2024 Vol. 47, No. 3
Article Contents

TENG Xuejian, FU Chao, LI Junjian, LI Zhidan, TANG Wenlong. 2024. Characteristics and geological implications of the Ophiolite Belts in the Sino-Mongolian Border Region. North China Geology, 47(3): 1-13.
Citation: TENG Xuejian, FU Chao, LI Junjian, LI Zhidan, TANG Wenlong. 2024. Characteristics and geological implications of the Ophiolite Belts in the Sino-Mongolian Border Region. North China Geology, 47(3): 1-13.

Characteristics and geological implications of the Ophiolite Belts in the Sino-Mongolian Border Region

  • This paper is the research of ophiolite.[Objective] Ophiolites, as fragments of ancient oceanic lithosphere, serve as a natural laboratory for studying the evolution of the lithospheric mantle, material cycling in subduction zones, and reconstructing paleogeographic patterns.The China-Mongolia border region is located within the Central Asian Orogenic Belt(CAOB), where ophiolite(mélange)belts intermittently crop out along both sides of the boundary, exhibiting blocky and zonal distributions.[Methods]To further clarify the tectonic evolution of the CentralAsian Orogenic Belt and restore its structural framework, this paper relies on the results of the China-Mongolia collaborative 1/1 000 000 geological map series compilation project, combined with previous studies on the ophiolite (mélange) belts in this region.[Results]Fourteen ophiolite (mélange) belts were identified in the study area.A comprehensive explanation of their spatial-temporal distribution characteristics was provided, and a spatial-temporal framework for the distribution of the ophiolite (mélange) belts was established.[Conclusions] The results indicate that the ophiolite belts along the China-Mongolia border exhibit a trend of progressively younger ages from west to east (Neoproterozoic to Early Permian).This reveals differences in the evolution of the oceanic lithospheric mantle between the western and eastern segments of the Central Asian Orogenic Belt.Most ophiolite (mélange)belts are of the SSZ (supra-subduction zone)type, closely related to subduction processes.However, the tectonic settings of fore-arc and back-arc environments remain controversial and require further study.
  • 加载中
  • [1] 白文吉,杨经绥,胡旭峰,等.1995.内蒙古贺根山蛇绿岩岩石成因和地壳增生的地球化学制约[J].岩石学报(S1):112-124.

    Google Scholar

    [2] 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[J].地球化学,23(4):339-349.

    Google Scholar

    [3] 卜国民,李华启,李文铅,等.2005.新疆塔克札勒蛇绿混杂岩中玄武质熔岩地球化学特征及其成因讨论[J].大地构造与成矿学,29(2):252-261.

    Google Scholar

    [4] 蔡文俊,李春昱.1983.新疆东准噶尔北缘板块构造初步研究[J].中国地质学会.中国地质科学院文集(1983 中英文合订本),2.

    Google Scholar

    [5] 曹荣龙,1994.新疆北部蛇绿岩及基性-超基性杂岩[J].新疆地质(1):25-31.

    Google Scholar

    [6] 陈森煌,刘道荣,包志伟,等.1991.华北地台北缘几个超基性岩带的侵位年代及其演化[J].地球化学,(2):128-133.

    Google Scholar

    [7] 陈哲夫,成守德,梁云海,等.1997.新疆开合构造与成矿[M].乌鲁木齐:新疆科技卫生出版社.

    Google Scholar

    [8] 崔日武.1988.新疆克拉麦里蛇绿岩的岩石化学特征及其生成环境探讨[D].

    Google Scholar

    [9] 董连慧,朱志新,屈迅,等.2010.新疆蛇绿岩带的分布特征及研究新进展[J].岩石学报,26(10):2894-2904.

    Google Scholar

    [10] 郭召杰,马瑞士,郭令智,等.1993.新疆东部三条蛇绿混杂岩带的比较研究[J].地质论评,39(3):236-247.

    Google Scholar

    [11] 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,(01):95-102.

