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      Laboratory earthquake forecasting: A machine learning competition

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          Abstract

          Earthquake prediction, the long-sought holy grail of earthquake science, continues to confound Earth scientists. Could we make advances by crowdsourcing, drawing from the vast knowledge and creativity of the machine learning (ML) community? We used Google’s ML competition platform, Kaggle, to engage the worldwide ML community with a competition to develop and improve data analysis approaches on a forecasting problem that uses laboratory earthquake data. The competitors were tasked with predicting the time remaining before the next earthquake of successive laboratory quake events, based on only a small portion of the laboratory seismic data. The more than 4,500 participating teams created and shared more than 400 computer programs in openly accessible notebooks. Complementing the now well-known features of seismic data that map to fault criticality in the laboratory, the winning teams employed unexpected strategies based on rescaling failure times as a fraction of the seismic cycle and comparing input distribution of training and testing data. In addition to yielding scientific insights into fault processes in the laboratory and their relation with the evolution of the statistical properties of the associated seismic data, the competition serves as a pedagogical tool for teaching ML in geophysics. The approach may provide a model for other competitions in geosciences or other domains of study to help engage the ML community on problems of significance.

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          Most cited references75

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          Propagation of slow slip leading up to the 2011 M(w) 9.0 Tohoku-Oki earthquake.

          Many large earthquakes are preceded by one or more foreshocks, but it is unclear how these foreshocks relate to the nucleation process of the mainshock. On the basis of an earthquake catalog created using a waveform correlation technique, we identified two distinct sequences of foreshocks migrating at rates of 2 to 10 kilometers per day along the trench axis toward the epicenter of the 2011 moment magnitude (M(w)) 9.0 Tohoku-Oki earthquake in Japan. The time history of quasi-static slip along the plate interface, based on small repeating earthquakes that were part of the migrating seismicity, suggests that two sequences involved slow-slip transients propagating toward the initial rupture point. The second sequence, which involved large slip rates, may have caused substantial stress loading, prompting the unstable dynamic rupture of the mainshock.
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            Connecting slow earthquakes to huge earthquakes.

            Slow earthquakes are characterized by a wide spectrum of fault slip behaviors and seismic radiation patterns that differ from those of traditional earthquakes. However, slow earthquakes and huge megathrust earthquakes can have common slip mechanisms and are located in neighboring regions of the seismogenic zone. The frequent occurrence of slow earthquakes may help to reveal the physics underlying megathrust events as useful analogs. Slow earthquakes may function as stress meters because of their high sensitivity to stress changes in the seismogenic zone. Episodic stress transfer to megathrust source faults leads to an increased probability of triggering huge earthquakes if the adjacent locked region is critically loaded. Careful and precise monitoring of slow earthquakes may provide new information on the likelihood of impending huge earthquakes.
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              • Article: not found

              Slow Earthquakes and Nonvolcanic Tremor

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                Author and article information

                Journal
                Proc Natl Acad Sci U S A
                Proc Natl Acad Sci U S A
                pnas
                pnas
                PNAS
                Proceedings of the National Academy of Sciences of the United States of America
                National Academy of Sciences
                0027-8424
                1091-6490
                02 February 2021
                25 January 2021
                25 January 2021
                : 118
                : 5
                : e2011362118
                Affiliations
                [1] aGeophysics Group, Los Alamos National Laboratory, Los Alamos, NM 87545;
                [2] bDepartment of Physics and Astronomy, Purdue University, West Lafayette, IN 47907;
                [3] cDepartment of Earth, Atmospheric and Planetary Sciences, Purdue University, West Lafayette, IN 47907;
                [4] dLyles School of Civil Engineering, Purdue University, West Lafayette, IN 47907;
                [5] eDepartment of Geophysics, Stanford University, Stanford, CA 94305;
                [6] fDepartment of Earth Science, La Sapienza Università di Roma, 00413 Rome, Italy;
                [7] gDepartment of Earth Science, Pennsylvania State University, University Park, PA 16802;
                [8] hLaboratoire de Géologie, Département de Géosciences, École Normale Supérieure, PSL University, CNRS UMR, 8538 Paris, France;
                [9] iKaggle, Google, LLC, Denver, CO 80301;
                [10] jH2O.ai, 1010 Vienna, Austria;
                [11] kPrivate individual, Athens 11364, Greece;
                [12] lPrivate individual, Jacksonville, FL, 32207;
                [13] mDepartment of Electrical Engineering, Rheinisch-Westfälische Technische Hochschule Aachen University, 52056 Aachen, Germany;
                [14] nPrivate individual, Bethesda, MD 20817
                Author notes
                2To whom correspondence may be addressed. Email: paj@ 123456lanl.gov .

