Research status and progress of Paleozoic ophiolites in Beishan orogenic belt
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摘要:
蛇绿混杂岩带作为造山带最重要的组成部分之一，其形成和就位过程与区域造山事件密切相关。通过系统梳理北山造山带蛇绿混杂岩的研究现状及存在问题，认为在北山造山带内卷入的4条蛇绿混杂岩带中，红柳河-牛圈子-洗肠井蛇绿混杂岩带为形成时代最古老的蛇绿岩，代表了北山洋盆最早于早寒武世即已开启，北山地区发育的洋盆最晚可能于二叠纪闭合，构造属性研究表明，已发现的各蛇绿混杂岩带单独作为一级构造单元划分的证据依然不足。以客观表达目标地质体为主的北山各蛇绿岩带的地质调查程度制约了蛇绿岩的识别、形成、就位时代、各洋盆之间演化关系及构造属性等问题的研究，建议未来区内的深入研究及解决热点问题时应采取如下关键手段：开展各蛇绿混杂岩带大比例尺的精细基础地质调查工作。
Abstract:As one of the most important parts of orogenic belt, the formation and emplacement of the ophiolitic mélange belt is closely related to regional orogenic events.Four ophiolitic mélanges belts are involved in the Beishan orogenic belt, of which the Hongliuhe-Niujuanzi-Xichangjing ophiolitic mélange belt is the oldest one, indicating that the Bishan Ocean was opened as early as Early Cambrian, and might be closed in Permian at the latest.The study of tectonic affinity also shows that the evidence for the division of the discovered ophiolitic mélange zones as the first-scale tectonic unit is still insufficient.Because the identification, formation, emplacement age of ophiolites and evolution of various ocean basins, as well as their tectonic properties are restricted by objective expression about geological survey of Beishan ophiolite belts, it is suggested that one of the key means to further study and solve hot issue in the area in the future is to pay attention to the large scale fine basic geological survey of each ophiolite belt.
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Key words:
- ophiolite /
- tectonic evolution /
- formation age /
- Paleozoic /
- Beishan orogenic belt
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[1] 张进, 邓晋福, 肖庆辉, 等. 蛇绿岩研究的最新进展[J]. 地质通报, 2012, 31(1): 1-12. doi: 10.3969/j.issn.1671-2552.2012.01.001
[2] 张旗. 蛇绿岩研究中的几个问题[J]. 岩石学报, 1995, (S1): 228-240. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201501002.htm
[3] Dilek Y. Ophiolite concept and its evolution[J]. The Geological Soeiety of AmerieaSpecial Paper, 2003, 373: 1-16. http://petrology.oxfordjournals.org/cgi/ijlink?linkType=ABST&journalCode=papersgsa&resid=373/0/1
[4] Dilek Y, Furnes H. Ophiolite genesis and global tectonics: Geochemical and tectonic fingerprinting of ancient oceanic lithosphere[J]. Geological Society of America Bulletin, 2011, 123(3/4): 387-411.
[5] 闫臻, 王宗起, 付长垒, 等. 混杂岩基本特征与专题地质填图[J]. 地质通报, 2018, 37(2/3): 167-191. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=2018020301&flag=1
[6] 王根厚, 韩芳林, 杨运军, 等. 藏北羌塘中部晚古生代增生杂岩的发现及其地质意义[J]. 地质通报, 2009, 28(9): 15-21. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20090903&flag=1
[7] Dobretsov N L, Berzin N A, Buslov M M. Opening and Tectonic Evolution of the Paleo-Asian Ocean[J]. International Geology Review, 1995, 37(4): 335-360. doi: 10.1080/00206819509465407
[8] 任纪舜, 王作勋, 陈炳蔚, 等. 从全球看中国大地构造——中国及邻区大地构造图简要说明[M]. 北京: 地质出版社, 1999.
