Using platinum-group elements and Au geochemistry to constrain the genesis of podiform chromitites and associated peridotites from the Soghan mafic–ultramafic complex, Kerman, Southeastern Iran

Najafzadeh, Alireza; Ahmadipour, Hamid

doi:10.1016/j.oregeorev.2013.12.014

Cited by 21 publications

(6 citation statements)

References 95 publications

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“…The Sanandaj-Sirjan Zone, which occupied an upper plate position during subduction from the middle Jurassic onwards (e.g. Omrani et al, 2008;Agard et al, 2011;Najafzadeh and Ahmadipour, 2014), shows no indication of HP-LT subduction-related imprint during the Zagros subduction event.…”

Section: Geological Contextmentioning

confidence: 99%

Zagros blueschists: Episodic underplating and long-lived cooling of a subduction zone

Agard¹,

Glodny

Omrani

et al. 2016

Earth and Planetary Science Letters

107

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Section: Geological Contextmentioning

confidence: 99%

Zagros blueschists: Episodic underplating and long-lived cooling of a subduction zone

Agard¹,

Glodny

Omrani

et al. 2016

Earth and Planetary Science Letters

107

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“…The Pd/Ir values, an indicator of PGE fractionation, are relatively constant in all chromitites and vary from 0.04 to 0.25 (Table 1). These patterns and the low PGE abundances are typical of ophiolitic chromitites elsewhere (Figure 4b) and indicating a high degree of partial melting of the mantle source very similar to nearby mafic-ultramafic complexes of Soghan and Abdasht [6,7]. The binary plots of TiO 2 wt.% vs. Cr# show that the massive and most disseminated chromian spinels fall in the boninitic field (Figure 5a).…”

Section: Resultsmentioning

confidence: 85%

Distribution of Platinum-Group Elements in Chromite Ores of the Sorkhband Ultramafic Complex, Kerman, Southeastern Iran

Najafzadeh

Arvin

Ahmadipour

et al. 2016

IOP Conf. Ser.: Earth Environ. Sci.

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Abstract. The Ordovician Sorkhband ultramafic complex lies in southern Kerman Province of Iran. The wedge shape complex covers an area of more than 100 km 2 and is divided into: lower part comprises of dunites, largest podiform chromitite deposits in Iran (Faryab mine), olivine clinopyroxenite dykes and massive's, wehrlite and olivine websterite dykes; and upper part comprises of clinopyroxene bearing harzburgites, with subordinate lenses and dykes of dunite, massive and dyke like olivine clinopyroxenite and minor orthopyroxenite dykes with no significant chromitite mineralization. Chromitite orebodies exhibit variable sizes and shapes, forming pods, lenses, bands, vein-like bodies and rich dissemination. Podiform chromitites in dunite form tabular to lenticular bodies although may occur also as pencil-like masses. The chromitites occur in four distinct textural modes. Massive, disseminated, banded and nodular chromitites are the most common textural types and commonly grade into one other. Massive chromitites have sharp contacts with the enclosing dunite whereas disseminated bodies grade outward into dunite and occasionally pass into interbanded chromitite and dunite. A detailed electron microprobe study reveals very high Cr#, Mg# and very low TiO2 contents for chromian spinels in chromitites. The Sorkhband chromitites contain up to 440 ppb total PGE, and display a systematic enrichment in IPGE relative to PPGE, with a steep negative slope in the PGE spidergrams and very low PPGE/IPGE ratios, a feature typical of ophiolitic podiform chromitites worldwide. The mineral chemistry data and PGE geochemistry of the chromitites indicates that the Sorkhband ultramafic complex was generated from an arc-related magma with boninitic affinity in a supra-subduction zone setting.

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“…Hickey and Frey, 1982). Similar melts of boninitic affinity have been suggested to be responsible for the formation of high-Cr chromitites from many localities such as Kempirsai in Kazakhstan (Melcher et al, 1997), Muğla in Turkey (Uysal et al, 2009a), Elekdag ophiolite in Turkey (Dönmez et al, 2014), Nidar ophiolite chromitites (Ravikant et al, 2004), Mayari-Cristal ophiolitic massif in eastern Cuba (González-Jiménez et al, 2011) and Sorkhband, Soghan and Dehsheikh ultramafic complex in Iran (Najafzadeh et al, 2008;Najafzadeh and Ahmadipour, 2014a;Peighambari et al, 2015) (Table 6). Parental melts to…”

Section: Accepted Manuscriptmentioning

confidence: 70%

Geochemistry of platinum-group elements and mineral composition in chromitites and associated rocks from the Abdasht ultramafic complex, Kerman, Southeastern Iran

Najafzadeh

Ahmadipour

2016

Ore Geology Reviews

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Using platinum-group elements and Au geochemistry to constrain the genesis of podiform chromitites and associated peridotites from the Soghan mafic–ultramafic complex, Kerman, Southeastern Iran

Cited by 21 publications

References 95 publications

Zagros blueschists: Episodic underplating and long-lived cooling of a subduction zone

Zagros blueschists: Episodic underplating and long-lived cooling of a subduction zone

Distribution of Platinum-Group Elements in Chromite Ores of the Sorkhband Ultramafic Complex, Kerman, Southeastern Iran

Geochemistry of platinum-group elements and mineral composition in chromitites and associated rocks from the Abdasht ultramafic complex, Kerman, Southeastern Iran

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