ABSTRACT The Paleoproterozoic Talvivaara mudstone is a very large sulfidic Ni‐Co deposit that records enhanced organic matter accumulation during the global Shunga Event. Here, rock geochemistry and microscale S and Fe isotope composition of in situ pyrrhotites and pyrites are studied in well‐characterised, well‐preserved drill core samples.
Raimo Lahtinen +3 more
wiley +1 more source
Abstract Low‐velocity layers (LVLs) above the 410‐km discontinuity are commonly attributed to partial melt generated by dehydration melting when hydrous mantle transition‐zone material rises into the upper mantle, where water solubility in nominally anhydrous minerals decreases.
Takashi Yoshino, Longjian Xie
wiley +1 more source
Petrography and physical-mechanical evaluation of mafic-ultramafic rocks from Atud-Um Khasila, Egypt for dimension stone. [PDF]
Abdel-Rahman AM +4 more
europepmc +1 more source
Membrane-free electrochemical production of acid and base solutions capable of processing ultramafic rocks. [PDF]
Charnay BP +8 more
europepmc +1 more source
Characterization of talc deposits in ultramafic rocks of Gebel El Maiyit and its economic feasibility. [PDF]
Salem IA, Aly SM, Shebl A, Thabet IA.
europepmc +1 more source
An integrated experimental-modeling approach to identify key processes for carbon mineralization in fractured mafic and ultramafic rocks. [PDF]
Neil CW +8 more
europepmc +1 more source
Controls on natural hydrogen generation during serpentinization of mantle rocks. [PDF]
Christiansen R +8 more
europepmc +1 more source
Finding natural [Formula: see text] generation zones in Midcontinent Rift in the U.S. by identifying the geophysical signatures of a serpentinization system. [PDF]
Zhang M, Li Y.
europepmc +1 more source
Advanced multi-technique aeromagnetic and remote sensing characterization of a small-scale gold prospect: a case study from the Um Salim area. [PDF]
Nagy M +3 more
europepmc +1 more source

