ライフサイエンスコーパス: fault

1 ss transfer and critical stress state of the fault.

2 per kilometre within the hanging wall of the fault.

3 rities embedded within an otherwise aseismic fault.

4 eration in a lake located within 2 km of the fault.

5 try based on the cross section of the Tohoku fault.

6 s on the creeping section of the San Andreas Fault.

7 quare site adjacent to a subsurface stacking fault.

8 es with respect to the subduction megathrust fault.

9 ty induced by fluid injection into a natural fault.

10 association to any twin boundary or stacking fault.

11 slip) or relocking of different parts of the fault.

12 stacking, to serve as a nucleus of stacking fault.

13 ped fault that is conjugate to the mainshock fault.

14 icline along the proposed controlling normal fault.

15 eismic studies of fast-moving plate-boundary faults.

16 and landscape development at plate-bounding faults.

17 of Earth's great earthquakes occur on thrust faults.

18 withdrawal triggers collapse along bounding faults.

19 and slow-slip events, occurs along tectonic faults.

20 trol the spatial and temporal development of faults.

21 usly over large areas, than on highly curved faults.

22 al dislocation in between these two stacking faults.

23 tion across partially coupled plate-boundary faults.

24 uid pressure data from active plate-bounding faults.

25 f a tetrahedron bounding triangular stacking faults.

26 duce earthquakes on near-critically stressed faults.

27 ow slip has been reported, including seismic faults.

28 ca fault and, by inference, other intraplate faults.

29 emporal variations in the mechanical work of faulting.

30 e-varying deformation associated with normal faulting.

31 mate the ground velocity (~1.2 m/s) near the fault, 2) that GPS waveforms inversions constrain that t

32 The ring fault accommodated deflation during the eruption and pro

33 are much lower, and activity shifts between faults across strike.

34 It ruptured a previously unmapped fault and triggered aftershocks along a complex conjugat

35 ong-term seismic behavior of the Loma Blanca fault and, by inference, other intraplate faults.

36 ~4 billion years old that are extensionally faulted and extensively mantled and perhaps eroded by gl

37 th's crust deform by distributed extensional faulting and complex fault interactions are often observ

38 Using quantitative models of faulting and magma emplacement, we demonstrate that, in

39 rain is accommodated by repeated episodes of faulting and magmatism.

40 eld surveys are consistent with dike-induced faulting and not with faults soling into an active detac

41 s in the LNO precursor material (2D stacking faults and 3D inclusions) for determining the reaction p

42 d, structural pattern of the bedrock through faults and joints appears to be the primary control on l

43 in rural areas, those with litter, drainage faults and pets or other animals outdoors tended to have

44 hts can vary by means of SbTe-based stacking faults and using a vacancy-mediated kink motion, and als

45 y capability with strong tolerances to input faults and variations, which shows the feasibility of us

46 esult of interplay among injection, tectonic faults, and foreshocks.

47 deformation and mineralization on geological faults, and hence the distribution of earthquakes.

48 equential, oceanward-younging, upper crustal faults, and is balanced through lower crustal flow.

49 ed on the ability to self-insulate breakdown faults, and we enhance fundamental understanding of the

50 t mappings reveal that the Ruddlesden-Popper faults are Ba-O layer terminated, and two kinds of kink

51 poorly understood as shallow parts of thrust faults are considered to be frictionally stable.

52 Although the physical properties of these faults are difficult to observe directly, their friction

53 such that annealing takes place and stacking faults are eliminated from the core.

54 ploit ancient faults, but not all intraplate faults are equally active.

55 ng the surrounding groundwater since natural faults are likely to be a preferential migration pathway

56 lectron microscopy reveals that these planar faults are precursors of directional amorphization.

57 Longer paleoseismic records for intraplate faults are required both to better quantify their earthq

58 ince laws governing frictional resistance of faults are vital ingredients in physically-based predict

59 depth on a surface rupturing (i.e. capable) fault array, as a direct and immediate response to the 3

60 be accommodated by <30% of the across-strike fault array.

