Differential compaction of interbedded sandstone and coal

Tipo de material: materialTypeLabel

Artículo de libro Serie Geological Society Special Publications, n.169.Editor: London: Geological Society of London, 2000Descripción: pp. 51-60 ilus.Tema(s): ARENISCAS

Tipo de ítem	Ubicación actual	Signatura	Estado	Fecha de vencimiento	Código de barras
Artículo de libro	Biblioteca INGEMMET	551.243/C79\|3 (Navegar estantería)	Disponible		8415
Libro	Biblioteca INGEMMET	551.243/C79 (Navegar estantería)	Disponible		13394

Previo								Siguiente
Previo	551.243/C79\|14 Stratal fold patterns adjacent to normal faults: observations from the Gulf of Mexico	551.243/C79\|15 The interplay of faulting and folding during the evolution of the Zagros deformation belt	551.243/C79\|2 Complex metamorphic zonation of the Thaya Dome: result of buckling and gravitational collapse of an imbricated nappe sequence	551.243/C79\|3 Differential compaction of interbedded sandstone and coal	551.243/C79\|4 Displacement transfer and forced folding in the Maritimes Basin of Nova Scotia, Eastern Canada	551.243/C79\|5 Effects of interlayer slip in model forced folds	551.243/C79\|6 Extensional forced folding and decollement of the pre-rift series along the Rhine Graben and their influence on the geometry of the syn-rift sequences	Siguiente

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Previo								Siguiente
Previo	551.243/C79\|14 Stratal fold patterns adjacent to normal faults: observations from the Gulf of Mexico	551.243/C79\|15 The interplay of faulting and folding during the evolution of the Zagros deformation belt	551.243/C79\|2 Complex metamorphic zonation of the Thaya Dome: result of buckling and gravitational collapse of an imbricated nappe sequence	551.243/C79\|3 Differential compaction of interbedded sandstone and coal	551.243/C79\|4 Displacement transfer and forced folding in the Maritimes Basin of Nova Scotia, Eastern Canada	551.243/C79\|5 Effects of interlayer slip in model forced folds	551.243/C79\|6 Extensional forced folding and decollement of the pre-rift series along the Rhine Graben and their influence on the geometry of the syn-rift sequences	Siguiente

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