Eclogites

Geology Today Pub Date : 2024-02-08 DOI:10.1111/gto.12462
Ralf Halama
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Abstract

The beauty of an eclogite is something to behold: any petrologist marvels in the combination of red garnet and green omphacite that are the main mineral constituents of the rock. But besides their stunning appearance, there is much more to eclogites: fundamental concepts in metamorphic petrology and geodynamics were developed based on scientific investigations of eclogites. It is well established that they derive from precursor rocks of basaltic composition and form under high-pressure conditions at more than c. 45 km depth, but other aspects of their occurrences and geological significance remain debated. The relative scarcity of eclogites among crustal rocks renders them largely unknown to the layperson, so following the 200th anniversary of the term eclogite in 2022, there is an opportunity to take a closer look at this fascinating rock.

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埃克索格岩
埃洛石的美丽令人叹为观止:任何岩石学家都会惊叹于这种岩石的主要矿物成分--红色石榴石和绿色辉绿岩的组合。然而,除了令人惊叹的外表,埃洛ogite 还有更多内涵:变质岩石学和地球动力学的基本概念是在对埃洛ogite 进行科学研究的基础上发展起来的。夕卡岩源自玄武岩成分的前岩,在深度超过约 45 千米的高压条件下形成,这一点已得到公认,但关于夕卡岩的出现和地质意义的其他方面仍存在争议。在地壳岩石中,蚀变岩的数量相对较少,因此外行人对它们大多一无所知,因此在 2022 年蚀变岩这一术语诞生 200 周年之际,我们有机会近距离了解这种迷人的岩石。
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