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| GEOCHEMISTRY OF LIGHT HYDROCARBONS AND DIAMONDOIDS AND SOURCE ANALYSIS OF OIL FROM TC1 WELL IN TUQUAN BASIN |
| SUN Peng1, TANG You-jun1, LI Shi-zhen2, GONG Fan-hao3 |
1. Yangtze University, Wuhan 430100, China;
2. Oil and Gas Resources Survey Center, CGS, Beijing 100029, China;
3. Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, China |
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Abstract The techniques of gas chromatography(GC) and gas chromatography-mass spectrometry(GC-MS) are adopted to study the characteristics of light hydrocarbon and diamondoids from TC1 well in Tuquan Basin, which can help reveal the parent material type, depositional environment, maturity and other geochemical and geological information of crude oil. The obvious superiority of pristane content to phytane (Pr/Ph=3.17) of the oil from TC1 well indicates that the source rock was deposited in a relatively oxidizing environment. The discrimination diagram shows that the parent material belongs to Ⅱ2-Ⅲ type, with methyl cyclohexane (MCH) index of 46%, cyclohexane (CH) index of 25% and predominant 3,4-DMD relative amount of 48% in 2 methyl adamantane. With the data of heptane(IH) index(27.6%), isoheptane(Ⅱ) index(33%), IMA (0.63) and IMD (0.38), the Ro value can be calculated to be 1.2%, revealing that the oil is in mature-highly mature stage. Combined with the previous research data, the crude oil from TC1 well is deduced to generate in the mudstone of Middle Jurassic Wanbao Formation.
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Received: 07 June 2015
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2016, Vol. 25 
