首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Panafrican basement and Mesozoic gabbro in the Zagros orogenic belt in the Dorud-Azna region (NW Iran): Laser-ablation ICP-MS zircon ages and geochemistry
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Panafrican basement and Mesozoic gabbro in the Zagros orogenic belt in the Dorud-Azna region (NW Iran): Laser-ablation ICP-MS zircon ages and geochemistry

机译:Dorud-Azna地区(伊朗西北部)的Zagros造山带中的泛非基底和中生辉长岩:激光烧蚀ICP-MS锆石的年龄和地球化学

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The Dorud-Azna region of the Sanandaj-Sirjan metamorphic zone (sswz) in NW Iran is part of the Zagros orogenic belt and exposes an amphibolite-grade metamorphic succession of mixed continental (e.g., the granitic Galeh-Doz orthogneiss) and oceanic or rift (e.g., various amphibolites) origin, which is intruded by the Darijune gabbro. Laser-ablation ICP-MS U-Pb zircon ages of 608 +/- 18 Ma and 588 +/- 41 Ma of the granitic Galeh-Doz orthogneiss indicate a Panafrican basement similar to that of the Yazd block of Central Iran. We therefore interpret this part of the SSMZ to represent a previously subducted part of the Panafrican basement of the Iranian microcontinent Based on geochemistry, amphibolites and metagabbros from the Amphibolite unit representially potentially the cover on the Panafrican Galeh-Doz orthogneiss are interpreted to have their origin in a likely Upper Paleozoic to Mesozoic rift or E-MORB ophiolite succession. One of the metagabbros, here termed Dare-Hedavand metagabbro yield a Pb-206/U-238 mean age of 314.6 +/- 3.7 Ma. Talc-bearing greenschists to epidote amphibolites of the Triassic June complex formed in a similar, but younger environment. Furthermore, the metamorphic complex is intruded by the Darijune gabbro, which yields a mean ICP-MS U-Pb zircon age of 170.2 +/- 3.1 Ma. The final stage of likely Jurassic greenschist facies-grade metamorphism postdates the gabbro intrusion. We interpret the Darijune gabbro to have resulted from the initial subduction of Neotethyan oceanic lithosphere in a continental arc setting. The new data combined with data from literature indicate that the SSMZ represents a tectonic element of a mixed continental and oceanic origin, likely accreted to Central Iran during a Jurassic tectonic process. The new data also constrains thick-skinned nappe stacking within the Sanandaj-Sirjan zone. (C) 2015 Elsevier B.V. All rights reserved.
机译:伊朗西北部Sanandaj-Sirjan变质带(sswz)的Dorud-Azna地区是Zagros造山带的一部分,暴露了混合大陆(例如,花岗岩Galeh-Doz Orthogneiss)和海洋或裂谷的闪石级变质演替。 (例如,各种角闪石)起源,这是由Darijune gabbro入侵的。花岗岩Galeh-Doz斜长岩的激光烧蚀ICP-MS U-Pb锆石年龄为608 +/- 18 Ma和588 +/- 41 Ma,表明该Panafrican基底类似于伊朗中部亚兹德区块。因此,我们将SSMZ的这一部分解释为代表伊朗微洲Panafrican地下室的先前俯冲部分。根据地球化学,来自Amphibolite单元的角闪石和变质辉长岩很有可能被解释为Panafrican Galeh-Doz Orggneiss的盖层可能是上古生界到中生代裂谷或E-MORB蛇绿岩的继承。一种变种,这里称为Dare-Hedavand metagabbro,产生的Pb-206 / U-238平均年龄为314.6 +/- 3.7 Ma。含滑石粉的绿主义者将三叠纪六月复合物的闪石闪现出来,形成于一个相似但较年轻的环境中。此外,该变形复合物被Darijune gabbro侵入,从而产生的ICP-MS U-Pb锆石平均年龄为170.2 +/- 3.1 Ma。侏罗纪绿岩相相变质的最后阶段要晚于辉长岩入侵。我们认为,Darijune gabbro是由大陆弧环境中的新特提斯洋岩石圈的初始俯冲产生的。新数据与文献数据相结合,表明该地区代表了大陆和海洋混合的构造元素,可能在侏罗纪构造过程中沉积到伊朗中部。新数据还限制了Sanandaj-Sirjan区内厚皮的尿布堆积。 (C)2015 Elsevier B.V.保留所有权利。

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