, 1996 Quartz-monzodiorite is generally considered to represent the parent magma of high-Mg quartz-monzodiorite plutonic suites; thus such suites are thought to be melts from a metasomatized mantle wedge.
Bédard, L. Paul
core
Petrological and geochemical characterization of Abu Murrat syn-orogenic I-type and post-orogenic A-type neoproterozoic granitoids, North Eastern Desert, Egypt. [PDF]
Sci RepEl-Awady A +4 more
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Lithology Identification of Metamorphic Basement Reservoirs in the J Oilfield Using a Linear Discriminant Analysis-Assisted Supervised Self-Organizing Map. [PDF]
ACS OmegaWang Y, Liu K, Liu T.
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Integrated geophysical, mineralogical, and geochemical investigation of gold and associated hydrothermal minerals in the Um Balad Area, Eastern Desert, Egypt. [PDF]
Sci RepH Mahmoud M +3 more
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Integrating multi-source remote sensing, field work, and petrography for automatic lithological mapping and mineralization potential in the Gabal El-Faraid, Egypt. [PDF]
Sci RepOsman H +5 more
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Variable redox states of sulfur in porphyry copper-fertile arc magmas. [PDF]
Sci AdvMeng X +5 more
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Petrogenesis and geodynamics of the Early Miocene Kashan granitoids in the central Urumieh-Dokhtar Magmatic Arc, Iran. [PDF]
Sci RepKou C, Zhang H, Zhu M.
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Characterization of newly identified N-S shear zones in the Egyptian Nubian Shield by integrating geophysical, remote sensing and field data. [PDF]
Sci RepAbd El-Wahed MA, Eldosouky AM.
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Laboratory spectral X-ray tomography for the differentiation of common rock-forming minerals. [PDF]
Sci RepKularatne K +4 more
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Zamzam, the World's Most Sacred Groundwater Well: Mecca, Saudi Arabia. [PDF]
Ground WaterWhincup P.
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