Application of OPS to Division of Tectonic-Strata Regions in Orogenic Belts
-
摘要: 自元古宙以来地球表面洋陆位置不断变化，洋的面积总比陆地面积大.分布于大陆造山带区的古缝合带是古大洋或古大陆边缘小洋盆消亡的残迹，是洋板块地层研究的主要对象.针对占中国陆域3/5面积的造山带洋板块地层分布区，提出一级（称“构造-地层大区”）和二级（称“构造-地层区”）构造-地层的区划准则.将洋板块地层分为对接带型和叠接带型两大类，分别对应于构造-地层大区和构造地层区.对接带型以含N-MORB型蛇绿岩为标志，是古大洋消亡的残迹；叠接带型以含SSZ型蛇绿岩为标志，是古大陆边缘小洋盆消亡的残迹.对接带内的洋脊（蛇绿岩）、洋岛海山、洋内弧等亚型建造因卷入俯冲带内被肢解，多数呈残缺不全的岩块包裹在强烈构造剪切形变的远洋细碎屑和海沟浊积岩建造（称为基质）之中，呈俯冲增生杂岩带展布，对应于构造-地层区；对某些形体巨大的亚类（巨大的洋岛海山、裂离地块、大面积的深海平原硅质岩等建造），进入海沟俯冲带内很难被完全肢解，呈逆（仰）冲地质体大面积分布，可归为构造-地层区.叠接带型可进一步划分出与弧前盆地、火山弧（含弧间和弧背盆地建造）和弧后盆地等二级构造-地层区划单元.Abstract: The paleo-position of ocean and continent has been changing on the earth since the Proterozoic and the oceanic acreage is always larger than the continent's. A paleo-suture zone represents the remant of a paleo-ocean and is considered as the focus on the research of Ocean Plate Stratigraphy (OPS). The paper is aiming to propose the regulations for the division of tectonic-strata super regions and regions in the orogenic belts,based on OPS in China. The OPS can be subdivided into two types in China,N-MORB-type and SSZ-type,respectively corresponding to the main suture zone and subordinate suture zone. The current position for a main suture zone is roughly considered as the position of a tectonic-strata super region. A main suture zone was formed during the disappearing of a large ocean,marked by N-MORB-type ophiolite. The current position for a subordinate suture zone is roughly corresponding to the position of a tectonic-strata region. A subordinate suture zone was formed during the disappearing of a small ocean,marked by SSZ-type ophiolite and developed along the edge of a block or continent. The geological units in a main suture zone mainly consist of ophiolite,seamount and intra-oceanic arc. The positions for these units could be also generally considered as the positions of tectonic-strata regions. The geological units in a subordinate suture zone mainly consist of back-arc,inter-arc and retro-arc and for-arc basins. The positions for these units are basically considered as the positions of tectonic-strata subregions.
-
图 1 中国陆域克拉通、造山带和混杂岩分布
据张克信等(2015a, 2015b, 2016)修改; 该图基于据自然资源部1:1 600万中国地图, 审图号为GS（2016）2927号制作，底图无修改
Fig. 1. The distribution diagram of cratons, orogenic belts and mélange in China
图 2 洋板块地层形成的构造环境、分类示意图
据Isozaki et al.（1990）; Wakita（2012）; Kusky et al.（2013）；张克信等（2016）修改
Fig. 2. A model showing the tectonic settings, the formation-process and the division of OPS
图 3 中国北方中亚造山带蛇绿岩与测年值分布图
(1)倪康等(2013)；(2)王玉往等(2011)；(3)Wang et al.(2012)；(4)沈晓明等(2013)；(5)张海祥等(2003)；(6)张越等(2012)；(7)褚方等(2013)；(8)吴波等(2006)；(9)肖文交等(2006)；(10)张越(2012)；(11)Zeng et al.(2014)；(12)Wang et al.(2003)；(13)张元元等(2010)；(14)赵磊等(2013)；(15)朱永峰和徐新(2006)；(16)翁凯等(2016)；(17)杨高学等(2013)；(18)赵文平等(2012)；(19)魏荣珠(2010)；(20)Jian et al.(2008)；(21)辜平阳等(2009)；(22)Yang et al.(2012)；(23)马中平(2007)；(24)李纲等(2014)；(25)李超等(2013)；(26)徐学义等(2005)；(27)徐学义等(2006)；(28)徐学义等(2003)；(29)董书云(2010)；(30)王莹等(2012)(31)郝杰等(1993)；(32)龙灵利等(2006)；(33)马中平等(2007)；(34)杨经绥等(2011)；(35)黄岗等(2011)；(36)高俊等(2009)；(37)李文铅等(2008)；(38)任秉琛和郭召杰(2001)；(39)张元元等(2008)；(40)王国强等(2014)；(41)武鹏等(2012)；(42)代文军等(2008)；(43)周国庆等(2000)；(44)侯青叶等(2012)；(45)胡新茁等(2015)；(46)王行军(2012)；(47)Zhang et al.(2015)；(48)李尚林等(2012)；(49)Jian et al.(2010)；(50)Chen et al.(2011)；(51)徐备等(2001)；(52)刘敦一等(2003)；(53)Jian et al.(2008)；(54)Zhang et al.(2015)；(55)鲍庆中等(2007)；(56)包志伟等(1994)；(57)Jian et al.(2012)；(58)贺秋利(2014)；(59)佘宏全等(2012)；(60)李旭平等(2010)；(61)田东江(2007)；(62)张国宾(2014)；(63)李旭平等(2009)；(64)周建波等(2009)；(65)颉颃强等(2008)；(66)唐克东等(2007);据张克信等(2015a, 2015b, 2016)修改; 年龄单位：Ma
Fig. 3. Spatial distribution of ophiolites and the related isotope ages in the Central Asian orogenic belts in China
图 4 新疆青河县玛因鄂博蛇绿混杂岩带中的主要岩石类型(该图的地理位置参见图 3)
Fig. 4. Different types of rocks in the ophiolite mélanges in Mayin OBO, Qinghe County, Xinjiang, China
图 5 甘肃北山造山带马鬃山贾不泉口子地区增生杂岩带岩石组合分布特征
Fig. 5. Spatial distribution of different types of rocks in mélanges at Jiabuquankouzi of Mazongshan in the Beishan orogenic belt, Gansu, China
图 7 新疆卡拉麦利蛇绿混杂岩带内的“辉长岩-玄武岩-紫红色硅质岩” OPS序列及其对成生环境的解释(该图的地理位置参见图 3)
Fig. 7. The OPS sequence of gabbro-basalt-siliceous rocks of the ophiolite mélanges at Cara Mali, Xinjiang, China
图 8 中国二叠纪构造-地层区划图
该图基于自然资源部1:1 600万中国地图, 审图号为GS（2016）2927号标准地图制作，地图无修改
Fig. 8. Division of tectonic-strata regions of the Permian in China
图 9 内蒙索仑山蛇绿混杂岩带物质组成
该图的地理位置参见图 3;其中岩石野外照片为张克信拍照，放射虫化石李钢柱等(2017)
Fig. 9. Different types of rocks in the Solonker ophiolite mélanges, Inner Mongolia
表 1 造山带洋块地层类型划分
Table 1. The division of OPS in orogenic belt
洋板块地层类型 模式化的原始沉积-岩浆建造序列(不同类型的洋板块地层序列) (据Wakita, 2012和 Kusky et al., 2013 补充)进入俯冲增生杂岩带被肢解 混入增生杂岩带的不同环境不同类型蛇绿岩形成模式(Pearce, 2014a, 2014b) 型 亚型 (被肢解的)典型岩块 主要基质 对接带型 洋脊海岭亚型 辉长岩→玄武岩→灰岩(可缺失) 辉长岩、玄武岩、灰岩 页岩浊积岩 深海平原 亚型1 辉长岩→玄武岩→灰岩(可缺失)→硅质岩 硅质岩 亚型2 辉长岩→玄武岩→灰岩(可缺失) →硅质岩→页岩 硅质岩 海沟 亚型1 辉长岩→玄武岩→灰岩(可缺失)→硅质岩→页岩→浊积岩(富含陆缘碎屑) 杂砾岩（浊积扇扇根杂砾岩楔） 亚型2 辉长岩→玄武岩→灰岩(可缺失)→硅质岩→页岩→→玄武岩→高镁安山岩→浊积岩→凝灰质浊积岩（无陆缘碎屑） 玄武岩高镁安山岩 洋中脊亚型 橄榄岩→辉长岩→席状辉绿岩墙→玄武岩 橄榄岩、辉长岩辉绿岩、玄武岩 页岩
浊积岩蛇纹岩洋内弧亚型 橄榄岩→辉长岩→席状辉绿岩墙→玄武岩→玻安岩→高镁安山岩 玄武岩、玻安岩高镁安山岩 洋岛海山亚型 玄武岩→灰岩 玄武岩、灰岩 页岩
