John H. Shaw
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View article: Structural styles and kinematic evolution of the Front Ranges of the Southern Canadian Rockies
Structural styles and kinematic evolution of the Front Ranges of the Southern Canadian Rockies Open
We establish a comprehensive three-dimensional geometric and kinematic description of the Front Ranges in the Bow Valley–Kananaskis region of the Southern Canadian Rocky Mountains to rigorously evaluate and expand upon fundamental paradigm…
View article: Supplemental Material: Structural styles and kinematic evolution of the Front Ranges of the Southern Canadian Rockies
Supplemental Material: Structural styles and kinematic evolution of the Front Ranges of the Southern Canadian Rockies Open
Included in the supplement are details of how we calculated the error for the data presented in our scatterplot, along with seven additional figures. One is additional examples of our binning and fold analysis procedure and the results on …
View article: Supplemental Material: Structural styles and kinematic evolution of the Front Ranges of the Southern Canadian Rockies
Supplemental Material: Structural styles and kinematic evolution of the Front Ranges of the Southern Canadian Rockies Open
Included in the supplement are details of how we calculated the error for the data presented in our scatterplot, along with seven additional figures. One is additional examples of our binning and fold analysis procedure and the results on …
View article: SCEC Community Fault Model (CFM)
SCEC Community Fault Model (CFM) Open
Introduction The Statewide California Earthquake Center (SCEC) Community Fault Model (CFM) is an object-oriented, fully three-dimensional geometric representation of active faults in California and adjacent offshore basins. For each fault …
View article: A framework for classifying methane monitoring requirements, emission sources and monitoring methods
A framework for classifying methane monitoring requirements, emission sources and monitoring methods Open
View article: Estimating shallow compressional velocity variations in California’s Central Valley
Estimating shallow compressional velocity variations in California’s Central Valley Open
SUMMARY A theory for modelling the evolution of elastic moduli of grain packs under increasing pressure is combined with a method that accounts for the presence of fine-grained particles to develop a new conceptual framework for computing …
View article: Identification and analysis of ground surface rupture patterns from thrust and reverse fault earthquakes using geomechanical models
Identification and analysis of ground surface rupture patterns from thrust and reverse fault earthquakes using geomechanical models Open
View article: SCEC Community Fault Model (CFM)
SCEC Community Fault Model (CFM) Open
Introduction The SCEC Community Fault Model (CFM) is an object-oriented, three-dimensional representation of active faults in southern California and adjacent offshore basins. For each fault object, the CFM provides triang…
View article: SCEC Community Fault Model (CFM)
SCEC Community Fault Model (CFM) Open
Introduction The SCEC Community Fault Model (CFM) is an object-oriented, three-dimensional representation of active faults in southern California and adjacent offshore basins. For each fault object, the CFM provides triang…
View article: Estimating shallow compressional velocity variations in California's Central Valley
Estimating shallow compressional velocity variations in California's Central Valley Open
A set of 44 sonic velocity well logs from the southern San Joaquin Valley are combined with soil textural data to derive a three-dimensional compressional velocity model. The compaction of a granular medium containing fines provides a conc…
View article: SCEC Community Fault Model (CFM)
SCEC Community Fault Model (CFM) Open
Introduction The SCEC Community Fault Model (CFM) is an object-oriented, three-dimensional representation of active faults in southern California and adjacent offshore basins (Plesch et al., 2007). This latest update of t…
View article: KINEMATIC EVOLUTION OF THE FRONT RANGES OF THE CANADIAN ROCKIES INCLUDING THE ROLE OF FAULT PROPAGATION FOLD BREAKTHROUGHS AND MULTIPLE DETACHMENTS IN DEFINING THE THRUSTING SEQUENCE
KINEMATIC EVOLUTION OF THE FRONT RANGES OF THE CANADIAN ROCKIES INCLUDING THE ROLE OF FAULT PROPAGATION FOLD BREAKTHROUGHS AND MULTIPLE DETACHMENTS IN DEFINING THE THRUSTING SEQUENCE Open
View article: SCEC Community Fault Model (CFM)
SCEC Community Fault Model (CFM) Open
Introduction The SCEC Community Fault Model (CFM) is an object-oriented, three-dimensional representation of active faults in southern California and adjacent offshore basins that currently includes 440 individually named…
View article: SCEC Community Fault Model (CFM)
SCEC Community Fault Model (CFM) Open
Introduction The SCEC Community Fault Model (CFM) is an object-oriented, three-dimensional representation of active faults in southern California and adjacent offshore basins that currently includes 440 individually named…
View article: Exploring the relationship between organic deposition resulting from marshes and autogenic scales in deltaic stratigraphy
Exploring the relationship between organic deposition resulting from marshes and autogenic scales in deltaic stratigraphy Open
<p>Many deltas contain extensive marshes, typically defined as laterally extensive, low energy settings tied to a narrow elevation window around sea level. Biological activity in marshes results in in-situ organic sediment accumulati…
View article: vda_regional_grid7_modelcoords.txt
vda_regional_grid7_modelcoords.txt Open
Finite element mesh for regional model in netcdf format.
