中国—吉尔吉斯斯坦天山构造格架与演化
|
摘要
中国—吉尔吉斯斯坦天山地处中亚天山造山带中段,地质构造复杂,矿产资源丰富。在前人资料基础上,基于区域构造-岩石组合的分布发育及时空属性特征,统一将研究区划分为哈萨克斯坦和塔里木两大板块,二者由南天山晚古生代缝合带所焊接。其中,进一步划分为5个二级单元,18个三级单元。研究认为,研究区内北、中、南天山构造格架连续,在800 Ma(相当于南华纪下限)前后都完成了大陆块体的拼合,成为全球新元古代罗迪尼亚超大陆的组成部分。此后经历了大致相同的构造演化史,从中二叠世开始全区转化成陆内盆山构造格局,新生代印度大陆同欧亚大陆碰撞使这一陆内盆山构造格局不断臻于完善。
Tianshan in China and Kyrgyzstan is located in the middle of Tianshan orogenic belt,with complex geological structure and abundant mineral resources. On the basis of previous studies,and according to the distribution and space-time characteristics of regional tectonic-rock combination,the authors divided the study area into Kazakhstan and Tarim plates,and the two plates are connected by Late Paleozoic suture zone of southern Tianshan. Then the study area was further divided into five secondary units and eighteen third-level units. The results show that the northern,middle and southern Tianshan tectonic frameworks are continuous in the study area and the continental blocks were split at 800 Ma( equivalent to the bottom of Nanhua),which become parts of the Neoproterozoic Rodinia supercontinent. Later,the study area has experienced roughly the same structural evolution.From the beginning of the Middle Permian,the area transferredin to continental basin-mountain tectonic pattern.In Cenozoic,the collision between subcontinent of India and Eurasia has improved the continental basin-mountain tectonics pattern.
Tianshan in China and Kyrgyzstan is located in the middle of Tianshan orogenic belt,with complex geological structure and abundant mineral resources. On the basis of previous studies,and according to the distribution and space-time characteristics of regional tectonic-rock combination,the authors divided the study area into Kazakhstan and Tarim plates,and the two plates are connected by Late Paleozoic suture zone of southern Tianshan. Then the study area was further divided into five secondary units and eighteen third-level units. The results show that the northern,middle and southern Tianshan tectonic frameworks are continuous in the study area and the continental blocks were split at 800 Ma( equivalent to the bottom of Nanhua),which become parts of the Neoproterozoic Rodinia supercontinent. Later,the study area has experienced roughly the same structural evolution.From the beginning of the Middle Permian,the area transferredin to continental basin-mountain tectonic pattern.In Cenozoic,the collision between subcontinent of India and Eurasia has improved the continental basin-mountain tectonics pattern.
引文
[1]夏林圻,夏祖春,徐学义,等.天山岩浆作用[M].北京:地质出版社,2007:4-18.
[2]Турсунгазиев Б Т,Петров О В.Геологическаяq,арта,Кыргызской,Республики(1∶500 000)[M].Бишкек:ВСЕГЕЧ,2008.
[3]李廷栋.亚欧地质图(1∶5 000 000)[M].北京:地质出版社,1997.
[4]李廷栋,Uzhkenov B S,Mazorov A K,等.亚洲中部及邻区地质图1∶2 500 000地质图[M].北京:地质出版社,2008.
[5]李宝强,孟广路.中国新疆及邻区大地构造图1∶1 500 000及说明书[M].北京:地质出版社,2014.
[6]王广瑞.中国新疆北部及邻区构造-建造图说明书[M].武汉:中国地质大学出版社,1996.
[7]何国琦,成守德,徐新,等.中国新疆及邻区大地构造图1∶2 500 000[M].北京:地质出版社,2005.
[8]王洪亮,徐学义,何世平,等.中国天山及邻区1∶100万地质图[M].北京:地质出版社,2007.
[9]何国琦,李茂松,韩宝福.中国西南天山及邻区大地构造研究[J].新疆地质,2001,19(1):7-11.
[10]成守德,刘通,王世伟.中亚五国大地构造单元划分简述[J].新疆地质,2010,28(1):16-21.
[11]王作勋,邬继易,吕喜朝,等.天山多旋回构造演化与成矿[M].北京:科学出版社,1990.
[12]肖序常,汤耀庆,冯益民,等.新疆北部及邻区大地构造[M].北京:地质出版社,1992.
[13]Дженчураева Р Д.Геодинамика,металлогения и рудогенез[M].Илим.Бишкек,2010.
[14]肖序常,刘训,高锐,等.新疆南部地壳结构和构造演化[M].北京:商务印书馆,2004.
