黑龙江东部大三江盆地群城子河组和穆棱组时期重矿物特征及物源分析  

Heavy mineral characteristics and provenance analysis of Chengzihe and Muling Formations in Dasanjiang basin group,East Heilongjiang Province

作　　者：张云鹏[1,2] 任建业[1,3] 侯艳平[4] 王珊[1] 杨承志[1] 

机构地区：[1]中国地质大学资源学院,湖北武汉430074 [2]中国地质调查局西安地质调查中心,陕西西安710054 [3]教育部含油气盆地构造研究中心,湖北武汉430074 [4]大庆油田勘探开发研究院,黑龙江大庆163712

出　　处：《岩石矿物学杂志》2011年第4期674-682,共9页Acta Petrologica et Mineralogica

基　　金：国家重大科技专项资助项目(2009ZX05009-001)

摘　　要：应用数理统计及Q型聚类分析方法,对大三江盆地群主要盆地20口钻井早白垩世城子河组和穆棱组砂岩中的重矿物进行了重矿物ZTR指数、稳定指数以及组合特征分析。城子河组和穆棱组重矿物ZTR指数等值线图都具有由边部向中心逐渐增大的趋势,而这两个组的重矿物稳定系数整体也较低,反映出成盆初期重矿物稳定性弱的特点,并根据重矿物种类将研究区分为六大重矿物组合带。最后,综合分析认为大三江盆地群城子河组和穆棱组物源方向上变化不大,两组之间是一种继承关系,主要存在3大物源体系:西部和西北部的物源主要来自小兴安岭-张广才岭;东部物源主要来自宝清地体及东三江隆起区;东南部物源主要由兴凯地体提供,那丹哈达地体和延吉褶皱带分别向虎林盆地北部和鸡西盆地南部提供物源,但影响范围有限。Although Dasanjing basin group is a residual basin at present,there existed a huge oil and gas potential in the uniform lake basin in Early Cretaceous,especially in the Chengzihe and Muling Formations,which now serve as important exploration strata.Based on mathematical statistics and Q type cluster analysis,the authors analyzed the heavy mineral ZTR indexes,stability coefficients and assemblage characteristics of the sandstones from Early Cretaceous Chengzihe and Muling Formations distributed in 20 drill holes in the main basins of Dasanjiang basin group,and then determined the direction of the provenance.The heavy mineral ZTR index contour maps of Chengzihe and Muling Formations are characterized by the gradually increasing trend from the edge towards the center,while their heavy mineral stability coefficients are relatively low,reflecting a lower heavy mineral stability at the early stage of the basin formation.According to the heavy mineral distribution,the study area can be divided into 6 heavy mineral assemblage zones.A comprehensive analysis shows that the provenance directions of Chengzihe and Muling Formations in Dasanjiang basin group did not change significantly,and both of the formations actually had an inheritance relationship.There mainly existed three provenance systems：the west and northwest provenance from Xiao Hinggan Mountain-Zhangguangcai Mountain,the east provenance mainly from Baoqing Block and Dongsanjiang uplift area and the southeast provenance mainly supplied by Xingkai Block.Nadanhada Block and Yanji fold belt provided source materials for northern Hulin Basin and southern Jixi Basin respectively,but the influence was limited.

关 键 词：大三江盆地群 重矿物 物源分析 聚类分析 

分 类 号：P588.212.3[天文地球—岩石学]