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• W2055602502 abstract "The Xayacatlán area (eastern Mixteca terrane, southern Mexico) was previously inferred to preserve the Ordovician‐Silurian thrust contact between vestiges of the Iapetus Ocean and the para‐autochthon bordering Oaxaquia. Detailed remapping indicates that the rocks occur in four vertically‐bounded, NS fault blocks. The latter record the following tectonothermal events that post‐date Iapetus and occurred along the margins of the Rheic (1) and Pacific (2 and 3) oceans: (1) dextral transtension accompanying intrusion of an NS, tholeiitic dike swarm at ∼442 Ma; (2) penetrative, greenschist‐facies deformation during the Mississippian related to extrusion of high‐pressure rocks; and (3) subgreenschist‐facies dextral transtension on NS faults during the generation of Middle Permian fabrics." @default.
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• W2055602502 date "2009-03-02" @default.
• W2055602502 modified "2023-10-17" @default.
• W2055602502 title "Palaeozoic structures in the Xayacatlán area, Acatlán Complex, southern Mexico: transtensional rift‐ and subduction‐related deformation along the margin of Oaxaquia" @default.
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• W2055602502 doi "https://doi.org/10.1080/00206810802688659" @default.
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