[9] 余吉远, 李向民, 王国强, 等. 北山地区辉铜山、帐房山蛇绿岩U-Pb年龄及其意义[J]. 地质通报, 2012, 31(12): 2038-2045. doi: 10.3969/j.issn.1671-2552.2012.12.013
[10] 于福生, 李金宝, 王涛. 东天山红柳河地区蛇绿岩U-Pb同位素年龄[J]. 地球学报, 2006, 27(3): 213-216. doi: 10.3321/j.issn:1006-3021.2006.03.004
[11] 张元元, 郭召杰. 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[J]. 岩石学报, 2008, 24(4): 803-809. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200804020.htm
[12] Cleven N, Lin S, Guilmette C, et al. Petrogenesis and implications for tectonic setting of Cambrian suprasubduction-zone ophiolitic rocks in the central Beishan orogenic collage, Northwest China[J]. Journal of Asian Earth Sciences, 2015, 113: 369-90. doi: 10.1016/j.jseaes.2014.10.038
[13] Shi Y R, Zhang W, Kröner A, et al. Cambrian ophiolite complexes in the Beishan area, China, southern margin of the Central Asian Orogenic Belt[J]. Journal of Asian Earth Sciences, 2018, 153: 193-205. doi: 10.1016/j.jseaes.2017.05.021
[14] Tian Z H, Xiao W J, Windley B F, et al. Structure, age, and tectonic development of the Huoshishan-Niujuanzi ophiolitic mélange, Beishan, southernmost Altaids[J]. Gondwana Research, 2014, 25(2): 820-841. doi: 10.1016/j.gr.2013.05.006
[15] 武鹏, 王国强, 李向民, 等. 甘肃北山地区牛圈子蛇绿岩的形成时代及地质意义[J]. 地质通报, 2012, 31(12): 2032-2037. doi: 10.3969/j.issn.1671-2552.2012.12.012
[16] Wang S, Zhang K, Song B, et al. Geochronology and geochemistry of the Niujuanzi ophiolitic mélange, Gansu Province, NW China: implications for tectonic evolution of the Beishan Orogenic Collage[J]. International Journal of Earth Sciences, 2018, 107(1): 269-289. doi: 10.1007/s00531-017-1489-2
[17] 任秉琛, 何世平, 姚文光, 等. 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[J]. 西北地质, 2001, 34(2): 21-27. doi: 10.3969/j.issn.1009-6248.2001.02.004
[18] 胡新茁, 赵国春, 胡新悦, 等. 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[J]. 地质通报, 2015, 34(2/3): 205-216. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=2015020318&flag=1
[19] 侯青叶, 王忠, 刘金宝, 等. 北山月牙山蛇绿岩地球化学特征及SHRIMP定年[J]. 现代地质, 2012, 26(5): 1008-1018. doi: 10.3969/j.issn.1000-8527.2012.05.022
[20] 周国庆, 赵建新. 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[J]. 地球化学, 2000, 29(2): 108-119. doi: 10.3321/j.issn:0379-1726.2000.02.002
[21] Ao S J, Xiao W J, Han C M, et al. Cambrian to early Silurian ophiolite and accretionary processes in the Beishan collage, NW China: implications for the architecture of the Southern Altaids[J]. Geological Magazine, 2012, 149(4): 606-625. doi: 10.1017/S0016756811000884
[22] 李向民, 余吉远, 王国强, 等. 甘肃北山地区芨芨台子蛇绿岩年代学研究及其意义[J]. 地质通报, 2012, 31(12): 2025-2031. doi: 10.3969/j.issn.1671-2552.2012.12.011
[23] 孙立新, 张家辉, 任邦方, 等. 北山造山带白云山蛇绿混杂岩的地球化学特征、时代及地质意义[J]. 岩石矿物学杂志, 2017, 36(2): 131-147. doi: 10.3969/j.issn.1000-6524.2017.02.001
[24] Wu T R, Zheng R G, Zhang W, et al.Tectonic framework of Beishan Mountain-Northern Alxa Area and the time constraints for the closing of the Paleo-Asian Ocean[C]//Proceedings of the Fifth Workshop on 1: 5M International Geological Map of Asia 2011.Beijing, 2011.
[25] 王国强, 李向民, 徐学义, 等. 甘肃北山红石山蛇绿岩锆石U-Pb年代学研究及构造意义[J]. 岩石学报, 2014, 30(6): 1685-1694. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201406011.htm
[26] Shi Y, Li L, Kröner A, et al. Carboniferous Alaskan-type complex along the Sino-Mongolian boundary, southern margin of the Central Asian Orogenic Belt[J]. Acta Geochim, 2017, 36(2): 276-290. doi: 10.1007/s11631-017-0145-7
[27] 牛文超, 辛后田, 段连峰, 等. 内蒙古北山地区百合山蛇绿混杂岩带的厘定及其洋盆俯冲极性——基于1: 5万清河沟幅地质图的新认识[J]. 中国地质, 2019, 46(5): 977-994. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201905004.htm
[28] 李向民, 张占武, 王国强, 等. 北山成矿带地质矿产图(1: 500000)[M]. 西安: 西安地图出版社, 2016.
