南澜沧江构造岩浆带下侏罗统就康组的建立  

THE ESTABLISHMENT OF LOWER JURASSIC JIUKANG FORMATION IN SOUTH LANCANGJIANG TECTONIC MAGMATIC ZONE

作　　者：田应贵 胡鹏[1] 王承平[1] 

机构地区：[1]云南省地矿局区域地质矿产调查大队,云南玉溪653100

出　　处：《云南地质》2006年第1期63-69,共7页Yunnan Geology

基　　金：<1:25万临沧县幅;滚龙幅区域地质调查报告>成果之一

摘　　要：新建就康组为厚度较大的碎屑岩夹陆相火山岩地层。其底以角度不整合覆于三叠系中酸性火山岩之上,顶部被中侏罗统花开左组平行不整合覆盖。化石较丰富,时代归下侏罗统。The Jiukang Formation established recently is the thick clastic rock with intercalation of land facies volcanic rock, which belongs to the Lower Jurassic. The bottom of it is superimposed uncomformably on the Triassic intermediate - acid volcanic rock. The top of it is superimposed discomformabiy by Middle Jurassic Huakaizuo Formation. There are plentiful fossils in this formation.

关 键 词：新建就康组 下侏罗统 层型剖面 构造岩浆带 南澜沧江 云南 

分 类 号：P623.1[天文地球—地质矿产勘探]