Lithotectonic setting, paleoweathering, maturity, sediment recycling and paleoredox conditions of quaternary alluvium from Mayo Sina (Tchad). A geochemical approach. [PDF]
Adama A +4 more
europepmc +1 more source
Water and moganite participation in agates from Bou Hamza (Morocco). [PDF]
Powolny T +3 more
europepmc +1 more source
Geological Hydrogen Prospectivity of Iron Ore Deposits in India Based on Semiquantitative Analysis. [PDF]
Kiran R +6 more
europepmc +1 more source
Cooling rates and melt extraction timescales determined by diffusion chronometry on shallow crustal plutonic rocks. [PDF]
Grocolas T +5 more
europepmc +1 more source
A Bronze Age lip-paint from southeastern Iran. [PDF]
Eskandari N +6 more
europepmc +1 more source
Gamma activity concentrations of <sup>226</sup>Ra, <sup>232</sup>Th, <sup>40</sup>K, and health hazard assessments of granites from Wadi El-Nabi' mining area, Egyptian Nubian Shield. [PDF]
Shereif AS +5 more
europepmc +1 more source
Petrological diversity of continental arc magmatism evidenced by Triassic magmatic complexes in East Kunlun Orogen. [PDF]
Gan J +6 more
europepmc +1 more source
Mercury isotope evidence for the importance of recycled fluids in collisional ore systems. [PDF]
Xu B +7 more
europepmc +1 more source
The paper provides information on the chemical composition of intrusive diorites the gold-porphyry deposit of Bolshoy Karan, located in the northern part of the Voznesensk-Prisakmar structural zone (MUF), in the north of the Uchaly ore district. Additional information is given on 1) primary magmatic, 2) accessory, 3) hydrothermal-metasomatic and ...
Alexandr Michailovich Kosarev +2 more
openaire +2 more sources
The Diorites and Associated Rocks of the Glen Tilt Complex, Perthshire. II. Diorites and Appinites
AbstractThe south-eastern margin of the Glen Tilt mass consists of a series of diorites showing a considerable variation in mineralogical and chemical composition. Associated with, and enclosed within, the diorites are a number of small masses of coarser hornblende-felspar rocks which are described as appinites.
W. A. Deer
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