The Dynamics of Unlikely Slip: 3D Modeling of Low-Angle Normal Fault Rupture at the Mai'iu Fault, Papua New Guinea

Biemiller, J.; Gabriel, A.-A. und Ulrich, T. (2022): The Dynamics of Unlikely Slip: 3D Modeling of Low-Angle Normal Fault Rupture at the Mai'iu Fault, Papua New Guinea. In: Geochemistry Geophysics Geosystems, Bd. 23, Nr. 5, e2021GC010298

Abstract

Despite decades-long debate over the mechanics of low-angle normal faults (LANFs) dipping less than 30 degrees, many questions about their strength, stress, and slip remain unresolved. Recent geologic and geophysical observations have confirmed that gently dipping detachment faults can slip at such shallow dips and host moderate-to-large earthquakes. Here, we analyze the first 3D dynamic rupture models to assess how different stress and strength conditions affect rupture characteristics of LANF earthquakes. We model observationally constrained spontaneous rupture under different loading conditions on the active Mai'iu fault in Papua New Guinea, which dips 16 degrees-24 degrees at the surface and accommodates similar to 8 mm/yr of horizontal extension. We analyze four distinct fault-local stress scenarios: (1) Andersonian extension, as inferred in the hanging wall;(2) back-rotated principal stresses inferred paleopiezometrically from the exhumed footwall;(3) favorably rotated principal stresses well-aligned for low-angle normal-sense slip;and (4) Andersonian extension derived from depth-variable static fault friction decreasing toward the surface. Our modeling suggests that subcritically stressed detachment faults can host moderate earthquakes within purely Andersonian stress fields. Near-surface rupture is impeded by free-surface stress interactions and dynamic effects of the gently dipping geometry and frictionally stable gouges of the shallowest portion of the fault. Although favorably inclined principal stresses have been proposed for some detachments, these conditions are not necessary for seismic slip on these faults. Our results demonstrate how integrated geophysical and geologic observations can constrain dynamic rupture model parameters to develop realistic rupture scenarios of active faults that may pose significant seismic and tsunami hazards to nearby communities.

• Dokumententyp: Zeitschriftenartikel
• Fakultät: Geowissenschaften > Department für Geo- und Umweltwissenschaften
• Themengebiete: 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie
• Sprache: Englisch