Scholl, David E. et al. (2010): Rapid forearc basin subsidence and bordering splay fault systems may identify nucleation areas of high-magnitude earthquakes and tsunamis; the example of the Atka forearc basin sector of the Aleutian subduction zone
Leg/Site/Hole:
Related Expeditions:
Identifier:
ID:
2013-002870
Type:
georefid
Creator:
Name:
Scholl, David E.
Affiliation:
University of Alaska Fairbanks, Department of Geology and Geophysics, Fairbanks, AK, United States
Role:
author
Name:
Ryan, Holly
Affiliation:
U. S. Geological Survey, United States
Role:
author
Name:
Keranen, Katie M.
Affiliation:
University of Oklahoma, United States
Role:
author
Name:
Wells, Ray E.
Affiliation:
Role:
author
Name:
Kirby, Stephen H.
Affiliation:
Role:
author
Name:
von Huene, Roland
Affiliation:
Role:
author
Identification:
Title:
Rapid forearc basin subsidence and bordering splay fault systems may identify nucleation areas of high-magnitude earthquakes and tsunamis; the example of the Atka forearc basin sector of the Aleutian subduction zone
Year:
2010
Source:
In: Anonymous, European Geosciences Union general assembly 2010
Publisher:
Copernicus GmbH on behalf of the European Geosciences Union (EGU), Katlenburg-Lindau, Germany
Volume:
12
Issue:
Pages:
Abstract:
Language:
English
Genre:
Rights:
URL:
Coverage: Geographic coordinates: Keywords: Structural geology; Seismology; Aleutian Islands subduction zone; Aleutian Ridge; Aleutian Terrace; Atka Basin; basins; case studies; causes; Cenozoic; crustal thinning; Deep Sea Drilling Project; earthquakes; erosion; faults; focus; fore-arc basins; Global Positioning System; great earthquakes; mechanism; North Pacific; Pacific Ocean; Pacific Plate; plate convergence; plate tectonics; splay faults; subduction zones; subsidence; systems; thrust faults; tsunamis;
.