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- W2100077798 abstract "In southwestern Mexico, Late Cretaceous to Early Tertiary deformation has been generally associated with the Laramide orogeny of the Cordillera. Several alternative models consider the deformation to result from the accretion of the Guerrero terrane, formed by the Zihuatanejo, Arcelia, and Teloloapan intraoceanic island arcs, to the continental margin of the North American plate. Here, we present a detailed geologic and structural study and new 40Ar/39Ar and U-Pb ages for a broad region in the central-eastern part of the Guerrero terrane that allow the accretion model to be tested. In the Huetamo–Ciudad Altamirano part of the region,..." @default.
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- W2100077798 date "2009-01-01" @default.
- W2100077798 modified "2023-10-18" @default.
- W2100077798 title "Cretaceous–Eocene magmatism and Laramide deformation in southwestern Mexico: No role for terrane accretion" @default.
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- W2100077798 doi "https://doi.org/10.1130/2009.1204(07)" @default.
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