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Origin of arc-like continental basalts: Implications for deep-Earth fluid cycling and tectonic discrimination
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Arc-like continental basalts have 4.0–5.0 wt% magma H2O concentration.

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Primary melts of CFBs have 1.0–2.0 wt% H2O concentration.

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Arc-like geochemical signatures related to deep-Earth water cycling.

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Arc-like continental basalts can be distinguished from arc basalts using the proposed factors.

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