塔里木地区寒武纪早期海陆格局
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摘要
寒武纪早期(基本相当于纽芬兰世和第二世)是塔里木地区海相烃源岩层的重要沉积期。对这一时期塔里木地区海陆格局的研究将有助于其海相油气资源潜力的评价。本文在前人研究的基础上,野外调查和收集分析地质露头剖面13条、钻井柱状剖面10条,并参考部分地震剖面资料,构建了塔里木地区寒武纪早期海陆环境格局,编制了海陆格局与构造-沉积环境图。在研究结果中,明确了铁门关一带的微陆块性质,并认为它与北库鲁克塔格台地同属塔里木北部被动陆缘;在塔里木陆表海盆地内,依据新的资料,划分了不同沉积环境区。
The Early Cambrian(corresponding to Terreneuvian and Series 2)is an important sedimentary period of marine source rocks in Tarim area.Researches on the framework of ocean and continent in Tarim area will help estimate the potential resources of the rocks.Based on previous studies,the authors investigated and analyzed 13 outcrops and 10 borehole sections,and consulted some seismic sections.By means of an analysis of stratigraphic and petrologic characteristics,the map for oceanic and continental framework and tectonic-sedimentary environment of Tarim area was compiled.It is pointed out that the area around Tiemenguan was a micro-landmass.The authors consider that both Tiemenguan micro-landmass and North Kuluketage underwater platform belonged to North Tarim passive continental margin.Furthermore,the authors divided the Tarim epeiric sea basin into different sedimentary environment areas on the basis of new data.
The Early Cambrian(corresponding to Terreneuvian and Series 2)is an important sedimentary period of marine source rocks in Tarim area.Researches on the framework of ocean and continent in Tarim area will help estimate the potential resources of the rocks.Based on previous studies,the authors investigated and analyzed 13 outcrops and 10 borehole sections,and consulted some seismic sections.By means of an analysis of stratigraphic and petrologic characteristics,the map for oceanic and continental framework and tectonic-sedimentary environment of Tarim area was compiled.It is pointed out that the area around Tiemenguan was a micro-landmass.The authors consider that both Tiemenguan micro-landmass and North Kuluketage underwater platform belonged to North Tarim passive continental margin.Furthermore,the authors divided the Tarim epeiric sea basin into different sedimentary environment areas on the basis of new data.
引文
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[2]黄汲清,姜春发,王作勋.新疆及邻区板块开合构造及手风琴式运动[J].新疆地质科学,1990,(1):3-16.Huang Jiqing,Jiang Chunfa,Wang Zuoxun.On the opening-closing tectonics and accordion movement of palte in Xinjiang andadjacent regions[J].Geoscience of Xinjiang,1990,(1):3-16(inChinese with English abstract).
[3]肖序常,汤耀庆,李锦轶,等.试论新疆北部大地构造演化[J].新疆地质科学,1990,(1):47-68.Xiao Xuchang,Tang Yaoqing,Li Jinyi,et al.On the tectonicevolution of the northern Xinjiang,Northwest China[J].Geoscienceof Xinjiang,1990,(1):47-68(in Chinese with English abstract).
[4]贾承造.中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997:390-424.Jia Chengzao.Tectonic Characteristics and Oil and Gas in Tarimbasin,China[M].Beijing:Petroleum Industry Press,1997:390-424(in Chinese with English abstract).
[5]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.He Guoqi,Li Maosong,Han Baofu.Geotectonic research ofsouthwest Tianshan and its west adjacent area,China[J].XinjiangGeology,2001,19(1):7-11(in Chinese with English abstract).
[6]冯增昭,鲍志东,吴茂炳,等.塔里木地区寒武纪岩相古地理[J].古地理学报,2006,8(4):427-439.Feng Zengzhao,Bao Zhidong,Wu Maobing,et al.Lithofaciespalaeogeography of the Cambrian in Tarim area[J].Journal ofPalaeogeography,2006,8(4):427-439(in Chinese with Englishabstract).
[7]朱杰辰,孙文鹏.新疆天山地区震旦系同位素地质研究[J].新疆地质,1987,5(1):55-61.Zhu Jiechen,Sun Wenpeng.Geochronology study of Sinian systemfor Tianshan region,Xinjiang[J].Xinjiang Geology,1987,5(1):55-61(in Chinese with English abstract).
[8]夏林圻,张国伟,夏祖春,等.天山古生代洋盆开启、闭合时限的岩石学约束—来自震旦纪、石炭纪火山岩的证据[J].地质通报,2002,21(2):55-62.Xia Linqi,Zhang Guowei,Xia Zuchun,et al.Constraints on thetiming of opening and closing of the Tianshan Paleozoic oceanicbasin:Evidence from Sinian and Carboniferous volcanic rocks[J].Geological Bulletin of China,2002,21(2):55-62(in Chinese withEnglish abstract).
[9]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.Yang Haibo,Gao Peng,Li Bing,et al.The geological character ofthe Sinian Dalubayi ophiolite in the West Tianshan,Xinjiang[J].Xinjiang Geology,2005,23(2):123-126(in Chinese with Englishabstract).
