Cretaceous magmatic evolution in the Deylaman igneous complex, Alborz zone, Iran: change from extensional to compressional regime
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DOI: 10.7306/gq.1500
Abstract: The Deylaman igneous complex, as a part of the Late Cretaceous rock unit that lies behind the Paleogene Alborz magmatic arc, in the northern Alborz zone, is composed of basaltic sheet lavas alternating with the… read more here.
Keywords: zone; deylaman igneous; igneous complex; lavas ... See more keywords