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Crustal magmatic system beneath the east pacific rise (8 degrees 20 to 10 degrees 10N): Implications for tectonomagmatic segmentation and crustal melt transport at fast-spreading ridges3

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Crustal magmatic system beneath the east pacific rise (8 degrees 20 to 10 degrees 10N): Implications for tectonomagmatic segmentation and crustal melt transport at fast-spreading ridges0000003

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