                Edited by David A. Weitz, Harvard University, Cambridge, MA, and approved November 28, 2020 (received for review August 3, 2020)

                Author contributions: P.A.J., L.J.P.-N., G.C.B., A.H., and W.R. designed research; B.R.-L., C.J.M., P.S., D.G., D.K., C.J.L., P.P., and K.M.P. performed research; P.A.J., C.H., P.S., D.G., D.K., C.J.L., P.P., and K.M.P. analyzed data; and P.A.J., B.R.-L. and L.J.P.-N. wrote the paper.

                1P.A.J., B.R.-L., and L.J.P-N. contributed equally to this work.

                3Member of Team Zoo, a team formed to compete in the Kaggle earthquake competition.

                Author information
                http://orcid.org/0000-0001-6826-5214
                http://orcid.org/0000-0002-8667-1838
                http://orcid.org/0000-0002-8888-0473
                http://orcid.org/0000-0001-7312-3237
                http://orcid.org/0000-0002-0455-9966
                http://orcid.org/0000-0002-6432-101X
                Article
                202011362
                10.1073/pnas.2011362118
                7865129
                33495346
                2b834717-6297-4eed-a282-15a2f369b596
                Copyright © 2021 the Author(s). Published by PNAS.

                This open access article is distributed under Creative Commons Attribution License 4.0 (CC BY).

                History
                Page count
                Pages: 10
                Funding
                Funded by: DOE | Office of Science (SC) 100006132
                Award ID: 9233218CNA000001
                Award Recipient : Paul A Johnson Award Recipient : Bertrand Rouet-LeDuc Award Recipient : Laura Pyrak-Nolte Award Recipient : Greg Beroza Award Recipient : Chris J Marone Award Recipient : Claudia Hulbert
                Funded by: DOE | Office of Science (SC) 100006132
                Award ID: DE-FG02-09ER16022
                Award Recipient : Paul A Johnson Award Recipient : Bertrand Rouet-LeDuc Award Recipient : Laura Pyrak-Nolte Award Recipient : Greg Beroza Award Recipient : Chris J Marone Award Recipient : Claudia Hulbert
                Funded by: DOE | Office of Science (SC) 100006132
                Award ID: DE-SC0020445
                Award Recipient : Paul A Johnson Award Recipient : Bertrand Rouet-LeDuc Award Recipient : Laura Pyrak-Nolte Award Recipient : Greg Beroza Award Recipient : Chris J Marone Award Recipient : Claudia Hulbert
                Funded by: DOE | Office of Science (SC) 100006132
                Award ID: 9233218CNA000001
                Award Recipient : Paul A Johnson Award Recipient : Bertrand Rouet-LeDuc Award Recipient : Laura Pyrak-Nolte Award Recipient : Greg Beroza Award Recipient : Chris J Marone Award Recipient : Claudia Hulbert
                Funded by: Google 100006785
                Award ID: N/A
                Award Recipient : Addison Howard Award Recipient : Walter Reade
                Funded by: Google 100006785
                Award ID: N/A
                Award Recipient : Addison Howard Award Recipient : Walter Reade
                Funded by: H20.ai
                Award ID: N/A
                Award Recipient : Bertrand Rouet-LeDuc Award Recipient : Philipp Singer Award Recipient : Dmitry Gordeev
                Funded by: H20.ai
                Award ID: N/A
                Award Recipient : Bertrand Rouet-LeDuc Award Recipient : Philipp Singer Award Recipient : Dmitry Gordeev
                Funded by: DOE | Office of Science (SC) 100006132
                Award ID: DE-SC0020512
                Award Recipient : Paul A Johnson Award Recipient : Bertrand Rouet-LeDuc Award Recipient : Laura Pyrak-Nolte Award Recipient : Greg Beroza Award Recipient : Chris J Marone Award Recipient : Claudia Hulbert
                Funded by: DOE | Office of Science (SC) 100006132
                Award ID: DE-EE0008763
                Award Recipient : Paul A Johnson Award Recipient : Bertrand Rouet-LeDuc Award Recipient : Laura Pyrak-Nolte Award Recipient : Greg Beroza Award Recipient : Chris J Marone Award Recipient : Claudia Hulbert
                Funded by: DOE | LDRD | Los Alamos National Laboratory (LANL)
                Award ID: 20200278ER
                Award Recipient : Bertrand Rouet-LeDuc Award Recipient : Philipp Singer Award Recipient : Dmitry Gordeev
                Categories
                447
                413
                Perspective
                Physical Sciences
                Earth, Atmospheric, and Planetary Sciences

                machine learning competition,laboratory earthquakes,earthquake prediction,physics of faulting

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