粉砂岩浊积岩裂离地块亚型 变质岩→陆源碎屑岩→灰岩 变质岩、砂砾岩、灰岩 高压-超高压带（岩片）亚型 高压-超高压变质岩组合 兰闪片岩、榴闪岩、榴辉岩、高压麻粒岩等 云母片岩、钙泥质板岩、千枚岩、蛇纹岩 叠接
带型弧前盆地亚型 火山岩→（灰岩）→浊积岩→页岩 （中基性、酸性）火山岩、灰岩（弧前构造高地上的孤立台地） 页岩
浊积岩火山岛弧亚型 火山岩→（灰岩）→凝灰质沉积岩 （中基性、酸性）火山岩、灰岩（座落在火山岩高地上的盖帽灰岩台地） 页岩
浊积岩弧间盆地亚型 玄武岩→火山岩→浊积岩→页岩→火山岩→浊积岩 页岩
浊积岩
蛇纹岩弧后盆地亚型 超基性岩→辉长岩→玄武岩→灰岩→硅质岩→页岩→浊积岩→火山岩 超基性岩、辉长岩、玄武岩、灰岩、硅质岩、（中酸性）火山岩 
下载: 导出CSV
表 2 对接带与叠接带的区别(据张克信等, 2018修改)
Table 2. The differentiation between main suture zone and subordinate suture zone(modified from Zhang et al., 2018)
序号 对接带(main suture zone) 叠接带(subordinate suture zone) 都发育有蛇绿岩带、弧岩浆岩带、双变质带与俯冲增生杂岩带，并行分布 1 缝合带所含蛇绿岩以N⁃MORB型为主，是大洋消亡的残迹 缝合带所含蛇绿岩以SSZ型为主，是弧后、弧间小洋盆消亡的残迹 2 蛇绿岩时代分布大于2亿年，通常为2~8亿年 蛇绿岩时代分布小于2亿年 3 缝合带呈狭带状分布数千千米 缝合带呈狭带状分布一般仅数百千米 4 远洋沉积(无陆源碎屑混入的极细粒的硅、灰、锰、炭、凝灰质)发育好 远洋沉积(无陆源碎屑混入的极细粒的硅、灰、锰、炭、凝灰质)发育差 5 缝合带两侧无统一的基底，两侧的陆块基底与盖层组成长期不同 两侧有统一的基底，分隔的两个大陆边缘沉积序列短期内不同 6 分隔的陆块古地磁位置长期各自处于不同位置，并相距远 分隔的陆块古地磁位置相距不大 7 是生物大区(底栖类)的长期分界线，后期混生 不是生物大区(底栖类)分界线
下载: 导出CSV
-
[1] Bao, Q. Z., Zhang, C. J., Wu, Z. L., et al., 2007. SHRIMP U-Pb Zircon Geochronology of a Carboniferous Quartz-Diorite in Baiyingaole Area, Inner Mongolia and Its Implications. Journal of Jilin University(Earth Science Edition), 37(1):15-23(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb200701003 [2] Bao, Z. W., Chen, S. H., Zhang, Z. T., 1994. Study on Ree and Sm-Nd Isotopes of Hegenshan Ophiolite, Inner Mongolia. Geochimica, 23(4):339-349(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX404.003.htm [3] Bu, J. J., He, W. H., Zhang, K. X., et al., 2019. Evolution of the Paleo-Asian Ocean:Evidence from Paleontology and Stratigraphy. Earth Science, 45(3):711-727(in Chinese with English abstract). [4] Cawood, P. A., Kröner, A., Collins, W. J., et al., 2009. Accretionary Orogens through Earth History. Geological Society, London, Special Publications, 318(1):1-36. https://doi.org/10.1144/sp318.1 [5] Chen, C., Zhang, Z. C., Guo, Z. J., et al., 2011. Geochronology, Geochemistry, and Its Geological Significance of the Permian Mandula Mafic Rocks in Damaoqi, Inner Mongolia. Science China Earth Sciences, 55(1):39-52. https://doi.org/10.1007/s11430-011-4277-z [6] Dai, W. J., Tan, S., 2008. The Properties and Tectonic Significance of Ophiolite and Related Volcanic Rocks in Gansu Beishan Yemajie-Mazongshan Structural Belt. Xinjiang Geology, 26(3):305-313(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-xjdi200803023.htm [7] Dong, S. Y., 2010. Studies of Petrology and Geochemistry on Basite in Ophiolite of Kokshal District, Wstsouth Tianshan Mountains(Dissertation). China University of Geosciences, Beijing, 1-77(in Chinese with English abstract). [8] Gao, J., Qian, Q., Long, L. L., et al., 2009. Accretionary Orogenic Process of Western Tianshan, China. Geological Bulletin of China, 28(12):1804-1816(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD200912014.htm [9] Gong, Y. M., Zhang, K. X., 2016. Basics and Frontiers in Stratigraphy. China University of Geosciences Press, Wuhan, 1-465(in Chinese). [10] Gu, P. Y., Li, Y. J., Zhang, B., et al., 2009. LA-ICP-MS Zircon U-Pb Dating of Gabbro in the Darbut Ophiolite, Western Junggar, China. Acta Petrologica Sinica, 25(6):1364-1372(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200906008 [11] Hao, J., Liu, X. H., 1993. Ophiolite Mélange Time and Tectonic Evolutional Model in South Tianshan Area. Scientia Geologica Sinica, 28(1):93-95(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX199301011.htm [12] He, Q. L., 2012. Geological Studies of Gabbro in Ophiolitic Mélange Belt in West Ujimqin Banner, Inner Mongolia(Dissertation). Shijiazhuang University of Economics, Shijiazhuang, 1-82(in Chinese with English abstract). [13] Hu, X. Z., Zhao, G. C., Hu, X. Y., et al., 2015. Geological Characteristics, Formation Epoch and Geotectonic Significance of the Yueyashan Ophiolitic Tectonic Mélange in Beishan Area, Inner Mongolia. Geological Bulletin of China, 34(2/3):425-436(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD2015Z1019.htm [14] Huang, G., Zhang, Z. W., Dong, Z. H., et al., 2011. Zircon LA-ICP-MS U-Pb Age of Plagiogranite from Tonghuashan Ophiolite in Southern Tianshan Mountains and Its Geological Implications. Geology in China, 38(1):94-102(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201101010 [15] Huang, T. K., Jiang, C. F., 1962. Preliminary Investigation on the Evolution of the Earth's Crust from the Point of View of Polycyclic Tectonic Movements. Acta Geologica Sinica, 42(2):105-152(in Chinese with English abstract). http://cn.bing.com/academic/profile?id=a93eaa5e739f9ebce8556c259a0053d8&encoded=0&v=paper_preview&mkt=zh-cn [16] Hou, Q. Y., Wang, Z., Liu, J. B., et al., 2012. Geochemistry Characteristics and SHRIMP Dating of Yueyashan Ophiolite in Beishan Orogen. Geoscience, 26(5):1008-1018(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz201205022 [17] Isozaki, Y., 1997. Contrasting Two Types of Orogen in Permo-Triassic Japan:Accretionary Versus Collisional. The Island Arc, 6(1):2-24. https://doi.org/10.1111/j.1440-1738.1997.tb00038.x [18] Isozaki, Y., Maruyama, S., Furuoka, F., 1990. Accreted Oceanic Materials in Japan. Tectonophysics, 181(1/2/3/4):179-205. https://doi.org/10.1016/0040-1951(90)90016-2 [19] Jian, P., Kröner, A., Windley, B. F., et al., 2012. Carboniferous and Cretaceous Mafic-Ultramafic Massifs in Inner Mongolia (China):A SHRIMP Zircon and Geochemical Study of the Previously Presumed Integral "Hegenshan Ophiolite". Lithos, 142-143:48-66. https://doi.org/10.1016/j.lithos.2012.03.007 [20] Jian, P., Liu, D. Y., Kröner, A., et al., 2008. Time Scale of an Early to Mid-Paleozoic Orogenic Cycle of the Long-Lived Central Asian Orogenic Belt, Inner Mongolia of China:Implications for Continental Growth. Lithos, 101(3/4):233-259. https://doi.org/10.1016/j.lithos.2007.07.005 [21] Jian, P., Liu, D. Y., Kröner, A., et al., 2010. Evolution of a Permian Intraoceanic Arc-Trench System in the Solonker Suture Zone, Central Asian Orogenic Belt, China and Mongolia. Lithos, 118(1/2):169-190. https://doi.org/10.1016/j.lithos.2010.04.014 [22] Kusky, T.M., Li, J.H., Tucker, R.T., 2001. The Archean Dongwanzi Ophiolite Complex, North China Craton:2.505-Billion-Year-Old Oceanic Crust and Mantle. Science, 292(5519):1142-1145. https://doi.org/10.1126/science.1059426 [23] Kusky, T. M., Windley, B. F., Safonova, I., et al., 2013. Recognition of Ocean Plate Stratigraphy in Accretionary Orogens through Earth History:A Record of 3.8 Billion Years of Sea Floor Spreading, Subduction, and Accretion. Gondwana Research, 24(2):501-547. https://doi.org/10.1016/j.gr.2013.01.004 [24] Kusky, T. M., Zhai, M. G., 2012. The Neoarchean Ophiolite in the North China Craton:Early Precambrian Plate Tectonics and Scientific Debate. Journal of Earth Science, 23(3):277-284. https://doi.org/10.1007/s12583-012-0253-6 [25] Kuzmichev, A.B., 2015. Neoproterozoic Accretion of the Tuva-Mongolian Massif, One of the Precambrian Terranes in the Central Asian Orogenic Belt. In: Kroner, K., ed., The Central Asian Orogenic Belt. Geology, Evolution, Tectonics, and Models. Borntraeger Science Publishers, Stuttgart, 66-92. [26] Li, C., Xiao, W. J., Han, C. M., et al., 2013. SHRIMP U-Pb Dating and Its Implications of Plagiogranite in Kuitunhe Ophiolite, North Tianshan, Xinjiang. Chinese Journal of Geology, 48(3):815-826(in Chinese with English abstract). [27] Li, G., Yang, B., Liang, E.Y., et al., 2014. SHRIMP Zircon U-Pb Age and Geochemical Characteristics of Mafic Rock from Liushugou-Darbut in Western Junggar, Xinjiang, China. Geology and Mineral Resources of South China, 30(3):194-205(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hndzykc201403002 [28] Li, G. Z., Wang, Y. J., Li, C. Y., et al., 2017. Discovery of Early Permian Radiolarian Fauna in the Solon Obo Ophiolite Belt, Inner Mongolia and Its Geological Significance. Chin. Sci. Bull., 62(5):400-406 (in Chinese). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb201705007 [29] Li, J. H., Wang, H. H., Li, W. B., et al., 2014. Discussion on Global Tectonics Evolution from Plate Reconstruction in Phanerozoic. Acta Petrolei Sinica, 35(2):207-218(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB201402001.htm [30] Li, S. L., Wang, X. L., Duan, J. M., et al., 2012. Findings and Its Geological Significance of the Upper Devonian Ophiolite in Hujierte Area, Damao County, Inner Mongolia, China. Earth Science, 37(1):18-23(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201201002 [31] Li, W. Q., Ma, H. D., Wang, R., et al., 2008. SHRIMP Dating and Nd-Sr Isotopic Tracing of Kangguertage Ophiolite in Eastern Tianshan, Xinjiang. Acta Petrologica Sinica, 24(4):773-780(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200804016 [32] Li, X. P., Jiao, L. X., Zheng, Q. D., et al., 2009. U-Pb Zircon Dating of the Heilongjiang Complex at Huanan, Heilongjiang Province. Acta Petrologica Sinica, 25(8):1909-1916(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200908015 [33] Li, X. P., Kong, F. M., Zheng, Q. D., et al., 2010. Geochronological Study on the Heilongjiang Complex at Luobei Area, Heilongjiang Province. Acta Petrologica Sinica, 26(7):2015-2024(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201007005 [34] Li, Y. C., Zhang, K. X., He, W. H., et al., 2018. Division of Tectonic-Strata Superregions in China. China Geology, 1(2):236-256. https://doi.org/10.31035/cg2018028 [35] Liu, D. Y., Jian, P., Zhang, Q., et al., 2003. SHRIMP Dating of Adakties in the Tulingkai Ophiolite, Inner Mongolia:Evidence for the Early Paleozoic Subduction. Acta Geologica Sinica, 77(3):317-329(in Chinese with English abstract). [36] Long, L. L., Gao, J., Xiong, X. M., et al., 2006. The Geochemical Characteristics and the Age of the Kule Lake Ophiolite in the Southern Tianshan. Acta Petrologica Sinica, 22(1):65-73(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200601007 [37] Lu, S.N., Hao, G.J., Wang, H.C., et al., 2015.The Instructions of Metamorphite Tectonic Map in China(1: 2 500 000). Geological Publishing House, Beijing (in Chinese). [38] Lu, S.N., Hao, G.J., Wang, H.C., et al., 2017. Metamorphite Tectonic of