    Google Scholar

    [12] 韩宝福,郭召杰,何国琦.2010.“钉合岩体”与新疆北部主要缝合带的形成时限[J].岩石学报,26(08):2233-2246.

    Google Scholar

    [13] 何国琦,李茂松,贾进斗,等.2001.论新疆东准噶尔蛇绿岩的时代及其意义[J].北京大学学报(自然科学版),37(6):852-858.

    Google Scholar

    [14] 何国琦,邵济安.1983.内蒙古东南部(昭盟)西拉木伦河一带早古生代蛇绿岩建造的确认及其大地构造意义[J].中国北方板块构造文集(第一集).北京:地质出版社:243-250.

    Google Scholar

    [15] 何世平,任秉琛,姚文光,等.2002.甘肃内蒙古北山地区构造单元划分[J].西北地质,35(4):30-40.

    Google Scholar

    [16] 黄金香,赵志丹,张宏飞,等.2006.内蒙古温都尔庙和巴彦敖包-交其尔蛇绿岩的元素与同位素地球化学:对古亚洲洋东部地幔域特征的限制[J].岩石学报,(12):2889-2900.

    Google Scholar

    [17] 黄萱,金成伟,孙宝山,等.1997.新疆阿尔曼太蛇绿岩时代的Nd-Sr同位素地质研究[J].岩石学报,13(1):85-91.

    Google Scholar

    [18] 黄增保,金霞.2006.甘肃红石山蛇绿岩地球化学特征及构造环境[J].地质科学,41(4):601-611.

    Google Scholar

    [19] 简平,刘敦一,张旗,等.2003.蛇绿岩及蛇绿岩中浅色岩的SHRIMP U-Pb 测年[J].地学前缘,10(4):439-456.

    Google Scholar

    [20] 金成伟,黄萱,徐永生,等.2001.洪古勒楞-阿尔曼太蛇绿岩及其与成矿关系[M].新疆金属矿产资源的基础研究.北京:科学出版社:21-57.

    Google Scholar

    [21] 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[J].科学通报,62(5):400-406.

    Google Scholar

    [22] 李锦轶.1995.新疆东准噶尔蛇绿岩的基本特征和侵位历史[J].岩石学报(S1):73-84.

    Google Scholar

    [23] 李锦轶.2004.新疆东部新元古代晚期和古生代构造格局及其演变[J].地质论评,50(3):304-322.

    Google Scholar

    [24] 李锦轶,肖序常,汤耀庆,等.1990.新疆东准噶尔卡拉麦里地区晚古生代板块构造的基本特征[J].地质论评, 36(4):305-316.

    Google Scholar

    [25] 李锦轶,杨天南,李亚萍,等.2009.东准噶尔卡拉麦里断裂带的地质特征及其对中亚地区晚古生代洋陆格局重建的约束[J].地质通报,28(12):1817-1826.

    Google Scholar

    [26] 李嵩龄,董富荣,冯新昌,等.2001.克拉麦里-塔克札勒-大黑山超镁铁岩岩石化学特征及其形成环境[J].新疆地质,19(2):155-156.

    Google Scholar

    [27] 李嵩龄,冯新昌,董富荣,等.1999.克拉麦里-塔克札勒-大黑山蛇绿岩建造稀土元素特征[J].新疆地质,(4):356-364.

    Google Scholar

    [28] 梁日暄.1994.内蒙古中段蛇绿岩特征及地质意义[J].中国区域地质,(01):37-45.

    Google Scholar

    [29] 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[J].地质学报,77(3):317-327.

    Google Scholar

    [30] 刘建峰.2009.内蒙古林西-东乌旗地区晚古生代岩浆作用及其对区域构造演化的制约[D].吉林大学.

    Google Scholar

    [31] 刘明强.2007.甘肃北山造山带红石山地区埃达克质花岗岩类的发现及其地质意义[J].岩石矿物学杂志,26(3):232-238.

    Google Scholar

    [32] 刘崴国.2011.东准噶尔玛因鄂博蛇绿混杂岩形成时代确定[J].新疆地质,29(4):385-388.

