首页|缝合线中有机质来源、流体运移以及地质意义

缝合线中有机质来源、流体运移以及地质意义

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[目的]缝合线作为碳酸盐岩的典型结构,其形成对于碳酸盐岩本身有机质的富集和流体运移具有重要的意义.然而,缝合线中有机质的来源和流体运移的机理目前尚未深入研究.[方法]以四川盆地东部大池干构造带含缝合线的碳酸盐岩岩心样品为研究对象,分别对岩心中缝合线和基质进行了有机碳、热解(Rock-Eval)、岩石薄片、荧光薄片、全岩X射线衍射、碳氧同位素以及扫描电镜等分析测试.[结果与结论]缝合线中的有机质主要以可溶有机质、焦沥青和沥青的形式赋存,表明缝合线中的有机质主要为运移而来的次生有机质.且缝合线中的次生白云石和黄铁矿发育,且保留了矿物的晶间孔隙和裂缝,为油气的聚集和运移提供了良好的条件.此外,沿缝合线方向存在明显的油气分馏效应,且在缝合线较薄的区域分馏效应越明显.综合分析认为,缝合线与基质接触界面上的强烈胶结作用及其附近次生矿物的形成是造成烃类流体从基质向缝合线运移时分馏效应的原因.当缝合线发育时,缝合线中的有机质会在高演化阶段裂解形成天然气,与其他成因的天然气混合时会影响天然气来源判别;缝合线作为原油的运移通道时,对原油造成的分馏效应也会对原油来源的判别造成一定困扰,因此应该选择合适的生物标志化合物对比参数来分析油源关系,同时原油性质的空间变化规律也应该被考虑.
Origin of Organic Matter,Fluid Transport and Geological Significance in Stylolites
[Objective]As a typical structure of carbonate rocks,the formation of stylolites is of great significance for the enrichment of organic matter and fluid migration within the carbonate rock itself.However,there is currently no in-depth research on the source of organic matter and the mechanism of fluid transport in stylolites.[Methods]This study collected carbonate core samples containing stylolites from the Dachigan structural belt in the eastern Sichuan Basin.The stylolites and matrix were respectively subjected to organic carbon and pyrolysis(Rock-Eval),common thin section observation,thin section observation under fluorescent light,whole rock X-ray diffraction,carbon and oxygen isotopes and scanning electron microscopy(SEM)and other testing items.[Results and Conclu-sions]The organic matter occurred in the stylolites is mainly in the form of three types including soluble organic mat-ter,pyrobitumen,and bitumen,indicating that the organic matter in the stylolites is mainly the secondary migrated organic matter.Secondary dolomite and pyrite are well developed in the stylolites that the intercrystalline pore spaces and fractures are retained,thereby to provide good conditions for the accumulation and migration of oil and gas.The strong cementation on the contact between the stylolites and matrix and the formation of secondary minerals nearby may be the results of fractionation when the hydrocarbon fluid migrates from the matrix to stylolites.Through analysis,it is believed that the strong cementation at the contact interface between the suture and the matrix,as well as the formation of nearby secondary minerals,are the reasons for the fractionation effect of hydrocarbon fluids when migrating from the matrix to the suture.Through this study,it was found that during the development of sutures,the organic matter in the sutures will crack and form natural gas during the high evolution stage.When mixed with natural gas of other origins,it will affect the identification of natural gas sources;When the suture line serves as a migration channel for crude oil,the fractionation effect on crude oil can also cause certain difficulties in identifying the source of crude oil.Therefore,appropriate biomarker comparison parameters should be selected to analyze the oil source relationship,and the spatial variation pattern of crude oil properties should also be considered.

carbonate rockstyloliteorganic matterbitumenpyrite

朱康乐、高岗、刘诗局、王成云、程光瑾、胡丹丹

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中国石油大学(北京)地球科学学院,北京 102249

中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249

华北油田分公司勘探开发研究院,河北任丘 062552

玉门油田勘探开发研究院,甘肃酒泉 735000

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碳酸盐岩 缝合线 有机质 沥青 黄铁矿

国家自然科学基金项目

411372142

2024

沉积学报
中国矿物岩石地球化学学会沉积学专业委员会 中国地质学会沉积地质专业委员会 中国科学院地质与地球物理研究所兰州油气资源研究中心

沉积学报

CSTPCD北大核心
影响因子:1.54
ISSN:1000-0550
年,卷(期):2024.42(2)
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