Deformation understanding in the Upper Paleozoic of Ventana Ranges
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Descrição
1) Geographic location of Sierra de la Ventana Foldbelt in the
Early Palaeozoic near-surface deformation in the Neptune Range
Deformation understanding in the Upper Paleozoic of Ventana Ranges
Frontiers Following the steps of CHIPA: Chilenia and Patagonia
Position of the El Centinela I and El Centinela II paleomagnetic
Major tectonic domains in SE Buenos Aires. The box in the upper
Late Paleozoic Gondwanide deformation in the Central Andes
Frontiers Following the steps of CHIPA: Chilenia and Patagonia
Magma transport in sheet intrusions of the Alnö carbonatite
Sedimentological constraints on the initial uplift of the West
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