    Google Scholar

    [33] 刘伟,张湘炳.1993.乌伦古-斋桑泊构造杂岩带特征及其地质意义[C].新疆北部固体地球科学新进展[M].北京:科学出版社,217-228.

    Google Scholar

    [34] 刘希军,许继峰,侯青叶,等.2007.新疆东准噶尔克拉麦里蛇绿岩地球化学:洋脊俯冲的产物[J].岩石学报,23(7):1591-1602.

    Google Scholar

    [35] 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[J].西北地质,34(2):21-27.

    Google Scholar

    [36] 史仁灯.2005.蛇绿岩研究进展,存在问题及思考[J].地质论评,51(6):681-693.

    Google Scholar

    [37] 舒良树,卢华复,印栋浩,等.2001.新疆北部古生代大陆增生构造[J].新疆地质,19(1):59-63.

    Google Scholar

    [38] 舒良树,王玉净.2003.新疆卡拉麦里蛇绿岩带中硅质岩的放射虫化石[J].地质论评,49(4):408-412.

    Google Scholar

    [39] 宋泰忠,王瑾,林海,等.2008.内蒙古北山地区小黄山蛇绿岩地质特征[J].西北地质,41(3):55-63.

    Google Scholar

    [40] 唐红峰,苏玉平,刘丛强,等.2007.新疆北部卡拉麦里斜长花岗岩的锆石U-Pb 年龄及其构造意义[J].大地构造与成矿学,31(1):110-117.

    Google Scholar

    [41] 陶继雄,苏茂荣,白立兵.2004.内蒙古达尔罕茂明安联合旗满都拉地区索伦山蛇绿混杂岩的特征及构造意义[J].地质通报,23(12):1238-1242.

    Google Scholar

    [42] 汪帮耀,姜常义,李永军,等.2009.新疆东准噶尔卡拉麦里蛇绿岩的地球化学特征及大地构造意义[J].矿物岩石,29(3):74-82.

    Google Scholar

    [43] 王金荣,宋春晖,高军平,等.1995.阿拉善北部恩格尔乌苏蛇绿混杂岩的形成机制[J].兰州大学学报,(2):140-146.

    Google Scholar

    [44] 王荃,刘雪亚,李锦轶.1991.中国内蒙古中部的古板块构造[J].中国地质科学院院报(1):1-15.

    Google Scholar

    [45] 王廷印,王金荣,王士政.1992.阿拉善北部恩格尔乌苏蛇绿混杂岩带的发现及其构造意义[J].兰州大学学报(自然科学版),28(2):194-196.

    Google Scholar

    [46] 王玉净,樊志勇.1997.内蒙古西拉木伦河北部蛇绿岩带中二叠纪放射虫的发现及其地质意义[J].古生物学报,36(1):58-69.

    Google Scholar

    [47] 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[J].地学前缘,18(3):151-165.

    Google Scholar

    [48] 魏志军,黄增保,金霞,等.2004.甘肃红石山地区蛇绿混杂岩地质特征[J].西北地质,37(2):13-18.

    Google Scholar

    [49] 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[J].中国地质,33(3):476-486.

    Google Scholar

    [50] 吴国干,夏斌,李文铅,等.2005.新疆塔克札勒蛇绿混杂岩中安山岩的地球化学特征及其构造环境[J].大地构造与成矿学,29(2):242-251.

    Google Scholar

    [51] 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[J].地质学报,80(1):32-37.

    Google Scholar

    [52] 谢力,尹海权,周洪瑞,等.2014.内蒙古阿拉善地区恩格尔乌苏缝合带二叠纪放射虫及其地质意义[J].地质通报,33(5):691-697.

    Google Scholar

    [53] 肖序常,汤耀庆.1991.古中亚复合巨型缝合带南缘构造演化[M].北京:科学出版社.1-136.

    Google Scholar

    [54] 许继峰,陈繁荣,于学元,等.2001a.新疆北部阿尔泰地区库尔提蛇绿岩:古弧后盆地系统的产物[J].岩石矿物学杂志,(3):344-352.

