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塔里木盆地轮台断隆带中新生代陆相原油成因及其源岩潜力评价 被引量:14

ORIGIN OF MESOZOIC-CENOZOIC CONTINENTAL FACIES OIL AND HY-DROCARBON-GENERATED POTENCIAL EVALUATION OF SOURCE ROCK, LUN-TAI FAULTED UPLIFT ZONE IN TARIM BASIN.
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摘要 通过油—油、油—岩地球化学性质对比后认为,轮台断隆带中西段原油来自库车坳陷三叠系黄山街组湖相泥岩地层,东段原油来自同一坳陷侏罗系湖沼相煤系地层。该两套岩系均具有相当高的生油潜力。 On the basis of correlation of geochemical characteristics of oil-oil and oil-source rock, it is considered that oil in the middle and western parts of Luntai faulted up-lift zone was generated from lacustrine mudstone of Huangshanjie formation (Triassic) inKuqa depression, and oil in the eastern part was from limnetic coal measure of Jurassic inKuqa depression, which have extremely high hydrocarbon-generated potencial.
出处 《新疆石油地质》 CAS CSCD 北大核心 1995年第4期307-311,共5页 Xinjiang Petroleum Geology
关键词 塔里木盆地 轮台断隆带 生油潜力 原油 成因 Tarim basin Luntai faulted uplift zone Kuqa depressionJurassic Triassic Strata Source rock evaluation
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