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层序地层学体系域划分的局限性--以二连盆地WL凹陷为例
引用本文:王婧韫.层序地层学体系域划分的局限性--以二连盆地WL凹陷为例[J].地层学杂志,2004,28(3):244-247,256.
作者姓名:王婧韫
作者单位:中原油田分公司勘探开发科学研究院,河南濮阳,457001
基金项目:中国石油化工集团公司资助项目
摘    要:陆相层序地层学的一个主要内容是将三级层序划分为“低水位体系域、湖进体系域和高水位体系域”等三个水位域沉积体系 ,分别代表着一个湖盆沉积的三个阶段。低水位体系域和高水位体系域水体较浅 ,沉积较粗 ,而湖进水位域则水体较深 ,沉积较细。长期以来 ,从国外传入的三个水位域沉积体系划分成为研究陆相沉积的经典模式。以内蒙古二连盆地 WL 凹陷为例 ,指出这种模式具有一定的局限性 ,生搬套用可能产生一些错误的认识 ,甚至直接影响研究成果的可靠性

关 键 词:沉积  层序地层学  体系域  不整合面  岩性  内蒙古
文章编号:0253-4959(2004)03-0244-04

LIMITATIONS OF DIVISION OF SYSTEMS TRACTS IN THE SEQUENCE STRATIGRAPHY--TAKING THE WL DEPRESSION OF THE ERLIAN BASIN FOR EXAMPLE
WANG Jing-yun.LIMITATIONS OF DIVISION OF SYSTEMS TRACTS IN THE SEQUENCE STRATIGRAPHY--TAKING THE WL DEPRESSION OF THE ERLIAN BASIN FOR EXAMPLE[J].Journal of Stratigraphy,2004,28(3):244-247,256.
Authors:WANG Jing-yun
Abstract:One of the main contents of continental sequence stratigraphy is dividing the three-order se-quence into “LST, TST and HST”, representing three stages of a lake basin deposition. Water body is shallow and sediments are coarse in LST and HST, but in TST, being deep and fine. For a long time, the above division of systems tracts has been a classical model in the study of continental deposition. Judging from the WL Depression of the Erlian Basin, Inner Mongolia, it must be pointed out in this paper that this model has its limitations and if applied mechanically, some misunderstanding may occur and even would produce direct influence on the reliability of the research results.
Keywords:deposition  sequence stratigraphics  systems tracts  unconformity  lithology  Inner Mongolia
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