北茶中发现d’éclogites冷杉林ı̂不会Mauritanides(西非)

Élisabeth Le Goff , Catherine Guerrot , Gilbert Maurin , Véra Johan , Monique Tegyey , Mustapha Ben Zerga
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引用次数: 19

摘要

在构成西撒哈拉海西推覆体延伸的单元(北毛里塔尼德)内发现了榴辉岩。榴辉岩组合为Grt + Omp (Jd30-40) +钡石+ Qtz + Rt±云母+ Ep。估计压力-温度条件为550-600°C, 13-15 kbar。通过对锆石的单一蒸发法获得的年代学数据表明,这是一次泛非事件(595 Ma),可能归因于原岩的岩浆结晶作用。用石榴石和辉长石进行的Sm-Nd测年表明在330 Ma发生海西期变质事件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Découverte d'éclogites hercyniennes dans la chaı̂ne septentrionale des Mauritanides (Afrique de l'Ouest)

Eclogites have been discovered within units constituting the prolongation of the Hercynian nappes of the Western Sahara (Northern Mauritanides). The eclogitic assemblage comprises Grt + Omp (Jd30–40) + barroisite + Qtz + Rt ± phengite + Ep. Estimated pressure–temperature conditions are 550–600 °C, 13–15 kbar. Geochronological data obtained by the single evaporation method on zircons characterise a Panafrican event (595 Ma), which could be attributed to the magmatic crystallisation of the protolith. Sm–Nd dating by using garnet and omphacite argue for an Hercynian metamorphic event at 330 Ma.

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