oa Geochemical Variation in the High Thermal Maturity Longmaxi Shale Gas, Sichuan Basin

References

1. Burruss, R.C., Laughrey, CD.
   , 2010. Carbon and hydrogen isotopic reversals in deep basin gas: evidence for limits to the stability of hydrocarbons. Organic Geochemistry41(12), 1285–1296.
   [Google Scholar]
2. Chen, C, Mu, C.L., Zhou, K.K., Liang, W., Ge, X.Y., Wang, X.P., WangQ.Y., ZhengB.S.
   , 2016. The geochemical characteristics and factors controlling the organic matter accumulation of the late ordovician-early silurian black shale in the upper yangtze basin, south china. Marine & Petroleum Geology76, 159–175.
   [Google Scholar]
3. Zhang, M., Tang, Q., Cao, C, Lv, Z., Zhang, T., Zhang, D., Li, Z., Du, L.
   , 2018. Molecular and carbon isotopic variation in 3.5 years shale gas production from Longmaxi Formation in Sichuan Basin, China. Marine & Petroleum Geology89, 27–37.
   [Google Scholar]