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划分成岩作用与埋藏变质作用的指标及其界线
引用本文:赵孟为.划分成岩作用与埋藏变质作用的指标及其界线[J].地质论评,1995,41(3):238-244.
作者姓名:赵孟为
作者单位:格丁根大学地质与岩石圈动力学研究所 德国
摘    要:本文是对“陕北鄂尔多斯盆地埋藏变质作用研究”一文的讨论,它综述并讨论了划分成岩作用和埋藏变质作用的指标,界线及其在鄂尔多斯盆地中的应用。伊利石结晶度、粘土矿物、浊沸石胶结物,石油形成,镜质体反射率,煤阶和地温等指标一致表明,鄂尔多斯盆地中生代地层处于中期成岩作用阶段,从而否定了本区为埋藏变质地区的结论。

关 键 词:成岩作用  变质作用  鄂尔多斯盆地

THE INDICATORS AND BOUNDARY FOR SEPARATING DIAGENESIS FROM BURIAL METAMORPHISM
Zhao Mengwei.THE INDICATORS AND BOUNDARY FOR SEPARATING DIAGENESIS FROM BURIAL METAMORPHISM[J].Geological Review,1995,41(3):238-244.
Authors:Zhao Mengwei
Abstract:This paper is a discussion of the paper "Study of Burial Metamorphism of the Ordos Basin, Northern Shaanxi". The indicators and boundary for separating diagenesis from burial metamor- phism and their application in the study of the Ordos basin are reviewed and discussed. The indicators including clay minerals, illite crystallinity, laumontite cement, Vitrinite reflectance, coal rank, paleo-temperatures and formation of petroleum-all these show that the Mesozoic strata in the Ordos basin are in the middle diagenetic stage, thus negating the conclusion that this area is a region of burial metamorphism.
Keywords:diagenesis  burial metamorphism  Ordos basin  
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