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根据孢粉组合推论西藏伦坡拉盆地第三纪地层时代及其古地理
引用本文:王开发,杨蕉文,李哲,李增瑞.根据孢粉组合推论西藏伦坡拉盆地第三纪地层时代及其古地理[J].地质科学,1975,10(4):366-374.
作者姓名:王开发  杨蕉文  李哲  李增瑞
作者单位:湖北省石油地质研究大队
摘    要:伦坡拉盆地位于藏北高原南部,海拔4000多米,是藏北新生代地层甚为发育的地区,第三系沉积厚达三千米以上,自下而上划分为:迪欧组、牛堡组、丁青组和伦坡拉组。自1967年以来,我们先后分析了采自伦坡拉盆地的伦坡拉构造两个剖面,丁青构造两个剖面,牛堡构造两个剖面,阿利开拍构造一个剖面,猪头山一个剖面,伦坡拉西拗陷一个剖面以及四口钻井的岩心样品近300块。

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ON THE TERTIARY SPORO-POLLEN ASSEMBLAGES FROM LUNPOLA BASIN OF XIZANG, CHINA AND THEIR PALAEOGEOGRAPHIC SIGNIFICANCE
WANG KAIFA,YANG JIAOWEN,LI ZHE,LI ZENGRTJI.ON THE TERTIARY SPORO-POLLEN ASSEMBLAGES FROM LUNPOLA BASIN OF XIZANG, CHINA AND THEIR PALAEOGEOGRAPHIC SIGNIFICANCE[J].Chinese Journal of Geology,1975,10(4):366-374.
Authors:WANG KAIFA  YANG JIAOWEN  LI ZHE  LI ZENGRTJI
Institution:Hubei Petro-Geologie Team
Abstract:Being widely distributed in Lunpola basin of Xizang, the Tertiary sediments there may be divided, in ascending order, into De-ou formation, Niubao formation, Dingqing formation and Lunpola formation. Quite a number of interesting finds of the various fossil spores and pollens have been made by sporo-pollen analysis of the specimens available. Six fossil sporo-pollen assemblages may be distinguished respectively by their characteristics, thus rendering it possible to determine with success the geological age for each formation and member and to reconstruct correspondingly the palaeogeography of the various geologic ages concernd.
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