Results 81 to 90 of about 355 (139)

Hydrothermal origin of platinum-group minerals during serpentinization of the podiform chromitites from the Kizildag ophiolite in southern Turkiye

open access: yes
Platinum-group minerals (PGMs) in podiform chromitites usually occur in the interior and/or edge of chromite. However, the origin of PGMs in podiform chromitites has long been a matter of debate. Here we examined sub-micro to nanoscale textural features,
Chen, Chen   +3 more
core   +1 more source

ASTER and Landsat TM remote sensing data application for chromite prospecting: case study from south Iran

open access: yes, 2015
Chromite deposits in Iran are located in the ophiolite complexes, which have mostly podiform types and irregular in their settings . Exploration for podiform chromite deposits associated with ophiolite complexes has been a challenge for the prospectors ...
Hashim, Mazlan, Pour, Amin Beiranvand
core  

Occurrence and Emplacement of Chromite Ores in Sindhudurg District Maharashtra, India

open access: yes, 2010
We present the occurrence and emplacement of chromite ore deposits of two abandoned mines (Kankavali/Janoli and Wagda) in the sindhudurg district of Maharashtra, India.
Loveson, V.J.
core  

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

Metamorphism on Chromite Ores from the Dobromirtsi ultramafic massif, Rhodope Mountains (SE Bulgaria)

open access: yes
Podiform chromitite bodies occur in highly serpentinized peridotites at Dobromirtsi Ultramafic Massif (Rhodope Mountains, southeastern Bulgaria). The ultramafic body is believed to represent a fragment of Palaeozoic ophiolite mantle.
González-Jiménez, J. M.   +3 more
core  

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 ...
openaire  

Podiform chromitite-bearing ultramafic rocks from the Braganca Massif, northern Portugal: fragments of island arc mantle.

open access: yes
The Upper Allochthonous Thrust Complex (UATC) of the Braganca massif in northern Portugal contains a set of ultrabasic rocks interthrust with granulites.
Meireles, C. A.   +2 more
core  

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