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鄂拉山查查香卡地区晚三叠世火山岩产出环境分析
引用本文:芦文泉,童海奎,仓索南尖措,马永胜.鄂拉山查查香卡地区晚三叠世火山岩产出环境分析[J].西北地质,2012,45(1):48-55.
作者姓名:芦文泉  童海奎  仓索南尖措  马永胜
作者单位:1. 青海省国土资源勘查项目管理中心,青海西宁,810001
2. 青海省第四地质矿产勘查院,青海西宁,810001
基金项目:中国地质调查局地质大调查项目“青海省地质找矿工作跟踪研究”(121201140119)
摘    要:通过对查查香卡地区晚三叠世火山岩岩石学研究,确定该套火山岩属晚三叠世鄂拉山组,属钙碱性系列。喷出时的大地构造环境为陆内造山环境,该火山岩最初可能形成于大陆边缘环境,由于A型俯冲构造活动,测区乃至鄂拉山地区产生一系列右旋走滑断裂带,受北西向右旋走滑断裂的影响,岩石孔隙加大,并出现强烈的热流活动,导致岩浆沿这些断裂带喷出地表。

关 键 词:岩石学  陆内造山  构造环境  东昆仑晚三叠世火山岩带  查查香卡

Analysis of Environment for Late Triassic Volcanic Rocks in Chachaxiangka, Elashan
LU Wen-quan , TONG Hai-kui , CANG Suo-nanjiancuo , MA Yong-sheng.Analysis of Environment for Late Triassic Volcanic Rocks in Chachaxiangka, Elashan[J].Northwestern Geology,2012,45(1):48-55.
Authors:LU Wen-quan  TONG Hai-kui  CANG Suo-nanjiancuo  MA Yong-sheng
Institution:Center for Land Resources Exploration Projict Management in Qinghai Provinec, Xining 810001, China Quaternary Geology and Mineralresources Exploration in Qinghai Province, Xining 810001, China
Abstract:Through study on Petrology of the Late Triassic volcanic rocks from Chachaxiangka area, the volcanic rocks belong to Elashan Formation and are calc- alkaline series. Considering the tectonic setting of intra-continental orogenic environment, the Late Triassic volcanic rocks initially may form in the continen- tal marginal environment. Researched area and even Elashan area produced a series of right rotary sliding fault zone because "A" type subduction. Affected by northwestern Right-lateral strike slip fault zone, rock pore increased and strongly heat flow activities appears coursing magma spray out surface along these fault zone.
Keywords:petrology intra-continental orogenic tectonic environments Late Triassic volcanic belt ofEastern Kunlun mountains ~ Chachaxiangka
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