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辽宁北票四合屯盆地下白垩统义县组沉积相

Sedimentary facies of the Yixian Formation of Lower Cretaceous in Sihetun Basin of Beipiao,Liaoning Province

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【作者】 张立军巩恩普徐德亮刘雪飞李金

【Author】 Zhang Lijun 1,2 Gong Enpu 1 Xu Deliang 2 Liu Xuefei 2 Li Jin 2 1 Institute of Resources and Civil Engineering,Northeast University,Shenyang 110004,Liaoning2 Administration of Fossil Resources Protection of Liaoning Province,Shenyang 110032,Liaoning

【机构】 东北大学资源与土木工程学院辽宁省化石资源保护管理处辽宁省化石资源保护管理处 辽宁沈阳110004辽宁沈阳110032辽宁沈阳110004辽宁沈阳110032

【摘要】 本文系统地论述了北票四合屯盆地下白垩统义县组沉积相及其演化 ,将盆地演化划分为继承性初始坳陷、火山洼地、湖盆沉降与扩展等阶段 ,其后由于火山作用而使盆地封闭。与盆地演化相对应 ,建立了盆内义县组的沉积相序 ,自下而上依次为冲积扇与河流相、火山沉积相、河流相、湖相、火山溢流相 ,并指出火山喷发间歇期湖盆的湖水进退规律、水体性质以及沉积环境特征。

【Abstract】 This paper systematically discusses the formation and evolution of the Sihetun Basin during the sedimentary period of the Yixian Formation of Lower Cretaceous.The evolution of the basin may be divided into three stages,namely,inherited initial depression,volcanic swale,and the subsidence and expansion of the lacustrine basin.The subsequent volcanism closed the basin.According to the evolution of the basin,a sedimentary facies sequence of the Yixian Formation is established as follows in an ascending order: the alluvial fan and fluvial facies,volcanic sediment facies,fluvial facies,lacustrine facies and volcanic effusive facies.The paper emphasizes on the dividing indicators of sedimentary facies and their origins and analyzes the transgression and regression of lake water,as well as the characters of water body and the sedimentary environment during the volcanic dormant period.

【基金】 辽宁省科技攻关计划项目 (编号 :2 0 0 12 3 0 0 0 1)“辽宁北票四合屯鸟化石形成地质环境研究”项目;教育部博士点专项基金 (编号 :2 0 0 2 14 5 0 0 2 )“辽西中生代反鸟类起源、早期辐射与演化序列研究”项目资助
  • 【文献出处】 古地理学报 ,Journal of Palaeogeography , 编辑部邮箱 ,2005年01期
  • 【分类号】P512.2
  • 【被引频次】13
  • 【下载频次】279
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