Geo‐fO2: Integrated Software for Analysis of Magmatic Oxygen Fugacity

W Li, Y Cheng, Z Yang - Geochemistry, Geophysics …, 2019 - Wiley Online Library
Oxygen fugacity (fO2) is a fundamental thermodynamic property governing redox potential in
solid Earth systems. Analysis of magmatic fO2 aids our understanding of the valence state …

SHRIMP zircon dating and Sm/Nd isotopic investigations of Neoproterozoic granitoids, Eastern Desert, Egypt

EMM Moussa, RJ Stern, WI Manton, KA Ali - Precambrian Research, 2008 - Elsevier
There is an increasing evidence for the involvement of pre-Neoproterozoic zircons in the
Arabian–Nubian Shield, a Neoproterozoic crustal tract that is generally regarded to be …

Geochemical, mineralogy, and Sr–Nd–Pb isotopic compositions of the gold-related lamprophyre in the Bengbu–Wuhe Area, southeastern North China Craton …

C Li, J Yan - Ore Geology Reviews, 2021 - Elsevier
Besides granite porphyries, many mafic dikes also have a close temporal and spatial
relationship with orebodies in the BWGB. However, compared with the granite porphyries …

[HTML][HTML] Silicates chemistry as indicators of physicochemical and geothermometry conditions on porphyry ore system: A case study of the Haftcheshmeh Cu–Mo …

N Zaheri–Abdehvand, S Hassanpour, I Rassa… - Ore Geology …, 2022 - Elsevier
Abstract The Haftcheshmeh porphyry Cu–Mo deposit is located in the northwestern part of
the Arasbaran Metallogenic Zone (AMZ), NW Iran. The Cu–Mo mineralization in this deposit …

Remote sensing techniques and geochemical constraints on the formation of the Wadi El-Hima mineralized granites, Egypt: new insights into the genesis and …

MZ Khedr, SM Abo Khashaba, NH El-Shibiny… - International Journal of …, 2022 - Springer
Abstract The Wadi El-Hima Neoproterozoic I-and A-type granites in the Southern Eastern
Desert of Egypt are rich in garnets (up to 30 vol%) and are cut by NW–SE strike-slip faults …

Origin of I-and A-type granitoids from the Eastern Desert of Egypt: implications for crustal growth in the northern Arabian–Nubian Shield

ES Farahat, HA Mohamed, AF Ahmed… - Journal of African Earth …, 2007 - Elsevier
I-and A-type granitoid rocks, emplaced during pre-and post-collision stages, respectively, of
the Neoproterozoic Pan-African Orogeny, are widely distributed in the Eastern Desert of …

A downgoing Indian lithosphere control on along-strike variability of porphyry mineralization in the Gangdese belt of southern Tibet

X Sun, Y Lu, Q Li, R Li - Economic Geology, 2021 - pubs.geoscienceworld.org
The E-trending Gangdese porphyry copper belt in southern Tibet is a classic example of
porphyry mineralization in a continental collision zone. New zircon U-Pb geochronological …

Structural and tectonic framework of Neoproterozoic basement of Egypt: from gneiss domes to transpression belts

AR Fowler, Z Hamimi - The geology of Egypt, 2020 - Springer
The Neoproterozoic tectonic evolution of the Egyptian Eastern Desert (EED) basement is
documented, principally through its history of structural events, and to a lesser degree …

Formation of magmatic titanite and titanite–ilmenite phase relations during granite alteration in the Tribeč Mountains, Western Carpathians, Slovakia

I Broska, D Harlov, P Tropper, P Siman - Lithos, 2007 - Elsevier
In this study, formation of titanite, in Carboniferous I-type granites/granitoids from the Tribeč
Mountains (Slovakia), and its subsequent alteration products are described. Titanite occurs …

Lu–Hf and O isotopic compositions on single zircons from the North Eastern Desert of Egypt, Arabian–Nubian Shield: Implications for crustal evolution

KA Ali, BA Zoheir, RJ Stern, A Andresen… - Gondwana …, 2016 - Elsevier
Neoproterozoic juvenile crust is exposed in the Eastern Desert of Egypt, between the Nile
and the Red Sea, forming the basement to Cambrian and younger sedimentary strata in the …