ライフサイエンスコーパス: earthquake

1 ted with very light seismicity (magnitude <5 earthquakes).

2 and immediate response to the 30(th) October earthquake.

3 23.7%), which was the epicenter of the main earthquake.

4 k slip exceeding 40 metres in the Tohoku-oki earthquake.

5 ismometers during the 2011 Mw 9.0 Tohoku-Oki earthquake.

6 ture extent or the amplitude of slip in this earthquake.

7 rthquakes, including the 2011 M 9 Tohoku-oki earthquake.

8 quake rose by nearly 7 centimetres after the earthquake.

9 han increased following the Great East Japan Earthquake.

10 undwater in nearby mountains released by the earthquake.

11 s associated with a Cascadia subduction zone earthquake.

12 h Napa earthquake, started to flow after the earthquake.

13 , who all experienced the 2008 Sichuan major earthquake.

14 tress were probably too small to trigger the earthquake.

15 e within one to two decades after each large earthquake.

16 atients presenting to TIO following repeated earthquake.

17 struck by a major moment magnitude (Mw) 7.8 earthquake.

18 ce of the 2011, moment magnitude 9.1, Tohoku earthquake.

19 d consumption for comparable days before the earthquake.

20 better-constrained model for the South Napa earthquake.

21 ndary is a source of destructive teleseismic earthquakes.

22 cilitate co-seismic slip along faults during earthquakes.

23 lithosphere are not required to produce mega-earthquakes.

24 power law scaling in magnitude, as found in earthquakes.

25 rturbations such as the ones following large earthquakes.

26 s and modulate the occurrence time of larger earthquakes.

27 past the seismogenic zone in previous large earthquakes.

28 ng improved probabilities of impending large earthquakes.

29 l tool to minimize the likelihood of induced earthquakes.

30 pogenic fluid injections are known to induce earthquakes.

31 sm is consistent with observations of hybrid earthquakes.

32 terials and structures, from nanocrystals to earthquakes.

33 associated with reduced dilatancy and micro-earthquakes.

34 s plausible that human activity caused these earthquakes.

35 tion about the likelihood of impending large earthquakes.

36 , accompanied by a series of magnitude M > 5 earthquakes.

37 t faults produce most of the world's largest earthquakes.

38 is more than one rupture mechanism for deep earthquakes.

39 ket crashes, insurance claims, flooding, and earthquakes.

40 as Oklahoma, face sharply rising numbers of earthquakes.

41 ting stress changes on fault planes of small earthquakes.

42 time-scale magnitude determination for great earthquakes.

43 ss field derived from neighbouring 1976-2015 earthquakes.

44 ic emissions, a laboratory-scale analogue of earthquakes.

45 ogical faults, and hence the distribution of earthquakes.

46 erseismically locked, has a history of large earthquakes (18 with Mw > 7 since 1896) and produced pea

47 Intermediate-depth earthquakes (30-300 km) have been extensively documented

48 the first three years after the Indian Ocean earthquake, 37 continuous Global Navigation Satellite Sy

49 e data, we infer that during large magnitude earthquakes a step-over along the fault zone results in

50 Uplift during the 1964 Great Alaska Earthquake abruptly created freshwater ponds on multiple

51 d at 3950 years before the present (B.P.) by earthquakes accompanied with mudflows, whereas the lands

52 r the trench observed in the 2011 Tohoku-oki earthquake and predicted the possibility of a large slip

53 The average duration between the earthquake and presentation was 13 .

54 rgettable disaster of the 9 magnitude Tohoku earthquake and quickly followed by the devastating Tsuna

55 about how much a fault can slip in a single earthquake and the seismic potential of a partially coup

56 even months before the 2011 Great East Japan Earthquake and Tsunami in a survey of older community-dw

57 om Twitter shortly before and after the 2011 earthquake and tsunami in Japan.

58 sociated with a lower risk of PTSD after the earthquake and tsunami in Tohoku, Japan, on March 11, 20

59 oser to the trench than expected, increasing earthquake and tsunami size.