[29] Sengör A M C, Natal'in, B. A. , Burtman, V. S. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia[J]. Nature, 1993, 364(22): 299-307. http://www.researchgate.net/publication/237130145_Evolution_of_the_Altaid_Tectonic_Collage_and_Paleozoic_Crustal_Growth_in_Eurasia
[30] Han B F, Wang S G, Jahn B M, et al. Depleted-mantle source for the Ulungur River A-type granites from North Xinjiang, China: geochemistry and Nd-Sr isotopic evidence, and implications for Phanerozoic crustal growth[J]. Chemical Geology, 1997, 138(3/4): 135-159.
[31] 韩宝福, 季建清, 宋彪, 等. 新疆喀拉通克和黄山东含铜镍矿镁铁-超镁铁杂岩体的SHRIMP锆石U-Pb年龄及其地质意义[J]. 科学通报, 2004, 49(22): 2324-2328. doi: 10.3321/j.issn:0023-074X.2004.22.012
[32] Jahn B, Wu F, Chen B. Massive granitoid generation in Central Asia: Nd isotope evidence and implication for continental growth in the Phanerozoic[J]. Episodes, 2000, 23(2): 82-92. doi: 10.18814/epiiugs/2000/v23i2/001
[33] Jahn B. Phanerozoic continental growth in Central Asia[J]. Journal of Asian Earth Sciences, 2004, 23(5): 599-603. doi: 10.1016/S1367-9120(03)00124-X
[34] Wang Q, Wyman D A, Zhao Z H, et al. Petrogenesis of Carboniferous adakites and Nb-enriched arc basalts in the Alataw area, northern Tianshan Range(western China): implications for Phanerozoic crustal growth in the Central Asia orogenic belt[J]. Chemical Geology, 2007, 236(1): 42-64. http://www.sciencedirect.com/science/article/pii/S0009254106003810
[35] Windley B F, Alexeiev D, Xiao W J, et al. Tectonic models for accretion of the Central Asian Orogenic Belt[J]. Journal of the Geological Society, 2007, 164(1): 31-47. doi: 10.1144/0016-76492006-022
[36] Xiao W J, Windley B F, Han C M, et al. End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia[J]. International Journal of Earth Sciences, 2009, 98(6): 1189-1217. doi: 10.1007/s00531-008-0407-z
[37] Xiao W J, Mao Q G, Windley B F, et al. Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage[J]. American Journal of Science, 2010, 310(10): 1553-1594. doi: 10.2475/10.2010.12
[38] Xiao W J, Huang B, Han C M, et al. A review of the western part of the Altaids: a key to understanding the architecture of accretionary orogens[J]. Gondwana Research, 2010, 18(2): 253-273. http://www.sciencedirect.com/science/article/pii/S1342937X10000262
[39] Xiao W J, Windley B F, Allen M B, et al. Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage[J]. Gondwana Research, 2013, 23(4): 1316-1341. doi: 10.1016/j.gr.2012.01.012
[40] Su B X, Qin K Z, Sakyi P A, et al. U-Pb ages and Hf-O isotopes of zircons from Late Paleozoic mafic-ultramafic units in the southern Central Asian Orogenic Belt: Tectonic implications and evidence for an Early-Permian mantle plume[J]. Gondwana Research, 2011, 20(2): 516-531. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ201201001074.htm
[41] Xiao W J, Windley B F, Badarch G, et al. Palaeozoic accretionary and convergent tectonics of the southern Altaids: implications for the growth of Central Asia[J]. Journal of the Geological Society, 2004, 161(3): 339-342. doi: 10.1144/0016-764903-165
[42] 王宝瑜, 郎智君, 李向东, 等. 中国天山西段地质剖面综合研究[M]. 北京: 科学出版社, 1994.
[43] 肖序常, 汤耀庆, 冯益民, 等. 新疆北部及其邻区大地构造[M]. 北京: 地质出版社, 1992.
[44] Xia L Q, Xu X Y, Xia Z C. Petrogenesis of Carboniferous rift-related volcanic rocks in the Tianshan, northwestern China[J]. Geological Society of America Bulletin, 2004, 116(3/4): 419-433.
