HYDROCARBON POTENTIAL AND PALAEO‐DEPOSITIONAL ENVIRONMENT OF LACUSTRINE SOURCE ROCKS: MIDDLE JURASSIC SHIMENGOU FORMATION, NORTHERN QAIDAM BASIN, NW CHINA,Journal of Petroleum Geology

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HYDROCARBON POTENTIAL AND PALAEO‐DEPOSITIONAL ENVIRONMENT OF LACUSTRINE SOURCE ROCKS: MIDDLE JURASSIC SHIMENGOU FORMATION, NORTHERN QAIDAM BASIN, NW CHINA
Journal of Petroleum Geology ( IF 1.8 ) Pub Date : 2018-12-10 , DOI: 10.1111/jpg.12723
Q. T. Meng _{1,

2} , A. Bechtel ₃ , R. F. Sachsenhofer ₃ , Z. J. Liu _{1,

2} , D. Gross ₃ , P. C. Sun _{1,

2} , F. Hu _{1,

2} , L. Li _{1,

2} , K. B Wang _{1,

2} , C. Xu _{1,

2} , L. L. Chen _{1,

2} , W. R. Zeng _{1,

2}

Affiliation

The Middle Jurassic Shimengou Formation in the Qaidam Basin, NW China, includes coals and lacustrine source rocks which locally reach oil shale quality (i.e. yielding >3.5 % oil on low‐temperature distillation). In the present study, the palaeo‐depositional environment and hydrocarbon potential of the 84.5 m thick Shale Member of the Shimengou Formation are investigated based on bulk geochemical parameters, organic petrographic data, biomarker analysis, and stable isotope geochemistry of 88 core samples.

更新日期：2018-12-10

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