The formation mechanism of high dibenzothiophene series concentration in Paleozoic crude oils from Tazhong area, Tarim Basin, China
- Author
- GUANGYOU ZHU1 ; NAIHUANG JIANG1 ; JIN SU1 ; JIANFA HAN2 ; HAIJUN YANG2 ; JIE CUI1 ; LIJING GU1
[1] PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China
[2] Research Institute of Petroleum Exploration and Development, Tarim Oilfield Company, PetroChina, Korla 841000, China - Source
Energy exploration & exploitation. 2011, Vol 29, Num 5, pp 617-632, 16 p ; ref : 4 p
- Publisher
- Multi-Science, Brentwood
- Publication country
- United Kingdom
- Document type
- Article
- Language
- English
- Keyword (fr)
- Bactérie Biodégradation Cambrien Carbonate Eau formation Maturation thermique Milieu marin Ordovicien Paléozoïque Pétrole brut Roche mère Réduction chimique Soufre Sulfate Dibenzothiophène Bassin Tarim Chine Paléozoïque inf Procaryote Asie Extrême Orient Xinjiang
- Keyword (en)
- bacteria biodegradation Cambrian carbonates formation water thermal maturity marine environment Ordovician Paleozoic crude oil source rocks chemical reduction sulfur sulfates Tarim Basin China lower Paleozoic prokaryotes Asia Far East Xinjiang China
- Keyword (es)
- Biodegradación Cámbrico Carbonato Medio marino Roca madre Reducción química Azufre Sulfato China Asia Extremo Oriente
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01G Sedimentary rocks / 001E01G03 Hydrocarbons
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01I Stratigraphy
- Discipline
- Earth sciences
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 24755812
Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS
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DOI
10.1260/0144-5987.29.5.617 
https://dx.doi.org/10.1260/0144-5987.29.5.617
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