About: Tom Parsons

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An Entity of Type : wikibase:Item, within Data Space : wikidata.demo.openlinksw.com associated with source document(s)

geophysicist

Attributes	Values
rdf:type	Item
description	geophysicist (en) geofysicus (nl)
rdfs:label	Tom Parsons (en) Tom Parsons (es) Tom Parsons (nl) Tom Parsons (sq) Tom Parsons (ast)
skos:prefLabel	Tom Parsons (en) Tom Parsons (es) Tom Parsons (nl) Tom Parsons (sq) Tom Parsons (ast)
name	Tom Parsons (en) Tom Parsons (es) Tom Parsons (nl) Tom Parsons (sq) Tom Parsons (ast)
Scopus author ID	wds:Q57777394-20FBA7F6-D9B8-4DDA-B670-E24DE39A0DC9
Scopus author ID	7103344997
given name	wds:Q57777394-AFB17C74-48BA-464B-8C9C-2CA82EA4C816
given name	Tom
instance of	wds:Q57777394-2F732038-4802-4890-8494-38374340094B
instance of	Homo sapiens
ResearchGate profile ID	wds:Q57777394-04d43b8f-49bd-43cb-c8f5-2721a28bdf77
ResearchGate profile ID	Tom_Parsons9
occupation	wds:Q57777394-6aaadd7d-4607-c9f8-a557-ddd1c62bbc33
employer	wds:Q57777394-4F2C975B-9082-45BB-A0A2-C174F7D2D2CB
NUKAT ID	wds:Q57777394-C121CD68-EC01-49B0-9E51-56EBBFB3B02F
ISNI	wds:Q57777394-350C3634-1AA0-41D4-A1BC-13E2A8AC1C76
VIAF ID	wds:Q57777394-BA1DCAAA-FD9C-4474-A7EE-1B762BB6E156
educated at	wds:Q57777394-3AF96BC2-A318-436C-80D0-5BF4478E7CD1 wds:Q57777394-C5F4828B-E84A-4E63-9A9B-7A076D4DFC0D wds:Q57777394-D8E39012-E420-4FCC-9961-476C3993D238
family name	wds:Q57777394-6548C4B1-E9F6-4F7D-9457-CE9897E80395
VIAF ID	http://viaf.org/viaf/33827911
occupation	geophysicist
employer	United States Geological Survey
NUKAT ID	n2005030287
ISNI	0000000114412653
VIAF ID	33827911
educated at	University of California, Los Angeles Golden West College Stanford University
family name	Parsons
ORCID iD	wds:Q57777394-04BA10E1-C47E-498D-A1FD-FC4A6FA96F4F
ORCID iD	https://orcid.org/0000-0002-0582-4338
ORCID iD	0000-0002-0582-4338
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q57777394
is author of	Heightened odds of large earthquakes near istanbul: An interaction-based probability calculation Three-dimensional model of Hellenic Arc deformation and origin of the Cretan uplift Probabilistic Analysis of Tsunami Hazards* Undersampling power-law size distributions: effect on the assessment of extreme natural hazards Absence of remotely triggered large earthquakes beyond the mainshock region Evaluation of static stress change forecasting with prospective and blind tests Upper crustal structure in Puget Lowland, Washington: Results from the 1998 Seismic Hazards Investigation in Puget Sound Three-dimensional velocity structure of Siletzia and other accreted terranes in the Cascadia forearc of Washington Seismic survey probes urban earthquake hazards in Pacific Northwest M ≥ 7 earthquake rupture forecast and time-dependent probability for the sea of Marmara region, Turkey Recalculated probability of M≥ 7 earthquakes beneath the Sea of Marmara, Turkey Global Omori law decay of triggered earthquakes: Large aftershocks outside the classical aftershock zone From coseismic offsets to fault-block mountains. Vertical deformation associated with normal fault systems evolved over coseismic, postseismic, and multiseismic periods Static-stress impact of the 1992 Landers earthquake sequence on nucleation and slip at the site of the 1999 M=7.1 Hector Mine earthquake, southern California Stress changes from the 2008 Wenchuan earthquake and increased hazard in the Sichuan basin Uniform California Earthquake Rupture Forecast, Version 3 (UCERF3)--The Time-Independent Model Long-Term Time-Dependent Probabilities for the Third Uniform California Earthquake Rupture Forecast (UCERF3) Significance of stress transfer in time-dependent earthquake probability calculations Prospective Earthquake Forecasts at the Himalayan Front after the 25 April 2015M 7.8 Gorkha Mainshock The stress shadow problem in physics-based aftershock forecasting: Does incorporation of secondary stress changes help? Comparative evaluation of physics-based and statistical forecasts in Northern California No correlation between Anderson Reservoir stage level and underlying Calaveras fault seismicity despite calculated differential stress increases A global search for stress shadows Distribution of tsunami interevent times Tectonic stressing in California modeled from GPS observations A hypothesis for delayed dynamic earthquake triggering Correction to “A hypothesis for delayed dynamic earthquake triggering” Triggering of tsunamigenic aftershocks from large strike-slip earthquakes: Analysis of the November 2000 New Ireland earthquake sequence New seismic images of the Cascadia subduction zone from cruise SO108 — ORWELL Post-1906 stress recovery of the San Andreas fault system calculated from three-dimensional finite element analysis Stress, Distance, Magnitude, and Clustering Influences on the Success or Failure of an Aftershock Forecast: The 2013 M 6.6 Lushan Earthquake and Other Examples Comparison of characteristic and Gutenberg-Richter models for time-dependent M ≥ 7.9 earthquake probability in the Nankai-Tokai subduction zone, Japan Earthquake recurrence on the south Hayward fault is most consistent with a time dependent, renewal process Monte Carlo method for determining earthquake recurrence parameters from short paleoseismic catalogs: Example calculations for California Probabilistic Tsunami Hazard Analysis: Multiple Sources and Global Applications The global aftershock zone Estimation of submarine mass failure probability from a sequence of deposits with age dates Global ubiquity of dynamic earthquake triggering A Synoptic View of the Third Uniform California Earthquake Rupture Forecast (UCERF3) Uniform California Earthquake Rupture Forecast, Version 2 (UCERF 2) Thank You to Our 2020 Peer Reviewers Diffuse Pacific−North American plate boundary: 1000 km of dextral shear inferred from modeling geodetic data Missing link between the Hayward and Rodgers Creek faults. Unraveling the apparent magnitude threshold of remote earthquake triggering using full wavefield surface wave simulation On near-source earthquake triggering Chapter 7 The basin and range province Probabilistic tsunami hazard assessment at Seaside, Oregon, for near- and far-field seismic sources Were Global M>=8.3 Earthquake Time Intervals Random between 1900 and 2011? Stress-based aftershock forecasts made within 24 h postmain shock: Expected north San Francisco Bay area seismicity changes after the 2014 M = 6.0 West Napa earthquake Thank You to Our 2021 Peer Reviewers

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