摘要
江汉石油学院在研究塔里木盆地石炭－二叠纪地层时，曾对前人提出的“巴楚运动”及其相关地层作了详细研究。根据野外观察和室内对剖面上牙形石的详细分析、研究后认为，所谓“巴楚运动”并不存在，对“运动”所依据的牙形类化石资料和所建立的“平行不整合”提出疑问。
The 'Bachu movement' and correlated formations proposed by predeces-sors has been studied in detail when researching the Carboniferous-permian in Tarimbasin. It is considered that the socalled' Bachu movement' doesn't really exist based onfield observation and indoor analvsis of conodont in section. It is in doubt about Conodon-tophoridia fossil's data on which were based and ' parallel-unconformity' established fromthat' movement' .
出处
《新疆石油地质》
CAS
CSCD
北大核心
1995年第2期173-176,共4页
Xinjiang Petroleum Geology
关键词
塔里木盆地
地壳运动
石炭纪
牙形石
巴楚运动
Tarim basin Bachu Crust movement CarhoniferousConodont Unconformity