[45] Xia L Q, Xu X Y, Xia Z C, et al. Carboniferous post-collisional rift volcanism of the Tian Shan Mountains, northwestern China[J]. Acta Geologica Sinica(English Edition), 2003, 77(3): 338-360. doi: 10.1111/j.1755-6724.2003.tb00751.x
[46] Xia L Q, Xia Z C, Xu X Y, et al. Relative contributions of crust and mantle to the generation of the Tianshan Carboniferous rift-related basic lavas, northwestern China[J]. Journal of Asian Earth Sciences, 2008, 31(4/6): 357-378. http://www.sciencedirect.com/science/article/pii/S1367912007001344
[47] Wang B, Shu L, Faure M, et al. Paleozoic tectonics of the southern Chinese Tianshan: Insights from structural, chronological and geochemical studies of the Heiyingshan ophiolitic mélange(NW China)[J]. Tectonophysics, 2011, 497(s1/4): 85-104. http://www.sciencedirect.com/science/article/pii/S0040195110004786
[48] Wang B, Ruffet G. Structural and Geochronological Study of High-Pressure Metamorphic Rocks in the Kekesu Section(Northwestern China): Implications for the Late Paleozoic Tectonics of the Southern Tianshan[J]. Journal of Geology, 2010, 118(1): 59-77. doi: 10.1086/648531
[49] Dong Y P, Zhang G W, Neubauer F, et al. Syn-and post-collisional granitoids in the Central Tianshan orogen: geochemistry, geochronology and implications for tectonic evolution. Gondwana Res[J]. Gondwana Research, 2011, 20(2/3): 568-581. http://www.sciencedirect.com/science/article/pii/S1342937X11000396
[50] Volkova N I, Sklyarov E V. High-pressure complexes of Central Asian Fold Belt: Geologic setting, geochemistry, and geodynamic implications[J]. Russian Geology & Geophysics, 2007, 48(1): 83-90. http://www.sciencedirect.com/science/article/pii/S1068797106000095
[51] Klemd R, Bröcker M, Hacker B, et al. New age constraints on the metamorphic evolution of the high-pressure/low-temperature belt in the western Tianshan Mountains, NW China[J]. The Journal of Geology, 2005, 113(2): 157-168. doi: 10.1086/427666
[52] Gao J, Klemd R. Formation of HP-LT rocks and their tectonic implications in the western Tianshan Orogen, NW China: geochemical and age constraints[J]. Lithos, 2003, 66(1/2): 1-22. http://www.sciencedirect.com/science/article/pii/S0024493702001536
[53] Seltmann R, Konopelko D, Biske G, et al. Hercynian post-collisional magmatism in the context of Paleozoic magmatic evolution of the Tien Shan orogenic belt[J]. Journal of Asian Earth Sciences, 2011, 42(5): 821-838. doi: 10.1016/j.jseaes.2010.08.016
[54] Li Q L, Lin W, Su W, et al. SIMS U-Pb rutile age of low-temperature eclogites from southwestern Chinese Tianshan, NW China[J]. Lithos, 2011, 122(1/2): 76-86. http://www.sciencedirect.com/science/article/pii/S0024493710003208
[55] Gao J, Klemd R, Qian Q, et al. The collision between the Yili and Tarim blocks of the Southwestern Altaids: Geochemical and age constraints of a leucogranite dike crosscutting the HP-LT metamorphic belt in the Chinese Tianshan Orogen[J]. Tectonophysics, 2011, 499(1/4): 118-131.
[56] 肖序常, 何国琦, 徐新. 中国新疆地壳结构与地质演化[M]. 北京: 地质出版社, 2010.
[57] Su W, Gao J, Klemd R, et al. U-Pb zircon geochronology of Tianshan eclogites in NW China: implication for the collision between the Yili and Tarim blocks of the southwestern Altaids[J]. European Journal of Mineralogy, 2010, 22(4): 473-478. doi: 10.1127/0935-1221/2010/0022-2040
[58] Glorie S, Grave J D, Buslov M M, et al. Multi-method chronometric constraints on the evolution of the Northern Kyrgyz Tien Shan granitoids(Central Asian Orogenic Belt): From emplacement to exhumation[J]. Journal of Asian Earth Sciences, 2010, 38(s3/4): 131-146. http://www.sciencedirect.com/science/article/pii/S1367912009002636
[59] Konopelko D, Seltmann R, Biske G, et al. Possible source dichotomy of contemporaneous post-collisional barren Ⅰ-type versus tin-bearing A-type granites, lying on opposite sides of the South Tien Shan suture[J]. Ore Geology Reviews, 2009, 35(2): 206-216. doi: 10.1016/j.oregeorev.2009.01.002
