ライフサイエンスコーパス: slip

1 altic Siberian Traps large igneous province (SLIP).

2 unt for the elastic response to gradients in slip.

3 ion of extreme tsunami-producing near-trench slip.

4 ther sequence is sufficient to eliminate the slip.

5 dehydration reaction induces unstable fault slip.

6 ed by static stress changes due to coseismic slip.

7 tress state that in turn controls co-seismic slip.

8 es, such as water repellency and interfacial slip.

9 rongly on the anisotropy in crystallographic slip.

10 ntain a fixed statistical confidence against slip.

11 od of ice-sheet uplift and/or enhanced basal slip.

12 thought to favour twinning over dislocation slip.

13 and the energy barriers to dislocation cross-slip.

14 l of VOR adaption be expanded beyond retinal slip.

15 lastic instability by source-limited crystal slip.

16 suggesting existence of precursory aseismic slip.

17 y by decreasing stride length and increasing slipping.

18 of permeability, which transitions to faster slip (~10 mum/s) associated with reduced dilatancy and m

19 he case of silicate-bearing rocks the abrupt slip acceleration results in melting at asperity contact

20 Both aseismic and seismic slip accommodate relative motion across partially couple

21 y motors/generators, FO and F1, which do not slip against each other.

22 We study the systematic depth-dependence of slip along a thrust fault with a number of 2D dynamic si

23 ason why, in continental domains, co-seismic slip along faults can propagate up to the Earth's surfac

24 at phyllosilicates can facilitate co-seismic slip along faults during earthquakes.

25 at least 12 major faults, including possible slip along the southern Hikurangi subduction interface;

26 ately the Peierls barrier to prismatic plane slip and argue that Y, Ca, Ti, and Zr should interact st

27 Slip and catch bonds have respectively been explained by

28 c biomolecular interaction can be divided in slip and catch bonds, respectively.

29 ain in the right hip for 5 days, following a slip and fall accident while playing soccer.

30 including recent discoveries of tremor, slow-slip and low-frequency earthquakes, are less understood.

31 hts into the relationship between interplate slip and permanent deformation.

32 quantifies the controlling features of cross-slip and pyramidal I/II stability across the family of h

33 , and the motor was observed occasionally to slip and reattach.

34 We directly measure fault slip and seismicity induced by fluid injection into a na

35 the values of correction factor fall in the slip and transition regime, with no Darcy flow regime ob

36 Observations and models of slow slip and tremor require the presence of near-lithostatic

37 locally switching adhesions from gripping to slipping and further accelerating actin flow in the pros

38 the smallest crevice height (4 mm), whereas slipping and the probability of zigzag paths increased.

39 unassisted, showing a reduced number of paw slips and misses.

40 t can be used to manipulate the behaviors of SLIPS and open the door to new applications of this emer

41 able to regulate the relative activities of slips and twinning, as a result, overcome the inherent l

42 fusion barrier, reduction in activated cross-slip, and enhancement of covalent character and bond str

43 lastic moduli, the Schmid factor for primary slip, and the propensity for simultaneous slip on multip

44 cation, and thereby decrease the dislocation slip anisotropy in the alloy.

45 In this range single phase-slips are unable to produce dark counts and the fluctuat

46 An analytic model explains these slips as avalanches of slipping weak spots and predicts

47 [~4 micrometers per second (mum/s)] aseismic slip associated with a 20-fold increase of permeability,

48 We confirm that some of the co-seismic slip at shallow depth (<5 km) constrained by InSAR data

49 n agreement with recent mean-field theory of slip avalanches in elasto-plastic materials, revealing t

50 es at 77 K, characteristic of the prevailing slip bands and dislocations, as well as lattice disorder

51 -fault parallelepipeds, and arrest at planar slip bands of undissociated dislocations.

52 The observation of pop-in events and slip bands on the surface of the indented crystals demon

53 e concurrent nucleation of a large number of slip bands.

54 ical model is developed to predict the cross-slip barrier as a function of the near-core energy diffe

55 ely believed to have fed the eruption of the SLIP basalts.

56 Our results suggest that the diversity of slip behavior observed during landslides can be describe

57 previously unrecognized quasi-periodic slow-slip behavior that is widespread in the megathrust zone.

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

59 d, and show greater synchrony in their stick-slip behaviour.

60 We show that a spectrum of slow-slip behaviours arises near the threshold between stable

61 ism of [Formula: see text] dislocation cross-slip between pyramidal I and II planes, which occurs by

62 hways for dislocation glide along, and cross-slip between, intersecting TB-matrix interfaces.