60 pite the 1-hour warning interval between the earthquake and tsunami, many coastal residents lost thei

61 rs west of the epicenter 7 months before the earthquake and tsunami.

62 tly in the line of the 2011 Great East Japan Earthquake and Tsunami.

63 lowing exposure to the 2011 Great East Japan Earthquake and Tsunami.

64 ecelerating afterslip after large interplate earthquakes and as relatively steady slip on uncoupled a

65 tions are proxies for potential tsunamigenic earthquakes and benefit hazard assessment.

66 to understand the relationship between past earthquakes and Holocene vertical deformation.

67 disastrous intermittent phenomena including earthquakes and landslides.

68 ls of significant correlations between small earthquakes and ongoing low-amplitude periodic stresses

69 diverse range of sliding behavior, including earthquakes and slow-slip events, occurs along tectonic

70 lization induced fracturing that can trigger earthquakes and weathering, as well as, sequestration of

71 nking collapses) and physical systems (e.g., earthquakes), and yet it remains unclear the extent to w

72 -mortality associations before and after the earthquake, and used meta-analysis to generate combined

73 While regular earthquakes are catastrophic events with rupture velocit

74 ldspar relieves stress by aseismic creep and earthquakes are infrequent.

75 ad range of geologic environments where slow earthquakes are observed.

76 r strike-slip faults known to have had large earthquakes are silent in the interseismic period is a l

77 ayas, such as that following the 2015 Gorkha earthquake, are unlikely to drive increased gravel aggra

78 eries of tremor, slow-slip and low-frequency earthquakes, are less understood.

79 1), with the remainder living outside of the earthquake area.

80 line basement do not strongly correlate with earthquake association.

81 hopathology in survivors of the 2008 Sichuan earthquake at an individual level.

82 ndent series was interrupted by a cluster of earthquakes at approximately 430 ka.

83 Our understanding of the frequency of large earthquakes at timescales longer than instrumental and h

84 s of the fault rupture of the 2004 Parkfield earthquake based on 1 Hz GPS records only.

85 In November 2013, a series of earthquakes began along a mapped ancient fault system ne

86 aseismic slip in this experiment, with micro-earthquakes being an indirect effect mediated by aseismi

87 ng the 2013 moment magnitude (M(w)) 6.7 deep earthquake beneath the Sea of Okhotsk, an aftershock of

88 One SSE occurred several months before the earthquake, but changes in Mohr-Coulomb failure stress w

89 Here we decipher the mechanism of these earthquakes by performing deformation experiments on deh

90 With a high-resolution earthquake catalog, we observe propagating foreshocks le

91 For assessing the earthquake cause, our research underscores the necessity

92 Great earthquakes cause large coseismic crustal deformation in

93 uring the 30(th) October 2016 Mw 6.6 Vettore earthquake (Central Italy), using low-cost Global Naviga

94 iod cycles (>1 ky) punctuated by destructive earthquake clusters.

95 At about 40 days before, two earthquakes clusters started, with one M3 earthquake occ

96 he Loma Blanca fault produced periodic large earthquakes, consistent with a time-dependent model of e

97 Our results show that the November 9 earthquake could have been triggered by the October 23 s

98 ndamental to understanding the nature of the earthquake cycle and critical to determining time-depend

99 We also surveyed 491 glacier lakes for earthquake damage but found only nine landslide-impacted

100 This complex earthquake defies many conventional assumptions about th

101 scoelastic finite-element models of the post-earthquake deformation show that a thin (30-200 kilometr

102 e laboratory analogues of intermediate-depth earthquakes demonstrate that little dehydration is requi

103 In March 2011, the Great East Japan Earthquake devastated several power stations and caused

104 cted daily electricity consumption after the earthquake did not significantly modify daily heat-relat

105 ponsive satellite data acquisitions over the earthquake disaster zone, our team undertook a satellite

106 We argue that felt induced earthquakes due to geologic CO2 storage are unlikely bec

107 Implications for earthquake dynamics are discussed.

108 overcome fundamental limitations of current earthquake early-warning systems imposed by the propagat

109 r earthquake rupture physics, as well as for earthquake early-warning systems.

