Geochemistry and possible origin of the hydrocarbons from Wells Zhongshen1 and Zhongshen1C, Tazhong Uplift

Author:

Song DaoFu,Wang TieGuan,Li MeiJun

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference48 articles.

1. Bray E E, Evans E D. 1961. Distribution of n-paraffins as a clue to recognition of source beds. Geochim Cosmochim Acta, 22: 2–15

2. Brincat D, Abbott G. 2001. Some aspects of the molecular biogeochemistry of laminated and massive rocks from the Naples Beach Section. In: Isaacs C M, Rullkötter J, eds. The Monterey Formation: From Rocks to Molecules. New York: Columbia University Press. 140–149

3. Cai C F, Hu W S, Worden R H. 2001. Thermochemical sulphate reduction in Cambro-Ordovician carbonates in Central Tarim. Mar Petrol Geol, 18: 729–741

4. Cai C F, Li K K, Ma A L, Zhang C M, Xu Z M, Worden R H, Wu G H, Zhang B S, Chen L X. 2009. Distinguishing Cambrian from Upper Ordovician source rocks: Evidence from sulfur isotopes and biomarkers in the Tarim Basin. Org Geochem, 40: 755–768

5. Chen L X, Yang H J, Wu G H, Han J F, Cai C F, Zhai S L. 2008. Characteristics of the Ordovician reef–shoal reservoir in Tazhong No. 1 Slope-break Zone, Tarim Basin (in Chinese). Xinjiang Petrol Geol, 29: 327–330

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