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The Timpa delle Murge ophiolitic gabbros, southern Apennines: insights from petrology and geochemistry and consequences to the geodynamic setting

机译:Timpa Delle武吉武吉博士莫希蒂替斯科省,南部亚平宁山脉:从岩石学和地球化学的见解以及地球动力学环境的后果

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摘要

The Timpa delle Murge ophiolite in the North Calabrian Unit is part of the Liguride Complex (southern Apennines). The study is concentrated on the gabbroic part of the ophiolite of the Pollino area. They preserve the high-grade ocean floor metamorphic and locally developed flaser textures under ocean floor conditions. The primary magmatic assemblages are clinopyroxene, plagioclase, and opaques. Brown hornblende is a late magmatic phase. Green hornblende, actinolite, albite, chlorite and epidote display metamorphic recrystallization under lower amphibolite facies conditions, followed by greenschist facies.
机译:Timpa在北卡拉比亚单位中掠夺Murge Ophiolite是Liguride Complex(南赤龄)的一部分。 该研究集中在Pollino地区的眼镜矿石的Gabbroice部分。 它们保留高档海底变质和局部开发的瓶纹理在海底条件下。 主要岩石组合物是临床,Plagioclase和Opaques。 棕色Hornblende是晚期岩石阶段。 绿色角势,Actinolite,Albite,氯酸盐和环虫在较低的倒数倒数下显示变质重结晶,其次是绿色植物相。

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