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延边金谷山地区早二叠世"柯岛岩组"火山喷发-沉积构造划分及构造环境
引用本文:王建新,常建平,赵志,解成波.延边金谷山地区早二叠世"柯岛岩组"火山喷发-沉积构造划分及构造环境[J].吉林大学学报(地球科学版),2004,34(3):333-337.
作者姓名:王建新  常建平  赵志  解成波
作者单位:1. 吉林大学,地球科学学院,吉林,长春,130061
2. 吉林省地勘局,吉林,长春,130061
基金项目:中国地质调查局矿产资源调查补偿基金
摘    要:延边金谷山地区二叠纪"柯岛岩组"为一套低绿片岩相变质岩系,其原岩为一套酸性-中酸性火山碎屑沉积岩系.通过剖面详细测量和岩石学研究,建立了该地区"柯岛岩组"层序,划分了6个火山喷发-沉积旋回,并依据各旋回序列岩相组合特征,恢复了该地区在陆表海裂陷(槽)构造条件水下火山喷发-沉积作用及演化环境.

关 键 词:延边金谷山地区  柯岛岩组  变质原岩  火山喷发-沉积旋回  沉积构造环境  延边金谷山地区  早二叠世  柯岛岩组  火山喷发  沉积构造  划分  构造环境  area  Formation  rock  Early  Permian  structures  tectonic  settings  演化  沉积作用  构造条件  裂陷  陆表海  恢复  特征
文章编号:1671-5888(2004)03-0333-05
修稿时间:2003年7月10日

Classification and tectonic settings of the volcanic-sedimentary structures of the Early Permian Kedao rock Formation in the Jingushan area,Yanbian
WANG Jian-xin.Classification and tectonic settings of the volcanic-sedimentary structures of the Early Permian Kedao rock Formation in the Jingushan area,Yanbian[J].Journal of Jilin Unviersity:Earth Science Edition,2004,34(3):333-337.
Authors:WANG Jian-xin
Institution:WANG Jian-xin~
Abstract:The Permian Kedao Formation in the Jingushan area,Yanbian belongs to a succession of metamorphic rocks of low greenschist facies. Their parental rocks consist of a set of acid-intermediate-acid pyroclastics. Based on detailed profile measurement and petrological studies, the sequence of the Kedao rock Formation in the area has been set up and six volcanic eruption-sedimentation cycles are divided. Based on the lithofacies and their association of each cycle, a tectonic setting in which marine volcanic eruption and sedimentation in an inland rift is reconstructed.
Keywords:Jingushan area  Yanbian  Kedao rock Formation  parental rocks of metamorphic rocks  cycle of volcanic eruption-sedimentation  sedimentation-tectonic setting
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