. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201405008.htm LI Hailong, ZHANG Hongren, QU Hongjie, et al. Initiation, the first stage of the Yanshan (Yenshan) movement in western hills, constraints from zircon U-Pb dating[J]. Geological Review, 2014, 60(5): 1026~1042. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201405008.htm
[53]	黄迪颖.燕辽生物群和燕山运动[J].古生物学报, 2015, 54(4): 501~546. http://www.cnki.com.cn/Article/CJFDTOTAL-GSWX201504008.htm HUANG Diying. Yanliao biota and Yanshan movement[J]. Acta Palaeontologica Sinica, 2015, 54(4): 501~546. http://www.cnki.com.cn/Article/CJFDTOTAL-GSWX201504008.htm
[54]	Yin A, Harrison T M. Geologic evolution of the Himalayan-Tibetan orogen[J]. Annual Review of Earth and Planetary Sciences, 2000, 28: 211~280. doi: 10.1146/annurev.earth.28.1.211
[55]	Chu M F, Chung S L, Song B, et al. Zircon U-Pb and Hf isotope constraints on the Mesozoic tectonics and crustal evolution of southern Tibet[J]. Geology, 2006, 34(9): 745~748. doi: 10.1130/G22725.1
[56]	Zhu D C, Zhao Z D, Niu Y L, et al. The Lhasa Terrane: record of a microcontinent and its histories of drift and growth[J]. Earth and Planetary Science Letters, 2011, 301(1/2): 241~255.
[57]	Kapp J L D, Harrison T M, Kapp P, et al. Nyainqentanglha Shan: a window into the tectonic, Thermal, and geochemical evolution of the Lhasa block, southern Tibet[J]. Journal of Geophysical Research: Solid Earth, 2005, 110(B8): B08413.
[58]	潘桂棠, 莫宣学, 侯增谦, 等.冈底斯造山带的时空结构及演化[J].岩石学报, 2006, 22(3): 521~533. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200603001.htm PAN Guitang, MO Xuanxue, HOU Zengqian, et al. Spatial-temporal framework of the Gangdese orogenic belt and its evolution[J]. Acta Petrologica Sinica, 2006, 22(3): 521~533. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200603001.htm
[59]	Zhang Z M, Dong X, Santosh M, et al. Metamorphism and tectonic evolution of the Lhasa terrane, Central Tibet[J]. Gondwana Research, 2014, 25(1): 170~189. doi: 10.1016/j.gr.2012.08.024
[60]	王鸿祯.试论西藏地质构造分区问题[J].地球科学—武汉地质学院学报, 1983, (1): 1~8. WANG Hongzhen. On the Geotectonic units of Xizang (Tibet) region[J]. Earth Science-Journal of Wuhan College of Geology, 1983, (1): 1~8.
[61]	黄汲清, 陈炳蔚.中国及邻区特提斯海的演化[M].北京:地质出版社, 1987, 1~78. HUANG Jiqing, CHEN Bingwei. The evolution of the Tethys in China and adjacent regions[M]. Beijing: Geologic Publishing House, 1987, 1~78.
[62]	赵文津, 刘葵, 蒋忠惕, 等.西藏班公湖-怒江缝合带:深部地球物理结构给出的启示[J].地质通报, 2004, 23(7): 623~635. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200407000.htm ZHAO Wenjin, LIU Kui, JIANG Zhongti, et al. Bangong Co-Nujiang suture zone, Tibet-a suggestion given by deep geophysical structure[J]. Geological Bulletin of China, 2004, 23(7): 623~635. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200407000.htm
[63]	Wang Q, Wyman D A, Xu J F, et al. Triassic Nb-enriched basalts, magnesian andesites, and adakites of the Qiangtang terrane (central Tibet): Evidence for metasomatism by slab-derived melts in the mantle wedge[J]. Contributions to Mineralogy and Petrology, 2008, 155(4): 473~490. doi: 10.1007/s00410-007-0253-1
[64]	Zhang Z J, Deng Y F, Teng J W, et al. An overview of the crustal structure of the Tibetan plateau after 35 years of deep seismic soundings[J]. Journal of Asian Earth Sciences, 2011, 40(4): 977~989. doi: 10.1016/j.jseaes.2010.03.010
[65]	王希斌, 鲍佩声, 邓万明, 等.西藏蛇绿岩[M].北京:地质出版社, 1987. WANG Xibin, BAO Peisheng, DENG Wanming, et al. Xizang (Tibet) Ophiolite[M]. Beijing: Geological Publishing House, 1987.
[66]	刘敏, 赵志丹, 管琪, 等.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[J].岩石学报, 2011, 27(7): 1931~1937. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201107003.htm LIU Min, ZHAO Zhidan, GUAN Qi, et al. 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[J]. Acta Petrologica Sinica, 2011, 27(7): 1931~1937. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201107003.htm
[67]	李奋其, 刘伟, 耿全如.西藏冈底斯带那曲地区中生代火山岩的LA-ICP-MS锆石U-Pb年龄和地质意义[J].地球学报, 2010, 31(6): 781~790. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201006003.htm LI Fenqi, LIU Wei, GENG Quanru. Zircon LA-ICP-MS U-Pb ages of the Mesozoic volcanic rocks in Nagqu area of Gangdise in Tibet and their geological significance[J]. Acta Geoscientica Sinica, 2010, 31(6): 781~790. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201006003.htm
[68]	Guynn J H, Kapp P, Pullen A, et al. Tibetan basement rocks near Amdo reveal "missing" Mesozoic tectonism along the Bangong suture, central Tibet[J]. Geology, 2006, 34(6): 505~508. doi: 10.1130/G22453.1
[69]	Harris N B W, Inger S, Xu R H. Cretaceous plutonism in central Tibet: an example of post-collision magmatism?[J]. Journal of Volcanology and Geothermal Research, 1990, 44(1/2): 21~32.
