Potential for Continental Scientific Drilling to Inform Fault Mechanics and Earthquake Science

Our understanding of fault mechanics and earthquake processes remains limited, largely due to minimal direct observations near active faults at seismogenic depths. This lack of data restricts our ability to accurately assess and mitigate both natural and human-induced seismic hazards. However, recent advancements in drilling capabilities and downhole sensing technologies offer an opportunity: the ability to observe the physical conditions within a volume near active fault zones. In this contribution, we highlight how scientific drilling can provide access to the near-fault environment, enabling measurements of the stress, temperature, fluid pressure, and rock properties at depths where ruptures initiate, propagate, and arrest. These observations are essential to refine models of earthquake nucleation and dynamic rupture, bridging gaps between laboratory experiments, numerical simulations, and surface observations. These insights can advance fundamental understanding in earthquake science but also support the development of more effective seismic hazard assessments and risk mitigation strategies.

Authors

Institutions

Publication Details

Journal
Seismica
Published
2025-11-07
DOI
https://doi.org/10.26443/seismica.v4i2.1700
Primary Topic
earthquake and tectonic studies
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Potential for Continental Scientific Drilling to Inform Fault Mechanics and Earthquake Science

B. M. Carpenter, Nicholas W. Hayman, Harold Tobin, William L. Ellsworth et al.
Seismica
earthquake and tectonic studies
article

Potential for Continental Scientific Drilling to Inform Fault Mechanics and Earthquake Science

B. M. Carpenter, Nicholas W. Hayman, Harold Tobin, William L. Ellsworth, Natalia Zakharova, Hiroki Sone, Folarin Kolawole, Yves Guglielmi, Stephen H. Hickman, Douglas R. Schmitt, Peter Eichhubl, E. S. Cochran
article en

Abstract

Our understanding of fault mechanics and earthquake processes remains limited, largely due to minimal direct observations near active faults at seismogenic depths. This lack of data restricts our ability to accurately assess and mitigate both natural and human-induced seismic hazards. However, recent advancements in drilling capabilities and downhole sensing technologies offer an opportunity: the ability to observe the physical conditions within a volume near active fault zones. In this contribution, we highlight how scientific drilling can provide access to the near-fault environment, enabling measurements of the stress, temperature, fluid pressure, and rock properties at depths where ruptures initiate, propagate, and arrest. These observations are essential to refine models of earthquake nucleation and dynamic rupture, bridging gaps between laboratory experiments, numerical simulations, and surface observations. These insights can advance fundamental understanding in earthquake science but also support the development of more effective seismic hazard assessments and risk mitigation strategies.

SeismicaVol. 4(2)
United States Geological Survey (US), University of Wisconsin–Madison (US), Lawrence Berkeley National Laboratory (US), Central Michigan University (US), University of Washington (US), Geoscience BC (CA), Oklahoma Biological Survey (US), Centre de Géosciences (FR), Environmental Earth Sciences (AU), Columbia University (US), Stanford University (US)
U.S. Geological Survey
Openalex Percentile: Top 65%
earthquake and tectonic studies
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.