    Google Scholar

    [55] 许继峰,梅厚钧,于学元,等.2001b.准噶尔北缘晚古生代岛弧中与俯冲作用有关的adakite 火山岩:消减板片部分熔融的产物[J].科学通报,46(8):684-688.

    Google Scholar

    [56] 薛建平,苏尚国,陈海舰,等.2017.内蒙古索伦山地区地幔橄榄岩中豆荚状铬铁找矿前景[J].科学技术与工程,17(25):25-32.

    Google Scholar

    [57] 薛建平,苏尚国,李成元,等.2017.内蒙古索伦山地区蛇绿岩岩石单元地质特征, 就位机制及时限[J].现代地质,31(3):498-507.

    Google Scholar

    [58] 杨合群,李英,赵国斌,等.2010.北山蛇绿岩特征及构造属性[J].西北地质,43(1):26-36.

    Google Scholar

    [59] 杨梅珍,吴宏恩,杨高学.2009.东准噶尔卡拉麦里SSZ 型蛇绿岩地球化学及其构造意义[J].岩石矿物学杂志,28(3):251-263.

    Google Scholar

    [60] 杨志华,董连慧,陈明勇,等.2005.在阿尔泰造山带富蕴-青河发现新的蛇绿岩混杂岩系[J].地学前缘,12(3):177-178.

    Google Scholar

    [61] 于福生,李金宝,王涛.2006.东天山红柳河地区蛇绿岩U-Pb 同位素年龄[J].地球学报,27(3):213-216.

    Google Scholar

    [62] 袁超,孙敏,龙晓平,等.2007.阿尔泰哈巴河群的沉积时代及其构造背景[J].岩石学报,23(7):1635-1644.

    Google Scholar

    [63] 张弛.1981.新疆蛇绿岩某些地质特征[J].地质论评,27(4):307-314.

    Google Scholar

    [64] 张海祥,牛贺才,于学元.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[J].科学通报,48(12):1350-1354.

    Google Scholar

    [65] 张旗,周国庆.2001.中国蛇绿岩.北京:科学出版社.

    Google Scholar

    [66] 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[J].岩石学报,24(4):803-809.

    Google Scholar

    [67] 张元元,郭召杰,刘畅.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[J].岩石学报,26(2):421-430.

    Google Scholar

    [68] 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[J].地质通报,31(6):834-842.

    Google Scholar

    [69] 赵茹石,周振环,毛金海,等.1994.甘肃省板块构造单元划分及其构造演化[J].中国区域地质,1:28-36.

    Google Scholar

    [70] 郑荣国,吴泰然,张文,等.2012.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,86(6):961-971.

    Google Scholar

    [71] 左国朝,何国琦,李红诚.1990.北山板块构造及成矿规律[Z].北京:北京大学出版社.

    Google Scholar

    [72] Ao S J, Xiao W J, Han C M, et al.2012.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, 149:606-625.

    Google Scholar

    [73] Coleman R G.1989.Continental growth of northwest China[J].Tec-tonics, 8:621-635.

    Google Scholar

    [74] Dewey J F, Bird J M.1971.Origin and emplacement of the ophiolite suite:Appalachian ophiolites in Newfoundland[J].Journal of Geo-physical Research(1896-1977), 76:3179-3206.

    Google Scholar

    [75] Dilek Y, Furnes H.2011.Ophiolite genesis and global tectonics: Geo-chemical and tectonic fingerprinting of ancient oceanic litho-sphere[J].GSA Bulletin, 123:387-411.

    Google Scholar

    [76] Iwata K, Obut O, Buslov M.1997.Devonian and Lower Carbonifer-ous radiolaria from the Chara ophiolite belt, East Kazakhstan[J].News of Osaka Micropaleontologist, 10:27-32.

    Google Scholar

    [77] Iwata K, Watanabe T, Akiyama M, et al.1994.Paleozoic microfossils from the Chara Belt (eastern Kazakhstan)[J].Russian Geology and Geophysics, 35:145-151.