China. Geological Publishing House, Beijing (in Chinese). [39] Ma, Z. P., 2007. Research on Ophiolites and Paleozoic Ocean in Tianshan Area(Dissertation). Northwest University, Xi'an, 1-129(in Chinese with English abstract). [40] Ma, Z. P., Xiao, L. Q., Xu, X. Y., et al., 2007. Dating for Zircons of Gabbro from Kulehu Ophiolite, Southern Tianshan and Its Geological Implication. Journal of Northwest University(Natural Science Edition), 37(1):107-110(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdxxb200701027 [41] Ni, K., Lei, Y. X., Hu, X. J., et al., 2013. Zircon U-Pb Age and Its Implications of the Kekesentao Ophiolite in the South of the Erqis Suture Zone in Xinjiang. Northwestern Geology, 46(3):64-69(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz201303004 [42] Pan, G. T., Lu, S. N., Xiao, Q. H., et al., 2016. Divisiong of Tectonic Stages and Tectonic Evolution in China. Earth Science Frontiers, 23(6):001-023 (in Chinese with English abstract). https://www.researchgate.net/publication/316514059_Division_of_tectonic_stages_and_tectonic_evolution_in_China [43] Pan, G. T., Xiao, Q. H., Yin, F. G., et al., 2015. The Instructions of Tectonic Map in China(1: 2 500 000). Geological Publishing House, Beijing(in Chinese). [44] Pan, G. T., Xiao, Q. H., Yin, F. G., et al., 2017. Tectonic of China. Geological Publishing House, Beijing(in Chinese). [45] Pan, G. T., Xiao, Q. H., Zhang, K. X., et al., 2019. Recognition of the Oceanic Subduction-Accretion Zones from the Orogenic Belt in Continents and Its Important Scientific Significance. Earth Science, 44(5):1544-1564(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201905012 [46] Pearce, J. A., 2014a. Immobile Element Fingerprinting of Ophiolites. Elements, 10(2):101-108. https://doi.org/10.2113/gselements.10.2.101 [47] Pearce, J. A., 2014b. Geochemical Fingerprinting of the Earth's Oldest Rocks. Geology, 42(2):175-176. https://doi.org/10.1130/focus022014.1 [48] Ren, B. C., He, S. P., Yao, W. G., et al., 2001. Rb-Sr Isotope Age of Niuquanzi Ophiolite and Its Tectonic Significance in Beishan District, Gansu. Northwestern Geology, 34(2):21-27(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz200102004 [49] Ren, J. S., Hao, J., Xiao, L. W., 2002. Tectonic Research of China:Review and Prospect. Geological Review, 48(2):113-124(in Chinese with English abstract). [50] She, H. Q., Li, J. W., Xiang, A. P., et al., 2012. U-Pb Ages of the Zircons from Primary Rocks in Middle-Northern Daxinganling and Its Implications to Geotectonic Evolution. Acta Petrologica Sinica, 28(2):571-594(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201202018 [51] Shen, X. M., Zhang, H. X., Ma, L., 2013. Zircon U-Pb and Amphibole 40Ar/39Ar Geochronology of Kuerti Ophiolite in Altay and Geological Implication. Journal of Guilin University of Technology, 33(3):394-405(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=glgxy201303002 [52] Shmelev, V. R., Arai, S., Tamura, A., 2019. Heterogeneity of Mantle Peridotites from the Polar Urals (Russia):Evidence from New LA-ICP-MS Data. Journal of Earth Science, 30(3):431-450. https://doi.org/10.1007/s12583-019-1224-y [53] Tang, K. D., Zhao, A. L., 2007. New Evidence of Palaeozoic Stratigraphy in the Kaishantun Area, Yanbian, Jilin. Journal of Stratigraphy, 31(2):141-150(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dcxzz200702006 [54] Tian, D. J., 2007. The Geological-Geochemical Composition and Evolution of the Wandashan Orogenic Belt(Dissertation). Jilin University, Changchun, 1-62(in Chinese with English abstract). [55] Wakita, K., 2012. Mappable Features of Mélanges Derived from Ocean Plate Stratigraphy in the Jurassic Accretionary Complexes of Mino and Chichibu Terranes in Southwest Japan. Tectonophysics, 568-569: 74-85. https://doi.org/10.1016/j.tecto.2011.10.019 [56] Wakita, K., Metcalfe, I., 2005. Ocean Plate Stratigraphy in East and Southeast Asia. Journal of Asian Earth Sciences, 24(6):679-702. https://doi.org/10.1016/j.jseaes.2004.04.004 [57] Wang, G. Q., Li, X. M., Xu, X. Y., et al., 2014. Zircon U-Pb Chronological Study of the Hongshishan Ophiolite in the Beishan Area and Their Tectonic Significance. Acta Petrologica Sinica, 30(6):1685-1694(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201406011.htm [58] Wang, H. Z., 1978. Discussion on Stratigraphic Distribution of China. Acta Stratigraphica Sinica, 2(2):81-104(in Chinese). [59] Wang, H. Z., 1985. Atlas of the Palaeogeography of China. Map Press, Beijing, 1-139(in Chinese). [60] Wang, X. F., Stouge, S., Chen, X. H., et al., 2005. Advances on the Potential GSSP for the Base of Middle Ordovician Series:Huanghuachang Section. Journal of Stratigraphy, 29(S1):467-489+649-650+0(in Chinese with English abstract). [61] Wang, L. J., Zhang, K. X., Lin, S. F., et al., 2019. Turbidite Record of a Middle Neoproterozoic Active Continental Margin in the West Cathaysia Terrane, South China:Implications for the Relationships between the Yangtze and Cathaysia Blocks and Their Positions in Rodinia. Precambrian Research, 