63 through which the beta-diketiminate ligand "slips" between bidentate and arene-bound forms: rather t

64 d Thy-1/alphavbeta3 dissociation, indicating slip bond behavior.

65 d to the GAG 6-O-sulfation site whereas only slip bond interaction can be observed in a GAG system wh

66 lts from an asymmetrical bond that acts as a slip bond under forward tension and a slip-ideal bond un

67 ecrease monotonically with force, indicating slip-bond behavior.

68 nd allow identification of these two coupled slip-bond states that behave consistently within the Kra

69 ediated cytoskeleton contractility and catch-slip-bond-like behaviours in FAs and the cytoskeleton as

70 ork of a two state two path model, where two slip bonds are coupled forming a double-well interaction

71 Actin catch-slip bonds are suppressed by single residue replacements

72 ton and molecularly modulated integrin catch-slip bonds biased the rheostasis and induced non-homeost

73 Conceptually, slip bonds exhibit a reduced bond lifetime under increas

74 erestingly, force elicited TCR-pMHC-II catch-slip bonds for agonists but slip-only bonds for antagoni

75 ymerization under force is governed by catch-slip bonds mediated by force-induced K113:E195 salt-brid

76 rengthened by constant forces, as opposed to slip bonds that are weakened by constant forces.

77 controlled by RhoA switches the actin catch-slip bonds to slip-only bonds.

78 cal forces can strengthen (catch) or weaken (slip) bonds between biological molecules.

79 mplexity, such as oblique subduction, strike-slip boundaries that are subparallel to plate motion, an

80 scover a general breakdown of traditional no-slip boundary condition at short time scales and we show

81 ow concentrations, potentially yielding a no-slip boundary condition on the air-water interface (the

82 Assuming a slip boundary condition, in which the liquid slides agai

83 verning Stokes equations, including a Navier slip boundary condition.

84 how evidence that not only the statistics of slips but also their dynamics are remarkably similar, i.

85 rious codons along the slippery sequence and slip by not just -1 but also -4 or +2 nucleotides.

86 competition between twinning and dislocation slip can be mediated by loading orientation, which is at

87 ting-mechanisms (normal, reverse, and strike-slip) can trigger early aftershocks.

88 excluded adolescents with Blount disease and slipped capital femoral epiphyses.

89 Slipped capital femoral epiphysis (SCFE), a fracture thr

90 based, direct-writing, stereolithography and slip casting technologies.

91 ixational eye movements; i.e., retinal image slip caused by physiological drift.

92 g either from moving objects or from retinal slip caused by self-motion.

93 Frequent pausing and slipping caused by changes A78V and R79K suggest that th

94 We rationalize that relatively easier <c+a> slip characteristic of this alloy plastically relaxed th

95 s of the ligands come together to generate a slipped-cofacial orientation of the porphyrinatozinc(II)

96 s-free boundary conditions, compared with no-slip conditions, may yield qualitatively different dynam

97 Both as wetting phase, water exhibited no-slip Darcy flow in all cores; however, flow enhancement

98 ands of square nanometers) and indicate a no-slip Darcy-like behavior inside the GOAL nanochannels.

99 the known NOP antagonists, as being slightly slipped deeper inside the protein core.

100 tial correlation between fluctuations of the slip distribution and geometrical fault structure.

101 y, explaining why Hector Mine has a smoother slip distribution as it occurred on a geometrically simp

102 allowed us to retrieve the geometry and the slip distribution of the seismic source and to compute t

103 We obtain a probability density for the slip distribution, which varies both with depth, earthqu

104 We propose a method to modify stochastic slip distributions according to this dynamically-derived

105 ed to produce large numbers of heterogeneous slip distributions for probabilistic tsunami hazard anal

106 Fault slip distributions provide important insight into the ea

107 eals that, unlike what is commonly supposed, slip does not occur by such shear melting, and indicates

108 nd a transition from twinning to dislocation-slip-dominated plasticity at high pressure (more than 15

109 provide a sufficient surface to render a non-slip droplet condition, and while the PCL fibers lend a

110 Near-trench slip during large megathrust earthquakes (megaquakes) is

111 asses have strikingly similar effects on the slip dynamics.

112 ncludes only the slip statistics or also the slip dynamics.

113 opic receding line as compared to the "stick-slip" dynamics reported in previous studies.