[70]	中国地质大学地质调查研究院. 1: 25万安多县幅地质图[M]. 北京: 地质出版社, 2004. Geological Survey Academy of China University of Geosciences (Beijing) (AGSC). Regional geological map of Ando (1:250000)[M]. Beijing: Geological Publishing House, 2004.
[71]	西藏自治区地质调查院. 1: 25万那曲县幅地质图[M]. 北京: 地质出版社, 2004. Geological Survey Academy of Xizang (AGSXZ). Regional geological map of Nagqu (1:250000)[M]. Beijing: Geological Publishing House, 2004.
[72]	Dallmeyer R D, VanBreeman O. Rb-Sr whole-rock and ⁴⁰Ar/³⁹Ar mineral ages of the Togus and Hallowell quartz monzonite and Three Mile Pond granodiorite plutons, South-Central Maine: their bearing on post-Acadian cooling history[J]. Contributions to Mineralogy and Petrology, 1981, 78(1): 61~73. doi: 10.1007/BF00371144
[73]	Dewey J F, Shackelton R M, Chang C, et al. The tectonic evolution of the Tibetan Plateau[J]. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 1988, 327(1594): 379~413. doi: 10.1098/rsta.1988.0135
[74]	邱瑞照, 周肃, 邓晋福, 等.西藏班公湖-怒江西段舍马拉沟蛇绿岩中辉长岩年龄测定——兼论班公湖-怒江蛇绿岩带形成时代[J].中国地质, 2004, 31(3): 262~268. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200403003.htm QIU Ruizhao, ZHOU Su, DENG Jinfu, et al. Dating of gabbro in the Shemalagou ophiolite in the western segment of the Bangong Co-Nujiang ophiolite belt, Tibet-with a discussion of the age of the Bangong Co-Nujiang ophiolite belt[J]. Geology in China, 2004, 31(3): 262~268. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200403003.htm
[75]	黄强太, 李建峰, 夏斌, 等.西藏班公湖-怒江缝合带中段江错蛇绿岩岩石学、地球化学、年代学及地质意义[J].地球科学—中国地质大学学报, 2015, 40(1): 34~48. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201501003.htm HUANG Qiangtai, LI Jianfeng, XIA Bin, et al. Petrology, geochemistry, chronology and geological significance of Jiang Tso ophiolite in middle segment of Bangonghu-Nujiang Suture zone, Tibet[J]. Earth Science-Journal of China University of Geosciences, 2015, 40(1): 34~48. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201501003.htm
[76]	Li H L, Zhang Y Q, Zhang C H, et al. Middle Jurassic syn-kinematic magmatism, anatexis and metamorphism in the Zheduo-Gonggar massif, implication for the deformation of the Xianshuihe fault zone, East Tibet[J]. Journal of Asian Earth Sciences, 2015, 107: 35~52. doi: 10.1016/j.jseaes.2015.03.038
[77]	Yuan Y J, Yin Z X, Liu W L, et al. Tectonic evolution of the Meso-Tethys in the western segment of Bangonghu-Nujiang suture zone: insights from geochemistry and geochronology of the Lagkor Tso ophiolite[J]. Acta Geologica Sinica (English Edition), 2015, 89(2): 369~388. doi: 10.1111/1755-6724.12436
[78]	董瀚, 苟国宁, 齐玥, 等.拉萨地块北缘早白垩世晚期地壳生长:来自改则亚多~106 Ma侵入岩的证据[J].大地构造与成矿学, 2016, 40(6): 1226~1238. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201606010.htm DONG Han, GOU Guoning, QI Yue, et al. Late Early cretaceous crustal growth in northern Lhasa block: evidence from ca. 106 Ma intrusive rocks in the Yaduo Area, Gerze county[J]. Geotectonica et Metallogenia, 2016, 40(6): 1226~1238. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201606010.htm
[79]	Murphy M A, Yin A, Harrison T M, et al. Did the indo-Asian collision alone create the Tibetan plateau?[J]. Geology, 1997, 25(8): 719~722. doi: 10.1130/0091-7613(1997)025<0719:DTIACA>2.3.CO;2
[80]	许荣科, 郑有业, 赵平甲, 等.西藏东巧北尕苍见岛弧的厘定及地质意义[J].中国地质, 2007, 34(5): 768~777. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200705002.htm XU Rongke, ZHENG Youye, ZHAO Pingjia, et al. Definition and geological significance of the Gacangjian volcanic arc north of Dongqiao, Tibet[J]. Geology in China, 2007, 34(5): 768~777. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200705002.htm