川中川南过渡带须家河组二段沉积相研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
在了解区域沉积背景的情况下,通过对大量野外剖面观察、地震剖面资料、测井资料、取心井段和单井沉积微相研究的基础上,确定了研究区须家河组二段为河流三角洲-湖泊沉积体系,主要发育三角洲前缘、前三角洲、浅湖3种沉积亚相。三角洲前缘亚相以水下分流河道微相占优势,先期形成的河口坝往往受后期水下分流河道冲刷侵蚀而得不到完整保存,所以须家河组二段河口坝不甚发育,在剖面上水下分流河道与河口坝多呈冲刷截切叠置关系。
Based on the understanding of background of regional sedimentation, observing for large amount of drilling, coring and field section plane, analyzing for seismic data, logging information, as well as the study on the sedimentary microfacies of coring section and single well, it is determined that the region of interest of the second member of Xujiahe Formation is formed in a sedimentary system of river delta to lake. Three subfacies have been mainly developed, which are deltafront, prodelta and shallow lake. The deltafront subfaceies is dominantly of underwater distributary channel. The pre-formed mouth bars are not preserved completely because of the erosion by the underwater distributary channel that formed latter, so the mouth bar in the second member of Xujiahe Formation is not well developed. Underwater distributary channel and mouth bar are often in relations of flushing, intercepting and overlaying in the section.
引文
[1]朱仕军,黄继详.川中-川南过渡带香溪群地层划分与对比[J].西南石油学院学报:自然科学版,1996,18(2):1-7.
    [2]赵澄林,朱筱敏.沉积岩石学[M],北京:石油工业出版社,2001.
    [3]张庆国,鲍志东,那末红,等.松辽盆地中央坳陷南部下白至统泉头组四段沉积相[J].古地理学报,2007,9(3):267-276.
    [4]高红灿,郑荣才,柯光明,等.川西上侏罗统遂宁组沉积相特征[J].古地理学报,2006,8(4):468-476.
    [5]董贵能,姜在兴,张本琪.济阳坳陷埕东地区新近系馆上段下部三角洲沉积特征[J].油气地质与采收率,2007,14(3):22-25.
    [6]王海林,田家祥.不同类型三角洲特征探讨[J].大庆石油学院学报,1994,18(4):135-139.
    [7]蒋维红,董春梅,闫家宁.岩相古地理学研究现状及发展趋势[J].断块油气田,2007,14(3):1-4.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心