[60] Solomovich L I. Postcollisional magmatism in the South Tien Shan Variscan Orogenic Belt, Kyrgyzstan: Evidence for high-temperature and high-pressure collision[J]. Journal of Asian Earth Sciences, 2007, 30(1): 142-153. doi: 10.1016/j.jseaes.2006.08.003
[61] Konopelko D, Biske G, Seltmann R, et al. Hercynian post-collisional A-type granites of the Kokshaal Range, Southern Tien Shan, Kyrgyzstan[J]. Lithos, 2007, 97(1/2): 140-160. http://www.sciencedirect.com/science/article/pii/S0024493706003215
[62] Solomovich L I, Trifonov B A. Postcollisional granites in the South Tien Shan Variscan Collisional Belt, Kyrgyzstan[J]. Journal of Asian Earth Sciences, 2002, 21(1): 7-21. doi: 10.1016/S1367-9120(02)00008-1
[63] Windley B F, Allen M B, Zhang C, et al. Paleozoic accretion and Cenozoic redeformation of the Chinese Tien Shan range, Central Asia[J]. Geology, 1990, 18(2): 128-131. doi: 10.1130/0091-7613(1990)018<0128:PAACRO>2.3.CO;2
[64] Allen M B, Windley B F, Zhang C. Paleozoic collisional tectonics and magmatism of the Chinese Tien Shan, Central Asia[J]. Tectonophysics, 1992, 220: 89-115. http://www.researchgate.net/publication/303210886_Paleozoic_collisional_tectonics_and_magmatism_of_the_Chinese_Tien_Shan_Central_Asia
[65] Chen C, Lu H, Jia D, et al. Closing history of the southern Tianshan oceanic basin, western China: an oblique collisional orogeny[J]. Tectonophysics, 1999, 302(1/2): 23-40. http://www.onacademic.com/detail/journal_1000035475124310_5e61.html
[66] Zhang L, Ai Y, Li X, et al. Triassic collision of western Tianshan orogenic belt, China: evidence from SHRIMP U-Pb dating of zircon from HP/UHP eclogitic rocks[J]. Lithos, 2007, 96(1): 266-280. http://www.researchgate.net/publication/228963627_Triassic_collision_of_western_Tianshan_orogenic_belt_China_Evidence_from_SHRIMP_U-Pb_dating_of_zircon_from_HPUHP_eclogitic_rocks
[67] Brookfield M E. Geological development and Phanerozoic crustal accretion in the western segment of the southern Tien Shan(Kyrgyzstan, Uzbekistan and Tajikistan)[J]. Tectonophysics, 2000, 328(1): 1-14.
[68] Xiao W J, Windley B F, Han C M, et al. End Permian to mid-Triassic termination of the southern Central Asian Orogenic Belt[J]. International journal of earth sciences, 2009, 98(6): 1189-1217. doi: 10.1007/s00531-008-0407-z
[69] Xiao W J, Han C M, Chao Y, et al. Middle Cambrian to Permian subduction-related accretionary orogenesis of North Xinjiang NW China: Implications for the tectonic evolution of Central Asia[J]. Journal of Asian Earth Sciences, 2008, 32(2/4): 102-117.
[70] Song D F, Xiao W J, Han C M, et al. Progressive accretionary tectonics of the Beishan orogenic collage, Southern Altaids: insights from zircon U-Pb and Hf isotopic data of high-grade complexes[J]. Precambrian Research, 2012, 227: 368-388.
[71] 肖文交, 宋东方, Windley B F, 等. 中亚增生造山过程与成矿作用研究进展[J]. 中国科学: 地球科学, 2019, 49: 1512-1545. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201910003.htm
[72] 左国朝, 何国琦, 李红诚. 北山板块构造及成矿规律[M]. 北京: 北京大学出版社, 1990: 1-226.
[73] 辛后田, 牛文超, 田健, 等. 内蒙古北山造山带时空结构与古亚洲洋演化[J]. 地质通报, 2020, 39(9): 1297-1316. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20200901&flag=1
[74] 刘雪亚, 王荃. 中国西部北山造山带的大地构造及其演化[J]. 地学研究, 1995, 28: 37-48. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199500001007.htm
[75] 龚全胜, 刘明强, 李海林, 等. 甘肃北山造山带类型及基本特征[J]. 西北地质, 2002, 35(3): 28-34. doi: 10.3969/j.issn.1009-6248.2002.03.004
[76] 何世平, 任秉琛, 姚文光, 等. 甘肃内蒙古北山地区构造单元划分[J]. 西北地质, 2002, 35(4): 30-40. doi: 10.3969/j.issn.1009-6248.2002.04.004
[77] 聂凤军, 江思宏, 白大明, 等. 北山地区金属矿床成矿规律及找矿方向[M]. 北京: 地质出版社, 2002: 1-408.
[78] 杨合群, 李英, 赵国斌, 等. 北山蛇绿岩特征及构造属性[J]. 西北地质, 2010, 43(1): 26-36. doi: 10.3969/j.issn.1009-6248.2010.01.002
[79] 左国朝, 张淑玲, 何国琦, 等. 北山地区早古生代板块构造特征[J]. 地质科学, 1990, 25(4): 305-314. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX199004000.htm
[80] 左国朝, 李茂松. 甘肃北山地区早古生代岩石圈形成与演化[M]. 兰州: 甘肃科学技术出版社, 1996: 1-92.
