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The Mississippi valley type Zn-Pb-celestite deposits at Wadi Essel, the Eastern Desert of Egypt: fluid inclusions and microthermometry evidences
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The Mississippi valley type Zn-Pb-celestite deposits at Wadi Essel, the Eastern Desert of Egypt: fluid inclusions and microthermometry evidences
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Journal Article
The Mississippi valley type Zn-Pb-celestite deposits at Wadi Essel, the Eastern Desert of Egypt: fluid inclusions and microthermometry evidences
2023
Overview
Sedimentary rocks of the Upper Cretaceous, Middle Miocene, Plio-Pleistocene, and Quaternary periods are present in the Red Sea coastal plain from south of El Quseir to Marsa Alam, and they are dispersed over Late Proterozoic basement rocks. The zinc and lead ores intercalated with celestite in Wadi Essel are dispersed throughout the adjacent rocks and intense in Middle Miocene sedimentary strata in clastic rocks. This work studied the fluid inclusions hosted in the celestite, which is in close to the lead–zinc mineralization, to measure the microthermometric parameters giving knowledge about the nature, composition and the condition of formation of celestite as well as lead- zinc mineralization. The fluid inclusions study for the celestite revealed that this celestite deposited from saline water (up to 9.054 wt% NaCl eq.) with density up to 1.045 g/cm
3
and the deposition of the celestite probably took place at temperatures between 50 and 75 °C for Wadi Essel celestite as well as accompanying lead–zinc sulphide, which considered as Mississippi valley type (MVT) Pb–Zn deposits.
