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水下碎屑流沉积:深水沉积研究热点与进展 被引量:49
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作者 鲜本忠 安思奇 施文华 《地质论评》 CAS CSCD 北大核心 2014年第1期39-51,共13页
自20世纪50年代以来,作为沉积物搬运两大主要动力之一的重力流因其在记录地质事件、改造地表地貌和勘查油气资源方面的特殊意义而引起广泛关注。重力流研究历史经历了现象观测、概念体系建立、沉积模式建立、工业应用与质疑和碎屑流研... 自20世纪50年代以来,作为沉积物搬运两大主要动力之一的重力流因其在记录地质事件、改造地表地貌和勘查油气资源方面的特殊意义而引起广泛关注。重力流研究历史经历了现象观测、概念体系建立、沉积模式建立、工业应用与质疑和碎屑流研究深化5个阶段。近期,以深海水下碎屑流为核心的研究重建了“砂质碎屑流”概念,新建立了以碎屑流细分为主要内容的3套重力流分类,提出并讨论了水下碎屑流“滑水”搬运机制特征、形成条件,系统分析沉积物浓度、粘土含量及成分对水下重力流性质及搬运沉积过程的影响。继20世纪60—70年代重力流研究热潮后,1996年以来水下碎屑流为主的研究再次掀起新一轮研究热潮。综合沉积物重力流研究现状、进展和当前油气工业勘探开发需求,指出未来水下碎屑流研究动态包括:①水下碎屑流成因分类体系的建立及重力流分类体系的完善;②实地观测与模拟实验结合下水下碎屑流发育机制深化;③重力流泥岩沉积机制及油气意义和④水下碎屑流主控型重力流沉积模式的建立及其在油气勘探开发中的应用。 展开更多
关键词 水下碎屑流 重力 搬运机制 分类体系
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渤中凹陷东南斜坡带大型湖底扇沉积特征及勘探潜力 被引量:2
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作者 李俊伟 牛成民 +1 位作者 官大勇 岳军培 《石油钻采工艺》 CAS CSCD 北大核心 2018年第A01期1-3,共3页
渤海海域渤南低凸起东南斜坡带在东二下段时期分布大面积的湖底扇,其展布面积及物源来源与渤海常规湖底扇的沉积特征截然不同。这种显著差异导致对其相带类型及划分存在些许争议,将其作为储集体存在一定风险。随着对渤海中深层砂体勘探... 渤海海域渤南低凸起东南斜坡带在东二下段时期分布大面积的湖底扇,其展布面积及物源来源与渤海常规湖底扇的沉积特征截然不同。这种显著差异导致对其相带类型及划分存在些许争议,将其作为储集体存在一定风险。随着对渤海中深层砂体勘探程度的日益加深,确定其沉积体的沉积相类型及富砂性是首要任务,分析其成因机制更是研究的重点。该区无钻探井、且埋藏较深,因此,以层序地层学理论为指导,重建古地貌背景、古水深环境、结合源-渠-汇耦合理论及地震几何形态特征,确定物源属于期次性事件,分析其水下碎屑流搬运机制,明确了沉积体的发育部位、形成机制及沉积类型。最后应用多属性分析对研究区大型湖底扇内幕进行刻画,预测有利储层分布,对该区岩性油气藏勘探具有一定指导意义。 展开更多
关键词 渤中凹陷 东二下段 水下碎屑流 大型湖底扇 沉积类型 富砂性 气藏勘探
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Characteristics of carbonate cementation in clastic rocks from the Chang 6 sandbody of Yanchang Formation, southern Ordos Basin 被引量:11
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作者 LIU ChunYan ZHENG HeRong +1 位作者 HU ZongQuan YIN Wei LI Song 《Science China Earth Sciences》 SCIE EI CAS 2012年第1期58-66,共9页
Densification of reservoir is an important factor that restricts oil and gas exploration from low porosity and extra-low permeability reservoirs. Carbonate cementation was heavily developed in Chang 6 sandbody, a faci... Densification of reservoir is an important factor that restricts oil and gas exploration from low porosity and extra-low permeability reservoirs. Carbonate cementation was heavily developed in Chang 6 sandbody, a facies of underwater distributary channel in delta front, of Upper Triassic Yanchang Formation in Fuxian area, southern Ordos Basin, and the cementation is one of the major factors that affect quality of reservoir. Based on the macro-microcosmic petrology and geochemistry features, the genesis of densification of carbonate-cemented reservoir was systematically discussed. The carbonate cementation can be classified into endogenous and exogenous, and the essential differences between them are that they were formed in different fluids and in different diagenesis periods. With the aid of identification of thin sections, analyses on electron probe, trace and rare-earth elements, carbon and oxygen isotope, we propose that the endogenous fluid for cementation came from the rock itself during early diagenetic stage. The minerals related to endogenous fluid had good shapes. The reservoir property was enhanced with porosity increasing by 3%-8% because of later dissolution by endogenous fluid. The exogenous fluid might be water combining with CO 2 , likely released from organic matter-rich mudstone. Calcite cement, in form of substrate cementation, was precipitated from the fluid and filled in the remaining pores of sandstones in late diagenetic stage as variations of physical and chemical conditions. The exogenous cement reduced rock porosity, damaged reservoir property, affected some oil enrichment, and seriously caused Chang 6 reservoir densification. Some of the dense layers that formed on top of sandbody could have served as diagenetic traps, and thus the exogenous cementation area could be favorable for oil exploration. 展开更多
关键词 Upper Triassic Yanchang Formation densified clastic reservoir carbonate cementation substrate cement genetic mechanism
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