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关于地层剥蚀厚度求取方法的讨论:以吐—哈盆地为例
引用本文:柳益群,周立发.关于地层剥蚀厚度求取方法的讨论:以吐—哈盆地为例[J].西北大学学报,1997,27(4):337-339.
作者姓名:柳益群  周立发
作者单位:西北大学地质学系
摘    要:以吐-哈油田为例,用镜质体反射率和磷灰石裂变径迹方法综合求取了地层剥蚀厚度。据此求得吐-哈盆地南部地区三叠系剥蚀厚度多小于500m;盆地北部的台北凹陷侏罗系剥蚀厚度介于600m到未剥蚀之间;台北凹陷北部山前带侏罗系剥蚀厚度多在1300~1800m之间。

关 键 词:剥蚀厚度  镜质体反射率  磷灰石裂变径迹  吐-哈盆地

Discussion on a Method about Eroded Strata Thickness References with Turpan and Hami Basin
Liu Yiqun,Zhou Lifa.Discussion on a Method about Eroded Strata Thickness References with Turpan and Hami Basin[J].Journal of Northwest University(Natural Science Edition),1997,27(4):337-339.
Authors:Liu Yiqun  Zhou Lifa
Abstract:It is a better way to seek eroded strata thikness by means of synthetical methods including vitrinite reflectance and apatite fission track.According to this method,the eroded thickness of strata of Turpan and Hami basin can be obtained as follows:the Triassic is less than 500m in the southern area of basin;the Jurassic is between 600m and no erosion in Taibei depression in the northern area of basin;and is from 800m to 1800m in the foreland mountains of Taibei depression.
Keywords:eroded thickness  vitrinite reflectance  apatite fission track  Turpan and Hami basin  
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