Hydrous mafic–ultramafic intrusives at the roots of a proto-arc: implications for crust building and...
Hydrous mafic–ultramafic intrusives at the roots of a proto-arc: implications for crust building and mantle source heterogeneity in young forearc regions
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Berlin/Heidelberg: Springer Berlin Heidelberg
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English
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Berlin/Heidelberg: Springer Berlin Heidelberg
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The New Caledonia ophiolite represents a rare example of proto-arc section originated during subduction infancy. The sequence is dominated by refractory harzburgites overlain by ultramafic (dunites and wehrlites) and mafic (gabbronorites) lithologies.
In this contribution, we report the first occurrence of amphibole-bearing intrusives in the New...
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Full title
Hydrous mafic–ultramafic intrusives at the roots of a proto-arc: implications for crust building and mantle source heterogeneity in young forearc regions
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Record Identifier
TN_cdi_hal_primary_oai_HAL_hal_04362989v1
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_04362989v1
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ISSN
0010-7999
E-ISSN
1432-0967
DOI
10.1007/s00410-022-01912-x
