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The relationship between dolomite textures and their formation temperature: a case study from the Permian-Triassic of the Sichuan Basin and the Lower Paleozoic of the Tarim Basin
Huang Sijing
2014
卷号11页码:39-51
关键词三叠纪地层 形成温度 白云石化 塔里木盆地 下古生界 四川盆地 二叠纪 质地
URL标识查看原文
内容类型期刊论文
URI标识http://www.corc.org.cn/handle/1471x/3378977
专题成都理工大学
作者单位1.[1]State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu,Sichuan 610059, China
2.[2]Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China
3.[3]College of Earth Sciences, Chengdu University of Technology, Chengdu, Sichuan 610059, China
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GB/T 7714
Huang Sijing. The relationship between dolomite textures and their formation temperature: a case study from the Permian-Triassic of the Sichuan Basin and the Lower Paleozoic of the Tarim Basin[J],2014,11:39-51.
APA Huang Sijing.(2014).The relationship between dolomite textures and their formation temperature: a case study from the Permian-Triassic of the Sichuan Basin and the Lower Paleozoic of the Tarim Basin.,11,39-51.
MLA Huang Sijing."The relationship between dolomite textures and their formation temperature: a case study from the Permian-Triassic of the Sichuan Basin and the Lower Paleozoic of the Tarim Basin".11(2014):39-51.
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