中国—吉尔吉斯天山成矿单元划分及其特征
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摘要
中国—吉尔吉斯天山地处中亚天山造山带中段,是古亚洲构造域的重要组成部分,地质构造复杂,矿产资源丰富。在收集境内、外大量地质、矿产资料及图件的基础上,通过近年来对研究区内地层、构造、岩浆及矿产的研究,在大地构造单元划分基础上对研究区内天山进行了成矿单元划分,划分出北天山—伊犁、中天山和南天山—塔里木3个成矿省,进一步划分为22个成矿带和58个成矿亚带,总结了各成矿单元的地质及矿产特征,为天山成矿带矿产勘查和地质大调查工作部署提供有益的思路和依据。
Located in the middle of Tianshan orogenic belt, the study area in Tianshan Mountains of China and Kyrgyzstan has complex geological structure and rich mineral resources. Previous work in Tianshan was conducted respectively in China and Kyrgyzstan.On the basis of previous studies, the authors investigated the extending trends of various tectonic units and their relationships. The examination of stratigraphy,tectonics,magmatism and ore deposits in the Tianshan Mountains of China and Kyrgyzstan in recent years has disclosed that the study area may be classified into one first-order metallogenic domain(the Paleo-Asia metallogenic domain),three second-order metallogenic provinces, 22 third-order metallogenic belts and 58 fourth-order metallogenic subbelts. This paper gives a detailed description of the geology and metallogenesis in individual metallogenic belts in the study area.
Located in the middle of Tianshan orogenic belt, the study area in Tianshan Mountains of China and Kyrgyzstan has complex geological structure and rich mineral resources. Previous work in Tianshan was conducted respectively in China and Kyrgyzstan.On the basis of previous studies, the authors investigated the extending trends of various tectonic units and their relationships. The examination of stratigraphy,tectonics,magmatism and ore deposits in the Tianshan Mountains of China and Kyrgyzstan in recent years has disclosed that the study area may be classified into one first-order metallogenic domain(the Paleo-Asia metallogenic domain),three second-order metallogenic provinces, 22 third-order metallogenic belts and 58 fourth-order metallogenic subbelts. This paper gives a detailed description of the geology and metallogenesis in individual metallogenic belts in the study area.
引文
[1]夏林圻.天山岩浆作用[M].北京:地质出版社,2007:4-18.
[2]陈哲夫,周守澐,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,1999:26-27.
[3]何国琦,成守德,徐新,等.中国新疆及邻区大地构造图1:2500000[M].北京:地质出版社,2005.
[4]王洪亮,徐学义,何世平,等.中国天山及邻区地质图1∶1000000[M].北京:地质出版社,2007:35-42.
[5]ТурсунгазиевБТ,ПетровОВ.ГеологическаякартаКыргызскойРеспублики(1∶500000)[M].Бишкек:ВСЕГЕЧ,2008.
[6]李廷栋.亚欧地质图(1∶5000000)[M].北京:地质出版社,1997.
[7]李廷栋,Daukeev S Z,Kim B C,等.亚洲中部及邻区1∶2500000地质图[M].北京:地质出版社,2008.
[8]Setlman R,Shatov V,Yakubchuk A.Mineral Deposits map of Central Asia(1∶1500000)[M].London:Cercams-NHM,IAGOD and IGCP-473,2004.
[9]王广瑞.中国新疆北部及邻区构造-建造图[M].武汉:中国地质大学出版社,1996.
[10]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.
[11]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.
[12]王作勋,邬继易,吕喜朝,等.天山多旋回构造演化及成矿[M].北京:科学出版社,1990:53-59.
[13]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,1992:47-68.
[14]ДженчураеваРД..Геодинамикаметаллогенияирудогенез[M].Бишкек:Илим,2010:1-71.
[15]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.
[16]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.
[17]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):1-13.
[18]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,1996:105-109.
[19]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,1993:27-28.
[20]Simonov V A,Sakiev K S,Volkova N I,et al.Conditions of formation of the Atbashi Ridge eclogites(South Tien Shan)[J].Russ.Geol.Geophys.,2008,49:803-815.
[21]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.
[22]Buslov M M,Saphonova I Y,Watanabe O 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.
1李宝强,孟广路,贾群子,等.中吉天山1∶100万成矿规律图编制与研究项目成果报告.地质调查项目成果报告.2013:60-176.
[2]陈哲夫,周守澐,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,1999:26-27.
[3]何国琦,成守德,徐新,等.中国新疆及邻区大地构造图1:2500000[M].北京:地质出版社,2005.
[4]王洪亮,徐学义,何世平,等.中国天山及邻区地质图1∶1000000[M].北京:地质出版社,2007:35-42.
[5]ТурсунгазиевБТ,ПетровОВ.ГеологическаякартаКыргызскойРеспублики(1∶500000)[M].Бишкек:ВСЕГЕЧ,2008.
[6]李廷栋.亚欧地质图(1∶5000000)[M].北京:地质出版社,1997.
[7]李廷栋,Daukeev S Z,Kim B C,等.亚洲中部及邻区1∶2500000地质图[M].北京:地质出版社,2008.
[8]Setlman R,Shatov V,Yakubchuk A.Mineral Deposits map of Central Asia(1∶1500000)[M].London:Cercams-NHM,IAGOD and IGCP-473,2004.
[9]王广瑞.中国新疆北部及邻区构造-建造图[M].武汉:中国地质大学出版社,1996.
[10]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.
[11]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.
[12]王作勋,邬继易,吕喜朝,等.天山多旋回构造演化及成矿[M].北京:科学出版社,1990:53-59.
[13]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,1992:47-68.
[14]ДженчураеваРД..Геодинамикаметаллогенияирудогенез[M].Бишкек:Илим,2010:1-71.
[15]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.
[16]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.
[17]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):1-13.
[18]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,1996:105-109.
[19]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,1993:27-28.
[20]Simonov V A,Sakiev K S,Volkova N I,et al.Conditions of formation of the Atbashi Ridge eclogites(South Tien Shan)[J].Russ.Geol.Geophys.,2008,49:803-815.
[21]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.
[22]Buslov M M,Saphonova I Y,Watanabe O 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.
1李宝强,孟广路,贾群子,等.中吉天山1∶100万成矿规律图编制与研究项目成果报告.地质调查项目成果报告.2013:60-176.