[10]潘裕生.青藏高原第五缝合带的发现与论证[J].地球物理学报,1994,37(2):184-192.Pan Yusheng.Discovery and evidence of the fifth suture zone ofQinghai-xizang plateau[J].Acta Geophysica Sinica,1994,37(2):184-192(in Chinese with English abstract).
[11]肖序常,王军,苏犁,等.再论西昆仑库地蛇绿岩及其构造意义[J].地质通报,2003,22(10):745-750.Xiao Xuchang,Wang Jun,Su Li,et al.A further discussion of theKudi ophiolite,West Kunlun,and its tectonic significance[J].Geological Bulletin of China,2003,22(10):745-750(in Chinesewith English abstract).
[12]许志琴,杨经绥,李海兵,等.造山的高原——青藏高原的地体拼合、碰撞造山及隆升机制[M].北京:地质出版社,2007:3-36.Xu Zhiqin,Yang Jingsui,Li Haibing,et al.0rogenic Plateaux—Terrane Amalgamation,Collision and Uplift in the Qinghal-TibetPlateau[M].Beijing:Geological Publishing House,2007:3-36(inChinese with English abstract).
[13]韩芳林,崔建堂,计文化,等.西昆仑其曼于特蛇绿混杂岩的发现及其地质意义[J].地质通报,2002,21(8-9):573-578.Han Fanglin,Cui Jiantang,Ji Wenhua,et al.Discovery of theQimanyute ophiolite in the West Kunlun and its geologicalsignificance[J].Geological Bulletin of China,2002,21(8-9):573-578(in Chinese with English abstract).
[14]李博秦,姚建新,王炬川,等.西昆仑柳什塔格峰西侧火山岩的特征、时代及地质意义[J].岩石学报,2007,23(11):2801-2810.Li Boqin,Yao Jianxin,Wang Juchuan,et al.Composition,age andgeological significance of the Liushitage volcanics in West Kunlunmountains[J].Acta Petrologica Sinica,2007,23(11):2801-2810(inChinese with English abstract).
[15]李荣社,计文化,赵振明,等.昆仑早古生代造山带研究进展[J].地质通报,2007,26(4):373-382.Li Rongshe,Ji Wenhua,Zhao Zhenming,et al.Progress in thestudy of the Early Paleozoic Kunlun orogenic belt[J].GeologicalBulletin of China,2007,26(4):373-382(in Chinese with Englishabstract).
[16]贾承造,魏国齐,姚慧君,等.盆地构造演化与区域构造地质[M].北京:石油工业出版社,1995:71-81.Jia Chengzao,Wei Guoqi,Yao Huijun,et al.Tectonic evolutionand regional structural geology[M].Beijing:Petroleum IndustryPress,1995:71-81(in Chinese with English abstract).
[17]贾承造,张师本,吴绍祖,等.塔里木盆地及周边地层[M].北京:科学出版社,2004:1-110.Jia Chengzao,Zhang Shiben,Wu Shaozu,at al.Stratigraphy of theTarim Basin and Adjacent Areas[M].Beijing:Science Press,2004:1-110(in Chinese with English abstract).
[18]何登发,李德生,吕修祥.中国西北地区含油气盆地构造类型[J].石油学报,1996,17(4):8-18.He Dengfa,Li Desheng,Lu Xiuxiang.Tectonic types ofpetroliferous basins in NW China[J].Acta Petrolei Sinica,1996,17(4):8-18(in Chinese with English abstract).
[19]何登发,周新源,张朝军,等.塔里木地区奥陶纪原型盆地类型及其演化[J].科学通报,2007,52(增刊):126-135.He Dengfa,Zhou Xinyuan,Zhang Chaojun,at al.Ordovicianprototype basins and evolution in Tarim area[J].Chinese ScienceBulletin,2007,52(supp.):126-135(in Chinese with Englishabstract).
[20]郭召杰,李茂松.中天山早古生代离散地体构造的讨论[J].北京大学学报(自然科学版),1993,29(3):356-362.Guo Zhaojie,Li Maosong.On the early Paleozoic dispersedterranes in Mid-Tianshan[J].Acta Scientiarum NaturaliumUnivereitatis Pekinensis,1993,29(3):356-362(in Chinese withEnglish abstract).
[21]冯增昭,鲍志东,吴茂炳,等.塔里木地区寒武纪和奥陶纪岩相古地理[M].北京:地质出版社,2005:59-71.Feng Zengzhao,Bao Zhidong,Wu Maobing,at al.Lithofaciespaleogeography of the Cambrian and Ordovician in Tarim Area[M].Beijing:Ceological Publishing House,2005:59-71(in Chinesewith English abstract).
[22]汪新文,陈发景.塔北—南天山地区震旦—奥陶纪盆-山构造演化及其与油气关系[J].现代地质,1997,11(3):313-321.Wang Xinwen,Chen Fajing.Sinian-Ordovician tectonic evolutionof North Tarim and South Tianshan region and its relation to oiland gas[J].Geoscience(Journal of Graduate School,ChinaUniversity of Geosciences),1997,11(3):313-321(in Chinese withEnglish abstract).
[23]周志毅.塔里木盆地各纪地层[M].北京:科学出版社,2001:1-80.Zhou Zhiyi.Stratigraphy of the Tarim Basin[M].Beijing:SciencePress,2001:1-80(in Chinese with English abstract).
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