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Supplemental material: The Pinal Schist of southern Arizona: A Paleoproterozoic forearc complex with evidence of spreading ridge–trench interaction at ca. 1.65 Ga and a Proterozoic arc obduction event
journal contribution
posted on 2014-01-01, 00:00 authored by A. MeijerGSA Data Repository Item 2014173, GSA Bulletin. File size: about 602 KB.
