The doubly vergent inverted structures in the Mesozoic basins of northern Chile (28°S): A comparative analysis from field data and analogue modeling

Doubly vergent contractional structures are common features in many regions of the Central Andes. They represent the first-order structural style observed in the inverted Mesozoic basins located along the flat-slab subduction segment of northern Chile. Here, we present a comparative analyses based o...

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Autores principales: Martínez, F., Cristallini, E.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08959811_v77_n_p327_Martinez
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