Development of a numerical model for the Sumatra subduction zone constrained by satellite gravimetry

with special focus on gravity sensitivity studies

Master Thesis (2018)
Author(s)

L.Z.F. van Rossum (TU Delft - Aerospace Engineering)

Contributor(s)

B.C. C. Root – Mentor

W. van der Wal – Graduation committee member

Faculty
Aerospace Engineering
Copyright
© 2018 Leon van Rossum
More Info
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Publication Year
2018
Language
English
Copyright
© 2018 Leon van Rossum
Coordinates
2.656001,98.760391
Graduation Date
27-08-2018
Awarding Institution
Delft University of Technology
Project
['European Space Agency - 3D Earth']
Programme
['Aerospace Engineering']
Related content

Abstract for poster presentation at European Geosciences Union (EGU) General Assembly 2018 in Vienna

https://meetingorganizer.copernicus.org/EGU2018/EGU2018-19690.pdf
Faculty
Aerospace Engineering
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Abstract

Satellite-derived gravity models have been used in modelling of several subduction zones, but not yet for the Sumatra subduction zone. There, gravity models can shed light on the geometry and density of the plate, and whether a slab tear is present under northern Sumatra, as seismic and tomographic studies present contradicting conclusions.

Ten different gravity sensitivity tests were carried out. Those tests investigated the sensitivities of the radial gravity (gR) and the second gravity gradient tensor invariant (I1) to different slab parameters (depth, thickness, density), three isostatic scenarios, and the inclusion of subduction-specific characteristics, e.g. a slab tear, and subducting crust. An innovative approach was implemented to determine slab thickness estimates based on oceanic lithospheric age, subduction direction, and a weighted half-space cooling model. Thereafter, a numerical model for the Sumatra subduction zone was developed which approximates the XGM2016 satellite-terrestrial gravity observations and supports a slab tear.

The gravity sensitivity test results together with the numerical model for the Sumatra subduction zone provide a valuable and universal foundation for future gravity-based subduction zone research.

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