$$S$$_Hmax orientation in the Alpine region from observations of stress-induced anisotropy of nonlinear elasticity

Journal Article · Wed Sep 13 00:00:00 EDT 2023 · Geophysical Journal International

DOI:https://doi.org/10.1093/gji/ggad353· OSTI ID:2246841

Aiman, Yongki A. ^[1]; Delorey, A. A. ^[2]; Lu, Y. ^[1]; Bokelmann, G. ^[1]

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1. University of Vienna (Austria)
2. Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)

The orientation of $$S$$_Hmax is commonly estimated from in situ borehole breakouts and earthquake focal mechanisms. Borehole measurements are expensive, and therefore sparse, and earthquake measurements can only be made in regions with many well-characterized earthquakes. Here, we derive the stress-field orientation using stress-induced anisotropy in nonlinear elasticity. In this method, we measure the strain derivative of velocity as a function of azimuth. We use a natural pump-probe (NPP) approach which consists of measuring elastic wave speed using empirical Green’s functions (probe) at different points of the earth tidal strain cycle (pump). The approach is validated using a larger data set in the Northern Alpine Foreland region where the orientation of maximum horizontal compressive stress is known from borehole breakouts and drilling-induced fractures. The technique resolves NNW-SSW to N-S directed $$S$$_Hmax which is in good agreement with conventional methods and the recent crustal stress model. We confirm that the NPP method can be applied to dense large-scale seismic arrays. The technique is then applied to the Southern Alps to understand the contemporary stress pattern associated with the ongoing deformation due to counterclockwise rotation of the Adriatic plate with respect to the European plate. Our results explain why the two major faults in Northeastern Italy, the Giudicarie Fault and the Periadriatic Line (Pustertal–Gailtal Fault) are currently inactive, while the currently acting stress field allows faults in Slovenia to deform actively. We have demonstrated that the pump-probe method has the potential to fill in the measurement gap left by conventional approaches, both in terms of regional coverage and in depth.

• Research Organization: Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
• Sponsoring Organization: USDOE National Nuclear Security Administration (NNSA)
• Grant/Contract Number: 89233218CNA000001
• OSTI ID: 2246841
• Report Number(s): LA-UR--22-32977
• Journal Information: Geophysical Journal International, Journal Name: Geophysical Journal International Journal Issue: 3 Vol. 235; ISSN 0956-540X
• Publisher: Oxford University Press
• Country of Publication: United States
• Language: English

Related Subjects

58 GEOSCIENCES
Coda waves
Dynamics: seismotectonics
Nonlinear elasticity
Seismic interferometry
Seismic noise
Stress-induced anisotropy