Results 81 to 90 of about 43,392 (192)
Distribution of iron between coexisting olivines and calcium-poor pyroxenes in peridotites, gabbros, and other magnesian environments [PDF]
M. J. O’Hara
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Olivine dissolution rates: A critical review
E. Oelkers+4 more
semanticscholar +1 more source
Redox-influenced seismic properties of upper-mantle olivine
C. Cline+4 more
semanticscholar +1 more source
ABSTRACT Rationale Matrix effects by secondary ion mass spectrometry (SIMS) are empirically corrected by calibration using matrix‐matched reference materials. However, conventional parametric regression cannot estimate the prediction uncertainty to account for the difference in compositions of new data and reference materials. Applying Gaussian process
Keita Itano+5 more
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Corrections [to “The iron, magnesium, and calcium distribution in coexisting olivines and rhombic pyroxenes of chondrites” by Klaus Keil and Kurt Fredriksson] [PDF]
Klaus Keil, K. Fredriksson
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ABSTRACT Fluid–rock interactions play a key role in the formation, evolution and recycling of the Earth's crust. For fluids to infiltrate rocks and enable and sustain fluid‐mediated mineral transformations, fluid pathways are required. In this study, we examined the potential mechanisms of formation of such pathways via detailed mineralogical ...
Saskia Grund+4 more
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Abstract At the subduction zone interface, a combination of mechanical deformation and (fluid‐mediated) chemical mixing of oceanic crust, sediment and mantle lithologies yields heterogeneous mélange lithologies. These mélanges have compositions and metamorphic mineral assemblages dissimilar to their endmember source lithologies, resulting in a ...
Benjamin Z. Klein, Mark D. Behn
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Unit cell dimensions of some synthetic olivine group solid solutions
Yoshito Matsui, Yasuhiko Syono
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Vibrational studies of olivine-type compounds—I. The i.r. and Raman spectra of the isotopic species of Mg2SiO4 [PDF]
M.Th. Pâques-Ledent, P. Tarte
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Abstract Triassic calc‐alkaline volcanics that are mainly exposed in the Hellenides—Dinarides orogen, as well as eastwards in the Afyan Zone, are considered to constrain the petrogenetic mechanisms that led to their formation, and to unravel the geodynamic processes that occurred in the western Tethys, related to the NW Gondwana (Apulia) promontory and
Petros Koutsovitis+10 more
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