全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

塔里木盆地西北缘晚新生代印干断层的运动学特征及其区域构造意义

, PP. 184-193

Keywords: 塔里木西北缘,晚新生代,印干断层,运动学特征,区域构造意义

Full-Text   Cite this paper   Add to My Lib

Abstract:

塔里木盆地西北缘NW走向的印干断层为逆冲断层,断层带指向构造证据表明印干断层的逆冲方向为NE向,与柯坪冲断系SE向推覆明显不同。地层学、断层切割关系等证据显示印干断层形成早于更新世活动的柯坪冲断系,活动期主要在上新世至早更新世。研究结果表明,柯坪塔格地区晚新生代发育两期方向不同的逆冲推覆构造,印干断层是上新世帕米尔构造结前陆冲断带的前缘冲断层,而柯坪冲断系是更新世以来南天山向塔里木盆地方向的前陆冲断带。

References

[1]  蔡东升,卢华复,贾东.1996.塔里木盆地西北缘柯坪造山带变形分析.北京:科学出版社:131-138.
[2]  卢华复,贾东,蔡东升,吴世敏,陈楚铭,施央申,郭令智.1998.塔西北柯坪剪切挤压构造. 高校地质学报,4(1):49-58.
[3]  孟庆龙,李曰俊,师骏,敬兵,冯晓军,赵岩.2008.塔里木盆地西部色力布亚断裂和康西断裂的主要特征及活动时代.地质科学,43(2):282-293.
[4]  肖安成,杨树锋,李曰俊,王清华,陈汉林,程晓敢.2005.塔里木盆地巴楚隆起断裂系统主要形成时代的新认识.地质科学,40(2):291-302.
[5]  朱德丰,刘和甫,吴根耀.2008.塔里木盆地西部吐木休克断裂带的主要特征和构造演化.地质科学,43(2):209-227.
[6]  Allen M B and Stephen V J.1999.Late Cenozoic tectonics of the Kepingtage thrust zone:Interaction between the Tian Shan and the Tarim Basin,northwest China.Tectonics, 18(4):639-654.
[7]  Chen J,Burbank D W,Scharer K M,Sobel E,Yin J H,Rubin C and Rubin Z.2002.Magnetochronology of the upper Cenozoic strata in the southwestern Chinese Tian Shan:Rates of pleistocene folding and thrusting.Earth and Planetary Science Letters, 195:113-130.
[8]  Cowgill E.2010.Cenozoic right?slip faulting along the eastern margin of the Pamir salient,northwestern China.GSA Bulletin, 122(1/2): 145-161.
[9]  Dupont?Nivet G,Guo Z,Butler R F and Jia C.2002.Discordant paleomagnetic direction in Miocene rocks from the central Tarim Basin:Evidence for local deformation and inclination shallowing.Earth and Planetary Science Letters, 199:473-482.
[10]  Fu B H,Lin A M,Keni?ichi K,Tadashi M and Guo J M.2003.Active faulting in the northeastern Pamir,NW China.Xinjiang Geology,21 (1):1-8.
[11]  H e D F,Suppe J and Guan S W.2005.Large?scale thrusting along the north margin of the Qinghai?Tibetan Plateau:Growth fault?bend folding of He tian′nan anticline,southwest Tarim Basin,China // International Conference on Theory and Application of Fault?related Folding in Foreland Basins (abstract). Jia D,Lu H F,Cai D S,Wu S M,Shi Y S and Chen C M.1998.Structural features of northern Tarim Basin:Implications for regional tectonics and petroleum traps.AAPG,82(1):147.
[12]  Robinson A C,Yin A,Manning C E,Harrison T M,Zhang S H and Wang X F.2007.Cenozoic evolution of the eastern Pamir:Implications for strain?accommodation mechanisms at the western end of the Himalayan?Tibetan orogen.Geological Society of America,119:882-896.