337:105457. https://doi.org/10.1016/j.precamres.2019.105457 [62] Wang, X. J., 2012. The Geochemical Characters and Its Tectonic Implication of Ophiolites in Alax Area, Inner Mongolia(Dissertation). China University of Geosciences, Beijing(in Chinese with English abstract). [63] Wang, Y., Huang, H., Zhang, D. Y., et al., 2012. SHRIMP Dating of the Qiqijianake Ophiolitic Mélange in the Kokshal Region, Southwestern Tianshan and Its Tectonic Implications. Acta Petrologica Sinica, 28 (4):1273-1281(in Chinese with English abstract). [64] Wang, Y. W., Wang, J. B., Wang, L. J., et al., 2011. Discovery of Tuerkubantao Ophiolitic Mélange in Xinjiang and Its Significance. Earth Sciences Frontiers, 18(3):151-165(in Chinese with English abstract). http://www.researchgate.net/publication/307632040_Discovery_of_Tuerkubantao_Ophiolitic_Melange_in_Xinjiang_and_Its_Significance [65] Wang, Y. W., Wang, J. B., Wang, L. J., et al., 2012. The Tuerkubantao Ophiolite Mélange in Xinjiang, NW China:New Evidence for the Erqis Suture Zone. Geoscience Frontiers, 3(5):587-602. https://doi.org/10.1016/j.gsf.2012.02.002 [66] Wang, Z. H., Sun, S., Li, J. L., et al., 2003. Paleozoic Tectonic Evolution of the Northern Xinjiang, China:Geochemical and Geochronological Constraints from the Ophiolites. Tectonics, 22(2):9-15. https://doi.org/10.1029/2002tc001396 [67] Weng, K., Xu, X. Y., Ma, Z. P., et al., 2016. The Geochemistry and Chronology Characteristics and the Geological Significance of Ultramafic Rock in Mayile Ophiolite, West Junggar, Xinjiang. Acta Petrologica Sinica, 32(5):1420-1436(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201605012 [68] Wei, R. Z., 2010. The Mayileshan Pillow Lavas (Western Junggar, Xinjiang) and Their Tectonic Implications:Constraints from the Geological and Geochemical Characteristics and Rb-Sr Isochron Ages. Xinjiang Geology, 28(3):229-235(in Chinese with English abstract). [69] Wu, B., He, G. Q., Wu, T. R., et al., 2006. Discovery of the Buergen Ophiolitic Mélange Belt in Xinjiang and Its Tectonic Significance. Geology in China, 33(3):476-486(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200603004 [70] Wu, P., Wang, G. Q., Li, X. M., et al., 2012. The Age of Niujuanzi Ophiolite in Beishan Area of Gansu Province and Its Geological Significance. Geological Bulletin of China, 31(12):2032-2037(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201212012 [71] Xiao, W. J., Windley., B. F., Yan, Q. R., et al., 2006. SHRIMP Zircon Age of the Aermantai Ophiolite in the North Xinjiang Area, China and Its Tectonic Implications. Acta Geologica Sinica, 80(1):32-37(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200601004 [72] Xie, H. Q., Zhang, F. Q., Miao, L. C., et al., 2008. Zircon SHRIMP U-Pb Dating of the Amphibolite from "Heilongjiang Group" and the Granite in Mudanjiang Area, NE China, and Its Geological Significance. Acta Petrologica Sinica, 24(6):1237-1250(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200806007 [73] Xu, B., Charvet, J., Zhang, F. Q., 2001. Primary Study on Petrology and Geochronology of Blueschists in Sunitezuoqi, Northern Inner Mongolia. Chinese Journal of Geology, 36(4):424-434(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZKX200104005.htm [74] Xu, X. Y., Ma, Z. P., Xia, L. Q., et al., 2003. The Discovery of P-MORB in Jigen Area of Southwest Tianshan Mountains and Its Tectonic Implications. Acta Petrologica et Mineralogica, 22(3):245-253(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz200303006 [75] Xu, X. Y., Ma, Z. P., Xia, L. Q., et al., 2005. SHRIMP Dating of Plagiogranite from Bayingou Ophiolite in the Northern Tianshan Mountains. Geological Review, 51(5):523-527(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200505006 [76] Xu, X. Y., Xia, L. Q., Ma, Z. P., et al., 2006. SHRIMP Zircon U-Pb Geochronology of the Plagiogranites from Bayingou Ophiolite in North Tianshan Mountains and the Petrogenesis of the Ophiolite. Acta Petrologica Sinica, 22(1):83-94(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200601009 [77] Yang, G. X., Li, Y. J., Gu, P. Y., et al., 2012. Geochronological and Geochemical Study of the Darbut Ophiolitic Complex in the West Junggar (NW China):Implications for Petrogenesis and Tectonic Evolution. Gondwana Research, 21(4):1037-1049. https://doi.org/10.1016/j.gr.2011.07.029 [78] Yang, G. X., Li, Y. J., Yang, B. K., et al., 2013. Zircon U-Pb Geochronology and Geochemistry of the Mayile Ophiolitic Mélange in West Junggar and Implications for Source Nature. Acta Petrologica Sinica, 29(1):303-316(in Chinese with English abstract). [79] Yang, J. S., Xu, X. Z., Li, T. F., et al., 2011. U-Pb Ages of Zircons from Ophiolite and Related Rocks in the Kumishi Region at the Southern Margin of Middle Tianshan, Xinjiang:Evidence of Early Paleozoic Oceanic Basin. Acta Petrologica Sinica, 27(1):77-95(in Chinese with English abstract). [80] Yin, H. F., Zhang, K. X., Chen, N. S., et al., 2003. The People's Republic of China, Regional Geological Report, Donggi Conag Hu Map(1: 2 500 000). China University of