长江大学主页平台管理系统 Li Xi--Home-- Genesis mechanism and Mg isotope difference between the Sinian and Cambrian dolomites in Tarim Basin

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李茜，男，湖北孝感人，1996年8月生，工学博士，长江大学地球科学学院特任副教授，毕业于中国石油勘探开发研究院矿产普查与勘探专业，导师沈安江、朱光有教授，主要研究方向为超深层常规油气与非常规油气成储-成藏理论及实验技术。主持国家深地/油气重大专项专题项目2项，油气资源与勘探技术教育部重点实验室开放基金项目1项、湖北省教育厅科学技术研究计划青年人才项目1项、中国油气地质调查中心与中石油勘探开发研究院...

李茜

Paper Publications

Genesis mechanism and Mg isotope difference between the Sinian and Cambrian dolomites in Tarim Basin

Release time:2026-02-23 Hits:

Journal:

Science China Earth Sciences

Co-author:

Li, T., Zhou, L., Wu, Y., Shen, B., & Ning, M.

First Author:

Zhu, G.

Correspondence Author:

Li, X

Date of Publication:

2023-05-09

Pre One:Mg isotopic geochemistry and origin of Early Ordovician dolomite and implications for the formation of high-quality reservoir in the Tabei area, Tarim Basin, NW China

Next One:Genesis and reservoir preservation mechanism of 10 000-m ultradeep dolomite in Chinese craton basin