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松辽盆地十屋断陷登娄库组沉积相分析
引用本文:卢山,刘朋波.松辽盆地十屋断陷登娄库组沉积相分析[J].云南地质,2010,29(4):484-488.
作者姓名:卢山  刘朋波
作者单位:两北大学地质学系,西安710069
基金项目:陕西省普通高校重点学科专项基金
摘    要:十屋断陷登娄库组沉积体系可分为三段-半深湖-深湖、扇三角洲及少量河流相沉积。平面上,扇三角洲发育在断陷西部陡坡带,东南缓坡带则发育辫状河三角洲;中央凹陷带发育半深湖、深湖相。

关 键 词:扇三角洲沉积相  轴向砂体发育  扇形组合  多河道砂岩密集  松辽十层断陷

AN ANALYSIS OF SEDIMENTARY FACIES OF DENGLOUKU FORMATION IN SHIWU FAULT DEPRESSION OF SONGLIAO BASIN
LU Shan,LIU Peng-bo.AN ANALYSIS OF SEDIMENTARY FACIES OF DENGLOUKU FORMATION IN SHIWU FAULT DEPRESSION OF SONGLIAO BASIN[J].Yunnan Geology,2010,29(4):484-488.
Authors:LU Shan  LIU Peng-bo
Institution:HE Yuan-fang, WU Chun-yan, LI Wei ( 1. Department of Geology, NW University, Xi'an 710069 ) (2. Institute of Yanchang Oil Comparty (Group) , Yanchartg 710075 ) ( 3. Xi'an Geological Survey Centre, China Geological Survey Bureau, Xi'an 710069 )
Abstract:The sediment of Laojunmiao oil reservoir K belongs to the front subfacies of delta. The microfacies of submerged distributary channel and interdistributary bay are developed, which are the important oil - gas reservoir. The oil- gas distribution is controlled by the sedimentary facies.
Keywords:Delta Sedimentary System  3 Types of Microfacies  Sedimentary Model  Oil Reservoir K  Laojunrniao  Jiuxi  Gansu
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