Geosciences Press, Wuhan, 1-457(in Chinese). [81] Zamoras, L. R., Matsuoka, A., 2001. Malampaya Sound Group:A Jurassic-Early Cretaceous Accretionary Complex in Busuanga Island, North Palawan Block (Philippines). The Journal of the Geological Society of Japan, 107(5):316-336. https://doi.org/10.5575/geosoc.107.316 [82] Zeng, L. J., Niu, H. C., Bao, Z. W., et al., 2014. Petrogenesis and Tectonic Significance of the Plagiogranites in the Zhaheba Ophiolite, Eastern Junggar Orogen, Xinjiang, China. Journal of Asian Earth Sciences, 113:137-150. https://doi.org/10.1016/j.jseaes.2014.09.031 [83] Zhang, G. B., 2014. Study on Metallogenic System of Wandashan Massif, Eastern Heilongjiang Province(Dissertation). Jilin University, Changchun(in Chinese with English abstract). [84] Zhang, H. X., Niu, H. C., Terada, K., et al., 2003. SHRIMP Chronology of Plagiogranite from Kuerti Ophiolite in Altay, Northern Xinjiang. Chinese Science Bulletin, 48(12):1350-1354(in Chinese). [85] Zhang, K. X., Yin, H. F., Zhu, Y. H., et al., 2001. Geological Survey Theory, Method and Practice of Mélange Zone in Orogenic Belt. China University of Geosciences Press, Wuhan(in Chinese). [86] Zhang, K. X., Yin, H. F., Zhu, Y. H., et al., 2003. Smith Strata and Non-Smith Strata. Earth Science, 28(4):361-369(in Chinese with English abstract). http://cn.bing.com/academic/profile?id=91cc77a821b57f881455a04d993aaccb&encoded=0&v=paper_preview&mkt=zh-cn [87] Zhang, K. X., He, W. H., Xu, Y. D., et al., 2015a. The Instructions of Sedimentary Tectonic Map in China(1: 2 500 000). Geological Publishing House, Beijing, 1-127(in Chinese). [88] Zhang, K. X., He, W. H., Xu, Y. D., et al., 2016. Palaeogeographic Distribution and Tectonic Evolution of OPS in China. Earth Science Frontiers, 23(6):24-30(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201606002 [89] Zhang, K. X., He, W. H., Luo, M. S., et al., 2017. The Sedimentary Construction and Tectonic of China. Geological Publishing House, Beijing, 1-604(in Chinese). [90] Zhang, K. X., He, W. H., Xu, Y. D., et al., 2018. Explanatory Note of the Sedimentary Tectonic Map of China (1: 2 500 000). Geological Publishing House, Beijing, 1-38. [91] Zhang, K. X., Luo, M. S., Xu, Y. D., et al., 2015. Sedimentary Tectonic Map of China(1: 250 000). Geological Publishing House, Beijing, 1-127(in Chinese). [92] Zhang, K. X., Pan, G. T., He, W. H., et al., 2015b. New Division of Tectonic-Strata Superregion in China. Earth Science, 40(2):206-233(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201502004 [93] Zhang, K. X., Xu, Y. D., He, W. H., et al., 2018. Oceanic and Continental Blocks Distribution during Neoproterozoic Early Qingbaikouan Period (1 000-820 Ma) in China. Earth Science, 43(11):3837-3851(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201811004 [94] Zhang, Y., 2012. The Study about the Composition, the Structure, the Emplacement Mechanism and Significance of Tectonic of the Armantai Ophiolite Mélange, East Junggar, Xinjiang, China(Dissertation). Chang'an University, Xi'an(in Chinese with English abstract). [95] Zhang, Y., Xu, X. Y., Chen, J. L., et al., 2012. Geological Characteristics and LA-ICP-MS Zircon U-Pb Age of Mayinebo Ophiolite in Altay Orogenic Belt. Geological Bulletin of China, 31(6):834-842(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201206002 [96] Zhang, Y. Y., Guo, Z. J., 2008. Accurate Constraint on Formation and Emplacement Age of Hongliuhe Ophiolite, Boundary Region between Xinjiang and Gansu Provinces and Its Tectonic Implications. Acta Petrologica Sinica, 24(4):803-809(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200804019 [97] Zhang, Y. Y., Guo, Z. J., 2010. New Constraints on Formation Ages of Ophiolites in Northern Junggar and Comparative Study on Their Connection. Acta Petrologica Sinica, 26(2):421-430(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201002006 [98] Zhang, Z. C., Li, K., Li, J. F., et al., 2015. Geochronology and Geochemistry of the Eastern Erenhot Ophiolitic Complex:Implications for the Tectonic Evolution of the Inner Mongolia-Daxinganling Orogenic Belt. Journal of Asian Earth Sciences, 97:279-293. https://doi.org/10.1016/j.jseaes.2014.06.008 [99] Zhao, G. C., Wang, Y. J., Huang, B. C., et al., 2018. Geological Reconstructions of the East Asian Blocks:From the Breakup of Rodinia to the Assembly of Pangea. Earth-Science Reviews, 186:262-286. https://doi.org/10.1016/j.earscirev.2018.10.003 [100] Zhao, L., He, G. Q., Zhu, Y. B., 2013. Discovery and Its Tectonic Significance of the Ophiolite in the South of Xiemisitai Mountain, West Junggar, Xinjiang. Geological Bulletin of China, 32(1):195-205(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201301019 [101] Zhao, W. P., Jia, Z. K., Wen, Z. G., et al., 2012. The Discovery of the Blueschists from the Baerluke Ophiolitic Mélange Belt in Western Junggar, Xinjiang. Northwestern Geology, 45(2):136-138(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz201202014 [102] Zhou, G. Q., Zhao, J. X., Li, X. H., 2000. Characteristics of the Yueyashan Ophiolite