110 Studying small repeating earthquakes enables better understanding of fault physic

111 ic perturbations (TIDs) moving away from the earthquake epicenter at an approximate speed of 316 m/s.

112 a, reveal this to be one of the most complex earthquakes ever recorded.

113 e during the 2004 Sumatra-Andaman subduction earthquake extended closer to the trench than expected,

114 Earthquakes far from tectonic plate boundaries generally

115 Earthquake faulting at 600 km depth remains puzzling.

116 = 7.3 Landers and 1999 Mw = 7.1 Hector Mine earthquakes, finding a spatial correlation between fluct

117 the potential to help refine time-dependent earthquake forecasts.

118 ce intervals and to test competing models of earthquake frequency (e.g., time-dependent, time-indepen

119 The 2011 East Japan earthquake generated a massive tsunami that launched an

120 cate increased fault susceptibility to large earthquake generation.

121 rogeneous water release and directly impacts earthquakes generation and mantle wedge dynamics.

122 These forces are the source of glacial earthquakes, globally detectable seismic events whose pr

123 A large earthquake had been expected in the subduction zone adja

124 rs of tsunamis from the 2004 Sumatra-Andaman earthquake had increased risks of psychiatric disorders

125 Notably, these two earthquakes had a maximum slip that was very close to th

126 imit of rupture during large subduction zone earthquakes has important implications for tsunami gener

127 Many of these earthquakes have been documented as induced by wastewate

128 astewater formation pressures and monitoring earthquakes having magnitudes of approximately M2 and gr

129 re area, this has important implications for earthquake hazard assessment.

130 has important implications for understanding earthquake hazard since laws governing frictional resist

131 e and critical to determining time-dependent earthquake hazard.

132 The 2004 Sumatra-Andaman and 2011 Tohoku-Oki earthquakes highlighted gaps in our understanding of meg

133 Earthquake hypocenters occur within disposal formations

134 that the likelihood of another tsunamigenic earthquake in Aceh province is high, these variable recu

135 zones, such as the 1999 moment magnitude 7.7 earthquake in Chi-Chi, Taiwan.

136 The 25 April 2015 moment magnitude 7.8 earthquake in Gorkha, Nepal was the first large continen

137 he types of ocular injuries sustained in the earthquake in Nepal and its management in Tilganga Insti

138 r service provision in the event of a future earthquake in Nepal, or in countries, which are similarl

139 n all-cause heat-related mortality after the earthquake in the 15 prefectures with the greatest reduc

140 ion and expected to rupture in a magnitude 8 earthquake in the coming decades.

141 tural disaster (the Canterbury, New Zealand, earthquakes in 2010-2011), with the remainder living out

142 d anthropogenic, influence the occurrence of earthquakes in active tectonic settings or 'stable' plat

143 Intermediate-depth earthquakes in cold subduction zones are observed within

144 n facilitate seismic slip propagation during earthquakes in continental domains, possibly enhancing s

145 In contrast, intermediate-depth earthquakes in hot subduction zones predominantly occur

146 n of ocular trauma resulting from the recent earthquakes in Nepal has not been described thus far.

147 the two events represent end members of deep earthquakes in terms of energy partitioning and imply th

148 cations and waveform attenuation analyses of earthquakes in the Campi Flegrei area (Southern Italy) d

149 quently the potential for future destructive earthquakes in the central Gulf is greater than in the s

150 nd thus the location and style of intraplate earthquakes in the central United States with no influen

151 sent a study of the interaction of repeating earthquakes in the framework of rate-and-state fault mod

152 riction during spontaneously developing mini-earthquakes in the laboratory, enabled by our ultrahigh

153 hold magnitude between 2.7 and 3.4 for local earthquakes in the noisiest of the three environments.

