Fluid processes in deep crustal fault zones

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Artículo de libro Serie Dahlem Workshop Reports, .Editor: Cambridge, MA: MIT Press, 2007Descripción: pp. 295-318 ilus.Tema(s): CORTEZA

Tipo de ítem	Ubicación actual	Signatura	Estado	Fecha de vencimiento	Código de barras
Artículo de libro	Biblioteca INGEMMET	551.243.1/H21\|4 (Navegar estantería)	Disponible		13234
Libro	Biblioteca INGEMMET	551.243.1/H21 (Navegar estantería)	Disponible		34414

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Previo	551.243.1/H21\|1 Seismic fault rheology and earthquake dynamics	551.243.1/H21\|2 Topography, denudation, and deformation: the role of surface processes in fault evolution	551.243.1/H21\|3 Constraining the denudational response to faulting	551.243.1/H21\|4 Fluid processes in deep crustal fault zones	551.243.1/H21\|5 Deformation in the presence of fluids and mineral reactions	551.243.1/H21\|6 Effects of melting on faulting and continental deformation	551.243.4/M331\|1 Kinematics of a hybrid thick-thin-skinned fold and thrust belt recorded in Neogene syntectonic wedge-top basins, southern Central Andes between 35° and 36°S, Malargüe, Argentina	Siguiente

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Previo								Siguiente
Previo	551.243.1/H21\|1 Seismic fault rheology and earthquake dynamics	551.243.1/H21\|2 Topography, denudation, and deformation: the role of surface processes in fault evolution	551.243.1/H21\|3 Constraining the denudational response to faulting	551.243.1/H21\|4 Fluid processes in deep crustal fault zones	551.243.1/H21\|5 Deformation in the presence of fluids and mineral reactions	551.243.1/H21\|6 Effects of melting on faulting and continental deformation	551.243.4/M331\|1 Kinematics of a hybrid thick-thin-skinned fold and thrust belt recorded in Neogene syntectonic wedge-top basins, southern Central Andes between 35° and 36°S, Malargüe, Argentina	Siguiente

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