61 ents may also reveal polytypism and stacking fault, as supported by first principles calculations and

62 e's three rings and suggests the presence of faults associated with the outer two that penetrate to t

63 strain accumulation on the southern Wasatch Fault at c. 0.5 mm yr(-1) tensile dislocation opening in

64 Earthquake faulting at 600 km depth remains puzzling.

65 erved in the final products, due to stacking faults at the boundary between newly deposited and resid

66 70 kilometers along both mapped and unmapped faults before continuing offshore at the island's northe

67 his conclusion with numerical simulations of fault behavior and observations of recent major events.

68 ormation, including the 8-meter uplift of a fault-bounded block.

69 and delta front, depth, and location within fault-bounded zones of the region.

70 nced by the presence of basal-plane stacking faults (BSFs).

71 Shear heating may occur within the fault but is not required to explain our observations.

72 c plate boundaries generally exploit ancient faults, but not all intraplate faults are equally active

73 challenged prior knowledge about how much a fault can slip in a single earthquake and the seismic po

74 n continental domains, co-seismic slip along faults can propagate up to the Earth's surface is still

75 h belt, with evidence of near-surface thrust faults caused by convergence between Eastern Tibet and t

76 ntle serpentinites rise through lithospheric faults caused by incipient rifting and the collapse of t

77 We propose as a physical explanation that fault complexity induces a heterogeneous stress state th

78 individual layers, and SbTe bilayer stacking faults connecting one block to an adjacent block which a

79 thymetry in a region they highlight as being fault controlled, however, shows strong evidence for a s

80 Fault-controlled localization of magma constrains potent

81 results in high density nanotwins, stacking fault, dislocation around the CNT/metal interface.

82 l defects such as grain boundaries, stacking faults, dislocations, and point defects, as well as to p

83 ing an earthquake is important for assessing fault displacement, defining seismic hazard and for pred

84 Rupture fronts can cause fault displacement, reaching speeds up to several ms(-1)

85 The earthquake ruptured conjugate faults down to great depths, compatible with dry olivine

86 on system by plate convergence; lithospheric faults driving margin segmentation act as windows throug

87 5 and 1813 CE were displaced by the Polochic fault during a long period of seismic quiescence, from 1

88 Displacement on the Polochic fault during at least the last 480 years included a comp

89 licates can facilitate co-seismic slip along faults during earthquakes.

90 hat were juxtaposed by several cross-cutting faults during peak-ring formation.

91 r and other metals exhibiting small stacking fault energies and/or large elastic anisotropy, which in

92 And both intrinsic and extrinsic stacking fault energies in the vicinity Al layers are negligibly

93 ation mechanism in metals with high stacking fault energies.

94 lling suggests that it has negative stacking-fault energy at 0K and high propensity for twinning.

95 ling an effective bypassing of the high twin-fault energy barrier.

96 in face-centered cubic metals with high twin-fault energy barriers, such as Al, Ni, and Pt, but inste

97 First principle generalized stacking fault energy calculations revealed an intrinsic stacking

98 tomic-scale deformation and general stacking fault energy landscapes, it is unequivocally demonstrate

99 t prior studies have focused on low stacking-fault energy nanotwinned metals with coherent twin bound

100 o ~5-8 nm near the edge, yielding a stacking fault energy of 30 +/- 5 mJ/m(2).

101 The generalized stacking fault energy surfaces associated with shearing on nine d

102 common features of the generalized stacking fault energy surfaces of hcp pyramidal planes and is thu

103 undary-dominated plasticity in high stacking-fault energy twinned metals.

104 nt void swelling in metals with low stacking fault energy.

105 a full dislocations due to its high stacking fault energy.

106 uminium simply because of its giant stacking fault energy.

107 ely little or no uplift of the mountainside (fault footwall).