[15]肖序常,汤跃庆,冯益民,等.新疆北部大地构造及其演化[M].北京:地质出版社,1990.
[16]肖序常,汤耀庆.古中亚复合巨型缝合带南缘构造演化[M].北京:科学技术出版社,1991.
[17]肖文交,韩春明,袁超,等.新疆北部石炭纪—二叠纪独特的构造-成矿作用:对古亚洲洋构造域南部大地构造演化的制约[J].岩石学报,2006,22(5):1062-1076.
[18]车自成,刘良,罗金海.中国及其邻区区域大地构造学[M].北京:科学出版社,2002.
[19]左国朝,张作衡,王志良,等.新疆西天山地区构造单元划分、地层系统及其构造演化[J].地质论评,2008,54(6):748-767.
[20]何国琦,朱永峰.中国新疆及其邻区地质矿产对比研究[J].中国地质,2006,33(3):451-460.
[21]李锦轶,何国琦,徐新,等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报,2006,80(1):148-168.
[22]李锦轶.中国大陆地壳"镶嵌与叠覆"的结构特征及其演化[J].地质通报,2004,23(9/10):986-1004.
[23]李锦轶,王克卓,李亚萍,等.天山山脉地貌特征、地壳组成与地质演化[J].地质通报,2006,25(8):896-909.
[24]吴世敏,马瑞士,卢华复,等.新疆西天山古生代构造演化[J].桂林工学院学报,1996,16(2):95-101.
[25]李曰俊,杨海军,赵岩,等.南天山区域大地构造与演化[J].大地构造与成矿,2009,33(1):94-104.
[26]左国朝,刘义科,张招崇,等.中亚地区中、南天山造山带构造演化及成矿背景分析[J].现代地质,2011,25(1):1-14.
[27]陈哲夫,周守云,乌统旦.中亚大型金属矿床特征与成矿环境[M].乌鲁木齐:新疆科技卫生出版社,1999.
[28]孟广路,王斌,范堡程,等.中国—吉尔吉斯天山成矿单元划分及其特征[J].地质通报,2015,34(4):696-709.
[29]李宝强,孟广路,曹新,等.中亚天山—帕米尔地区成矿地质背景[J].地质通报,2015,34(4):686-695.
[30]查显锋,李荣社,辜平阳,等.北阿尔金红柳沟—拉配泉构造混杂岩带东段的结构、构造[J].中国地质调查,2015,2(8):35-42.
[31]李荣社,陈隽璐,马中平,等.中国西北部造山带中几个古生代俯冲增生楔的识别与确认[J].中国地质调查,2016,3(1):44-51.
[30]孟广路,王斌,李宝强,等.乌兹别克斯坦穆龙套金矿床研究进展[J].地质科技情报,2013,32(5):160-166.
[31]Buslov M M,Saphonova I Y,Watanabe T,et al.Evolution of the Paleo-Asian Ocean(Altai-Sayan Region,Central Asia)and collision of possible Gondwana-derived terranes with the southern marginal part of the Siberian continent[J].Geoscience Journal,2001,5(3):203-224.
[32]杨蔚华,刘友梅,高计元.新疆北部石炭系拗拉槽与浊流盆地沉积序列中铅、锌、金等层控矿床[M].北京:科学出版社,1993.
[33]Qian Q,Gao J,Reiner K,et al.Early Paleozoic tectonic evolution of the Chinese South Tianshan Orogen:Constraints from SHRIMP zircon U-Pb geochronology and geochemistry of basaltic and dioritic rocks from Xiate,NW China[J].International Journal of Earth Sciences,2009,98(3):551-569.
[34]Simonov V A,Sakiev K S,Volkova N I,et al.Conditions of formation of the Atbashi Ridge eclogites(South Tien Shan)[J].Russian Geology and Geophysics,2008,49:803-815.
[35]杨经绥,徐向珍,李天福,等.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[J].岩石学报,2011,27(1):77-95.
[36]高俊,钱青,龙灵利,等.西天山的增生造山过程[J].地质通报,2009,28(12):1804-1816.
[37]Gao J,Klemd R.Primary fluids entrapped at blueschist to eclogite transition:Evidence from the Tianshan meta-subduction complex in northwestern China[J].Contributions to Mineralogy and Petrology,2001,142(1):1-14.
[38]Klemd R,Br9cker M,Hacker B R,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.
[39]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,2010,22:473-478.
[40]郝杰,刘小汉.南天山蛇绿混杂岩形成时代及大地构造意义[J].地质科学,1993,19(1):93-95.
