松辽盆地南部东南隆起区白垩系登娄库组沉积特征  

Sedimentary characteristics of the Cretaceous Denglouku Formation in the southeast uplift of the southern Songliao Basin

作　　者：李占东[1] 李阳[2] 刘云利 胡慧婷[4] 马凤荣[4] 张小刚[5] 

机构地区：[1]东北石油大学石油工程学院,黑龙江大庆163318 [2]大庆职业学院,黑龙江大庆163255 [3]中国石油新疆油田分公司风城油田作业区,新疆克拉玛依834000 [4]东北石油大学地球科学学院,黑龙江大庆163318 [5]中国石油长庆油田分公司勘探部,陕西西安710018

出　　处：《石油与天然气地质》2014年第3期401-409,共9页Oil & Gas Geology

基　　金：国家高技术研究发展计划(863计划)项目(SS2012AA060203)

摘　　要：为了查明松辽盆地南部东南隆起区登娄库组沉积特征及演化规律,开展了层序格架内的沉积相展布特征及演化研究。研究表明,登娄库组物源具有四周向中央汇聚的继承性特征,沉积相分布受盆地构造演化控制明显,主要发育了5种沉积相——冲积扇、扇三角洲、辫状河、辫状河三角洲和湖相。层序Ⅳ-d1为断-坳转换期的早期,沉积受断陷控制明显,致使沉积物快速卸载,各沉积体系向盆地内部进积的距离受到了限制,共发育了5个规模较大的分割式断陷和2个小型断陷。断陷周缘古凸起为冲积扇沉积体系的主要发育区,扇三角洲沉积分布于断陷的四周,扇三角洲前缘延伸到入湖处。沉积相主要以冲积扇、扇三角洲和湖相为主;层序Ⅳ-d2为断坳转换期的末期,研究区基本上形成了统一沉积物卸载区域,湖泊范围扩大,主要发育了冲积扇、扇三角洲、辫状河、辫状河三角洲和湖相沉积。以泛滥平原与滨浅湖的接触带为界,该界限以西主要发育来自西部和北部物源高地的冲积扇、辫状河沉积体系,该界限以东湖泊相大面积发育,伴随高地物源区碎屑沉积物陆续注入湖盆,构成了规模不等的退积式扇三角洲。其中,扇三角洲前缘和辫状河三角洲前缘亚相带是油气富集的主要储集体,是今后该区登娄库组油气勘探的有利相带。Sedimentary characteristics and evolution of the Denglouku Formation in the southeast uplift area of southern Songliao basin was studied based on analyses of sedimentary facies distribution and evolution in the context of sequence framework .The results show that the provenance of the Formation were distributed around the basin and supplied sediments from all directions to the center of the basin and the sedimentary facies distri-bution was controlled by basin tectonic evolution .Five major sedimentary facies were recognized in the area ：al-luvial fan ,fan delta ,braided river ,braided delta ,and lake .The sequence Ⅳ-d1 was formed during the early stage of transformation from a fault depression to a sag .The deposition was mostly controlled by the fault depression and the sediments were downloaded rapidly ,restricting the distance of progradation to the inner basin .There de-veloped five separated fault depressions and two small fault depression .Alluvial fan sedimentary systems were developed on the paleohighs around the fault depressions ,fan delta systems were located around the fault de-pressions ,while the fronts of the fan delta extended into the mouth of the lake .The sedimentary facies were dominated by alluvial fan ,fan delta and lake .Sequence Ⅳ-d2 was formed during the late stage of transformation from fault depression to a sag when an unified sediment unloading area was developed ,and the lake expanded . The sedimentary facies were dominated by alluvial fan ,fan delta ,braided river ,braided river delta ,littoral and lake .The contact zone of the flood plains and the shore-shallow lake can be regarded as a boundary ,to the west＆amp;nbsp;of which formed allu-vial fan and braided river systems with sediments sourced from the western and the north-ern highland provenances ;and to the east of which developed retrograded fan deltas of different scales with clas-tic sediments sourced from highlands .Among the facies ,the fan delta front and braided river delta front are con-sidered to be home to hyd

关 键 词：沉积相 登娄库组 白垩系 松辽盆地东南隆起区 

分 类 号：TE121.3[石油与天然气工程—油气勘探]