108 ls demonstrate, in unprecedented detail, how faults formed in the earliest phases of continental exte

109 by diagenetic strengthening of deeply buried fault-forming sediments, contrasting with weakening prop

110 A synthetic, fault-free gmelinite (GME) zeolite is prepared using a s

111 updip of the rupture zone; our knowledge of fault friction based on these estimates therefore needs

112 ium melting induced via rapid heating during fault friction experiments, demonstrating that friction

113 ing of fault physics and characterization of fault friction properties.

114 by frictional dynamics via the interplay of fault frictional properties, effective normal stress and

115 perity contacts causing a large reduction in fault frictional strength (i.e., flash weakening).

116 production and wastewater injection near the fault generated subsurface pressures sufficient to induc

117 preceded by planar defects such as stacking faults generated by partial dislocations.

118 I argue that abyssal hills are primarily fault-generated rather than volcanically generated featu

119 ty correlates to the spatial distribution of fault geometrical complexity, explaining why Hector Mine

120 reading rate is best explained by a model of fault growth and abandonment under a steady magma input.

121 predominantly subsidence of the basin side (fault hanging wall), with comparatively little or no upl

122 of bilayer complexion stabilized at stacking faults has also been identified.

123 sliver, although a system of active crustal faults has been described in central Costa Rica.

124 Similar study of intraplate faults has been limited until now, because intraplate ea

125 he Sevier Desert Detachment low-angle normal fault, have been debated for nearly four decades.

126 lattice distortions of the Ruddlesden-Popper faults illustrates that the local lattice spacing poses

127 857 Fort Tejon earthquake on the San Andreas Fault in Southern California penetrated below the seismo

128 g a carbonate-hosted seismogenic extensional fault in the central Apennines, Italy.

129 The nature of faulting in the Sevier Desert, located in eastern Basin

130 es that subduction zone megathrusts are weak faults in a low-stress environment.

131 Grave faults in design and conduct of clinical trials have als

132 ty and the presence of long segment stacking faults in gamma phase.

133 from the gamma' to eta phase along stacking faults in gamma' precipitates, which would normally be t

134 d respect a safe distance from major natural faults in the bedrock when planning the localization of

135 s this challenge for an array of seismogenic faults in the central Italian Apennines, where crustal e

136 ction plays a key role in how ruptures unzip faults in the Earth's crust and release waves that cause

137 etwork that lead to cancer are abstracted as faults in the equivalent circuit and the Boolean circuit

138 is shows high densities of Ruddlesden-Popper faults in the film, which are on {100} planes with trans

139 e strains exist around the Ruddlesden-Popper faults in the film.

140 ings that are domain boundaries and stacking faults in the growing ice layers, which lead to the form

141 undwater chemistry and distance to the major faults in the studied area.

142 emor and low-frequency earthquakes (LFEs) on faults in the vicinity of the brittle-ductile (seismic-a

143 in ribosome biogenesis may result in varied faults in translation of mRNAs causing cellular toxiciti

144 eal surface ruptures along at least 12 major faults, including possible slip along the southern Hikur

145 We find stacking faults, inherent to the highly two-dimensional nature of

146 mplex architecture of rifted margins through fault interaction processes, hereby creating the widely

147 distributed extensional faulting and complex fault interactions are often observed.

148 n, which explains the presence of the normal faults interpreted in 3-D seismic profiles collected fro

149 ructure that inhibits thickening of stacking faults into twins, leading to significant improvement in

150 These angles indicate that the megathrust fault is not substantially weaker than its surroundings.

151 Goff comments that faulting is important for creation of abyssal hills and

152 We respond that faulting is indeed important but cannot alone explain th

153 Seismicity along continental transform faults is usually confined to the upper half of the crus

154 calculations revealed an intrinsic stacking fault (ISF) along 112{111}, which is the partial disloca

155 Why many major strike-slip faults known to have had large earthquakes are silent in

156 rtially relieved by the creation of stacking fault layers near the twin boundaries.

