Very high CO2 contents (≥3 wt%) in olivine-hosted magmatic inclusions from the Bas-Vivarais volcanic province (Ardèche, France): Implications for magma genesis in a continental intraplate region | Zendy

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Very high CO2 contents (≥3 wt%) in olivine-hosted magmatic inclusions from the Bas-Vivarais volcanic province (Ardèche, France): Implications for magma genesis in a continental intraplate region

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