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Updated: Apr 8, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
Published on: August 5, 2016
Variable Holocene deformation above a shallow subduction zone extremely close to the trench
Kaustubh Thirumalai1,2, Frederick W Taylor1, Chuan-Chou Shen3
1Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, J. J. Pickle Research Campus, Building 196, 10100 Burnet Road (R2200), Austin, Texas 78758, USA.
Vertical crustal motion records reveal heterogeneous uplift histories near convergent margins. This variability impacts hazard assessment and understanding of megathrust earthquake processes.
Area of Science:
- Geophysics
- Tectonics
- Paleoseismology
Background:
- Convergent margins exhibit vertical crustal motions crucial for understanding interplate slip and permanent deformation.
- Past abrupt vertical motions serve as proxies for tsunamigenic earthquakes, aiding hazard assessment.
- Holocene vertical deformation records are essential for linking past earthquakes to tectonic activity.
Purpose of the Study:
- To reconstruct the uplift event history in the western Solomon Islands, close to a trench.
- To investigate the relationship between past earthquakes and Holocene vertical deformation.
- To analyze spatiotemporal heterogeneity in vertical crustal motion.
Main Methods:
- Measuring elevations of in situ corals.
- Determining (230)Th ages of corals.
- Constructing an uplift event history.
Main Results:
- Identified marked spatiotemporal heterogeneity in uplift from mid-Holocene to the present.
- Observed variations in permanent uplift accumulation across different areas.
- Data collected from corals near the trench (4-40 km depth).
Conclusions:
- Uplift from megathrust events may be retained in some locations but removed in others before subsequent ruptures.
- Variability in uplift suggests significant changes in strain accumulation and interplate thrust processes between events.
- Findings enhance understanding of earthquake cycles and deformation at convergent margins.
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