from Western Nei Mongol and Its Tectonic Setting:Geochemistry and Sm-Nd Isotopic Constraints. Geochimica, 29(2):108-119(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dqhx200002001.htm [103] Zhou, J. B., Zhang, X. Z., Wilde, S. A., et al., 2009. Detrital Zircon U-Pb Dating of Heilongjiang Complex and Its Tectonic Implications. Acta Petrologica Sinica, 25(8):1924-1936(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200908017 [104] Zhu, F., Zhao, T. Y., Zhang, J. D., et al., 2013. Geochemical Characteristics and Geochronology of Sherbulake Ophiolite in Xinjiang. Xinjiang Geology, 31(3):167-172(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xjdz201303006 [105] Zhu, Y. F., Xu, X., 2006. The Discovery of Early Ordovician Ophiolite Mélange in Taerbahatai Mts., Xinjiang, NW China. Acta Petrologica Sinica, 22(12):2833-2842(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200612002 [106] 鲍庆中, 张长捷, 吴之理, 等, 2007.内蒙古白音高勒地区石炭纪石英闪长岩SHRIMP锆石U-Pb年代学及其意义.吉林大学学报(地球科学版), (1):15-23. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb200701003 [107] 包志伟, 陈森煌, 张桢堂, 1994.内蒙古贺根山地区蛇绿岩稀土元素和Sm-Nd同位素研究.地球化学, (4):339-349. http://www.cnki.com.cn/Article/CJFDTotal-DQHX404.003.htm [108] 卜建军, 何卫红, 张克信, 等, 2020.古亚洲洋的演化:来自古生物地层学方面的证据.地球科学, 45(3):711-727. doi: 10.3799/dqkx.2019.068 [109] 代文军, 谈松, 2008.甘肃北山野马街-马鬃山构造带蛇绿岩与相关火山岩性质及构造意义.新疆地质, (3):305-313. http://www.cqvip.com/Main/Detail.aspx?id=28399497 [110] 董书云, 2010.西南天山阔克萨勒岭地区蛇绿岩中的基性岩岩石学和地球化学研究(博士学位论文).北京: 中国地质大学. [111] 高俊, 钱青, 龙灵利, 等, 2009.西天山的增生造山过程.地质通报, 28(12):1804-1816. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200912013 [112] 龚一鸣, 张克信, 2016.地层学基础与前沿(第二版).武汉:中国地质大学出版社, 1-465. [113] 辜平阳, 李永军, 张兵, 等, 2009.西准达尔布特蛇绿岩中辉长岩LA-ICP-MS锆石U-Pb测年.岩石学报, 25(6):1364-1372. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200906008 [114] 郝杰, 刘小汉, 1993.南天山蛇绿混杂岩形成时代及大地构造意义.地质科学, (1):93-95. http://www.cnki.com.cn/Article/CJFDTotal-DZKX199301011.htm [115] 贺秋利, 2014.内蒙西乌旗蛇绿混杂岩辉长岩地质研究(博士学位论文).石家庄: 石家庄经济学院. [116] 胡新茁, 赵国春, 胡新悦, 等, 2015.内蒙古北山地区月牙山蛇绿质构造混杂岩带地质特征、形成时代及大地构造意义.地质通报, 34(Z1):425-436. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201502019 [117] 黄岗, 张占武, 董志辉, 等, 2011.南天山铜花山蛇绿混杂岩中斜长花岗岩锆石LA-ICP-MS微区U-Pb定年及其地质意义.中国地质, 38(1):94-102. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201101010 [118] 黄汲清, 姜春发, 1962.从多旋回构造运动观点初步探讨地壳发展规律.地质学报, (2):105-152. http://www.cnki.com.cn/Article/CJFD1979-DZXE196202000.htm [119] 侯青叶, 王忠, 刘金宝, 等, 2012.北山月牙山蛇绿岩地球化学特征及SHRIMP定年.现代地质, 26(5):1008-1018. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz201205022 [120] 李超, 肖文交, 韩春明, 等, 2013.新疆北天山奎屯河蛇绿岩斜长花岗岩锆石SIMS U-Pb年龄及其构造意义.地质科学, 48(3):815-826. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkx201303018 [121] 李纲, 杨斌, 梁恩云, 等, 2014.新疆西准噶尔达尔布特蛇绿岩套柳树沟镁铁质杂岩SHRIMP锆石U-Pb年龄及地球化学特征.华南地质与矿产, 30(3):194-205. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hndzykc201403002 [122] 李钢柱, 王玉净, 李成元, 等, 2017.内蒙古索伦山蛇绿岩带早二叠世放射虫动物群的发现及其地质意义.科学通报, 62(5):400-406. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb201705007 [123] 李江海, 王洪浩, 李维波, 周肖贝, 2014.显生宙全球古板块再造及构造演化.石油学报, 35(2):207-218. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syxb201402001 [124] 李尚林, 王训练, 段俊梅, 等, 2012.内蒙古达茂旗胡吉尔特晚泥盆世蛇绿岩的发现及其地质意义.地球科学, 37(1):18-24. doi: 10.3799/dqkx.2012.002 [125] 李文铅, 马华东, 王冉, 等, 2008.东天山康古尔塔格蛇绿岩SHRIMP年龄、Nd-Sr同位素特征及构造意义.岩石学报, 24(4):773-780 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200804016 [126] 李旭平, 焦丽香, 郑庆道, 等, 2009.黑龙江桦南地区黑龙江杂岩锆石U-Pb定年.岩石学报, 25(8):1909-1916. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200908015 [127] 李旭平, 孔凡梅, 郑庆道, 等, 2010.黑龙江萝北地区黑龙江杂岩年代学研究.岩石学报, 26(7):2015-2024. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201007005 [128] 陆松年, 郝国杰, 王惠初, 等, 2015.中国变质岩大地构造图说明书(1:2 500 000).北京:地质出版社, 1-92. [129] 陆松年, 郝国杰, 王惠初, 等, 2017.中国变质岩大地构造.北京:地质出版社, 1-338. [130] 刘敦一, 简平, 张旗, 等, 2003.内蒙古图林凯蛇绿岩中埃达克岩SHRIMP测年:早古生代洋壳消减的证据.地质学报, (3):317-327. http://www.cnki.com.cn/Article/CJFDTotal-DZXE200303004.htm [131] 龙灵利, 高俊, 熊贤明, 等, 2006.南天山库勒湖蛇绿岩地球化学特征及其年龄.岩石学报, (1):65-73. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200601007 [132] 马中平, 2007.天山及其邻区蛇绿岩研究与古生代洋盆演化(博士学位论文).西安: 西北大学. [133] 马中平, 夏林圻, 徐学义, 等, 2007.南天山库勒湖蛇绿岩锆石年龄及其地质意义.西北大学学报(自然科学版), (1):107-110. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdxxb200701027 [134] 倪康, 雷永孝, 胡秀军, 等, 2013.新疆额尔其斯缝合带南侧科克森套蛇绿岩的时代及其意义.西北地质. 46(3):64-69. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz201303004 [135] 潘桂棠, 陆松年, 肖庆辉, 等, 2016.中国大地构造阶段划分和演化.地学前缘, 23(6):1-23. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201606001 [136] 潘桂棠, 肖庆辉, 尹福光, 等, 2015.中国大地构造图说明书(1:2 500 000).北京:地质出版社. [137] 潘桂棠, 肖庆辉, 尹福光, 等, 2017.中国大地构造.北京:地质出版社.1-617. [138] 任秉琛, 何世平, 姚文光, 等, 2001.甘肃北山牛圈子蛇绿岩铷-锶同位素年龄及其大地构造意义.西北地质, (2):21-27. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz200102004 [139] 任纪舜, 郝杰, 肖藜薇, 2002.回顾与展望:中国大地构造学.地质论评, (2):113-124. http://www.cnki.com.cn/Article/CJFDTotal-DZLP200202000.htm [140] 佘宏全, 李进文, 向安平, 等, 2012.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系.岩石学报, 28(2):571-594. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201202018 [141] 沈晓明, 张海祥, 马林, 2013.