伊朗高压-低温变质岩及其地球动力学意义综述

IF 2.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Mirmohammad Miri , Ali A. Sepahi
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引用次数: 0

摘要

榴辉岩和蓝片岩等高压低温岩石保存了有关俯冲带历史和地球动力学的宝贵信息。伊朗暴露的HP-LT岩石形成于伊朗微板下古特提斯和新特提斯海洋岩石圈的俯冲过程中,随后在二叠纪至始新世早期被挖掘出来。Shanderman和Anarak杂岩与古特提斯有关,Shahrekord、Hajibad-Esfandaghe、Sistan、Makran和Sabzevar杂岩与新特提斯有关。榴辉岩变质高峰期形成石榴石+绿帘石+角闪石(Na-,Na-Ca)+白云母+钠长石±帘石组合,蓝片岩形成角闪石(Na-,NaCa)+钠长石+白云母±帘石±绿帘石组合。逆行变质作用用绿帘石-角闪岩和绿片岩相矿物组合(Ca角闪石+Na Ca斜长石+绿帘石+绿泥石)取代了峰值组合。对于各种配合物,地热测量计算和相图建模显示峰值P-T条件为23 kbar-600°C(Shanderman)、14 kbar-560°C(Anarak)、25 kbar-670°C(Shahrekord)、17 kbar-530°C(Hajibad-Esfandaghe)、24 kbar-650°C(Sistan)、15 kbar-560C(Makran)和17 kbar-570°C(Sabzevar)。它们的逆行P-T条件分别为~6 kbar-470°C、7 kbar-500°C、6 kbar-530°C、10 kbar-450°C、8 kbar-500°C、700 kbar-5000°C和6 kbar-490°C。所获得的P-T条件表示古特提斯HP-LT杂岩的地热梯度为12–16°C/km,新特提斯为7–11°C/km。野外和岩相研究表明,俯冲变质作用主要沿顺时针P-T路径发生,但Hajibad-Esfandaghe、Makarn和Anarak杂岩的一个子单元除外,它们经历了逆时针路径。这种差异可能表明,新特提斯洋岩石圈的俯冲角比古特提斯大,导致中生代冷地热梯度和大陆弧后盆地的发育。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
High-pressure – Low-temperature metamorphic rocks of Iran and their geodynamic significance: A review

High-pressure-low-temperature (HP-LT) rocks such as eclogites and blueschists preserve valuable information about the history and geodynamics of subduction zones. HP-LT rocks exposed in Iran formed during subduction of Paleo-Tethys and Neo-Tethys oceanic lithosphere beneath the Iran microplate and were subsequently exhumed from the Permian to the Early Eocene. The Shanderman and Anarak complexes are associated with Paleo-Tethys, and the Shahrekord, Hajiabad-Esfandaghe, Sistan, Makran, and Sabzevar complexes are related to Neo-Tethys. The assemblage garnet + omphacite + amphibole (Na-, Na-Ca) + white mica + albite ± zoisite formed at the peak metamorphism stage of the eclogites, and amphibole (Na-, Na-Ca) + albite ± white mica ± zoisite ± epidote ± lawsonite formed in blueschists. Retrograde metamorphism replaced peak assemblages with epidote-amphibolite and greenschist facies mineral assemblage (Ca-amphibole + Na-Ca plagioclase + epidote + chlorite). For the various complexes, geothermobarometry calculations and phase diagram modeling show peak P-T conditions of 23 kbar - 600 °C (Shanderman), 14 kbar - 560 °C (Anarak), 25 kbar - 670 °C (Shahrekord), 17 kbar - 530 °C (Hajiabad-Esfandaghe), 24 kbar - 650 °C (Sistan), 15 kbar - 560 °C (Makran), and 17 kbar - 570 °C (Sabzevar). Their retrograde P-T conditions are ∼6 kbar - 470 °C, 7 kbar - 500 °C, 6 kbar - 530 °C, 10 kbar - 450 °C, 8 kbar - 500 °C, 7 kbar − 500 °C and 6 kbar - 490 °C, respectively. The obtained P-T conditions represent a geothermal gradient of 12–16 °C/km for the Paleo-Tethys HP-LT complexes and 7–11 °C/km for the Neo-Tethys. Field and petrographic studies reveal that subduction metamorphism occurred mostly along clockwise P-T paths, except for the Hajiabad-Esfandaghe, Makarn and a subunit of the Anarak complexes that endured counter-clockwise paths. The differences may show a greater subduction angle of Neo-Tethys oceanic lithosphere than Paleo-Tethys, resulting in a cold geothermal gradient and development of continental back-arc basins during the Mesozoic.

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来源期刊
Journal of Geodynamics
Journal of Geodynamics 地学-地球化学与地球物理
CiteScore
4.60
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: The Journal of Geodynamics is an international and interdisciplinary forum for the publication of results and discussions of solid earth research in geodetic, geophysical, geological and geochemical geodynamics, with special emphasis on the large scale processes involved.
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