Index Catalog // ScholarsArchive@OSU

Creator:: Kuna, Václav M.
Abstract:: The dissertation concentrates on seismicity of the Blanco Transform Fault (BTF), a 350-km-long oceanic transform fault (OTF) in the northeast Pacific Ocean. I analyze data collected during the Blanco Transform Fault OBS experiment, which comprised of a 1-year deployment of 55 three-component seismometers co-located with differential pressure gauges on and...
Resource Type:: Dissertation
Full Text:: @oregonstate.edu John L. Nábělek, email: nabelek@coas.oregonstate.edu 6 2.1. Abstract

Creator:: Li, Xiao-qing, 1963-
Abstract:: On November 6, 1988, two strong earthquakes (Mw: 7.0 and 6.8) separated by about 13 minutes occurred in Yunnan Province, China. The aftershocks located by Kunming Telemetered Seismic Network form a lineament approximately 120 km long and 20 km wide with the long dimension oriented approximately N30°W. The epicenter of...
Resource Type:: Masters Thesis
Full Text:: . Earthquake Sequence: Body Wave. Abstract Dr. John L. Nabelek On November 6, 1988, two strong earthquakes

Creator:: Li, Xiao-qing, 1963-
Resource Type:: Dissertation
Full Text:: would like to thank my advisor Dr. John Nabelek who provided support and guidance for my Ph.D. program

Creator:: Xia, Ganyuan
Resource Type:: Masters Thesis
Full Text:: Earthauakes in the Pacific Northwest Abstract approved: John L. Nabelek With the increasing volume of very

Creator:: Sapkota, Birat
Abstract:: The Juan de Fuca plate system is what remains of Farallon plate subducting under the continental North American plate. Blanco Transform Fault Zone (BTFZ) consists of a network of strike-slip faults discontinued by pull apart depressions which o↵sets the Juan de Fuca Ridge and the Gorda Ridge. Detailed analysis of...
Resource Type:: Masters Thesis
Full Text:: Boundaries Abstract approved: John L. Nabelek The Juan de Fuca plate system is what remains of Farallon

Creator:: Monigle, Patrick W.
Abstract:: Recent geophysical and geological investigations of the Tibetan plateau have given rise to conflicting models of plateau growth and deformation, where the presence and extent of partial melt in the crust could be a determining factor. Here we investigate the attenuation structure of the crust and upper mantle, as attenuation...
Resource Type:: Dissertation
Full Text:: : _____________________________________________________________________ John L. Nabelek Recent geophysical and geological investigations of the Tibetan plateau

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