Project Details
Projekt Print View

Inferring heterogeneity of fault properties and stress state of a megathrust fault from dynamic stress drop variations: A feasibility study in the northern Chilean subduction zone

Applicant Dr. Jonas Folesky
Subject Area Geophysics
Term from 2020 to 2024
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 442516884
 
Final Report Year 2024

Final Report Abstract

The principal objective of this research project was to contribute to a better understanding of earthquake rupture processes in subduction zones, and more specifically to resolve the role of stress and fault strength over different parts of the megathrust earthquake cycle. To achieve this, it was proposed to use stress drop as a primary marker. Therefore, the building of a comprehensive and robust stress drop map was the designated primary target of the project. This idea was realized for the northern Chilean subduction zone, where a recent large seismic catalog and excellent waveform data are available. Of the three initially planned stress drop estimation approaches, two approaches could be realized side by side, the spectral ratio method and the spectral decomposition method. First, a feasibility study using only the spectral ratios was implemented, followed by a large and robust stress drop catalog of over 51,000 estimates. This catalog, today, is amongst the largest compilations of stress drop, in general, and it resembles the only catalog covering an entire subduction zone from trench to a depth of about 200km. The great benefit of compiling a consistently processed catalog lies in the highly increased reliability of in-catalog variations of stress drop, which is usually difficult to compare between studies. The catalog revealed prior unknown features of stress drop variability: The stress drop segments the subduction tone into different regions, it is lowest all along the downgoing plate interface, highest in the upper plate crust and at great depth, where a depth dependency can be found. In combination with a b-value mapping, the comprehensive stress drop distribution was interpreted for assessing the nucleation conditions for earthquakes of different regions throughout the subduction zone. Analyzing spatio-temporal stress drop variability and the combination of such with remote sensing derived locking maps could not yet be realized and would be an important followup study worth pursuing. As an important byproduct of the search for suitable empirical Green’s functions for the spectral ratio derived stress drops large cross correlation matrices were computed. These have been searched extensively to identify repeating earthquakes in the target region. Improving methods and interpretation of the large number of repeaters and their variable characteristics have been started and will be continued in a subsequent project. The results will potentially be complementary to the stress drop catalog, which in itself bears a great potential fur further study.

Publications

 
 

Additional Information

Textvergrößerung und Kontrastanpassung