154 An unprecedented increase in earthquakes in the U.S. mid-continent began in 2009.

155 sruptive ecological changes triggered by the earthquake, in the context of appropriate climatic condi

156 subduction zone forearcs indicate that slow earthquakes, including episodic tremor and slip, recur a

157 cede clusters of large [magnitude (M) >/= 5] earthquakes, including the 2011 M 9 Tohoku-oki earthquak

158 e in rocks with low compressibility triggers earthquakes, including the 4.8-moment magnitude event th

159 am undertook a satellite image survey of the earthquakes' induced geohazards in Nepal and China and a

160 Here, we reconstruct an earthquake-induced landslide dam outburst flood on the Y

161 These findings indicate that earthquake-induced sediment pulses sourced from the Grea

162 Subsequent relaxation of the earthquake-induced stresses in the viscoelastic upper ma

163 Our results suggest that the Pawnee earthquake is a result of interplay among injection, tec

164 lution of slip on surface ruptures during an earthquake is important for assessing fault displacement

165 The Pawnee M5.8 earthquake is the largest event in Oklahoma instrument r

166 Understanding the causes of intraplate earthquakes is challenging, as it requires extending pla

167 the best-preserved topographic signature of earthquakes is expected to occur early in the postseismi

168 Establishing what controls the timing of earthquakes is fundamental to understanding the nature o

169 rs increased their online activity after the earthquake, Japanese speakers, who are assumed to be mor

170 found to correlate significantly with small earthquakes, just before large earthquakes occur.

171 arth tides modulate tremor and low-frequency earthquakes (LFEs) on faults in the vicinity of the brit

172 rican Great Plains exemplify such intraplate earthquake localization, with both natural and induced s

173 Rayleigh wave phase velocities with improved earthquake locations, we find that the flat slab is shal

174 of Okhotsk, an aftershock of the large deep earthquake (M(w) 8.3).

175 A recent major earthquake (M7.8), coupled with appropriate climatic con

176 Because earthquake magnitude depends on rupture area, this has i

177 for a highly valuable rapid estimate of the earthquake magnitude.

178 The Gorkha earthquake (magnitude 7.8) on 25 April 2015 and later af

179 Our observations suggest that earthquake magnitudes cannot be predicted from the chara

180 Pre-earthquake mean maximum monthly temperature and post-ear

181 ke mean maximum monthly temperature and post-earthquake mean monthly pressure were negatively associa

182 Near-trench slip during large megathrust earthquakes (megaquakes) is an important factor in the g

183 ful for qualitatively describing where large earthquakes might occur.

184 Here we present a simple earthquake model to investigate whether correlations bet

185 y align with those observed independently in earthquake moment tensors and borehole breakouts.

186 elling results and the absence of historical earthquakes near Azle, brine production combined with wa

187 milliseconds, at any distance away from the earthquake nucleation area.

188 nes, where crustal extension and devastating earthquakes occur in response to regional surface uplift

189 The largest observed earthquakes occur on subduction interfaces and frequentl

190 Many of Earth's great earthquakes occur on thrust faults.

191 ly with small earthquakes, just before large earthquakes occur.

192 wo earthquakes clusters started, with one M3 earthquake occurred two days before the mainshock.

193 On 1 April 2014 a M 8.2 earthquake occurred within this seismic gap.

194 rthward for ~50 kilometers until the 1 April earthquake occurred.

195 100 days before the mainshock, two M >/= 3.5 earthquakes occurred along a mapped fault that is conjug

196 over decades but relating this behaviour to earthquake occurrence over centuries, given numerous pot

197 The seasonal loading analysis reveals earthquakes occurring more frequently during stress cond

198 The moment magnitude (Mw) 8.1 Iquique earthquake of 1 April 2014 broke a highly coupled portio

199 e also reveals that the destructive Wenchuan earthquake of year 2008 occurred in the upper crust, dir

200 a new kinematic interpretation of two Mw7.6 earthquakes of November 24, 2015.

201 Nepal was struck by a massive earthquake on the 25th April 2015 and major aftershock o

202 The 5 September 2012 M(w) 7.6 earthquake on the Costa Rica subduction plate boundary f

203 ur modeling implies that the 1857 Fort Tejon earthquake on the San Andreas Fault in Southern Californ

204 ed subsurface pressures sufficient to induce earthquakes on near-critically stressed faults.

