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Constraints of Fe Isotopic Compositions on the Origin of the Luobusa Podiform Chromite Deposit, Tibet [PDF]

open access: yesActa Geologica Sinica - English Edition, 2015
Benxun SU   +5 more
openaire   +1 more source

Origin of podiform chromites from Southwest Japan as a melt-mantle interaction.

open access: yesOrigin of podiform chromites from Southwest Japan as a melt-mantle interaction.
identifier:oai:t2r2.star.titech.ac.jp ...
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Origin of podiform chromite deposits by magma mingling

Earth and Planetary Science Letters, 1998
Abstract I have oversaturated the immiscible system SiO2 Al2O3 FeO K2O with FeCr2O4 to study the fractionation of chromite between conjugate siliceous and fayalitic melts. Although both melts are oversaturated with chromite, chromite only nucleates in the fayalite-rich melt where the crystal/melt interfacial energy (γSL) is lowest. In less than three
Chris Ballhaus
exaly   +2 more sources

Trace Elements in Chromite as Indicators of the Origin of the Giant Podiform Chromite Deposit at Kempirsai, Kazakhstan

Economic Geology, 2022
Abstract This study presents a complete trace element data set of chromite from the world’s largest podiform chromite deposit at Kempirsai, Kazakhstan, together with platinum group element (PGE) and Re-Os isotope compositions, to explore the potential of trace elements in the study of podiform chromite deposits.
Wen-Jun Hu   +2 more
exaly   +2 more sources

A hypothesis of origin for podiform chromite deposits

Geochimica Et Cosmochimica Acta, 1975
Podiform chromite deposits are lenticular, chromite-rich autoliths in deformed dun-ites and harzburgites of ophiolite complexes. The ophiolite association is assumed to be created along accreting plate boundaries in the oceanic lithosphere. It is suggested that podiform chromite deposits form as magmatic cumulates in elongate magma pockets along the ...
exaly   +2 more sources

Textural Evidence for the Chromite‐Oversaturated Character of the Melt Involved in Podiform Chromitite Formation

Resource Geology, 2013
AbstractWell‐preserved oval‐shaped dunite clots occur within the exceptionally fresh massive podiform chromitites from the Coto Block of the Zambales Ophiolite Complex, the Philippines. The dunite/chromitite boundary shows an interlocking texture; olivine inclusions in chromites in the podiform chromitites show the same optical extinction with larger ...
Betchaida D Payot, Shoji Arai
exaly   +2 more sources

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