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Tectono-metamorphic evolution of Syros and Sifnos islands (Cyclades, Greece)

机译:锡罗斯岛和锡弗诺斯岛的构造变质演化(希腊基克拉泽斯)

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Miocene exhumation of metamorphic rocks in the Aegean Sea is partly a consequence of post-orogenic extension. If the postorogenic mechanism of exhumation is rather well understood, the earlier syn-orogenic Eocene exhumation is still largely enigmatic. Previous authors have argued in terms of extension or compression. New structural and petrological data on Sifnos and Syros islands show that exhumation of high pressure-low temperature (HP-LT) rocks involves crustal-scale extensional ductile shear zones during the Eocene. We observe a continuum of top-to-the-NE and -E ductile shear from the Eocene (in the blueschist facies) to the Miocene (in the greenschist facies). This deformation is distributed in the eclogites and blueschists, whereas it is rather localised along ductile shear zones in the greenschists. Eclogites, which are preserved only at the top of the structural pile, are exhumed with a 'cold' retrograde P-T path. In the lower part of the structural pile we observe a progressive retrogression of eclogites in blueschist then greenschist facies. This lower part of pile is subsequently exhumed with P-T paths showing a nearly isothermal decompression before cooling. P-T-t-deformation data suggest that the Cycladic blueschists are progressively exhumed by a continuum of accretion at the base of the orogenic wedge, and by a partly non-coaxial extensional deformation above, distributed during the syn-orogenic stage, then localised during the post-orogenic stage. We then compare the mechanism of syn-orogenic exhumation of Crete and the Cyclades and we discuss a simple geodynamic scenario for the Aegean domain and the external Hellenides which accounts for (1) the southward migration of the Hellenic trench and arc during the Cenozoic; (2) the P-T-t-deformation data for the Cycladic blueschists and the Phyllite-quartzite nappe; and (3) the transition from syn-orogenic to post-orogenic in the Cyclades. (C) 2001 Elsevier Science B.V. All rights reserved. [References: 58]
机译:爱琴海变质岩的中新世发掘部分是造山后扩张的结果。如果对掘尸的后造山机制很了解,则较早的同造山始新世的掘尸仍在很大程度上是个谜。先前的作者曾就扩展或压缩方面争论过。 Sifnos和Syros岛上的新结构和岩石学数据表明,在始新世期间,高压-低温(HP-LT)岩石的发掘涉及地壳尺度的伸展韧性剪切带。我们观察到从始新世(在蓝片岩相中)到中新世(在绿片岩相中)从上到下和上-E的韧性剪切的连续性。这种变形分布在榴辉岩和蓝岩岩中,而沿绿岩岩体中的韧性剪切带分布。仅保留在结构桩顶部的榴辉岩通过“冷”逆行P-T路径掘出。在结构桩的下部,我们观察到榴辉岩在蓝片岩相然后是绿片岩相中逐渐退化。随后在冷却之前,用下部的P-T路径挖掘桩的下部,该路径显示出几乎等温的减压。 PTt形变数据表明,基克拉迪岩性岩逐渐被造山楔底部的连续增生和上部的部分非同轴延伸变形所驱除,并在造山带阶段分布,然后在后造山阶段定位。造山阶段。然后,我们比较了克里特岛和基克拉泽斯山的同造山造化机制,并讨论了爱琴海域和外部Hellenides的简单地球动力学情景,这些情景解释了(1)新生代中希腊海沟和弧线的向南迁移; (2)基克拉迪蓝晶岩和辉绿岩-石英岩推覆的P-T-t变形数据; (3)基克拉泽斯地区从同造山过渡到后造山。 (C)2001 Elsevier Science B.V.保留所有权利。 [参考:58]

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