GEOCHEMISTRY OF OIL AND IDENTIFICATION OF SOURCE ROCKS IN THE DINAN ARCH-FUBEI SLOPE AREA OF JUNGGAR BASIN
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摘要: 滴南凸起-阜北斜坡区位于准噶尔盆地中央隆起带东段,其周缘地区有多个生烃凹陷,发育四套烃源岩,具复杂的油源关系。为厘清该区中上侏罗统油源关系,利用多项地化指标进行油源对比,结果表明:A类原油具轻碳同位素,植烷优势明显,高伽马蜡烷指数,表现出了湖相母质输入的特点,与二叠系泥岩具良好亲缘关系;B类原油具重碳同位素,姥鲛烷优势,几乎不含伽马蜡烷等特征,反映了原油母质形成于强氧化的沉积环境,与侏罗系泥岩同源;C类原油各项指标介于以上两类原油之间,是二叠系与侏罗系烃源岩的混源。
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关键词:
- 油源对比 /
- 碳同位素 /
- 伽马蜡烷 /
- 滴南凸起-阜北斜坡区
Abstract: The Dinan Arch and Fubei Slope are located in the east of the central uplift belt of the Junggar Basin. There are several hydrocarbon depressions and four kinds of source rocks, which make the oil-source rather complicated. In order to make correlation between the source rock and the oil, several geochemical indicators are used for subdivision of the oil into three categories. The A type of oil has light carbon isotope, phytane preponderance and high gammacerane, indicating a lacustrine origin with blood relation to the Permian source rock; the B type of oil has heavier carbon isotope, pristine preponderance and less gammacerane, suggesting that the proto kerogen was formed in a sedimentary environment of strong oxidation. The oil is believed coming from the Jurassic source rock; the C type of oil shows the features in between and is supposed to come from both the Permian and Jurassic source rocks.-
Key words:
- oil-source rock correlation /
- carbon isotope /
- gammacerane /
- Dinan Arch-Fubei Slope Area
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