首页> 外文OA文献 >Geochemical Signature of Mesozoic Volcanic and Granitic Rocks in Madina Regency Area, North Sumatra, Indonesia, and Its Tectonic Implication
【2h】

Geochemical Signature of Mesozoic Volcanic and Granitic Rocks in Madina Regency Area, North Sumatra, Indonesia, and Its Tectonic Implication

机译:印度尼西亚北苏门答腊岛麦地那摄政区中生代火山岩和花岗岩的地球化学特征及其构造意义

摘要

Http://dx.doi.org/10.17014/ijog.vol4no2.20094Five samples consisting of two Permian-Triassic basalts, two Triassic-Jurassic granitic rocks, and a Miocene andesite were collected from the Madina Regency area in North Sumatra that is regionally situated on the West Sumatra Block. Previous authors have proposed three different scenarios for the geological setting of West Sumatra Permian Plutonic-Volcanic Belt, namely an island-arc, subduction related continental margin arc, and continental break-up. Petrographic analysis of the Mesozoic basaltic samples indicates that they are island-arcs in origin; however their trace element spider diagram patterns (Rock/MORB ratio) also show the character of back-arc marginal basin, besides the island-arc. Furthermore, their REE spider diagram patterns (Rock/ Chondrite ratio) clearly reveal that they were actually generated in a back-arc marginal basin tectonic setting. Meanwhile, the two Mesozoic granitic rocks and the Miocene andesite reflect the character of an active continental margin. Their spider diagram patterns show a significant enrichment on incompat- ible elements, usually derived from fluids of the subducted slab beneath the subduction zone. The high enrichment on Th makes their plots on Ta/Yb versus Th/Yb diagram are shifted to outside the active continental margin field. Although the volcanic-plutonic products represent different ages, their La/Ce ratio leads to a probability that they have been derived from the same magma sources. This study offers another different scenario for the geological setting of West Sumatra Permian Plutonic-Volcanic Belt, where the magmatic activities started in a back-arc marginal basin tectonic setting during the Permian-Triassic time and changed to an active continental margin during Triassic to Miocene. The data are collected through petrographic and chemical analyses for major, trace, and REE includ- ing literature studies.
机译:http://dx.doi.org/10.17014/ijog.vol4no2.20094从北苏门答腊岛的Madina Regency地区收集了五个样品,这些样品包括两个二叠纪-三叠纪玄武岩,两个三叠纪-侏罗纪花岗岩和一个中新世安山岩。位于西苏门答腊街区。先前的作者针对西苏门答腊二叠系云母-火山带的地质环境提出了三种不同的方案,即岛弧,俯冲相关的大陆边缘弧和大陆破裂。中生代玄武岩样品的岩石学分析表明,它们起源于岛弧。然而,除了岛弧外,它们的痕量蜘蛛图模式(Rock / MORB比)也显示了弧后边缘盆地的特征。此外,它们的REE蜘蛛图模式(岩石/球粒比)清楚地表明它们实际上是在弧后边缘盆地构造环境中产生的。同时,两个中生代花岗岩和中新世安山岩反映了活跃的大陆边缘的特征。他们的蜘蛛图模式显示了不相容元素的大量富集,这些元素通常来自俯冲带下方俯冲板块的流体。 Th的高富集使他们在Ta / Yb与Th / Yb图上的图移到活动大陆边缘场之外。尽管火山-古生代产品代表不同的年龄,但它们的La / Ce比导致它们有可能来自相同的岩浆源。这项研究为西苏门答腊二叠纪云母-火山带的地质环境提供了另一种不同的情况,在这里,岩浆活动始于二叠纪-三叠纪时期的弧后边缘盆地构造环境,并在三叠纪至中新世时期转变为活跃的大陆边缘。 。通过岩石学和化学分析收集的数据用于主要的,痕量的和REE包括文献研究。

著录项

  • 作者

    Zulkarnain, Iskandar;

  • 作者单位
  • 年度 2009
  • 总页数
  • 原文格式 PDF
  • 正文语种 EN
  • 中图分类

相似文献

  • 外文文献
  • 中文文献
  • 专利

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号