塔里木盆地西南地区晚三叠世地层的发现及其地质意义

1998年 20卷 第4期
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THE DISCOVERY OF THE LATE TRIASSIC STRATA AND ITS GEOLOGICAL SIGNIFICANCE IN THE SOUTHWESTERN TARIM BASIN
陈荣林
Chen Ronglin
中国新星石油公司, 实验地质研究院, 无锡, 214151
Research Institute of Experimental Geology, CNSPC, Wuxi 214151
本文从岩石、生物地层角度介绍塔西南地区首次发现的晚三叠世地层。上三叠统仅分布在乌恰-库斯拉甫断陷中,它与塔西南前陆盆地分属两个原型盆地,这对于塔西南坳陷构造演化史分析和油气评价将起重要作用。
The first discovered Late Triassic strata was introduced in terms of its petrological and biostratigraphic characters in the paper.The upper Triassic was only distributed in Wuqia-Kusilapu fault depression,which was belonged to a different protobasin comparing with the southwestern foreland basin.This is important for analysis of structural evolution and evaluation of hydrocarbon potential in the southwes tern Tarim depression.
上三叠统; 断陷盆地; 塔西南地区;
国家"八五"重点科技攻关课题(85-101-02-02-04)部分成果
https://doi.org/10.11781/sysydz199804328