    Google Scholar

    [78] Jian P, Kröner A, Windley B F, et al.2012.Carboniferous and Creta-ceous mafic-ultramafic massifs in Inner Mongolia (China): A SHRIMP zircon and geochemical study of the previously pre-sumed integral“Hegenshan ophiolite”[J].Lithos, 142-143:48-66.

    Google Scholar

    [79] Jian P, Liu DY, Kröner A, et al.2008.Time scale of an early to mid-Pa-leozoic orogenic cycle of the long-lived Central Asian Orogenic Belt, Inner Mongolia of China: Implications for continental growth[J].Lithos, 101:233-259.

    Google Scholar

    [80] Jian P, Liu D Y, Shi Y R, et al.2005.SHRIMP dating of SSZ ophiol-ites from northern Xinjiang Province, China:implications for gen-eration of oceanic crust in the Central Asian Orogenic Belt[J].Structural and tectonic correlation across the Central Asia orogen-ic collage:North-eastern segment, 246.

    Google Scholar

    [81] Kepezhinskas P K, Kepezhinskas K B, Pukhtel I S.1991.Lower Paleo-zoic oceanic crust in Mongolian Caledonides: SM-ND isotope and trace element data[J].Geophysical Research Letters, 18:1301-1304.

    Google Scholar

    [82] Khain E V, Bibikova E V, Salnikova E B, ea tl.2003.The Palaeo-Asian ocean in the Neoproterozoic and early Palaeozoic:new geo-chronologic data and palaeotectonic reconstructions[J].Precam-brian Research, 122:329-358.

    Google Scholar

    [83] Miao L C, Fan W M, Liu D Y, ea tl.2008.Geochronology and geo-chemistry of the Hegenshan ophiolitic complex: Implications for late-stage tectonic evolution of the Inner Mongolia-Daxinganling Orogenic Belt, China[J].Journal of Asian Earth Sciences, 32:348-370.

    Google Scholar

    [84] Robinson P T, Zhou M F, Hu X F, et al.1999.Geochemical constraints on the origin of the Hegenshan Ophiolite, Inner Mongolia, Chi-na[J].Journal of Asian Earth Sciences, 17:423-442.

    Google Scholar

    [85] Şengör A M C, Natal'in B A, Burtman V S.1993.Evolution of the Al-taid tectonic collage and Palaeozoic crustal growth in Eurasia[J].Nature, 364:299-307.

    Google Scholar

    [86] Tomurtogoo O, Windley B F, Kröner A, et al.2005.Zircon age and oc-currence 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, 162:125-134.

    Google Scholar

    [87] Volkova N, Sklyarov E.2007.High-pressure complexes of Central Asian Fold Belt: geologic setting, geochemistry, and geodynamic implications[J].Russian Geology and Geophysics, 48:83-90.

    Google Scholar

    [88] Wang Q, Liu X.1986.Paleoplate tectonics between Cathaysia and An-garaland in inner Mongolia of China[J].Tectonics, 5:1073-1088.

    Google Scholar

    [89] 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[J].Tectonics, 22.

    Google Scholar

    [90] Xiao W J, Han C M, Yuan C, et al.2008.Middle Cambrian to Permian subduction-related accretionary orogenesis of Northern Xinjiang, NW China: Implications for the tectonic evolution of central Asia[J].Journal of Asian Earth Sciences, 32:102-117.

    Google Scholar

    [91] Xiao W J, Mao Q G, Windley B F, et al.2010.Paleozoic multiple ac-cretionary and collisional processes of the Beishan orogenic col-lage[J].American Journal of Science, 310:1553-1594.

    Google Scholar

    [92] Xiao W J, Windley B F, Badarch G, et al.2004.Palaeozoic accretion-ary and convergent tectonics of the southern Altaids: implications for the growth of Central Asia[J].Journal of the Geological Soci-ety 161:339-342.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(9) PDF downloads(0) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint