Deutsch
 
Datenschutzhinweis Impressum
  DetailsucheBrowse
  1. Detailsuche  / 
  2. Ablage / 
  3. Datensatz Übersicht

Datensatz

DATENSATZ AKTIONENEXPORT
Zur Ablage hinzufügen
  DetailsÜbersicht
 ZurückNächste 

Freigegeben
Hochschulschrift

Anatomy of an ancient subduction channel in the depth range of its seismogenic coupling zone - insights from field studies in the Swiss Alps and Southern Chile

Urheber*innen

Bachmann,  Raik
Scientific Technical Report STR, Deutsches GeoForschungsZentrum;
3.1 Lithosphere Dynamics, 3.0 Geodynamics and Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Externe Ressourcen
Es sind keine externen Ressourcen hinterlegt
Volltexte (frei zugänglich)

0801.pdf
(Verlagsversion), 13MB

Ergänzendes Material (frei zugänglich)
Es sind keine frei zugänglichen Ergänzenden Materialien verfügbar
Zitation

Bachmann, R. (2008): Anatomy of an ancient subduction channel in the depth range of its seismogenic coupling zone - insights from field studies in the Swiss Alps and Southern Chile, PhD Thesis, (Scientific Technical Report STR ; 08/01), Potsdam : Deutsches GeoForschungsZentrum GFZ, Getr. Zählung p.
https://doi.org/10.2312/GFZ.b103-08012


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_8754
Zusammenfassung
The here presented study contributes to the understanding of convergent plate boundaries in the depth range of their former seismogenic zone aiming at testing inferences and hypotheses of the various kinematic and mechanical concepts presented for the seismogenic zone. Therefore, we use the complete exposure of this part of a former plate interface in the European Alps, one of the best-studied mountain belts that has resulted from successive subduction, accretion and collision, where we analyzed a mélange zone tracing the plate interface zone of the fossil convergent plate margin. Additionally, we included information from Southern Chile, where material, which formerly underwent deformation along the plate interface, was exhumed to the surface by large scale basal accretion at a certain depth to the base of the upper plate. This part of the study provided additive hints for structures and processes occurring along the plate interface zone of convergent plate margins (i.e. within the subduction channel), at least for a restricted PT domain.