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Can I read Barite mineralisation in the south Um Monqul area, north Eastern Desert, Egypt on EtoBox?
Barite mineralisation in the south Um Monqul area, north Eastern Desert, Egypt by Mohamed A. Wetait; Nagy S. Botros is a Earth and Planetary Sciences article available to read on EtoBox.
What is Barite mineralisation in the south Um Monqul area, north Eastern Desert, Egypt about?
The barite mineralisation in the north Eastern Desert of Egypt is hosted by Pan-African dacite, dacite porphyry and granite. The host rocks are variably altered by potassic, phyllic, phyllic-argillic, propylitic and advanced argillic alteration. The barite mineralisation is in veins trending east-northeast -west-southwest and dipping 65"-80° to the southeast. The veins are mainly of barite with subordinate quartz, accessory magnetite and specularite with minor sulphides (chalcopyrite, pyrite, covellite, enargite, bornite and pyrrhotite) and traces of Au. The barite mineralisation is associated with advanced argillic alteration, which resulted from interaction of the host rocks with acid sulphate fluids. It is envisaged that these fluids were released from high level intrusives similar to Cu bearing porphyry rocks. o 1997 Elsevier Science Limited. RBsume-La mineraiisation en baryte dans le Nord du Desert Oriental d'Egypte, est lice aux dacites, porphyres dacitiques et granites panafricains. Les roches encaissantes ont subi des alterations potassiques, phyllitiques, phyllitiques-pelitiques, propylitiques et une alteration pelitique prononcee. La mineralisation en baryte est presente
Who reads Barite mineralisation in the south Um Monqul area, north Eastern Desert, Egypt?
It is typically read by researchers, students, and practitioners in Earth and Planetary Sciences.
- Author
- Mohamed A. Wetait; Nagy S. Botros
- Publisher
- Elsevier Science; Elsevier ; Elsevier Ltd.; Elsevier BV (ISSN 1464-343X)
- Published
- 1997
- Language
- EN
- Field
- Earth and Planetary Sciences (Physical Sciences)