[81] 李向民, 余吉远, 王国强, 等. 甘肃北山红柳园地区泥盆系三个井组和墩墩山群LA-ICP-MS锆石U-Pb测年及其意义[J]. 地质通报, 2011, 30(10): 1501-1507. doi: 10.3969/j.issn.1671-2552.2011.10.003
[82] Guo Q Q, Xiao W J, Hou Q L, et al. Construction of Late Devonian Dundunshan arc in the Beishan orogen and its implication for tectonics of southern Central Asian Orogenic Belt[J]. Lithos, 2014, 184/187: 361-378. doi: 10.1016/j.lithos.2013.11.007
[83] Song D F, Xiao W J, Han C M, et al. Provenance of metasedimentary rocks from the Beishan orogenic collage, southern Altaids: constraints from detrital zircon U-Pb and Hf isotopic data[J]. Gondwana Research, 2013, 24(3): 1127-1151.
[84] Zhang W, Wu T R, Zheng R G, et al. Post-collisional Southeastern Beishan Granites: Geochemistry, geochronology, Sr-Nd-Hf isotopes and their implications for tectonic evolution[J]. Journal of Asian Earth Sciences, 2012, 58: 51-63. doi: 10.1016/j.jseaes.2012.07.004
[85] Mao Q G, Xiao W J, Fang T H, et al. Late Ordovician to early Devonian adakites and Nb-enriched basalts in the Liuyuan area, Beishan, NW China: Implications for early Paleozoic slab-melting and crustal growth in the southern Altaids[J]. Gondwana Research, 2012, 22(2): 534-553. doi: 10.1016/j.gr.2011.06.006
[86] Mao Q G, Xiao W J, Windley B F, et al. The Liuyuan complex in the Beishan, NW China: a Carboniferous-Permian ophiolitic fore-arc sliver in the southern Altaids[J]. Geological Magazine, 2011, 149(3): 483-506.
[87] Zhang Y, Dostal J, Zhao Z, et al. Geochronology, geochemistry and petrogenesis of mafic and ultramafic rocks from Southern Beishan area, NW China: Implications for crust-mantle interaction[J]. Gondwana Research, 2011, 20(4): 816-830. doi: 10.1016/j.gr.2011.03.008
[88] Liu X, Chen B, Jahn B, et al. Early Paleozoic(ca. 465 Ma)eclogites from Beishan(NW China)and their bearing on the tectonic evolution of the southern Central Asian Orogenic Belt[J]. Journal of Asian Earth Sciences, 2011, 42(4): 715-731. http://www.sciencedirect.com/science/article/pii/S1367912010003147
[89] Qu J, Xiao W J, Windley B F, et al. Ordovician eclogites from the Chinese Beishan: Implications for the tectonic evolution of the southern Altaids[J]. Journal of Metamorphic Geology, 2011, 29: 803-820. doi: 10.1111/j.1525-1314.2011.00942.x
[90] Saktura W, Buckman S, Nutman A, et al. Continental origin of the Gubaoquan eclogite and implications for evolution of the Beishan Orogen, Central Asian Orogenic Belt, NW China[J]. Lithos, 2017, 294(294/295): 20-38. http://www.sciencedirect.com/science/article/pii/S002449371730347X
[91] 王立社, 杨建国, 谢春林, 等. 甘肃北山火石山地区早古生代蛇绿混杂岩的发现及其地质意义[J]. 现代地质, 2007, 21(3): 451-456. doi: 10.3969/j.issn.1000-8527.2007.03.003
[92] 周国庆. 古塔里木大陆东北缘加里东期蛇绿岩套的发现及其构造意义[J]. 南京大学学报(自然科学版), 1988, 24(1): 39-54. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ198801003.htm
[93] 郭召杰, 马瑞士, 郭令智, 等. 新疆东部三条蛇绿混杂岩带的比较研究[J]. 地质论评, 1993, 39(3): 236-247. doi: 10.3321/j.issn:0371-5736.1993.03.007
[94] 于福生, 王春英, 漆家福, 等. 甘新交界红柳河地区早志留世蛇绿混杂岩的厘定及大地构造意义[J]. 矿物岩石, 2000, 20(4): 60-66. doi: 10.3969/j.issn.1001-6872.2000.04.012
[95] 郭召杰, 史宏宇, 张志诚, 等. 新疆甘肃交界红柳河蛇绿岩中伸展构造与古洋盆演化过程[J]. 岩石学报, 2006, 22(1): 95-102. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200601010.htm
[96] 王国强. 北山古生代蛇绿岩、火山岩研究与构造演化[D]. 长安大学博士学位论文, 2015.