157 h magnitudes between >/=7 and 8 within a few fault lengths (approximately 300 kilometers), during tim

158 g rise to a pattern of coherent and stacking-fault-like regions at the interface.

159 icating effective pasteurization, mechanical faults likely to lead to incomplete pasteurization of pa

160 generally limited due to fragmentation along fault lines during chemical oxidation and exfoliation in

161 s of up to 2.5-fold enrichment situated near fault lines in the genome associated with mobile element

162 mic slip propagation is facilitated by along-fault low dynamic frictional resistance, which is contro

163 types of seeds with twin defects or stacking faults, making it an exciting time to design and synthes

164 rincipally a strike-slip plate boundary, the faulted margins of the Gulf display largely dip-slip ext

165 integrating laboratory-derived properties of fault materials and simulations of fault weakening and r

166 ed with a single model adapted from standard fault mechanics treatments.

167 boundaries, and mainshocks with all types of faulting-mechanisms (normal, reverse, and strike-slip) c

168 rthquakes in the framework of rate-and-state fault models using state-of-the-art simulation methods t

169 me hydrothermal conditions result from rapid fault movement, which transports rock and heat from dept

170 At-fault MVC involvement over the 5 years before enrollment

171 At-fault MVC involvement over the 5 years before enrollment

172 coma are more likely to have a history of at-fault MVC involvement than those without glaucoma.

173 s to have an independent association with at-fault MVC involvement, whereas visual acuity and CS impa

174 l faults that closely replicate the observed fault networks on Pluto.

175 re-activation and complex linkages of prior fault networks.

176 half of the crust, but the Newport-Inglewood fault (NIF), a major fault traversing the Los Angeles ba

177 d overpressure development and low effective fault-normal stress, and therefore shorter recurrence ti

178 trench observations of slip on the Polochic fault (North America-Caribbean plate boundary) with a 12

179 On-fault observations within 7 km of the lake show that soi

180 Experimentally produced faults, observed post-mortem, are sealed by fluid-bearin

181 a personal recollection (with all the known faults of self-reporting and retrospective memory) of th

182 the semi-molten morphology and the stacking faults of the primary M7C3 carbide are observed by scann

183 lly, after millions of years and hundreds of fault offsets, the mountain blocks display large uplift

184 o have been accommodated by low-angle normal faulting on the Sevier Desert Detachment and is instead

185 purities tended to segregate at the stacking faults or twinned boundaries.

186 artials, their interactions to form stacking-fault parallelepipeds, and arrest at planar slip bands o

187 of the seismic rupture in carbonate-bearing fault patches.

188 earthquakes enables better understanding of fault physics and characterization of fault friction pro

189 nt ruptured downward along a steeply dipping fault plane at an average speed of 8 kilometers per seco

190 A ramp/flat fault plane can introduce an anticline with bends on bot

191 ine with bends on both limbs, while a smooth fault plane will develop a roll-over anticline with a be

192 controlled by the geometry of the underlying fault-plane.

193 loading and the resulting stress changes on fault planes of small earthquakes.

194 Subduction zone megathrust faults produce most of the world's largest earthquakes.

195 emonstrate that for >400 ka, the Loma Blanca fault produced periodic large earthquakes, consistent wi

196 te that strain is highly localized along the fault (R1 and B shears), and that the fault surface deve

197 seismicity were induced, CO2 leakage through fault reactivation would be unlikely because the high cl

198 plate boundary) with a 1200 years-long 'near-fault' record of seismo-turbidite generation in a lake l

199 An alternative explanation suggests a normal fault-related fold under extensive stress.

200 asin and Range of central Utah, and how this faulting relates to the Sevier Desert Detachment low-ang

201 centuries, given numerous potentially active faults, remains a global problem in hazard assessment.

202 ore architecture and the absence of stacking faults, respectively.

