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• W2078418919 abstract "ABSTRACTA histogram of 778 isotopic ages of magmatic rocks younger than Eocene in centralMexico shows a multimodal distribution with peaks at about 30 Ma, 23 Ma, 10 Ma, and 5 Ma.The sample suite displays systematic spatial variations with age that likely reflect the pro-tracted transition from the north-northwest–trending arc of the Sierra Madre Occidental tothe east-west–trending Mexican Volcanic Belt. The reorientation of the arc is accompanied bya change in the dominant composition of the products from silicic ignimbrites and rhyolites toandesitic and basaltic lavas. The observed transition is related to the Miocene reorganization ofthe subduction system following the cessation of subduction off Baja California and the east-ward motion of the Caribbean–Farallon–North America triple junction along the southeast-ern margin of Mexico. Our data support an early–middle Miocene age for the initiation of sub-horizontal subduction in southern Mexico and confirm that the locus of arc volcanism wasprimarily controlled by the geometry of plate boundaries and the thermal structure of the sub-ducting slab." @default.
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• W2078418919 date "1999-01-01" @default.
• W2078418919 modified "2023-10-18" @default.
• W2078418919 title "Space-time patterns of Cenozoic arc volcanism in central Mexico: From the Sierra Madre Occidental to the Mexican Volcanic Belt" @default.
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• W2078418919 doi "https://doi.org/10.1130/0091-7613(1999)027<0303:stpoca>2.3.co;2" @default.
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