Geologica Acta, 2015 The Mesoarchean chromitites in the Singhbhum craton provide the main source of chromium in India. We report here results of dating zircon grains that were found in the chromitite of ultramafic rocks belonging to the southern part of the Archean Baula ...
P. V. SUNDER-RAJU, E. HANSKI, Y. LAHAYE
doaj
Mineral inclusion and exsolution in mantle rocks from the Luobusa ophiolite, Tibet: origin implication [PDF]
, 2013 HKT-ISTP 2013 ...
Liang, F. H. +3 more
core
Mineralogical and geochemical features of chromitites of the Apshak area (South Kraka ultramafic massif, South Urals) [PDF]
МинералогияMineral composition of chromitites of the Apshak area in the northwestern part of the South Kraka massif (the largest representative of the Kraka group ophiolites), which is confined to the northern closure of the Zilair Synclinorium on the western slope
T.D. Shabutdinov +2 more
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Hydrothermal Pt mineralization in ophiolitic chromitites [PDF]
Goldschmidt2021 abstracts, 2021 Júlia Farré de Pablo +6 more
openaire +1 more source
MINERALOGICAL-GEOCHEMICAL AND STRUCTURAL FEATURES OF ULTRAMAFIC ROCKS AND CHROMITITES OF THE MALY BASHART CHROMITE-BEARING ZONE OF THE SOUTH KRAKA MASSIF (SOUTH URALS) [PDF]
Минералогия, 2017 Results of structural-petrological and mineralogical-geochemical studies of chromitite-bearing zone within spinel peridotites of the South Kraka ophiolite massif are presented.
D.E. Saveliev +2 more
doaj
Chromian spinel geochemistry as a petrogenetic indicator in the chromitites and peridotites of the Bajgan Complex, Western Makran [PDF]
پترولوژیIntroductionEconomic chromite deposits are very common in ophiolite belts. These deposits usually occur in the uppermost horizons of the ophiolite mantle sequence or within the ultramafic cumulitic rocks at the base of the crustal sequence (González ...
Leila Vahedi +2 more
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Exploration for magmatic Ni-Cu-PGE sulphide deposits : a review of recent advances in the use of geochemical tools, and their application to some South African ores [PDF]
, 1998 Most major magmatic Cu-Ni-PGE sulphide deposits are thought to have formed by segregation of an immiscible sulphide melt from a silicate host magma, in response to processes such as magma mixing, rapid cooling, differentiation, and contamination.
Barnes, Sarah-Jane +2 more
core +1 more source
Provenance of Lower Cretaceous sediments in the Nariwa and Hokubo areas, Okayama Prefecture, deduced from detrital modes and geochemistry of sandstones [PDF]
, 1996 Petrographic and geochemical study of sandstones from the Kenseki Formation have shown that the sandstones are compositionally immature. The immaturity is reflected geochemically by their low SiO2 contents (52-66 wt%) and petrographically by low modal ...
Daniel K., Asiedu +2 more
core +1 more source
Discovery of a meteoritic ejecta layer containing unmelted impactor fragments at the base of Paleocene lavas, Isle of Skye, Scotland [PDF]
, 2017 Evidence for meteorite impacts in the geological record may include the presence of shocked minerals, spherule layers, and geochemical anomalies. However, it is highly unusual to nd unmelted crystals from the actual impactor within an ejecta layer ...
Baca, J. +8 more
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Chromite chemistry of a massive chromitite seam in the northern limb of the Bushveld Igneous Complex, South Africa: correlation with the UG-2 in the eastern and western limbs and evidence of variable assimilation of footwall rocks. [PDF]
Miner Depos, 2021 Langa MM +5 more
europepmc +1 more source