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中国西部三大盆地古生界典型海相砂体特征、分布及意义

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塔里木盆地、鄂尔多斯盆地和四川盆地是中国西部三大含油气大盆地,油气资源丰富,勘探领域广泛,其中海相成因的陆源碎屑岩砂体是油气勘探的重点对象之一.本论文在前人研究成果的基础上,针对中国西部三大盆地古生界典型海相砂体特征、分布进行刻画,并阐述其油气地质意义.研究结果表明,中国西部三大盆地主要发育四大类海相砂体:(1)滨岸砂体,通常发育于无障壁海岸附近,主要受波浪和沿岸流等动力作用的影响,砂体碎屑颗粒分选、磨圆好,发育典型的冲洗层理,主要发育于塔里木盆地泥盆系东河塘组和鄂尔多斯盆地寒武系辛集组;(2)潮汐砂体,形成于有障壁的海岸环境,主要受潮汐作用控制,砂体发育典型的潮汐层理,主要发育于塔里木盆地志留系柯坪塔格组和鄂尔多斯盆地本溪组、太原组;(3)陆棚砂体,主要发育于浅海陆棚环境,受海流和风暴潮等影响,具有沉积厚度大和储集性能好的特点,主要发育于鄂尔多斯盆地二叠系本溪组、太原组、山西组和四川盆地志留系石牛栏组;(4)浊积砂体,主要发育半深海—深海环境,由深海浊流沉积形成,通常具有高孔隙度和渗透性,是优良的储集层,主要发育于塔里木盆地奥陶系却尔却克组.上述四类海相碎屑岩砂体在三大盆地不同层位广泛发育,大面积分布,构成了良好的油气储集层.系统研究三大盆地古生界海相碎屑岩砂体具有重要的构造地质学意义、古地理学意义、古海洋学意义和重大的油气地质意义,对于深化认识海相碎屑砂体的油气地质意义具有重要的理论意义和实践价值.
CHARACTERISTICS,DISTRIBUTION AND SIGNIFICANCE OF PALEOZOIC TYPICAL MARINE SAND BODIES IN THREE MAJOR BASINS IN WESTERN CHINA
The Tarim Basin,Ordos Basin,and Sichuan Basin are the three major oil and gas-bearing ba-sins in western China,rich in oil and gas resources and encompassing extensive exploration areas.Among them,marine-origin terrigenous clastic sand bodies are one of the key targets for oil and gas exploration.Based on previous research,this paper characterizes the features and distribution of typical Paleozoic ma-rine sand bodies in these three major basins and elaborates on their petroleum geological significance.The study results indicate that there are four main types of marine sand bodies developed in the three major ba-sins of western China:(1)Shoreline Sand Bodies:Typically developed near barrier-free coastlines,prima-rily influenced by wave and coastal current dynamics.These sand bodies have well-sorted and well-rounded clastic particles,with typical washout stratification,mainly found in the Devonian Donghetang Formation of the Tarim Basin and the Cambrian Xinjie Formation of the Ordos Basin.(2)Tidal Sand Bodies:Formed in coastal environments with barriers,primarily controlled by tidal action.These sand bodies exhibit typi-cal tidal stratification,mainly found in the Silurian Kepingtage Formation of the Tarim Basin and the Benxi and Taiyuan Formations of the Ordos Basin.(3)Shelf Sand Bodies:Mainly developed in shallow marine shelf environments,influenced by ocean currents and storm surges.They are characterized by sig-nificant sedimentary thickness and good reservoir performance,primarily found in the Permian Benxi,Taiyuan,and Shanxi Formations of the Ordos Basin and the Silurian Shiniulan Formation of the Sichuan Basin.(4)Turbidite Sand Bodies:Mainly developed in semi-deep to deep-sea environments,formed by deep-sea turbidity currents.These sand bodies typically have high porosity and permeability,making them excellent reservoirs,mainly found in the Ordovician Queerquek Formation of the Tarim Basin.These four types of marine clastic sand bodies are extensively developed and widely distributed across different strati-graphic levels in the three basins,forming excellent oil and gas reservoirs.Systematic research on the ma-rine clastic sand bodies in the Paleozoic of the three major basins has significant tectonogeological,paleo-geographical,paleoceanographical,and petroleum geological implications.This research has important theoretical significance and practical value for deepening the understanding of the petroleum geological sig-nificance of marine clastic sand bodies.

Tarim BasinOrdos BasinSichuan BasinPaleozoicGenesis of Marine Clastic Sand BodyGeological Significance

田景春、王峰、郑启明、张翔、林小兵、梁庆韶

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成都理工大学沉积地质研究院,四川成都 610059

油气藏地质及开发工程国家重点实验室成都理工大学,四川成都 610059

北京派特杰奥科技有限公司,北京 100095

塔里木盆地 鄂尔多斯盆地 四川盆地 古生界 海相砂岩成因 地质意义

国家自然科学基金面上项目四川省科技计划项目-四川省自然科学基金项目

423721412024NSFSC0831

2024

矿物岩石
四川省矿物岩石地球化学学会 成都理工大学

矿物岩石

CSTPCD北大核心
影响因子:0.8
ISSN:1001-6872
年,卷(期):2024.44(3)