about
Cohesive zone length of metagabbro at supershear rupture velocity.Scale dependence of rock friction at high work rate.Estimation of fault strength: reconstruction of stress before the 1995 Kobe earthquake.The Nankai Trough earthquake tsunamis in Korea: numerical studies of the 1707 Hoei earthquake and physics-based scenariosConstraint of fault parameters inferred from nonplanar fault modelingSelectivity of spontaneous rupture propagation on a branched faultVoids and Rock Friction at Subseismic Slip VelocitySlip-Deficit Rate Distribution Along the Nankai Trough, Southwest Japan, With Elastic Lithosphere and Viscoelastic AsthenosphereRupture preparation process controlled by surface roughness on meter-scale laboratory faultSpatiotemporal complexity of 2-D rupture nucleation process observed by direct monitoring during large-scale biaxial rock friction experimentsVoids and Rock Friction at Subseismic Slip VelocitySlip-weakening distance and energy budget inferred from near-fault ground deformation during the 2016 Mw 7.8 Kaikōura earthquakeNear-fault deformation and Dc″ during the 2016 Mw 7.1 Kumamoto earthquakeNear-field tsunami forecast system based on near real-time seismic moment tensor estimation in the regions of Indonesia, the Philippines, and ChileSimple Crack Models Explain Deformation Induced by Subduction Zone Megathrust EarthquakesStress rotations due to the M 6.5 foreshock and M 7.3 main shock in the 2016 Kumamoto, SW Japan, earthquake sequenceUnusual stress rotations within the Philippines possibly caused by slip heterogeneity along the Philippine faultDynamic Overshoot Near Trench Caused by Large Asperity Break at DepthDynamic faulting on a conjugate fault system detected by near-fault tilt measurementsDynamic rupture activation of backthrust fault branchingStick–slip behavior of Indian gabbro as studied using a NIED large-scale biaxial friction apparatusPhysics-Based 3-D Simulation for Earthquake Generation Cycles at Plate Interfaces in Subduction ZonesProbing the slip-weakening mechanism of earthquakes with electrical conductivity: Rapid transition from asperity contact to gouge comminutionHigh-frequency source radiation during the 2011 Tohoku-Oki earthquake, Japan, inferred from KiK-net strong-motion seismogramsPreface for “Earthquake Hazard Evaluation”Subparallel Dipping Faults that Ruptured during the 2008 Wenchuan EarthquakeThe effect of thermal pressurization on dynamic fault branchingStrong localized asperity of the 2011 Tohoku-Oki earthquake, JapanA new BIEM for rupture dynamics in half-space and its application to the 2008 Iwate-Miyagi Nairiku earthquakeDynamic rupture scenarios of anticipated Nankai-Tonankai earthquakes, southwest JapanConstitutive parameters for earthquake rupture dynamics based on high-velocity friction tests with variable sliprateLaboratory measurements of rock friction at subseismic slip velocitiesReexamination of the present stress state of the Atera fault system, central Japan, based on the calibrated crustal stress data of hydraulic fracturing