[41]高俊,肖序常,汤耀庆,等.新疆西南天山蓝片岩的变质作用p TDt轨迹及构造演化[J].地质论评,1994,40(6):544-553.
[42]王宝瑜,朗智君,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]刘本培,王自强,张传恒,等.西南天山构造格局与演化[M].武汉:中国地质大学出版社,1996.
[44]胡蔼琴,张国新,李启新,等.新疆北部同位素地球化学与地壳演化[M].北京:科学出版社,1993.
[45]高振家,陈克强.新疆的南华系及我国南华系的几个地质问题——纪念恩师王曰伦先生诞辰一百周年[J].地质调查与研究,2003,26(1):8-14.
[46]朱宝清,冯益民,杨军录,等.新疆中天山干沟一带蛇绿混杂岩和志留纪前陆盆地的发现及其意义[J].新疆地质,2002,20(4):326-330.
[47]陈博,马中平,孟广路,等.吉尔吉斯斯坦中天山地质特征及研究进展[J].中国地质,2016,43(2):458-469.
[48]杨海波,高鹏,李兵,等.新疆西天山达鲁巴依蛇绿岩地质特征[J].新疆地质,2005,23(2):123-126.
[49]周鼎武,苏梨,简平,等.南天山榆树沟蛇绿岩地体中高压麻粒岩SHRIMP锆石U-Pb年龄及构造意义[J].科学通报,2004,49(14):1411-1415.
[2]Турсунгазиев Б Т,Петров О В.Геологическаяq,арта,Кыргызской,Республики(1∶500 000)[M].Бишкек:ВСЕГЕЧ,2008.
[3]李廷栋.亚欧地质图(1∶5 000 000)[M].北京:地质出版社,1997.
[4]李廷栋,Uzhkenov B S,Mazorov A K,等.亚洲中部及邻区地质图1∶2 500 000地质图[M].北京:地质出版社,2008.
[5]李宝强,孟广路.中国新疆及邻区大地构造图1∶1 500 000及说明书[M].北京:地质出版社,2014.
[6]王广瑞.中国新疆北部及邻区构造-建造图说明书[M].武汉:中国地质大学出版社,1996.
[7]何国琦,成守德,徐新,等.中国新疆及邻区大地构造图1∶2 500 000[M].北京:地质出版社,2005.
[8]王洪亮,徐学义,何世平,等.中国天山及邻区1∶100万地质图[M].北京:地质出版社,2007.
[9]何国琦,李茂松,韩宝福.中国西南天山及邻区大地构造研究[J].新疆地质,2001,19(1):7-11.
[10]成守德,刘通,王世伟.中亚五国大地构造单元划分简述[J].新疆地质,2010,28(1):16-21.
[11]王作勋,邬继易,吕喜朝,等.天山多旋回构造演化与成矿[M].北京:科学出版社,1990.
[12]肖序常,汤耀庆,冯益民,等.新疆北部及邻区大地构造[M].北京:地质出版社,1992.
[13]Дженчураева Р Д.Геодинамика,металлогения и рудогенез[M].Илим.Бишкек,2010.
[14]肖序常,刘训,高锐,等.新疆南部地壳结构和构造演化[M].北京:商务印书馆,2004.
[15]肖序常,汤跃庆,冯益民,等.新疆北部大地构造及其演化[M].北京:地质出版社,1990.
[16]肖序常,汤耀庆.古中亚复合巨型缝合带南缘构造演化[M].北京:科学技术出版社,1991.
[17]肖文交,韩春明,袁超,等.新疆北部石炭纪—二叠纪独特的构造-成矿作用:对古亚洲洋构造域南部大地构造演化的制约[J].岩石学报,2006,22(5):1062-1076.
[18]车自成,刘良,罗金海.中国及其邻区区域大地构造学[M].北京:科学出版社,2002.
[19]左国朝,张作衡,王志良,等.新疆西天山地区构造单元划分、地层系统及其构造演化[J].地质论评,2008,54(6):748-767.
[20]何国琦,朱永峰.中国新疆及其邻区地质矿产对比研究[J].中国地质,2006,33(3):451-460.
[21]李锦轶,何国琦,徐新,等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报,2006,80(1):148-168.
[22]李锦轶.中国大陆地壳"镶嵌与叠覆"的结构特征及其演化[J].地质通报,2004,23(9/10):986-1004.
[23]李锦轶,王克卓,李亚萍,等.天山山脉地貌特征、地壳组成与地质演化[J].地质通报,2006,25(8):896-909.
