TY - JOUR
T1 - Real-time earthquake monitoring during the second phase of the deep fault drilling project, Alpine fault, New Zealand
AU - Chamberlain, Calum J.
AU - Boese, Carolin M.
AU - Eccles, Jennifer D.
AU - Savage, Martha K.
AU - Baratin, Laura May
AU - Townend, John
AU - Gulley, Anton K.
AU - Jacobs, Katrina M.
AU - Benson, Adrian
AU - Taylor-Offord, Sam
AU - Thurber, Clifford
AU - Guo, Bin
AU - Okada, Tomomi
AU - Takagi, Ryota
AU - Yoshida, Keisuke
AU - Sutherland, Rupert
AU - Toy, Virginia G.
N1 - Funding Information:
The second phase of Deep Fault Drilling Project (DFDP-2) was funded by the International Continental Scientific Drilling Program (ICDP), the Marsden Fund of the Royal Society of New Zealand, GNS Science, Victoria University of Wellington, University of Otago, and governments of New Zealand (Ministry of Business, Innovation, and Employment), the United Kingdom (National Environmental Research Council), and the United States (National Science Foundation). Chamberlain and Townend acknowledge the support provided for this research by the Earthquake Commission (EQC) Programme in Seismology and Fault Mechanics and by Victoria University of Wellington. Thurber acknowledges support from the National Science Foundation under Award EAR-1114228. Chamberlain thanks Emily Warren-Smith for comments that improved the article, and for assistance administering the network. We acknowledge the New Zealand GeoNet project and its sponsors EQC, GNS Science, and Land Information New Zealand (LINZ), for providing data used in this study, and for assistance telemetering and archiving data from sites used in this study. We are particularly grateful to Colin Dyer, Mark Chadwick (GNS Science), and Aleksandr Beliaev (Victoria University of Wellington) for assistance with DFDP-2 telemetry and analysis, and Holly Godfrey, Stacey Martin, and Matt Swinbourn for assistance in preliminary seismicity analysis. Finally, we thank Bill Ellsworth and the other members of the DFDP-2 Earthquake Safety Review Panel for their conscientious and encouraging input into the seismic monitoring program and DFDP-2 operations overall.
Publisher Copyright:
© 2017 by the Seismological Society of America.
PY - 2017/11
Y1 - 2017/11
N2 - The Deep Fault Drilling Project (DFDP) is a multinational scientific drilling effort to study the evolution, structure, and seismogenesis of the Alpine fault, New Zealand, via in situ measurements of fault rock properties. The second phase of drilling (DFDP-2), undertaken in the Whataroa Valley in late 2014, was intended to intersect the Alpine fault at a depth of around 1 km. In conjunction with the drilling and on-site science activities, a real-time seismic monitoring scheme and traffic-light response protocol were established to detect, locate, and if necessary respond to seismicity within 30 km of the drill site. This network was operated around the clock between late August 2014 and early January 2015, and we detected and located 493 earthquakes of ML 0.6-4.2. None of these earthquakes occurred within 3 km of the drill site, and nor did any of the seismicity detected require changes to drilling operations. The monitoring was undertaken using open-source software operated by an international team of 16 seismologists (including eight postgraduate students) working in 7 institutions and 3 countries to provide rapid on- and off-site manual checking and relocating of events. The team's standard response time between detection and final location was less than 30 min under normal background seismicity conditions and up to 1 hr during swarm activity and for low-priority, distant (≥30 km epicentrally from the drill site) earthquakes. This article documents the methodology, infrastructure, protocols, outcomes, and key lessons of this monitoring.
AB - The Deep Fault Drilling Project (DFDP) is a multinational scientific drilling effort to study the evolution, structure, and seismogenesis of the Alpine fault, New Zealand, via in situ measurements of fault rock properties. The second phase of drilling (DFDP-2), undertaken in the Whataroa Valley in late 2014, was intended to intersect the Alpine fault at a depth of around 1 km. In conjunction with the drilling and on-site science activities, a real-time seismic monitoring scheme and traffic-light response protocol were established to detect, locate, and if necessary respond to seismicity within 30 km of the drill site. This network was operated around the clock between late August 2014 and early January 2015, and we detected and located 493 earthquakes of ML 0.6-4.2. None of these earthquakes occurred within 3 km of the drill site, and nor did any of the seismicity detected require changes to drilling operations. The monitoring was undertaken using open-source software operated by an international team of 16 seismologists (including eight postgraduate students) working in 7 institutions and 3 countries to provide rapid on- and off-site manual checking and relocating of events. The team's standard response time between detection and final location was less than 30 min under normal background seismicity conditions and up to 1 hr during swarm activity and for low-priority, distant (≥30 km epicentrally from the drill site) earthquakes. This article documents the methodology, infrastructure, protocols, outcomes, and key lessons of this monitoring.
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U2 - 10.1785/0220170095
DO - 10.1785/0220170095
M3 - Article
AN - SCOPUS:85034091878
SN - 0895-0695
VL - 88
SP - 1443
EP - 1454
JO - Seismological Research Letters
JF - Seismological Research Letters
IS - 6
ER -