Results 231 to 240 of about 41,907 (309)
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Rhodium, gold and other highly siderophile elements in orogenic peridotites and peridotite xenoliths
Chemical Geology, 2011Abstract The concentrations of Rh, Au and other highly siderophile elements (HSE: Re, Os, Ir, Ru, Pt, Rh, Pd and Au), and 187Os/188Os isotope ratios have been determined for samples from peridotite massifs and xenoliths in order to further constrain HSE abundances in the Earth's mantle and to place constraints on the distributions processes ...
Mario Fischer-Gödde, Frank Wombacher
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Arc-like magmas generated by mélange-peridotite interaction in the mantle wedge
The mechanisms of transfer of crustal material from the subducting slab to the overlying mantle wedge are still debated. Mélange rocks, formed by mixing of sediments, oceanic crust, and ultramafics along the slab-mantle interface, are predicted to ascend
Veronique Le Roux, Horst Marschall
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Global variations in abyssal peridotite compositions
Jessica M Warren
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Experimental constraints on the damp peridotite solidus and oceanic mantle potential temperature
Emily Sarafian +2 more
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The roles of pyroxenite and peridotite in the mantle sources of oceanic basalts
Nature Geoscience, 2017Bernard J Wood
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Partial Melting Experiments of Peridotite + CO2 at 3 GPa and Genesis of Alkalic Ocean Island Basalts
Rajdeep Dasgupta, marc Hirschmann
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An updated catalogue of New Zealand’s mantle peridotite and serpentinite
, 2020New Zealand has a remarkably large number of exhumed mantle occurrences for a small exposed landmass. Since the last regional syntheses of peridotite (1987) and serpentinite (1966) , new locations have been discovered and abundant geochemical and ...
J. Scott
semanticscholar +1 more source
American Mineralogist, 2018
Peridotites dredged from mid-ocean ridges and glassy mid-ocean ridge basalts (MORB) transmit information about the oxygen fugacity fo2) of Earth’s convecting upper mantle to the surface.
F. Davis, E. Cottrell
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Peridotites dredged from mid-ocean ridges and glassy mid-ocean ridge basalts (MORB) transmit information about the oxygen fugacity fo2) of Earth’s convecting upper mantle to the surface.
F. Davis, E. Cottrell
semanticscholar +1 more source
Melting of Peridotite to 140 Gigapascals
Science, 2010Under Pressure In order to understand the behavior of materials in the solid deep Earth, it is important to be able to estimate how a material melts at high pressure. To this end, Fiquet et al. (p.
Fiquet, G. +6 more
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