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塔里木盆地西部玛扎塔格山古董山青石沟剖面的石炭系自下而上划分为下统克里塔格组、和什拉普组、上统卡拉乌依组和阿孜干组,以微体化石的分析结果划分为:牙形刺Clydagnathus-Neoprioniodus组合带、Gnatho-dus bilineatus带、Idiognathoides sulcatus-Declinognathodus noduliferus组合带、Idiognathoides corrugatus-Neog-nathodus bassleri组合带、Streptognathodus parvus-S.suberectus组合带;Eostaf fella带、Pseudostaf fella带、Fusulina-Fusulinella组合带;非有孔虫Archaediscus-Earlandia-Endothyra组合带、Globivalvulina-Bradyina-Glomospira组合带。岩相序列和沉积环境分析显示其海相序列与铁克里克地层区的相似程度高。
The Carboniferous section of the ancient Shanbaishigou section of the Mazarita Mountain in the western Tarim Basin is divided into the Lower Cretaceous Group, the Shrapu Formation, the Upper Karaweiji Formation and the Aztec Formation by the micro The analysis results of fossil fossils are divided into the following groups: Clydagnathus-Neoprioniodus, Gnatho-dus bilineatus, Idiognathoides sulcatus-Declinognathodus noduliferus, Idiognathoides corrugatus-Neog-nathodus bassleri, Streptognathodus parvus-S.suberectus, Eostaf fella belt, Pseudostaf fella belt, Fusulina-Fusulinella combination belt; Non-foraminifera Archaediscus-Earlandia-Endothyra combination belt, Globivalvulina-Bradyina-Glomospira combination belt. The analysis of lithofacies sequence and sedimentary environment shows that their marine sequences are similar to those in the Tiekeli Formation.