205 s to large influxes of sediment triggered by earthquakes or storms.

206 malities of children with PTSD after a major earthquake, our results are consistent with the suggesti

207 Using a joint local and teleseismic earthquake P-wave seismic inversion, we revealed a basal

208 quake ruptures enhances our understanding of earthquake physics and associated ground shaking.

209 thquakes represent an important conundrum in earthquake physics.

210 agree with the recent observations of large earthquakes preceded by time periods of significant corr

211 These earthquakes predominantly occur within subduction zones,

212 uction zones of the world, showing that mega-earthquakes preferentially rupture flat (low-curvature)

213 ributions provide important insight into the earthquake process.

214 The 2011 Tohoku earthquake produced an unexpected large amount of shallo

215 Many earthquakes propagate up to the Earth's surface producin

216 ry shear apparatus at conditions relevant to earthquakes propagation.

217 tions between daily tidal stresses and small earthquakes provide information about the likelihood of

218 detect the deformation following megathrust earthquakes, providing methodological guidelines for thi

219 We find that the entire increase in earthquake rate is associated with fluid injection wells

220 dicates that, over the past 12 centuries, 10 earthquakes reaching ground-shaking intensities >/= VI g

221 nt that occurred on 17 May 2012, the largest earthquake recorded in eastern Texas.

222 ubduction zones including those with limited earthquake records.

223 of the saltmarsh, coseismic deformation and earthquake recurrence in a wide area of southern Califor

224 s are required both to better quantify their earthquake recurrence intervals and to test competing mo

225 s been limited until now, because intraplate earthquake recurrence intervals are generally long (10s

226 Long-term variations in the earthquake recurrence intervals of intraplate faults the

227 t, New Mexico, United States, that constrain earthquake recurrence intervals over much of the past ap

228 n sandsheet emplacement or that tsunamigenic earthquake recurrence may have been more frequent in the

229 s, consistent with a time-dependent model of earthquake recurrence.

230 following the 1999 Chi-Chi and 2008 Wenchuan earthquakes reduced channel capacity and increased flood

231 Characterizing the burden of earthquake-related ocular trauma will facilitate plannin

232 Slow earthquakes represent an important conundrum in earthqua

233 ku-oki earthquake, this result for the Maule earthquake represents only the second time that repeated

234 ng economic and humanitarian impact of large earthquakes requires signals for forecasting seismic eve

235 ence of up to about 4 centimetres during the earthquake rose by nearly 7 centimetres after the earthq

236 lastic relaxation of stresses induced by the earthquake rupture and continuing slip (afterslip) or re

237 pronounced rotation in one direction as the earthquake rupture approaches the free surface, and this

238 c synthetic aperture radar data to model the earthquake rupture as a slip pulse ~20 kilometers in wid

239 tal relationship between fault structure and earthquake rupture behavior, allowing for modeling of re

240 ctional-mechanical processes associated with earthquake rupture cycles, but there are few temperature

241 Here we use earthquake rupture experiments to reveal the existence o

242 Whether the earthquake rupture extended to the shallow part of the p

243 behavior of megathrust events is crucial for earthquake rupture physics, as well as for earthquake ea

244 ighlighted gaps in our understanding of mega-earthquake rupture processes and the factors controlling

245 Earthquake rupture speeds exceeding the shear-wave veloc

246 During the earthquake rupture, a signal exceeding the background no

247 expected to occur at all distances during an earthquake rupture, even before the arrival of seismic w

248 -resolution constraints on the kinematics of earthquake rupture, which have challenged prior knowledg

249 equently during stress conditions that favor earthquake rupture.

250 The earthquake ruptured conjugate faults down to great depth

251 tional assumptions about the degree to which earthquake ruptures are controlled by fault segmentation

252 Detailed geodetic imaging of earthquake ruptures enhances our understanding of earthq

253 Using numerous M9 earthquake scenarios, we demonstrate that incorporating

254 ution is one of the biggest uncertainties in earthquake science.