203 ed materials is known as rotational stacking fault (RSF), but the coexistence of multiple RSFs with d

204 Plate-boundary fault rupture during the 2004 Sumatra-Andaman subduction

205 of finite-source parameter inversions of the fault rupture of the 2004 Parkfield earthquake based on

206 e provided insights, but the physics of slow fault rupture remain enigmatic.

207 neated the right-lateral shear motion of the fault rupture with a maximum surface displacement of app

208 Observed fault-rupture geometry, demonstrated likelihood of seism

209 existence of a torquing mechanism of thrust fault ruptures near the free surface that causes them to

210 sing the retrieved 3D maps helps clarify the fault's nature and thus characterize its behaviour.

211 isplacement of approximately 45 cm along the fault's strike, showing the east and north components of

212 which earthquake ruptures are controlled by fault segmentation and should motivate reevaluation of t

213 uch deeper ruptures may occur on other major fault segments, potentially increasing the associated se

214 tiated through the formation of two stacking faults separated by a single atomic layer, and proceeded

215 of 45 approximately 50 GPa, multiple planar faults, slightly deviated from maximum shear direction,

216 ast to similar tests on antigorite, unstable fault slip (that is, stick-slip) occurred during dehydra

217 We directly measure fault slip and seismicity induced by fluid injection int

218 The range of fault slip behaviors near the trench at subduction plate

219 Fault slip distributions provide important insight into

220 wave speed, the processes that underlie slow fault slip phenomena, including recent discoveries of tr

221 d by positive feedbacks between processes of fault slip, rock fracturing and alteration, and landscap

222 We constrain fault slip-rates since 18 ka using variations in cosmog

223 sonite dehydration reaction induces unstable fault slip.

224 tent with dike-induced faulting and not with faults soling into an active detachment.

225 ment of the left-lateral strike-slip Haiyuan fault south of the northern Qilian suture.

226 ing experimentally determined parameters and fault-specific details into the model may provide new to

227 It is shown that at such interfaces, a faulted stacking structure is energetically preferred on

228 ies otherwise inaccessible information about fault strength and rheology.

229 slip initiated when stress exceeds the local fault strength.

230 ess at the studied wellbore is in the normal faulting stress regime within the Tarim Basin rather tha

231 detail the fundamental relationship between fault structure and earthquake rupture behavior, allowin

232 ons of the slip distribution and geometrical fault structure.

233 rmine the surface roughness and formation of faulted structure, which in turn affect the mechanical d

234 es twist GB is characterized with a stacking faulted structure.

235 s can be extended to any subduction zone and faulting style.

236 ng the fault (R1 and B shears), and that the fault surface develops slickensides (very smooth fault s

237 t surface develops slickensides (very smooth fault surfaces polished by frictional sliding).

238 plitude periodic stresses indicate increased fault susceptibility to large earthquake generation.

239 boundary is marked by a dextral strike-slip fault system active since Late Pleistocene time.

240 se foreshock activities within the conjugate fault system are near-instantaneously responding to vari

241 of earthquakes began along a mapped ancient fault system near Azle, Texas.

242 Here we propose that the Haciendas-Chiripa fault system serves as the northeastern boundary for the

243 Bove fault system, close to new surface ruptures.

244 on as it occurred on a geometrically simpler fault system.

245 ggered aftershocks along a complex conjugate fault system.

246 akes along the Newport-Inglewood/Rose Canyon fault system.

247 Both vacancy-type stacking fault tetrahedra (SFT) and interstitial loops coexist in

248 Stacking fault tetrahedra (SFTs) are ubiquitous defects in face-c

249 >/= 3.5 earthquakes occurred along a mapped fault that is conjugate to the mainshock fault.

250 resulting in a global network of extensional faults that closely replicate the observed fault network

251 basin's outer rings, which are large normal faults that formed at different times during the collaps

252 arthquake recurrence intervals of intraplate faults therefore are poorly understood.

