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MECHANISM OF HYDROCARBON MIGRATION OF MARINE CLASTIC ROCKS IN WESTERN AREA OF THE NORTHERN TARIM BASIN: A CASE OF YM34 SILURIAN RESERVOIR

机译:塔里木盆地北部海洋碎屑岩石泥土迁移机制:以YM34硅粉水库为例

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摘要

The oil and gas abundance in YM34 structural belt, so it is potential in exploration and develop- ment. However, due to complex geological struc- ture, it is difficult to further study in hydrocarbon 1n.igration and accumulation mechanism. Based on structural characteristics, crude property, group component characteristics, saturated hydrocarbon chromatography—mass spectrometry (GC/MS), analysis on the alkanes, steranes and terpanes of biomarkers of crude oil in YM32 buried-hill hydro- carbon reservoirs indicated that YM34 Silurian reservoir forming zonation are obviously as fol- lows: l)The western reservoir in wells YM342,YM343 as the representative of the “three low and one high” features, namely, low density and viscosity, low ratio of saturated/aromatic hy- drocarbon, followed by high fraction satLu‘ated and aromatic hydrocarbon. 2) Oil and gas migration in YM34 Silurian reservoir is from the west to the East, accumulation period of the West was later than the East. 3) The results of oil-source correla- tion from source rocks in the Kuqa depression indi- cated that source rock of the west in YM34 Silurian reservoir is superiority to the Triassic lacustrine mudstone, then that of the east is of Jurassic coal mudstone.
机译:YM34结构带的石油和天然气丰度,因此它是勘探和发展的潜力。然而,由于复杂的地质结构,难以进一步研究烃1N.迁移和积累机制。基于结构特征,原油性质,基团组分特征,饱和烃色谱 - 质谱(GC / MS),YM32埋藏山水库原油碱的烷烃,甾烷和萜酯的分析表明,YM34硅粉储层形成区间显然是井:l)井YM342,YM343中的西部储层作为“三个低”和一个高“特征,即低密度和粘度,饱和/芳香族HY-饱和/芳香族的低比例,其次是高馏分Satlu's和芳烃。 2)在YM34 Silurian Chockoir中的石油和天然气迁移来自西部到东方,西方的积累时间晚于东方。 3)从Kuqa抑郁症源岩层的油源相关结果的结果在YM34 Silurian储层中的西方源极岩体对Triassic Lapustine Mudstone的优势,而东部是侏罗纪煤泥的优势。

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