tests obtained by measuring the tensile strength of rocksA Physics-Based Simulation of the 2003 Tokachi-oki, Japan, Earthquake to Predict Strong Ground MotionsDependence of slip weakening distance (Dc) on final slip during dynamic rupture of earthquakesChapter 10 Dynamic Rupture Propagation of the 1995 Kobe, Japan, EarthquakeFault Heals Rapidly after Dynamic WeakeningHigh-velocity frictional behavior and microstructure evolution of fault gouge obtained from Nojima fault, southwest JapanChapter 1 IntroductionPreface
P50
Q30363758-2430C820-9F10-4EE5-8D37-B5761ACB1CD6Q41950017-62B5D4ED-0BA5-48BF-877B-4386850B6FECQ42028747-B9D9C435-CBE4-412B-8EBA-B2978CE175E6Q57660486-75C62A05-0293-46FB-B2D8-AA243C95EF25Q57716514-E189BE44-55E4-421E-9181-529C25527327Q57716520-4AD6BBE0-9A73-4F91-9FE3-5C050B9D3F46Q57868931-D672FB84-DD61-4716-80CC-BB0B4A027E87Q57868938-3139D726-E0F5-4156-A225-6DA1E4690B16Q57868946-1C06A68C-5CCC-42C2-9342-F3DD6ED3BCA7Q57868953-749121FA-1E2C-4BBF-A30F-4A51A7B40452Q57868959-DF9A985F-FB07-4203-97EA-DF5191B1C771Q57868966-D059E06A-BEBF-456C-9F46-27C29169103AQ57868970-7891E498-8233-495B-9123-BE0F8CA5E7B7Q57868980-028F2C90-7A6E-4C19-81F0-FE6A882184D5Q57868987-8E3085FF-36F5-4912-8621-359C8AC64BFBQ57868995-FDE165CB-1E79-4B63-92AF-A994C65DED92Q57868999-B50BB372-01F9-42EC-A95D-F8A737306CF2Q57869006-B56E59E3-38C7-44CF-88CD-39CF01FF06E6Q57869014-B0F8DAA5-7AE0-4B1C-8E05-E3B754011CB1Q57869020-8A968398-F903-4148-B2C6-7F4B8D5F86DCQ57869025-DF59C4E2-D33A-40D5-A440-21B0CE25A273Q57869032-D145AB6C-DEFE-4D31-B182-3BF1C88F32C6Q57869036-05266C19-86FA-41FC-A9D1-2C47C7E41753Q57869041-E34882FB-CAA7-49EB-86FE-981EFB6D7E0EQ57869045-4D3B8681-0B97-4B1A-8913-89DECC1139AAQ57869051-EA56E63D-E1D9-4369-BAA0-A47BDF7E7E22Q57869056-95900401-E15C-4398-9472-8275DE635088Q57869063-6A831997-6363-4E3E-B590-5424E4B68C1AQ57869069-4DFAC232-C827-466D-81EB-337EBCF156B5Q57869075-B57C0A48-6F2F-4751-9651-5BDB363E1329Q57869081-FC0D7CE5-8699-44AF-9A4A-02CB673CB7B1Q57869087-B88CA29D-42A1-4121-AB56-528CAC71BB4FQ57869097-C92C79DC-2865-4DDC-B03F-0D7A724A7CA6Q57869102-0A4FFE35-5F01-40F2-B753-546021A703FEQ57869107-01050438-FAAA-4F7B-AEEB-185E12998DF1Q57869113-1187BADF-D0EF-4285-8D39-938AEF6689F2Q57869120-826DB4E1-D9A2-4E59-A8B1-988B964CC356Q57869124-D9DC4833-65C4-49D5-AF2A-1E9BF43606E7Q57869131-2BE7A470-290A-408C-BBB4-CF30B605A0EEQ57869136-A1A2EEC2-E861-42F2-954A-3171C955D1AF
P50
description
Forscher
@de
Japans onderzoeker
@nl
chercheur
@fr
investigador
@es
researcher
@en
ricercatore
@it
հետազոտող
@hy
研究者
@zh
name
Eiichi Fukuyama
@ast
Eiichi Fukuyama
@de
Eiichi Fukuyama
@en
Eiichi Fukuyama
@es
Eiichi Fukuyama
@fr
Eiichi Fukuyama
@nl
type
label
Eiichi Fukuyama
@ast
Eiichi Fukuyama
@de
Eiichi Fukuyama
@en
Eiichi Fukuyama
@es
Eiichi Fukuyama
@fr
Eiichi Fukuyama
@nl
prefLabel
Eiichi Fukuyama
@ast
Eiichi Fukuyama
@de
Eiichi Fukuyama
@en
Eiichi Fukuyama
@es
Eiichi Fukuyama
@fr
Eiichi Fukuyama
@nl
P214
P244
P269
P106
P1556
fukuyama.eiichi
P21
P213
0000 0000 4116 9137
P214
P244
no2001022092
P269
P27
P31
P496
0000-0002-9405-9155
P734
P735
P7859
lccn-no2001022092