[13]  Sobel E R,Schoenbohmb L M,Chen J,Thiede R,Stockli D F,Sudo M and Strecker M R.2011.Late Miocene?Pliocene deceleration of dextral slip between Pamir and Tarim:Implications for Pamir orogenesis.Earth and Planetary Science Letters,304:369-378.
[14]  Tapponnier P,Peltzer G,Le Dain A Y and Armijo R.1982. Propagating extrusion tectonics in Asia:New insights from simple experiments with plasticine.Geology,10:611-616.
[15]  Turner S A,Jian L G and John C W.2011.Structural evolution of the Piqiang Fault Zone,NW Tarim Basin,China.Journal of Asian Earth Sciences,40:394-402.
[16]  Yang S M,Li J and Wang Q.2008.The deformation pattern and fault rate in the Tian Shan Mountains inferred from GPS observations.Science in China (Earth Science), 51: 1064-1080.
[17]  Yin A,Nie S,Craig P and Harrison T M.1998.Late Cenozoic tectonic evolution of the southern Chinese Tianshan.Tectonics,17:1-27.
[18]  陈杰,卢演俦,丁国瑜.2001a.塔里木西缘晚新生代造山过程的记录――磨石建造及生长地层和生长不整合.第四纪研究,21(6):528-539.
[19]  陈杰,丁国瑜,Burbank,D W, Scharer K, Rubin C, Sobel E, 曲国胜,沈军,尹金辉,赵瑞斌.2001b.中国西南天山山前的晚新生代构造与地震活动.中国地震,17(2):134-155.
[20]  何文渊,李江海,钱详麟,郑多明.2002.塔里木盆地柯坪断隆断裂构造分析.中国地质,29(1):37-43.
[21]  何文渊,杨宪一,刘胜.2003.塔里木盆地西北部构造演化特征――从皮羌断裂发育史想到.地球学报,24:17-21.
[22]  贾承造等.1997.中国塔里木盆地构造特征与油气.北京:石油工业出版社: 1-5.
[23]  李曰俊,吴根耀,雷刚林,张敬洲,王月然,刘亚雷.2008.新疆库车新生代前陆褶皱冲断带的变形特征、时代和机制.地质科学,43(3):488-506.
[24]  林畅松,刘景彦.2002.库车坳陷第三系构造层序的构成特征及其对前陆构造作用的响应.中国科学(D辑),32(3):177-183.
[25]  裴军令,李海兵,司家亮,潘家伟,吴富?,孙知明,赵越.2011.早更新世以来青藏高原隆升作用在塔里木盆地腹地的响应.岩石学报,27(11):3487-3498.
[26]  曲国胜,李亦刚,陈杰,宁宝坤,李岩峰,李军,尹军平.2003.柯坪塔格推覆构造几何学、运动学及其构造演化.地学前缘,10 (增刊):142-152.
[27]  任建业,张俊霞,阳怀忠,胡德胜,李朋,张云鹏.2011.塔里木盆地中央隆起带断裂系统分析.岩石学报,27(1):219-230.
[28]  田作基, 胡见义, 宋建国, 罗志立. 2002. 塔里木库车陆内前陆盆地及其勘探意义. 地质科学, 37(增刊): 105-112.
[29]  王国林,李曰俊,孙建华,黄智斌,赵岩,刘亚雷.2009.塔里木盆地西北缘柯坪冲断带构造变形特征.地质科学,44(1):50-62.
[30]  邬光辉,郑多明.2004.塔里木北部地区北北西向构造变换带特征及对石油勘探的启示.地质科学,39(4):551-560.
[31]  肖安成,杨树锋,王清华,陈汉林,谢会文,李曰俊.2002.塔里木盆地巴楚-柯坪地区南北向断裂系统的空间对应性研究.地质科学,37(增刊):64-72.
[32]  杨庚,郭华.2003.塔里木盆地西北缘柯坪逆冲构造带与巴楚隆起的叠加关系.铀矿地质,19(1):1-7.
[33]  杨庚,石昕,贾承造,张君峰,张朝军,何登发,李洪辉,孙方源.2008.塔里木盆地西北缘柯坪-巴楚地区皮羌断裂与色力布亚断裂空间关系.铀矿地质,24(4):201-207.
[34]  杨庚,李本亮,杨海军,陈竹新,王晓波,张朝军,雷永良.2012.塔里木盆地巴楚隆起北缘阿恰基底卷入构造.地质论评,58(1):32-40.
[35]  杨海军,李曰俊,冯晓军,郑民,张春莲,赵岩.2007.塔里木盆地玛扎塔格构造带断裂构造分析.地质科学,42(3):506-517.
[36]  杨海军,李曰俊,师骏,肖安成,黄少英,吴根耀,王怀盛,王霞,赵岩,刘亚雷.2010.南天山晚新生代褶皱冲断带构造特征.第四纪研究,30(5): 1030-1043.
[37]  杨明慧,金之钧,吕修祥,潘文庆,胡剑风.2007.塔里木盆地基底卷入扭压构造与巴楚隆起的形成.地质学报,81(2):158-165.
[38]  杨晓平,冉勇康,宋方敏,徐锡伟,程建武,闵伟,韩竹军,陈立春.2006.西南天山柯坪逆冲推覆构造带的地壳缩短分析.地震地质,28(2):194-204.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133