Ray J. Weldon
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Transition From Reverse to Left‐Slip on the Eastern Haiyuan Fault, NE Tibetan Plateau, From the Structure and Age of the Ganyanchi Pull‐Apart Basin Open
Because the active, left‐slip Haiyuan fault is a first‐order structure along the NE margin of the Tibetan Plateau, its tectonic evolution provides insight into deformation processes along this margin over time. Late Cenozoic deformation in…
Cenozoic Shortening and Propagation in the Eastern Kuqa Fold‐And‐Thrust Belt, South Tian Shan, NW China Open
In an orogen‐foreland basin system, syn‐orogenic sedimentation and deformation records within the foreland basin provide critical evidence for understanding uplift and erosion processes of adjacent orogenic belts. Foreland fold‐and‐thrust …
View article: 20thto 21stCentury Relative Sea and Land LevelChanges in Northern California:Tectonic Land Level Changes and theirContribution to Sea-Level Rise, Humboldt BayRegion, Northern California
20thto 21stCentury Relative Sea and Land LevelChanges in Northern California:Tectonic Land Level Changes and theirContribution to Sea-Level Rise, Humboldt BayRegion, Northern California Open
Sea-level changes are modulated in coastal northern California by land-level changes due to the earthquake cycle along the Cascadia subduction zone, the San Andreas plate boundary fault system, and crustal faults. Sea-level rise (SLR) subj…
20th to 21st Century Relative Sea and Land Level Changes in Northern California: Tectonic Land Level Changes and their Contribution to Sea-Level Rise, Humboldt Bay Region, Northern California Open
These data include a GIS ESRI shapefile for the geodetic stations and a GIS ESRI shapefile that shows the location of the subduction zone trench that we used to calculate trench distance for each geodetic station. These data also include t…
Cenozoic shortening and propagation in the Eastern Kuqa fold-and-thrust belt, South Tian Shan, NW China Open
Dataset S1: high-resolution interpreted seismic profiles A-A' to C-C' (Figures 4, 5, and 6 ). Supporting information submitted: Figure S1 and Table S1
View article: Latest Quaternary slip rates of the San Bernardino strand of the San Andreas fault, southern California, from Cajon Creek to Badger Canyon
Latest Quaternary slip rates of the San Bernardino strand of the San Andreas fault, southern California, from Cajon Creek to Badger Canyon Open
Four new latest Pleistocene slip rates from two sites along the northwestern half of the San Bernardino strand of the San Andreas fault suggest the slip rate decreases southeastward as slip transfers from the Mojave section of the San Andr…
An Assessment of Vertical Land Movement to Support Coastal Hazards Planning in Washington State Open
The sea and land change elevation spatially and temporally from a multitude of processes, so it is necessary to constrain the movement of both to evaluate how coastlines will evolve and how those evolving coastlines will impact the natural…
Fault Slip and GPS Velocities Across the Shan Plateau Define a Curved Southwestward Crustal Motion Around the Eastern Himalayan Syntaxis Open
Characterizing the 700 km wide system of active faults on the Shan Plateau, southeast of the eastern Himalayan syntaxis, is critical to understanding the geodynamics and seismic hazard of the large region that straddles neighboring China, …
A multiple-methods vertical land movement analysis and its integration into probabilistic sea level rise projections for coastal Washington Open
In order to support climate change planning and adaptation at the community scale, climate projections should ideally be down-scaled, and also provide meaningful representations of uncertainty. As part of the NOAA-funded Washington Coastal…
View article: A Synoptic View of the Third Uniform California Earthquake Rupture Forecast (UCERF3)
A Synoptic View of the Third Uniform California Earthquake Rupture Forecast (UCERF3) Open
Probabilistic forecasting of earthquake-producing fault ruptures informs all major decisions aimed at reducing seismic risk and improving earthquake resilience. Earthquake forecasting models rely on two scales of hazard evolution: long-ter…
Constraints on accumulated strain near the ETS zone along Cascadia Open
Current national seismic hazard models for Cascadia use the zone of episodic tremor and slip (ETS) to denote the lower boundary of the seismogenic zone. Recent numerical models have suggested that an appreciable amount of long-term strain …