Constraining long-term denudation and faulting history in intraplate regions by multisystem thermochronology: An example of the Sudetic Marginal Fault (Bohemian Massif, central Europe)

Tectonics

Volumn 31, Issue 2, 2012, Pages

  Danišík, Martin ^a,b   Štěpančíková, Petra ^c   Evans, Noreen J ^b,d  

^a UNIVERSITY OF WAIKATO   (New Zealand)

^b CURTIN UNIVERSITY   (Australia)

^c INSTITUTE OF ROCK STRUCTURE AND MECHANICS   (Czech Republic)

^d CSIRO   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

ANOXIC SEDIMENTS; FAULTING; PHOSPHATE MINERALS; SEDIMENTOLOGY; SILICATE MINERALS;

APATITE FISSION TRACKS; CENTRAL EUROPE; CRYSTALLINE BASEMENT; LANDSCAPE EVOLUTIONS; LATE CENOZOIC; LATE CRETACEOUS; MAGMATIC ACTIVITY; MOUNTAIN REGIONS; MULTI SYSTEMS; NATURAL LABORATORIES; NEAR-SURFACE; NEO GENES; NORMAL FAULTS; PALEOGEOGRAPHIC RECONSTRUCTION; REVERSE FAULTS; RIFT SYSTEMS; SEDIMENTARY SAMPLES; STUDY AREAS; THERMAL ACTIVITY; THERMAL MODELING; THERMOCHRONOLOGY;

BUILDINGS;

APATITE; BASEMENT ROCK; CRETACEOUS; DENUDATION; EOCENE-OLIGOCENE BOUNDARY; FAULTING; FISSION TRACK DATING; GEOCHRONOLOGY; INTRAPLATE PROCESS; LANDSCAPE EVOLUTION; PALEOGEOGRAPHY; PERMIAN; RIFT ZONE; THERMOCHRONOLOGY; UPLIFT; ZIRCON;

CZECH REPUBLIC; OLOMOUCKY; RYCHLEBSKE MOUNTAINS; SUDETES;

EID: 84858680282     PISSN: 02787407     EISSN: None     Source Type: Journal    
DOI: 10.1029/2011TC003012     Document Type: Review

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