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The effect of oil expulsion or retention on further thermal degradation of kerogen at the high maturity stage: A pyrolysis study of type II kerogen from Pingliang shale, ChinaWANGLU JIA; QIULING WANG; JINZHONG LIU et al.Organic geochemistry. 2014, Vol 71, pp 17-29, issn 0146-6380, 13 p.Article

Experimental study of decay conditions of organic matter and its significant for immature oil generationYUZHUANG SUN; JIALAN LU; JIANGPING CHEN et al.Energy exploration & exploitation. 2006, Vol 24, Num 3, pp 161-170, issn 0144-5987, 10 p.Article

The influence of hydrocarbon expulsion on carbon isotopic compositions of individual n-alkanes in pyrolysates of selected terrestrial kerogensYUHONG LIAO; ANSONG GENG; YONGQIANG XIONG et al.Organic geochemistry. 2004, Vol 35, Num 11-12, pp 1479-1488, issn 0146-6380, 10 p.Conference Paper

Thermal cracking history by laboratory kinetic simulation of Paleozoic oil in eastern Tarim Basin, NW China, implications for the occurrence of residual oil reservoirsYUNPENG WANG; SHUICHANG ZHANG; FEIYU WANG et al.Organic geochemistry. 2006, Vol 37, Num 12, pp 1803-1815, issn 0146-6380, 13 p.Conference Paper

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