摘要
研究区内晚石炭世塔哈奇组为一套浅海相碳酸盐岩建造,在该组中产有丰富的蜒类、珊瑚动物化石,根据化石组合特征,首次在该区建立了蜒类Triticites带,珊瑚Pseudozaphrentoides.mapingensis-P.nosovi组合带.
Taheqi Formation of Late Carboniferous in the researching area is made of shallow ser-facies carbonate formation,in which there are abundant fossils of Minojapanella and Corallina.According to assembled characters of the fossils,Minojapanella belt,Triticites belt, corallina assembled belt and Pseudozaphrentoides.mapingensis-p.nosovi belt have been set up.
出处
《新疆地质》
CAS
CSCD
北大核心
2009年第B12期76-79,共4页
Xinjiang Geology
基金
国家科学技术部科技支撑计划项目"兴都库什-西昆仑成矿带岩浆成矿作用对比研究"(2006BAB01A03-2-2)项目资助
关键词
西昆仑昆盖山北坡
剖面概述
生物组合带
生物地层对比
north slope of Kungaishan,section description,biological association belt,biologic stratum contrast
