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Structural and metallogenic map of late Variscan Arbus Pluton (SW Sardinia, Italy)

机译:瓦里斯卡纳阿不思·普鲁顿晚期(意大利撒丁岛,意大利)的结构和成矿图

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This paper presents the geological, structural and metallogenic map of the Arbus Pluton, a late Variscan composite intrusion belonging to the Corsica-Sardinia Batholith. The pluton is surrounded and crosscut by a wide variety of vein ore deposits. The Arbus Pluton was emplaced at shallow crustal levels at the end of the Variscan Orogeny, along an E–W trending shear zone located in the low-grade external nappe pile of the Sardinian basement. The architecture of the pluton is roughly concentric with a core of cordierite-bearing leucogranites and an outer shell composed of pyroxene-bearing and hornblende granodiorites. New U/Pb dating on zircons of granodiorite yields an emplacement age of 303.7?±?1.1 which improves previous Rb/Sr and Ar/Ar dating. The map has been compiled on the basis of new geological/structural surveys and petrographical studies coupled with in situ gamma ray spectrometry. All the data-sets have been processed using a geographical information system.
机译:本文介绍了Arbus Pluton(属于科西嘉-撒丁岛岩床)的晚期Variscan复合侵入体的地质,构造和成矿图。岩体被各种各样的脉状矿床包围和横切。 Arbus Pluton放在瓦里斯卡造山带末端的浅层地壳上,沿着撒丁岛地下室低品位外部推覆桩中的E-W趋势剪切带布置。岩体的结构大致与含堇青石的亮石英花岗岩核心和由辉石和角闪石花岗闪长岩组成的外壳同心。在花岗闪长岩的锆石上新的U / Pb测年产生了303.7±1.1的镶嵌年龄,这改善了以前的Rb / Sr和Ar / Ar测年。该地图是根据新的地质/构造勘测和岩石学研究以及原位伽马射线能谱法编制的。所有数据集均已使用地理信息系统进行了处理。

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