Further evidence of widespread permian remagnetization in the North Patagonian massif, Argentina

A paleomagnetic study on accurately dated (472-476. Ma) Early Ordovician undeformed granitoids exposed in the northeastern margin of the North Patagonian massif (41.5°S, 65.0°W) was carried out, with the main goal of comparing the Early Ordovician paleogeographic position of Patagonia relative to Go...

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Autores principales: Tomezzoli, R.N., Rapalini, A.E., de Luchi, M.G.L., Martínez Dopico, C.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_1342937X_v24_n1_p192_Tomezzoli
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