View article: Structural modeling of the Western Transverse Ranges: An imbricated thrust ramp architecture
Structural modeling of the Western Transverse Ranges: An imbricated thrust ramp architecture Open
Active fold-and-thrust belts can potentially accommodate large-magnitude earthquakes, so understanding the structure in such regions has both societal and scientific importance. Recent studies have provided evidence for large earthquakes i…
View article: Structural Architecture of the Western Transverse Ranges and Potential for Large Earthquakes - New Results of Trishear Forward Models
Structural Architecture of the Western Transverse Ranges and Potential for Large Earthquakes - New Results of Trishear Forward Models Open
View article: Validating novel boundary conditions for three-dimensional mechanics-based restoration: An extensional sandbox model example
Validating novel boundary conditions for three-dimensional mechanics-based restoration: An extensional sandbox model example Open
International audience
View article: Building Objective 3D Fault Representations in Active Tectonic Settings
Building Objective 3D Fault Representations in Active Tectonic Settings Open
Developing 3D representations of active faults is an important step to improve seismic‐hazard assessment. However, the geometries of faults can be difficult to constrain at depth, and building representations is often subjective. We presen…
View article: The E3 ubiquitin ligase NEDD4 is an LC3-interactive protein and regulates autophagy
The E3 ubiquitin ligase NEDD4 is an LC3-interactive protein and regulates autophagy Open
The MAP1LC3/LC3 family plays an essential role in autophagosomal biogenesis and transport. In this report, we show that the HECT family E3 ubiquitin ligase NEDD4 interacts with LC3 and is involved in autophagosomal biogenesis. NEDD4 binds …
View article: Accelerating slip rates on the Puente Hills blind thrust fault system beneath metropolitan Los Angeles, California, USA
Accelerating slip rates on the Puente Hills blind thrust fault system beneath metropolitan Los Angeles, California, USA Open
Slip rates represent the average displacement across a fault over time and are essential to estimating earthquake recurrence for probabilistic seismic hazard assessments. We demonstrate that the slip rate on the western segment of the Puen…
View article: Were the May 2012 Emilia‐Romagna earthquakes induced? A coupled flow‐geomechanics modeling assessment
Were the May 2012 Emilia‐Romagna earthquakes induced? A coupled flow‐geomechanics modeling assessment Open
Seismicity induced by fluid injection and withdrawal has emerged as a central element of the scientific discussion around subsurface technologies that tap into water and energy resources. Here we present the application of coupled flow‐geo…
View article: The 2015 Fillmore Earthquake Swarm and Possible Crustal Deformation Mechanisms near the Bottom of the Eastern Ventura Basin, California
The 2015 Fillmore Earthquake Swarm and Possible Crustal Deformation Mechanisms near the Bottom of the Eastern Ventura Basin, California Open
The 2015 Fillmore swarm occurred about 6 km west of the city of Fillmore in Ventura, California, and was located beneath the eastern part of the actively subsiding Ventura basin at depths from 11.8 to 13.8 km, similar to two previous swarm…
View article: Virtual specimens for analyzing strain distributions in textile ceramic composites
Virtual specimens for analyzing strain distributions in textile ceramic composites Open
View article: Three‐dimensional seismic velocity structure in the Sichuan basin, China
Three‐dimensional seismic velocity structure in the Sichuan basin, China Open
We present a new three‐dimensional velocity model of the crust in the eastern margin of the Tibetan Plateau. The model describes the velocity structure of the Sichuan basin and surrounding thrust belts. The model consists of 3‐D surfaces r…
View article: Supplemental material: Paleoseismologic evidence for large-magnitude (M<sub>w</sub> 7.5–8.0) earthquakes on the Ventura blind thrust fault: Implications for multifault ruptures in the Transverse Ranges of southern California
Supplemental material: Paleoseismologic evidence for large-magnitude (M<sub>w</sub> 7.5–8.0) earthquakes on the Ventura blind thrust fault: Implications for multifault ruptures in the Transverse Ranges of southern California Open
Geosphere, October 2015, v. 11, p. 1629-1650, doi:10.1130/GES01123.1, Supplemental Figure S7 - Raw CPT data.
View article: Paleoseismologic evidence for large-magnitude (M<sub>w</sub>7.5–8.0) earthquakes on the Ventura blind thrust fault: Implications for multifault ruptures in the Transverse Ranges of southern California
Paleoseismologic evidence for large-magnitude (M<sub>w</sub>7.5–8.0) earthquakes on the Ventura blind thrust fault: Implications for multifault ruptures in the Transverse Ranges of southern California Open
Detailed analysis of high-resolution seismic reflection data, continuously cored boreholes
\nand cone penetrometer tests (CPTs), and luminescence and 14 C dates from Holocene strata folded
\nabove the tip of the Ventura blind thrust fault …
View article: Rapid slip‐deficit rates at the eastern margin of the Tibetan Plateau prior to the 2008 <b><i>M</i><sub><i>w</i></sub></b> 7.9 Wenchuan earthquake
Rapid slip‐deficit rates at the eastern margin of the Tibetan Plateau prior to the 2008 <b><i>M</i><sub><i>w</i></sub></b> 7.9 Wenchuan earthquake Open
The Longmen Shan is the steepest topographic front at the India‐Asia collision zone and the site of the M w 7.9 Wenchuan earthquake. Here to explain the interseismic GPS velocities across the greater Longmen Shan region, we develop a bound…