| 阿尔金山东段喀腊大湾中基性火山岩岩石地球化学特征及成因探讨 |
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| 引用本文： | 崔玲玲,陈柏林,杨农,陈正乐,丁文君.阿尔金山东段喀腊大湾中基性火山岩岩石地球化学特征及成因探讨[J].地质力学学报,2010,16(1):96-107. |
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| 作者姓名： | 崔玲玲 陈柏林 杨农 陈正乐 丁文君 |
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| 作者单位： | 中国地质科学院地质力学研究所;中国地质大学(北京)地球科学与资源学院; |
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| 基金项目： | 国家科技支撑计划重点项目 |
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| 摘 要： | 新疆阿尔金山东段喀腊大湾地区位于北东向阿尔金走滑断裂北侧与东西向阿尔金北缘断裂所夹持的区域,区内发育一套火山沉积岩系。对其中中基性火山岩进行较为系统的岩石地球化学研究,结果显示为LREE微弱富集型和部分平坦型两种稀土配分曲线型式,为岛弧型火山岩;微量元素的Zr/Nb、Nb/Ta以及Zr/Hf比值分析等地球化学特征表明本区经受了地壳物质的混染作用,火山岩的La-La/Sm投影显示为部分熔融和分离结晶共同作用产生的;Hf-Tu-Ta和TFeO-Na2O+K2O-Mg的构造环境投图显示本区火山岩主要为拉斑系列的火山弧玄武岩,推测本区早古生代为板块俯冲带上盘的岛弧环境,玄武岩类以幔源为主。
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| 关 键 词： | 喀腊大湾 火山岩 岩石地球化学 构造环境 |
| 收稿时间： | 2009/12/27 0:00:00 |
GEOCHEMISTRY AND GENESIS OF BASIC-INTERMEDIATE VOLCANIC ROCKS FROM KALADAWAN, EAST ALTUN TAGH MOUNTAINS |
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| CUI Ling-ling,CHEN Bai-lin,YANG Nong,CHEN Zheng-le and DING Wen-jun.GEOCHEMISTRY AND GENESIS OF BASIC-INTERMEDIATE VOLCANIC ROCKS FROM KALADAWAN, EAST ALTUN TAGH MOUNTAINS[J].Journal of Geomechanics,2010,16(1):96-107. |
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| Authors: | CUI Ling-ling CHEN Bai-lin YANG Nong CHEN Zheng-le and DING Wen-jun |
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| Institution: | CUI Ling-ling1,CHEN Bai-lin1,YANG Nong1,CHEN Zheng-le1,DING Wen-jun1,2(1.Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China,2.School of Earth Science and Resource,China University of Geosciences,Beijing 100083,China) |
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| Abstract: | The Kaladawan area at eastern part of the Altyn Tagh Mountain is tectonically situated between the NE-trending Altyn Tagh strike-slip fault and the W-E-trending Northern Altyn Tagh margin fault.In the area,there appears a set of volcanic-sedimentary rocks.A geochemical study has been made on the basic-intermediate volcanic rocks.The results show two REE patterns: slight LREE-enrichment pattern and a partly flat pattern,indicating an island-arc origin.The Zr /Nb,Nb / Ta and Zr /Hf values indicates that the v... |
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| Keywords: | Kaladawan volcanic rock geochemistry tectonic setting |
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