Provenance analysis of Jurassic sandstones from the Otlaltepec Basin, southern Mexico; implications for the reconstruction of Pangea breakup

The structural evolution that accompanied the breakup of Pangea during Jurassic time has been constrained in Mexico only at the regional scale on the basis of global plate tectonics and geometric considerations. According to available regional-scale reconstructions, the Jurassic tectonic evolution o...

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Veröffentlicht in:	Geosphere (Boulder, Colo.) Colo.), 2016-12, Vol.12 (6), p.1842-1864
Hauptverfasser:	Martini, Michelangelo, Ramírez-Calderón, Monica, Solari, Luigi, Villanueva-Amadoz, Uxue, Zepeda-Martínez, Mildred, Ortega-Gutierrez, Fernando, Elías-Herrera, Mariano
Format:	Artikel
Sprache:	eng
Schlagworte:	absolute age Basins Breakup clastic rocks depositional environment faults garnet group Geological faults Jurassic lithofacies lithostratigraphy Matanza Fault Mesozoic Mexico nesosilicates orthosilicates Otlaltepec Basin Otlaltepec Formation paleogeography Pangaea Pangea petrography Piedra Hueca Formation Plate tectonics provenance Radioactive age determination Reconstruction rifting sandstone Sandstones sedimentary basins sedimentary rocks silicates southern Mexico stratigraphic units Stratigraphy Structural geology supercontinents tectonics U/Pb zircon zircon group
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