Structural modeling of the Western Transverse Ranges: An imbricated thrust ramp architecture Article Swipe
YOU?
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· 2019
· Open Access
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· DOI: https://doi.org/10.1130/l1124.1
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 in the Western Transverse Ranges of California, USA. However, the diverse set of conflicting structural models for this region highlights the lack of understanding of the subsurface geometry of faults. A more robust structural model is required to assess the seismic hazard of the Western Transverse Ranges. Toward this goal, we developed a forward structural model using Trishear in MOVE® to match the first-order structure of the Western Transverse Ranges, as inferred from surface geology, subsurface well control, and seismic stratigraphy. We incorporated the full range of geologic observations, including vertical motions from uplifted fluvial and marine terraces, as constraints on our kinematic forward modeling. Using fault-related folding methods, we predicted the geometry and sense of slip of the major faults at depth, and we used these structures to model the evolution of the Western Transverse Ranges since the late Pliocene. The model predictions are in good agreement with the observed geology. Our results suggest that the Western Transverse Ranges comprises a southward-verging imbricate thrust system, with the dominant faults dipping as a ramp to the north and steepening as they shoal from ∼16°–30° at depth to ∼45°–60° near the surface. We estimate ∼21 km of total shortening since the Pliocene in the eastern part of the region, and a decrease of total shortening west of Santa Barbara down to 7 km near Point Conception. The potential surface area of the inferred deep thrust ramp is up to 6000 km2, which is of sufficient size to host the large earthquakes inferred from paleoseismic studies in this region.
Related Topics
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1130/l1124.1
- https://pubs.geoscienceworld.org/gsa/lithosphere/article-pdf/11/6/868/4873307/868.pdf
- OA Status
- gold
- Cited By
- 14
- References
- 58
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W2989210458
Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W2989210458Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1130/l1124.1Digital Object Identifier
- Title
-
Structural modeling of the Western Transverse Ranges: An imbricated thrust ramp architectureWork title
- Type
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articleOpenAlex work type
- Language
-
enPrimary language
- Publication year
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2019Year of publication
- Publication date
-
2019-11-04Full publication date if available
- Authors
-
Yuval Levy, T. Rockwell, John H. Shaw, Andreas Plesch, N. W. Driscoll, Héctor PereaList of authors in order
- Landing page
-
https://doi.org/10.1130/l1124.1Publisher landing page
- PDF URL
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https://pubs.geoscienceworld.org/gsa/lithosphere/article-pdf/11/6/868/4873307/868.pdfDirect link to full text PDF
- Open access
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YesWhether a free full text is available
- OA status
-
goldOpen access status per OpenAlex
- OA URL
-
https://pubs.geoscienceworld.org/gsa/lithosphere/article-pdf/11/6/868/4873307/868.pdfDirect OA link when available
- Concepts
-
Geology, Seismology, Transverse plane, Shoal, Thrust, Structural geology, Thrust fault, Stratigraphy, Seismic hazard, Fault (geology), Paleontology, Kinematics, Tectonics, Geomorphology, Classical mechanics, Engineering, Structural engineering, Thermodynamics, PhysicsTop concepts (fields/topics) attached by OpenAlex
- Cited by
-
14Total citation count in OpenAlex
- Citations by year (recent)
-
2022: 3, 2021: 9, 2020: 2Per-year citation counts (last 5 years)
- References (count)
-
58Number of works referenced by this work
- Related works (count)
-
10Other works algorithmically related by OpenAlex
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