Elongated domes in extended orogens: A mode of mountain uplift in the Betics (southeast Spain)

Special Paper of the Geological Society of America

Volumn 380, Issue , 2004, Pages 243-265

  Martinez Martinez J M ^a   Soto, J I ^a   Balanya J C ^b  

^a CSIC   (Spain)

^b UNIVERSIDAD PABLO DE OLAVIDE   (Spain)

Author keywords

Betics; Crustal flow; Crustal rheology; Folding of extensional detachments; Mountain uplift; Sierra Nevada elongated dome

Indexed keywords

EROSION; FAULT SLIPS; HORIZONTAL WELLS; LANDFORMS; STRIKE-SLIP FAULTS; STRUCTURAL GEOLOGY; TOPOGRAPHY;

BETICS; CRUSTAL FLOW; CRUSTAL RHEOLOGY; FOLDING OF EXTENSIONAL DETACHMENTS; MOUNTAIN UPLIFT; SIERRA NEVADA;

DOMES;

CRUSTAL STRUCTURE; CRUSTAL THICKNESS; DOME; EXHUMATION; FOLDING; FOOTWALL; UPLIFT;

ANDALUCIA; BETIC CORDILLERA; SIERRA NEVADA [BETIC CORDILLERA]; SPAIN;

EID: 84870816642     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/0-8137-2380-9.243     Document Type: Article

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