新疆阿尔泰地区库尔提蛇绿岩的锆石U-Pb和角闪石40Ar/39Ar年代学及其地质意义.桂林理工大学学报, 33(3):394-405. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=glgxy201303002 [142] 唐克东, 赵爱林, 2007.吉林延边开山屯地区地层时代的新证据.地层学杂志, (2):141-150. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dcxzz200702006 [143] 田东江, 2007.完达山造山带的地质——地球化学组成及其演化(博士学位论文).长春: 吉林大学. [144] 王国强, 李向民, 徐学义, 等, 2014.甘肃北山红石山蛇绿岩锆石U-Pb年代学研究及构造意义.岩石学报, 30(6):1685-1694. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201406011 [145] 王鸿祯, 1978.论中国地层分区.地层学杂志, (2):81-104. http://www.cnki.com.cn/Article/CJFDTotal-DCXZ197802000.htm [146] 王鸿祯等, 1985.中国古地理图集.北京:地图出版社, 1-139. [147] 汪啸风, S. Stouge, 陈孝红, 等, 2005.全球下奥陶统-中奥陶统界线层型候选剖面-宜昌黄花场剖面研究新进展.地层学杂志, 29(S1):467-489+649-650+0. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=7065165 [148] 王行军, 2012.内蒙古阿拉善地区蛇绿岩的地球化学特征及其构造意义(博士学位论文).北京: 中国地质大学. [149] 王莹, 黄河, 张东阳, 等, 2012.南天山齐齐加纳克蛇绿混杂岩的SHRIMP年龄及其构造意义.岩石学报, 28(4):1273-1281. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201204023 [150] 王玉往, 王京彬, 王莉娟, 等, 2011.新疆吐尔库班套蛇绿混杂岩的发现及其地质意义.地学前缘. 18(3):151-165. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201103013 [151] 翁凯, 徐学义, 马中平, 等, 2016.新疆西准噶尔玛依勒蛇绿岩中镁铁-超镁铁质岩的地球化学、年代学及其地质意义.岩石学报, 32(5):1420-1436. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201605012 [152] 魏荣珠, 2010.西准噶尔玛依勒山枕状熔岩地质特征及大地构造意义.新疆地质, 28(3):229-235. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xjdz201003001 [153] 吴波, 何国琦, 吴泰然, 等, 2006.新疆布尔根蛇绿混杂岩的发现及其大地构造意义.中国地质. 2006(3):476-486. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200603004 [154] 武鹏, 王国强, 李向民, 等, 2012.甘肃北山地区牛圈子蛇绿岩的形成时代及地质意义.地质通报, 31(12):2032-2037. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201212012 [155] 肖文交, Windley B. F., 阎全人, 等, 2006.北疆地区阿尔曼太蛇绿岩锆石SHRIMP年龄及其大地构造意义.地质学报, 2006(1):32-37. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200601004 [156] 颉颃强, 张福勤, 苗来成, 等, 2008.东北牡丹江地区"黑龙江群"中斜长角闪岩与花岗岩的锆石SHRIMP U-Pb定年及其地质学意义.岩石学报, 24(6):1237-1250. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200806007 [157] 徐备, Charvet J., 张福勤, 2001.内蒙古北部苏尼特左旗蓝片岩岩石学和年代学研究.地质科学, (4):424-434. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkx200104005 [158] 徐学义, 马中平, 李向民, 等, 2003.西南天山吉根地区P-MORB残片的发现及其构造意义.岩石矿物学杂志, (3):245-253. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz200303006 [159] 徐学义, 马中平, 夏林圻, 等, 2005.北天山巴音沟蛇绿岩斜长花岗岩锆石SHRIMP测年及其意义.地质论评, (5):45-49. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200505006 [160] 徐学义, 夏林圻, 马中平, 等, 2006.北天山巴音沟蛇绿岩斜长花岗岩SHRIMP锆石U-Pb年龄及蛇绿岩成因研究.岩石学报, (1):83-94. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200601009 [161] 杨高学, 李永军, 杨宝凯, 等, 2013.西准噶尔玛依勒蛇绿混杂岩锆石U-Pb年代学、地球化学及源区特征.岩石学报, 29(1):303-316. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201301025.htm [162] 杨经绥, 徐向珍, 李天福, 等, 2011.新疆中天山南缘库米什地区蛇绿岩的锆石U-Pb同位素定年:早古生代洋盆的证据.岩石学报, 27(1):77-95. http://d.wanfangdata.com.cn/periodical/ysxb98201101005 [163] 殷鸿福, 张克信, 陈能松, 等, 2003.中华人民共和国区域地质调查报告, 冬给措纳湖幅(I47C001002).武汉:中国地质大学出版社, 1-457. [164] 张国宾, 2014.黑龙江省东部完达山地块区域成矿系统研究(博士学位论文).长春: 吉林大学. [165] 张海祥, 牛贺才, Terada K., 等, 2003.新疆北部阿尔泰地区库尔提蛇绿岩中斜长花岗岩的SHRIMP年代学研究.科学通报, 2003(12):1350-1354. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb200312023 [166] 张克信, 殷鸿福, 朱云海, 等, 2001.造山带混杂岩区地质填图理论、方法与实践, 武汉: 中国地质大学出版社. [167] 张克信, 殷鸿福, 朱云海, 等, 2003.史密斯地层与非史密斯地层.地球科学, 28(4):361-369. http://www.earth-science.net/article/id/1264 [168] 张克信, 骆满生, 徐亚东, 等.2015a.中国沉积大地构造图说明书(1:2 500 000).北京:地质出版社, 1-127. [169] 张克信, 潘桂棠, 何卫红, 等, 2015b.中国构造-地层大区划分新方案.地球科学, 40(2):206-233. doi: 10.3799/dqkx.2015.016 [170] 张克信, 何卫红, 徐亚东, 等.2016.中国洋板块地层分布及构造演化.地学前缘, 23(6):24-30. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201606002 [171] 张克信, 何卫红, 骆满生, 等, 2017.中国沉积岩建造与沉积大地构造演化.北京:地质出版社. 1-604. [172] 张克信, 徐亚东, 何卫红, 等, 2018.中国新元古宙青白口纪早期(1 000~820 Ma)洋陆分布.地球科学, 43(11):3837-3852. doi: 10.3799/dqkx.2018.339 [173] 张越, 2012.新疆东准噶尔阿尔曼太蛇绿混杂岩组成、结构、就位机制及大地构造意义研究(博士学位论文).西安: 长安大学. [174] 张越, 徐学义, 陈隽璐, 等, 2012.阿尔泰地区玛因鄂博蛇绿岩的地质特征及其LA-ICP-MS锆石U-Pb年龄.地质通报, 31(6):834-842. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201206002 [175] 张元元, 郭召杰, 2008.甘新交界红柳河蛇绿岩形成和侵位年龄的准确限定及大地构造意义.岩石学报, 24(4):803-809. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200804019 [176] 张元元, 郭召杰, 2010.准噶尔北部蛇绿岩形成时限新证据及其东、西准噶尔蛇绿岩的对比研究.岩石学报, 26(2):421-430. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201002006 [177] 赵磊, 何国琦, 朱亚兵, 2013.新疆西准噶尔北部谢米斯台山南坡蛇绿岩带的发现及其意义.地质通报, 32(1):195-205. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201301019 [178] 赵文平, 贾振奎, 温志刚, 等, 2012.新疆西准噶尔巴尔鲁克蛇绿混杂岩带发现蓝闪片岩.西北地质, 45(2):136-138. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz201202014 [179] 周国庆, 赵建新, 李献华, 2000.内蒙古月牙山蛇绿岩特征及形成的构造背景:地球化学和Sr-Nd同位素制约.地球化学, (2):108-119. [180] 周建波, 张兴洲, Wilde S.A., 等, 2009.黑龙江杂岩的碎屑锆石年代及其大地构造意义.岩石学报, 25(8):1924-1936. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200908017 [181] 褚方, 赵同阳, 张建东, 等, 2013.新疆沙尔布拉克蛇绿岩岩石地球化学特征及形成时代.新疆地质, 31(3):167-172. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xjdz201303006 [182] 朱永峰, 徐新, 2006.新疆塔尔巴哈台山发现早奥陶世蛇绿混杂岩.岩石学报, (12):2833-2842. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200612002 -
点击查看大图
图(9) / 表(2)
计量
- 文章访问数: 1643
- HTML全文浏览量: 203
- PDF下载量: 219
- 被引次数: 0
