Slow and fast deformation in the Dora Maira Massif, Italian Alps: Pseudotachylytes and inferences on exhumation history

Journal of Structural Geology

Volumn 29, Issue 7, 2007, Pages 1114-1130

  Zechmeister, M S ^a   Ferre E C ^b   Cosca, M A ^c   Geissman, J W ^d  

^a UNIVERSITY OF OKLAHOMA   (United States)

^b SOUTHERN ILLINOIS UNIVERSITY   (United States)

^c UNIVERSITY OF LAUSANNE   (Switzerland)

^d UNIVERSITY OF NEW MEXICO   (United States)

Author keywords

Brittle deformation; Exhumation; Pseudotachylyte; UHP

Indexed keywords

EXHUMATION; FRICTIONAL SLIDING INSTABILITY; SEISMIC SLIP; ULTRA-HIGH PRESSURE METAMORPHIC TERRAIN;

BRITTLENESS; DEFORMATION; LANDFORMS; METAMORPHIC ROCKS; SEISMIC RESPONSE; STRAIN RATE;

STRUCTURAL GEOLOGY;

BRITTLE DEFORMATION; EXHUMATION; FAULTING; PSEUDOTACHYLITE; SLIP; ULTRAHIGH PRESSURE METAMORPHISM;

ALPS; COTTIAN ALPS; DORA MAIRA MASSIF; EURASIA; EUROPE; ITALY; PIEDMONT [ITALY]; SOUTHERN EUROPE; WESTERN ALPS;

MICAS;

EID: 34250171191     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jsg.2007.03.009     Document Type: Article

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