[24]吴世敏,马瑞士,卢华复,等.新疆西天山古生代构造演化[J].桂林工学院学报,1996,16(2):95-101.
[25]李曰俊,杨海军,赵岩,等.南天山区域大地构造与演化[J].大地构造与成矿,2009,33(1):94-104.
[26]左国朝,刘义科,张招崇,等.中亚地区中、南天山造山带构造演化及成矿背景分析[J].现代地质,2011,25(1):1-14.
[27]陈哲夫,周守云,乌统旦.中亚大型金属矿床特征与成矿环境[M].乌鲁木齐:新疆科技卫生出版社,1999.
[28]孟广路,王斌,范堡程,等.中国—吉尔吉斯天山成矿单元划分及其特征[J].地质通报,2015,34(4):696-709.
[29]李宝强,孟广路,曹新,等.中亚天山—帕米尔地区成矿地质背景[J].地质通报,2015,34(4):686-695.
[30]查显锋,李荣社,辜平阳,等.北阿尔金红柳沟—拉配泉构造混杂岩带东段的结构、构造[J].中国地质调查,2015,2(8):35-42.
[31]李荣社,陈隽璐,马中平,等.中国西北部造山带中几个古生代俯冲增生楔的识别与确认[J].中国地质调查,2016,3(1):44-51.
[30]孟广路,王斌,李宝强,等.乌兹别克斯坦穆龙套金矿床研究进展[J].地质科技情报,2013,32(5):160-166.
[31]Buslov M M,Saphonova I Y,Watanabe T,et al.Evolution of the Paleo-Asian Ocean(Altai-Sayan Region,Central Asia)and collision of possible Gondwana-derived terranes with the southern marginal part of the Siberian continent[J].Geoscience Journal,2001,5(3):203-224.
[32]杨蔚华,刘友梅,高计元.新疆北部石炭系拗拉槽与浊流盆地沉积序列中铅、锌、金等层控矿床[M].北京:科学出版社,1993.
[33]Qian Q,Gao J,Reiner K,et al.Early Paleozoic tectonic evolution of the Chinese South Tianshan Orogen:Constraints from SHRIMP zircon U-Pb geochronology and geochemistry of basaltic and dioritic rocks from Xiate,NW China[J].International Journal of Earth Sciences,2009,98(3):551-569.
[34]Simonov V A,Sakiev K S,Volkova N I,et al.Conditions of formation of the Atbashi Ridge eclogites(South Tien Shan)[J].Russian Geology and Geophysics,2008,49:803-815.
[35]杨经绥,徐向珍,李天福,等.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[J].岩石学报,2011,27(1):77-95.
[36]高俊,钱青,龙灵利,等.西天山的增生造山过程[J].地质通报,2009,28(12):1804-1816.
[37]Gao J,Klemd R.Primary fluids entrapped at blueschist to eclogite transition:Evidence from the Tianshan meta-subduction complex in northwestern China[J].Contributions to Mineralogy and Petrology,2001,142(1):1-14.
[38]Klemd R,Br9cker M,Hacker B R,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.
[39]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,2010,22:473-478.
[40]郝杰,刘小汉.南天山蛇绿混杂岩形成时代及大地构造意义[J].地质科学,1993,19(1):93-95.
[41]高俊,肖序常,汤耀庆,等.新疆西南天山蓝片岩的变质作用p TDt轨迹及构造演化[J].地质论评,1994,40(6):544-553.
[42]王宝瑜,朗智君,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]刘本培,王自强,张传恒,等.西南天山构造格局与演化[M].武汉:中国地质大学出版社,1996.
[44]胡蔼琴,张国新,李启新,等.新疆北部同位素地球化学与地壳演化[M].北京:科学出版社,1993.
[45]高振家,陈克强.新疆的南华系及我国南华系的几个地质问题——纪念恩师王曰伦先生诞辰一百周年[J].地质调查与研究,2003,26(1):8-14.
[46]朱宝清,冯益民,杨军录,等.新疆中天山干沟一带蛇绿混杂岩和志留纪前陆盆地的发现及其意义[J].新疆地质,2002,20(4):326-330.
[47]陈博,马中平,孟广路,等.吉尔吉斯斯坦中天山地质特征及研究进展[J].中国地质,2016,43(2):458-469.
[48]杨海波,高鹏,李兵,等.新疆西天山达鲁巴依蛇绿岩地质特征[J].新疆地质,2005,23(2):123-126.
[49]周鼎武,苏梨,简平,等.南天山榆树沟蛇绿岩地体中高压麻粒岩SHRIMP锆石U-Pb年龄及构造意义[J].科学通报,2004,49(14):1411-1415.