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喀左盆地下白垩统九佛堂组油页岩特征及控矿条件
引用本文:王宇林,郭强,肖乾华,王威,杨春,魏恒飞,刘锦.喀左盆地下白垩统九佛堂组油页岩特征及控矿条件[J].吉林大学学报(地球科学版),2009,39(2).
作者姓名:王宇林  郭强  肖乾华  王威  杨春  魏恒飞  刘锦
作者单位:1. 辽宁工程技术大学,资源与环境工程学院,辽宁,阜新,123000
2. 浙江大学,地球科学系,杭州,310027
基金项目:辽宁省高等学校科学研究项目,中石油辽河石油勘探局项目 
摘    要:野外地质调查和岩石学、地球化学研究表明:喀左盆地3个油页岩层群分别发育于下白垩统九佛堂组的一、二、三段,以位于三段的第三油页岩层群的工业意义最大;油页岩常与上覆沉凝灰岩或其它凝灰质岩石呈伴生关系.油页岩(矿石)类型有泥岩、具粉砂质条带的含钙-钙质泥岩、泥灰岩和页岩4种类型,以前两者为主;低品级油页岩体积分数为50%,中品级油页岩体积分数为42%,高品级油页岩体积分数为8%,均属高灰分油页岩.油页岩的有机质类型为腐植-腐泥型,源于低等植物;浅湖-半深湖形成的油页岩(矿石)类型为含粉砂质条带的含钙-钙质泥岩,深湖形成的油页岩(矿石)类型主要为泥岩;物源区母岩类型对油页岩的化学成分特征及灰分成分类型具有明显的控制关系;火山喷发的灾变事件终止了油页岩的成矿作用.

关 键 词:喀左盆地  九佛堂组  油页岩  控矿条件  沉积环境  火山事件

Characteristic and Ore-Controlling Condition of Oil Shale of Jiufotang Formation of Lower Cretaceous in Kazuo Basin
WANG Yu-lin,GUO Qiang,XIAO Qian-hua,WANG Wei,YANG Chun,WEI Heng-fei,LIU Jin.Characteristic and Ore-Controlling Condition of Oil Shale of Jiufotang Formation of Lower Cretaceous in Kazuo Basin[J].Journal of Jilin Unviersity:Earth Science Edition,2009,39(2).
Authors:WANG Yu-lin  GUO Qiang  XIAO Qian-hua  WANG Wei  YANG Chun  WEI Heng-fei  LIU Jin
Institution:WANG Yu-lin1,GUO Qiang1,XIAO Qian-hua2,WANG Wei1,YANG Chun3,WEI Heng-fei1,LIU Jin11.Resource , Environment Engineering College,Liaoning Technical University,Fuxin,Liaoning 123000,China2.Resource Exploration , Development Division,Liaohe Petroleum Exploration Bureau,Panjin,Liaoning 124011,China3.Department of Earth Sciences,Zhejiang University,Hangzhou 310027,China
Abstract:Field geological investigation,petrology and geochemistry study showed that three oil shale groups in Kazuo basin were developed in Member 1,2,3 of the Jiufotang Formation of Lower Cretaceous,the third oil shale group located in 3rd member have the greatest industrial significance.Oil shale always has the accompanying relationship with overlying sedimentary tuff or other tuffaceous strata.The oil shale(ore) of this area have four types,including mudstone,calcareous mudstone containing silty band,marlite and...
Keywords:Kazuo basin  Jiufotang Formation  oil shale  ore-controlling condition  sedimentary environment  volcanic event  
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