[97] 何世平, 周会武, 姚文光, 等. 甘肃北山中泥盆统砾岩中放射虫的发现及其地质意义[J]. 西北地质, 2004, 37(3): 24-28. doi: 10.3969/j.issn.1009-6248.2004.03.005
[98] 郑荣国, 吴泰然, 张文, 等. 北山地区月牙山-洗肠井蛇绿岩的地球化学特征及形成环境[J]. 地质学报, 2012, 86(6): 961-971. doi: 10.3969/j.issn.0001-5717.2012.06.010
[99] Zhang W, Pease V, Wu T R, et al. Discovery of an adakite-like pluton near Dongqiyishan(Beishan, NW China): Its age and tectonic significance[J]. Lithos, 2012, 142/143: 148-160. doi: 10.1016/j.lithos.2012.02.021
[100] 何世平, 周会武, 任秉琛, 等. 甘肃内蒙古北山地区古生代地壳演化[J]. 西北地质, 2005, 38(3): 6-15. doi: 10.3969/j.issn.1009-6248.2005.03.002
[101] 杨合群, 李英, 李文明, 等. 北山成矿构造背景概论[J]. 西北地质, 2008, 41(1): 22-28. doi: 10.3969/j.issn.1009-6248.2008.01.002
[102] Song, D F, Xiao W J, Windley B F, et al. A Paleozoic Japan-type subduction-accretion system in the Beishan orogenic collage, southern Central Asian Orogenic Belt[J]. Lithos, 2015, 224/225: 195-213. doi: 10.1016/j.lithos.2015.03.005
[103] 宋泰忠, 王瑾, 林海, 等. 内蒙古北山地区小黄山蛇绿岩地质特征[J]. 西北地质, 2008, 41(3): 55-63. doi: 10.3969/j.issn.1009-6248.2008.03.005
[104] Zheng R G, Wu T R, Zhang W, et al. Late Paleozoic subduction system in the southern Central Asian Orogenic Belt: Evidences from geochronology and geochemistry of the Xiaohuangshan ophiolite in the Beishan orogenic belt[J]. Journal of Asian Earth Sciences, 2013, 62: 463-475. doi: 10.1016/j.jseaes.2012.10.033
[105] 杨合群, 赵国斌, 李英, 等. 新疆甘肃内蒙古衔接区古生代构造背景与成矿的关系[J]. 地质通报, 2012, 42(4): 60-75. doi: 10.3969/j.issn.1671-2552.2012.02.027
[106] 王小红, 杨建国, 谢燮, 等. 甘肃北山红石山基性-超基性岩体的成因类型及构造意义[J]. 西北地质, 2013, 46(1): 40-55. doi: 10.3969/j.issn.1009-6248.2013.01.005
[107] 赵茹石, 周振环, 毛金海, 等. 甘肃省板块构造单元划分及其构造演化[J]. 中国区域地质, 1994, 13(1): 28-36. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD401.004.htm
[108] 魏志军, 黄增保, 金霞, 等. 甘肃红石山地区蛇绿混杂岩地质特征[J]. 西北地质, 2004, 37(1): 13-18. doi: 10.3969/j.issn.1009-6248.2004.01.003
[109] 黄增保, 金霞. 甘肃北山红石山蛇绿混杂岩带中基性火山岩构造环境分析[J]. 中国地质, 2006, 33(5): 1030-1037. doi: 10.3969/j.issn.1000-3657.2006.05.011
[110] 王作勋, 邬继易, 吕喜超, 等. 天山多旋回构造演化及成矿[M]. 北京: 科学出版社, 1990: 1-217.
[111] Saunders A, Storey M, Kent R, et al. Consequences of plume-lithosphere interactions[J]. Geological Society, London, Special Publications, 1992, 68(1): 41-60. doi: 10.1144/GSL.SP.1992.068.01.04
[112] 徐学义, 夏林圻, 马中平, 等. 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[J]. 岩石学报, 2006, 22(1): 83-94. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200601009.htm
[113] Wilson M. Igneous petrogenesis[M]. London: Unwin Hyman, 1989: 1-464.
