Geodynamic implications of ophiolitic chromitites in the La Cabaña ultramafic bodies, Central Chile

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Timing the tectonic mingling of ultramafic rocks and metasediments in the southern section of the coastal accretionary complex of central Chile

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Geodynamic implications of ophiolitic chromitites in the La Cabaña ultramafic bodies, Central Chile

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наукова стаття, опублікована в серпні 2014

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Geodynamic implications of oph ...... tramafic bodies, Central Chile

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Geodynamic implications of oph ...... tramafic bodies, Central Chile

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Geodynamic implications of oph ...... tramafic bodies, Central Chile

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Geodynamic implications of oph ...... tramafic bodies, Central Chile

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Geodynamic implications of oph ...... tramafic bodies, Central Chile

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Geodynamic implications of oph ...... tramafic bodies, Central Chile

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Geodynamic implications of oph ...... tramafic bodies, Central Chile

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P2093

Fernando Gervilla

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José María González-Jiménez

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Ultradeep continental roots and their oceanic remnants: A solution to the geochemical “mantle reservoir” problem?

Anatomy and global context of the Andes: Main geologic features and the Andean orogenic cycle

High-Cr and high-Al chromitites from the Sagua de Tánamo district, Mayarí-Cristal ophiolitic massif (eastern Cuba): Constraints on their origin from mineralogy and geochemistry of chromian spinel and platinum-group elements

Distribution of platinum-group elements and Os isotopes in chromite ores from Mayarí-Baracoa Ophiolitic Belt (eastern Cuba)

Al- and Cr-rich chromitites from the Mayari-Baracoa ophiolitic belt (eastern Cuba); consequence of interaction between volatile-rich melts and peridotites in suprasubduction mantle

Transfer of Os isotopic signatures from peridotite to chromitite in the subcontinental mantle: Insights from in situ analysis of platinum-group and base-metal minerals (Ojén peridotite massif, southern Spain)

In situ Re–Os isotopic analysis of platinum-group minerals from the Mayarí-Cristal ophiolitic massif (Mayarí-Baracoa Ophiolitic Belt, eastern Cuba): implications for the origin of Os-isotope heterogeneities in podiform chromitites

Os isotope heterogeneity of the upper mantle: Evidence from the Mayarí–Baracoa ophiolite belt in eastern Cuba

Petrogenesis of highly depleted peridotites and gabbroic rocks from the Mayarí-Baracoa Ophiolitic Belt (eastern Cuba)

Chromite composition and platinum-group mineral assemblage in the Uktus Uralian-Alaskan-type complex (Central Urals, Russia)

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1466-1483

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scholarly article

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10.1080/00206814.2014.947334

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P478

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Fernando Barra

Martin Reich

Richard J. Walker

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2014-08-08T00:00:00Z

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Geodynamic implications of ophiolitic chromitites in the La Cabaña ultramafic bodies, Central Chile

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Geodynamic implications of ophiolitic chromitites in the La Cabaña ultramafic bodies, Central Chile

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