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首页> 外文期刊>Economic Geology >Eocene Gold Ore Formation at Muteh, Sanandaj-Sirjan Tectonic Zone, Western Iran: A Result of Late-Stage Extension and Exhumation of Metamorphic Basement Rocks within the Zagros Orogen
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Eocene Gold Ore Formation at Muteh, Sanandaj-Sirjan Tectonic Zone, Western Iran: A Result of Late-Stage Extension and Exhumation of Metamorphic Basement Rocks within the Zagros Orogen

机译:伊朗西部Sanandaj-Sirjan构造带Muteh的始新世金矿形成:Zagros造山带内变质基底岩后期扩展和掘出的结果

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摘要

A multidisciplinary study including field geology, microstructure analysis, 40Ar/39Ar dating, and fluid inclusion microthermometry and Raman spectrometry has been carried out on the Muteh gold deposit located in a greenschist to amphibolite facies metamorphic rock complex of the Sanandaj-Sirjan tectonic zone, Zagros orogen, Iran. The Muteh gold deposit has been previously interpreted as genetically related to Precambrian granitic intrusions, as an exhalative hot-spring deposit related to Paleozoic rhyolitic-acidic tuffs, and to local metamorphic processes.
机译:多学科研究,包括现场地质,微观结构 分析, 40 Ar / 39 Ar测年,流体包裹体温计 和拉曼光谱法已在位于绿岩岩上的Manteh金 矿床上进行了勘探,该矿床为萨格罗斯造山带Sanandaj-Sirjan构造带变质 岩石复合体的闪石岩相, < / sup>伊朗。穆特赫金矿床以前被解释为与前寒武纪花岗岩侵入岩在遗传上有关,而 为与古生代流变-酸性 有关的呼气温泉矿床。凝灰岩和局部变质过程。

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  • 来源
    《Economic Geology》 |2006年第8期|1497-1524|共28页
  • 作者单位

    Section des Sciences de la Terre, Université de Genève, Rue des Mara?chers 13, 1205 Genève, Switzerland;

    Faculty of Environment, University of Tehran, Ghods St 25, P.O. Box 14155-6135, Tehran, Iran;

    Department of Geology and Geophysics, University of Wisconsin-Madison, 1215 West Dayton Street, Madison, Wisconsin 53706;

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