Petrogenesis of the late Tonian arc-related Um Balad gabbro-diorite complex (Egypt) and insight into its spatially related orogenic gold mineralization-Reference-Cited by-同舟云学术

Petrogenesis of the late Tonian arc-related Um Balad gabbro-diorite complex (Egypt) and insight into its spatially related orogenic gold mineralization

Published:2022-02-06 Issue:1 Volume:65 Page:89-113
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Abd El-Rahman Yasser¹^ORCID,Seifert Thomas²,Schulz Bernhard²,Hofmann Mandy³^ORCID,Gärtner Andreas³,Linnemann Ulf³,Said Amir¹

Affiliation:

1. Geology Department, Faculty of Science, Cairo University, Giza, Egypt

2. Division of Economic Geology and Petrology, Technische Universität Bergakademie Freiberg, Institute of Mineralogy, Freiberg, Germany

3. Museum für Mineralogie und Geologie, GeoPlasmaLab, Senckenberg Naturhistorische Sammlungen Dresden, Dresden, Germany

Funder

Alexander von Humboldt postdoctoral fellowship

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2022.2034057

Reference146 articles.

1. Fluid evolution of Au-Cu zones in Um Balad area, North Eastern Desert of Egypt: Implications from mineral chemistry and fluid inclusions

2. Cryogenian ophiolite tectonics and metallogeny of the Central Eastern Desert of Egypt

3. The South Um Mongul Cu-Mo-Au prospect in the northern Eastern Desert of Egypt: Tonian porphyry-style mineralization with an Ediacaran hydrothermal iron oxide overprint

4. The South Um Mongul Cu-Mo-Au prospect in the Eastern Desert of Egypt: From a mid-Cryogenian continental arc to Ediacaran post-collisional appinite-high Ba-Sr monzogranite

5. Regional setting and characteristics of the Neoproterozoic Wadi Hamama Zn–Cu–Ag–Au prospect: evidence for an intra-oceanic island arc-hosted volcanogenic hydrothermal system

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