[114] Ao S J, Xiao W J, Han C M, et al. Geochronology and geochemistry of Early Permian mafic-ultramafic complexes in the Beishan area, Xinjiang, NW China: Implications for late Paleozoic tectonic evolution of the southern Altaids[J]. Gondwana Research, 2010, 18(2): 466-478. http://www.sciencedirect.com/science/article/pii/s1342937x10000237
[115] Guo Q Q, Xiao W J, Windley B F, et al. Provenance and tectonic settings of Permian turbidites from the Beishan Mountains, NW China: Implications for the Late Paleozoic accretionary tectonics of the southern Altaids[J]. Journal of Asian Earth Sciences, 2012, 49: 54-68. doi: 10.1016/j.jseaes.2011.03.013
[116] Song D F, Xiao W J, Han C M, et al. Polyphase deformation of a Paleozoic forearc-arc complex in the Beishan orogen, NW China[J]. Tectonophysics, 2014, 632: 224-243. doi: 10.1016/j.tecto.2014.06.030
[117] 王国强, 李向民, 徐学义, 等. 北山石炭纪-二叠纪火山岩成因及构造背景[J]. 岩石矿物学杂志, 2018, 37(6): 884-900. doi: 10.3969/j.issn.1000-6524.2018.06.002
[118] 许伟, 徐学义, 牛亚卓, 等. 北山南部早二叠世A型流纹岩地球化学特征及其地球动力学意义[J]. 岩石学报, 2018, 34(10): 3011-3032. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201810012.htm
[119] Wang Y, Luo Z, Santosh M, et al. The Liuyuan Volcanic Belt in NW China revisited: evidence for Permian rifting associated with the assembly of continental blocks in the Central Asian Orogenic Belt[J]. Geological Magazine, 2017, 154(2): 265-285. doi: 10.1017/S0016756815001077
[120] Xie W, Song X Y, Deng Y F, et al. Geochemistry and petrogenetic implications of a Late Devonian mafic-ultramafic intrusion at the southern margin of the Central Asian Orogenic Belt[J]. Lithos, 2012, 144/145(7): 209-230. http://www.sciencedirect.com/science/article/pii/S0024493712001028
[121] Su B X, Qin K Z, Santosh M, et al. The Early Permian mafic-ultramafic complexes in the Beishan Terrane, NW China: Alaskan-type intrusives or rift cumulates?[J]. Journal of Asian Earth Sciences, 2012, 66: 175-187.
[122] 李舢, 王涛, 童英, 等. 北山柳园地区双峰山早泥盆世A型花岗岩的确定及其构造演化意义[J]. 岩石矿物学杂志, 2009, 28(5): 407-421. doi: 10.3969/j.issn.1000-6524.2009.05.001
[123] 王立社, 杨建国, 谢春林, 等. 甘肃北山火石山哈尔根头口布花岗岩年代学、地球化学及其地质意义[J]. 地质学报, 2009, 83(3): 377-387. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200903008.htm
[124] 李舢, 王涛, 童英, 等. 北山辉铜山泥盆纪钾长花岗岩锆石U-Pb年龄、成因及构造意义[J]. 岩石学报, 2011, 27(10): 237-252. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201110022.htm
[125] Guo Q Q, Chung S, Xiao W J, et al. Petrogenesis and tectonic implications of Late Devonian arc volcanic rocks in southern Beishan orogen, NW China: Geochemical and Nd-Sr-Hf isotopic constraints[J]. Lithos, 2017, 278/281: 84-96. doi: 10.1016/j.lithos.2017.01.017
[126] Li S, Wilde S A, Wang T. Early Permian post-collisional high-K granitoids from Liuyuan area in southern Beishan orogen, NW China: Petrogenesis and tectonic implications[J]. Lithos, 2013, 179: 99-119. doi: 10.1016/j.lithos.2013.08.002
[127] Yuan Y, Zong K Q, He Z Y, et al. Geochemical evidence for Paleozoic crustal growth and tectonic conversion in the Northern Beishan Orogenic Belt, southern Central Asian Orogenic Belt[J]. Lithos, 2018, 302/303: 189-202. doi: 10.1016/j.lithos.2017.12.026
[128] 余吉远, 李建星, 孟勇, 等. 中澳合作填图试点1: 5万牛圈子幅区域地质图[M]. 西安; 西安地图出版社, 2016.
[129] Yu J Y, Guo L, Li J X, et al. The petrogenesis of sodic granites in the Niujuanzi area and constraints on the Paleozoic tectonic evolution of the Beishan region, NW China[J]. Lithos, 2016, 256/257: 250-268. doi: 10.1016/j.lithos.2016.04.003
[130] 李荣社, 计文化, 辜平阳. 造山带(蛇绿)构造混杂岩带填图方法[M]. 武汉: 中国地质大学出版社, 2016: 1-119.
① 李向民, 王国强, 余吉远, 等. 北山-祁连成矿带地质矿产综合研究报告. 2013.
② 甘肃省地质调查院. 1: 5万红岭幅区域地质调查报告. 2004.
③ 甘肃省地质调查院. 1: 25万红宝石幅区域地质调查报告. 2005.
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