253 cord of seismic frequency documented for any fault to date.

254 dination of these actions must occur without fault to prevent fatal blockages of the airway.

255 We predict gate fidelities within fault-tolerance thresholds using realistic noise models.

256 When combined with fault-tolerance, our approach becomes a general-purpose

257 structure and circuit simulation is stable, fault tolerant and efficient, which is a useful compleme

258 educed resource cost over other well-studied fault-tolerant architectures by using a new method, know

259 that overcome these shortcomings: we achieve fault-tolerant behavior based on the ability to self-ins

260 d by noise from multiplying and spreading, a fault-tolerant computational architecture is required.

261 To be compatible with universal fault-tolerant computations, it is essential that states

262 te the wide applicability of our responsive, fault-tolerant films by using our system for adjustable

263 tate by quantum phase transition may promise fault-tolerant light transport in optical communications

264 tions between redundantly encoded qubits for fault-tolerant quantum computation and communication.

265 al opens the prospect to realize large-scale fault-tolerant quantum computation within a single Paul

266 hat have been proposed as building blocks of fault-tolerant quantum computers.

267 parafermions, which may find applications in fault-tolerant quantum computing.

268 tum systems is a fundamental requirement for fault-tolerant quantum computing.

269 e noisy and error-prone, they will depend on fault-tolerant quantum error correction (FTQEC) to compu

270 ng block towards larger lattices amenable to fault-tolerant quantum error correction architectures su

271 to be reduced below the levels required for fault-tolerant quantum error correction, which is an ess

272 ized via a linear array of qubits, a general fault-tolerant quantum error-correcting code requires ex

273 of noise and mark an important step towards fault-tolerant quantum information processing.

274 ems supposedly approaching the threshold for fault-tolerant quantum information processing.

275 in recent years as a promising candidate for fault-tolerant quantum information processing.

276 lues, the random control sequence is robust, fault-tolerant, and insensitive to pulse strength deviat

277 t the Newport-Inglewood fault (NIF), a major fault traversing the Los Angeles basin, is seismically a

278 We combine 'on-fault' trench observations of slip on the Polochic fault

279 The (36)Cl data reveal that individual faults typically accumulate meters of displacement relat

280 nfer seismicity during this interval records fault-valve behavior.

281 compressive force introduced by a ramp/flat fault was suggested as its origin of formation; however,

282 7)O environments, the percentage of stacking faults was found to be ca. 10%.

283 erties of fault materials and simulations of fault weakening and rupture propagation.

284 red fluid at the Nankai Trough restrains the fault weakening.

285 High densities of dislocations and stacking faults were also observed in the parent metals close to

286 le drilled into the upper part of the Alpine Fault, which is late in its cycle of stress accumulation

287 n focuses along lithosphere-scale detachment faults, which migrate oceanwards through re-activation a

288 atic depth-dependence of slip along a thrust fault with a number of 2D dynamic simulations using stoc

289 of kink structures at the Ruddlesden-Popper faults with different element distributions are also dem

290 ctivation of an outward-dipping caldera ring fault, with strong tidal triggering indicating a critica

291 on were ascribed to the presence of stacking faults within the Li2MnO3 structure.

292 bution of lattice disorder (such as stacking faults) within the CdSe core particles.

293 numerical models of slip stabilization under fault zone dilatancy strengthening caused by decreasing

294 of seismic asperities embedded in a ductile fault zone matrix.

295 magnitude earthquakes a step-over along the fault zone results in the vertical displacement of an ap

296 the PCC fissure zone with the Liquine-Ofqui Fault zone was likely an influential factor that impeded

297 approximately 30-year gap in a narrow, deep fault zone, fully consistent with the stress field deriv

298 g of calcite veins in the Loma Blanca normal fault zone, Rio Grande rift, New Mexico, United States,

299 ontal stress orientations of the El Salvador Fault Zone.

300 ) aseismic uplift symmetrically spanning the fault zone.