255 Here we use joint active-source/local-earthquake seismic tomography to derive unprecedented co

256 der development could open new directions in earthquake seismology, and overcome fundamental limitati

257 the shallow water table before or during the earthquake sequence.

258 both realistic seismic events and long-term earthquake sequences.

259 g for climatic and socioeconomic conditions, earthquake severity was associated with incident ZIKV ca

260 hile, which had not ruptured in a megathrust earthquake since a M approximately 8.8 event in 1877.

261 f active seismic zones, similar to other M5+ earthquakes since 2011.

262 distribution, which varies both with depth, earthquake size and whether the rupture breaks the surfa

263 ear-lithostatic pore-fluid pressures in slow-earthquake source regions; however, direct evidence of f

264 in physically-based predictive models of the earthquake source.

265 er time and noticeably includes a cluster of earthquakes spread over a century at the end of the Clas

266 nearly dry before the 2014 Mw6.0 South Napa earthquake, started to flow after the earthquake.

267 The serendipitous recording of an earthquake swarm near the Indian Ocean triple junction e

268 ) are much more likely to be associated with earthquakes than lower-rate wells.

269 Ocean Tsunami (IOT) emanated from an Mw 9.2 earthquake that generated a 1600 km-long rupture along t

270 rupture, and indicate that this was not the earthquake that had been anticipated.

271 The Mw 8.8 megathrust earthquake that occurred on 27 February 2010 offshore th

272 ransient deformation in the aftermath of the earthquake that was recorded by continuous geodetic stat

273 ists no method to validate these results for earthquakes that have not yet occurred.

274 nship due to stress transfer between the two earthquakes that hit the province of Van, Eastern Turkey

275 After an earthquake, the earliest deformation signals are not exp

276 In the short time since the earthquake, the phenotypes of resident freshwater threes

277 the highly dissipative 1994 M(w) 8.3 Bolivia earthquake, the two events represent end members of deep

278 Besides impacting objects and earthquakes, the method could help in identifying the lo

279 After the Mw 9.0 Tohoku-oki earthquake, this result for the Maule earthquake represe

280 and can extend up to the trench during great earthquakes through a torquing mechanism.

281 rge (moment magnitude 8.6) 2012 Indian Ocean earthquake to constrain the stratification of water cont

282 e second giant (moment magnitude Mw >/= 9.0) earthquake to occur in the last 50 years and is the most

283 rge (moment magnitude 8.6) 2012 Indian Ocean earthquake to provide by far the most direct constraint

284 One would expect small earthquakes to occur at least at the bottom of the seism

285 pressure data required to unequivocally link earthquakes to wastewater injection are rarely accessibl

286 eismic creep dominates the interaction, with earthquake triggering occurring at distances much larger

287 field of the 24 August 2014 M6.0 South Napa earthquake using SAR data from the Italian Space Agency'

288 There were 59 cases of earthquake victims visiting TIO, Gaushala, Kathmandu fro

289 The March 2011 Tohoku-oki earthquake was only the second giant (moment magnitude M

290 founding factors, exposure to the Canterbury earthquakes was associated with a small to moderate incr

291 Following the earthquake we repeatedly surveyed the new flows, collect

292 akening mechanisms thought to operate during earthquakes, we propose an empirical velocity-weakening

293 validated using field observations of recent earthquakes, where we were able to calculate the eruptio

294 Deep earthquakes, which are spatially correlated with geochem

295 ears, so it is likely that future megathrust earthquakes will occur to the south and potentially to t

296 of interseismic creep, has not generated an earthquake with MJ > 7 (local magnitude estimated by the

297 ats can record between 35 and 63% of distant earthquakes with a moment magnitude M>/=6.5.

298 ntified large early aftershocks triggered by earthquakes with magnitudes between >/=7 and 8 within a

299 function (STF) data sets for subduction zone earthquakes, with moment magnitude Mw >/= 7, and show th

300 del slab that is nearly vertical in the deep-earthquake zone but stagnant below 660 km, consistent wi