Mohammad Boomeri
University of Sistan and Baluchestan
27 Papers
79 Citations
Mohammad Boomeri is an academic researcher from University of Sistan and Baluchestan. The author has contributed to research in topics: Geology & Hypogene. The author has an hindex of 8, co-authored 23 publications.
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Papers
The Miduk porphyry Cu deposit, Kerman, Iran: A geochemical analysis of the potassic zone including halogen element systematics related to Cu mineralization processes
TL;DR: In this paper, the halogen fugacity ratio contour lines are transected by the measured values of biotite composition; this suggests the fluid composition, fO2 and fS2 of the fluids, and reaction between wall rock and hydrothermal fluids play a key role in the resultant halogene fugacities recorded in biotites that are critical to interpreting metal complexing behaviour during magmatic-hydrothermal evolution.
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The Sarcheshmeh porphyry copper deposit, Kerman, Iran: A mineralogical analysis of the igneous rocks and alteration zones including halogen element systematics related to Cu mineralization processes
TL;DR: The Sarcheshmeh porphyry copper deposit is located 65 km southwest of Kerman City, southeastern Iran as discussed by the authors, where a number of pyroxene-pyrite-bearing assemblages occur as primary phenocrysts.
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Metallogeny and Mineralization Potential of the Bazman Granitoids, SE Iran
TL;DR: In this article, field, petrography, and geochemical data were used to discriminate the Mesozoic Bazman granitoid either as productive or barren granitoids.
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Two-tiered magmatic-hydrothermal and skarn origin of magnetite from Gol-Gohar iron ore deposit of SE Iran: In-situ LA–ICP-MS analyses
Rezvan Mirzaei,Ali Ahmadi,Hassan Mirnejad,Hassan Mirnejad,Jian-Feng Gao,Kazuo Nakashima,Mohammad Boomeri +6 more
TL;DR: In this paper, the authors studied the evolution of magnetite from the Gol-Gohar iron deposit (GGID) of southeastern Iran with reference to elemental composition and found that the massive magnetite was formed by metasomatic reactions between iron-rich residual magmatic fluids and the magnesian carbonate host rocks (i.e., skarn type).
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