新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2013年
3期
173-179
,共7页
靳刘圆%张济%朱志新%赵同阳%徐仕琪%李平%陈邦学
靳劉圓%張濟%硃誌新%趙同暘%徐仕琪%李平%陳邦學
근류원%장제%주지신%조동양%서사기%리평%진방학
哈尔里克山%火山岩%岩石地球化学特征%构造意义
哈爾裏剋山%火山巖%巖石地毬化學特徵%構造意義
합이리극산%화산암%암석지구화학특정%구조의의
Harlik Mountains%Volcanics%Petrological and Geochemical characteristics%Tectonic significance
通过对哈尔里克山地区火山岩岩性、岩相、岩石地球化学分析,确定研究区古生代火山岩可分为奥陶-泥盆纪钙碱性中基性火山岩建造,石炭纪为钙碱性中酸性火山岩建造,火山岩主要属钙碱性系列。岩类、岩相与岩石地球化学特征表明,本区火山岩在奥陶-泥盆纪为岛弧环境,随着吐哈盆地南缘活动陆缘逐渐向南迁移,石炭-二叠纪研究区变为弧后环境,研究区南侧存在泥盆-石炭纪向北俯冲的洋盆。
通過對哈爾裏剋山地區火山巖巖性、巖相、巖石地毬化學分析,確定研究區古生代火山巖可分為奧陶-泥盆紀鈣堿性中基性火山巖建造,石炭紀為鈣堿性中痠性火山巖建造,火山巖主要屬鈣堿性繫列。巖類、巖相與巖石地毬化學特徵錶明,本區火山巖在奧陶-泥盆紀為島弧環境,隨著吐哈盆地南緣活動陸緣逐漸嚮南遷移,石炭-二疊紀研究區變為弧後環境,研究區南側存在泥盆-石炭紀嚮北俯遲的洋盆。
통과대합이리극산지구화산암암성、암상、암석지구화학분석,학정연구구고생대화산암가분위오도-니분기개감성중기성화산암건조,석탄기위개감성중산성화산암건조,화산암주요속개감성계렬。암류、암상여암석지구화학특정표명,본구화산암재오도-니분기위도호배경,수착토합분지남연활동륙연축점향남천이,석탄-이첩기연구구변위호후배경,연구구남측존재니분-석탄기향북부충적양분。
Through the analysis of volcanics’lithology、lithofacies and rock geochemistry in Harlik area,to determine the Ordovician、Silurian and Devonian volcanic rocks combination is basalts-andesites-rhyolites, the Carboniferous vol-canics combination is andesites-dacites-rhyolites, basalts-rhyolites is Permain volcanic combination .The volcanics are mainly calc-alkalic series.Based on lithology、lithofacies and rock geochemistry characteristic indicate,volcanic rocks are forming in arc island setting at Ordovician-Devonian,with the active continental margin at southern sdge of Turpan-Ha-min basin was southward migration,the Harlik area become back arc setting.South of Harlik area exist northwards sub-ducted ocean basin at Devonian-Carboniferous.