Statistics for Clinopyroxene compositions of the isotropic gabbros from the Sarıkaman Ophiolite: New evidence on supra-subduction zone type magma genesis in Central Anatolia
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| Clinopyroxene compositions of the isotropic gabbros from the Sarıkaman Ophiolite: New evidence on supra-subduction zone type magma genesis in Central Anatolia | 0 |
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| October 2024 | 0 |
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