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昆盖山北坡苏古鲁克一带晚石炭世塔哈奇组生物地层特征
引用本文:高鹏,肖忠,卢兰英,刘通,田忠锋.昆盖山北坡苏古鲁克一带晚石炭世塔哈奇组生物地层特征[J].新疆地质,2009,27(Z1).
作者姓名:高鹏  肖忠  卢兰英  刘通  田忠锋
作者单位:1. 新疆维吾尔自治区地质矿产研究所,新疆,乌鲁木齐,830000
2. 新疆地矿局第一地质大队,新疆,昌吉,831100
基金项目:国家科学技术部科技支撑计划项目 
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.

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

Biostratigraphic features of Taheqi Formation of Late Carboniferous in SUGULUKE AREA,north slope of kungaishan
GAO Peng,XIAO-Zhong,LU Lan-ying,LIU Tong,TIAN Zhong-feng.Biostratigraphic features of Taheqi Formation of Late Carboniferous in SUGULUKE AREA,north slope of kungaishan[J].Xinjiang Geology,2009,27(Z1).
Authors:GAO Peng  XIAO-Zhong  LU Lan-ying  LIU Tong  TIAN Zhong-feng
Abstract: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.
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