陡坡型和缓坡型扇三角洲及其油气储层意义
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摘要
在陆相箕状凹陷,特别是凹陷的短轴陡岸区,扇三角洲十分发育。通过对辽河坳陷西部凹陷冷东-雷家地区沙河街组的沉积学、地震地层学和测井地质学的研究,识别了两种类型的砾质扇三角洲沉积体系,即陡坡型扇三角洲和缓坡型扇三角洲,并对两类扇三角洲的沉积特征及其油气储层意义进行了阐述。这一研究为陆相箕状凹陷断坡带的油气勘探和油藏描述提供了重要的地质理论依据。
In continental dustpan-shaped depression,fan deltas mainly develop in fault-slope beltwhich is in steep shore region along the direction of short-axis in the depression.By means ofsedimentology,well-logging geology and seismic stratigraphy of Shahejie formation in Leng-dong-Leijia region in western part of Liaohe depression,two types of fan deltas are recog-nized,i.e,steep slope-pattern fan delta and gentle slope-pattern fan delta,and their sedi-mentary and reservoir features are discussed.The result provides important geological theo-retical basis for hvdrocarbon exploration and reservoir description of the fault slope of contin-ertal dustpan-shaped deprsssion.
引文
[1]McPhersonJG,ShanmuganGandMoiolaRJ.Fan-deltasandbraiddeltas:varietiesofcoarse-graineddeltas.Geol.Soc.Amer.Bull,1987,V.99:331~340.[2]MassariFandCollellaA.Evolutionandtypesoffan-deltasystemsinsomernajortectonicsettings.InW.NernecandR.JSteel(eds.),Fandeltas:SedimentologyandTectonicsettings,1988,103~122.[3]薛良清,GallowayWF.扇三角洲、辫状河三角洲与三角洲体系的分类.地质学报,1991,(2):141~153.[4]刘宝君等,西藏日喀则地区第三系大竹卡组砾质扇三角洲─—片状颗粒流沉积,四川科学出版社,1990,第1辑,1~11.

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