114 the most sensitive modality for identifying slips early, ultrasound may be used as a cost-effective

115 on observations made during an offshore slow-slip event (SSE) in September and October 2014, using a

116 to six molecular layers during an individual slip event should result in film dilation of 0.4-0.5 nm,

117 Within the model, slip occurs in discrete slip events exclusively by individual dislocations emitt

118 esults suggest that inherently periodic slow-slip events result in periodic stress perturbations and

119 l plastic deformation includes local plastic slip events taken with an appropriate weight assigned to

120 ing behavior, including earthquakes and slow-slip events, occurs along tectonic faults.

121 s during the fleeting (ca. 20 ms) individual slip events.

122 18 with Mw > 7 since 1896) and produced peak slip exceeding 40 metres in the Tohoku-oki earthquake.

123 Modeling suggests this is compatible with slip extending seaward, at least, to within 6 km of the

124 lted margins of the Gulf display largely dip-slip extensional movement and accompanying footwall upli

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

126 Why many major strike-slip faults known to have had large earthquakes are sile

127 erally do not deal specifically with shallow slip features.

128 ir pressure, viscous flow is weakening, then slip flow and Knudsen diffusion are gradually becoming d

129 y fall in flow regimes such as viscous flow, slip flow and Knudsen diffusion.

130 the back-pressure requirements alleviated by slip flow.

131 -induced fluidization of the lubricant film (slip), followed by its resolidification (stick).

132 The unloading slope during the unstable slip follows the stiffness of the apparatus at all exper

133 We show that stick-slip friction can be tuned from maximal to nearly fricti

134 to the importance of considering the methane slip from combustion of LNG.

135 rved surface ruptures are the propagation of slip from depth on a surface rupturing (i.e. capable) fa

136 Methane slip from exhausts represented 44% of the total emission

137 oduced an unexpected large amount of shallow slip greatly contributing to the ensuing tsunami.

138 To reduce the risk of slip, grip force (GF) control includes a safety margin a

139 g the development of the left-lateral strike-slip Haiyuan fault south of the northern Qilian suture.

140 We find that slip has a strong influence on the droplet evolutions, b

141 r in the wide range of systems in which slow slip has been reported, including seismic faults.

142 xtensive work, quantitative studies of phase slips have been limited by uncertainty regarding the ord

143 This mechanisms' grip slips, however, when the feedback loop is intermittently

144 s as a slip bond under forward tension and a slip-ideal bond under backward tension.

145 rienced relatively minor (if any) co-seismic slip in 2011.

146 d prior knowledge about how much a fault can slip in a single earthquake and the seismic potential of

147 ation mode that competes against dislocation slip in crystalline solids.

148 ional theory to study the preferred modes of slip in the high-pressure omega phase of Zr.

149 ither the rupture extent or the amplitude of slip in this earthquake.

150 Fluid injection primarily triggers aseismic slip in this experiment, with micro-earthquakes being an

151 the SCM is found to proceed via dislocation slipping in the <100> or <110> mode with striking shear

152 enable studies of quantum and thermal phase slips in a well-characterized system and will provide ac

153 rn implies a threshold failure process, with slip initiated when stress exceeds the local fault stren

154 As the dislocations slip inside the crystal grains and pile up at the grain

155 ucts (DRiPs) and other short-lived proteins (SLiPs) into autophagosomes via sequestosome (SQSTM1, p62

156 SLIP involves transferring arrayed bacterial cultures fr

157 ents in which a contact line moves and where slip is a dominating and controllable factor.

158 ledge of the basic crystallographic modes of slip is critical to understanding and analyzing the plas

159 te that the observed variation of co-seismic slip is neither random nor artificial, but self-affine f

160 We also showed that SLiPs is an excellent source of antigen for cross-primin

161 free surface that causes them to unclamp and slip large distances.

162 ated, and exceptionally volatile and Cl-rich SLIP lavas, permitted a massive release of nickel-rich v

163 i into the atmosphere during eruption of the SLIP lavas.

164 micrometer-scale particles, and a convenient slip layer for timing incubation steps.

165 achment decreased via increased hydrodynamic slip length and reduced attraction and (2) under unfavor

166 itatively explained with a simple model with slip length correction for Darcy flow.

167 ion depth of a laminar flow field (i.e., the slip length) in a densely grafted, thin poly(N-isopropyl

168 in our system is the intrinsic contact-line slip length.

169 The experimental data reveals characteristic slip lengths are of order 500 and 1000 nm for 3M(R) and

170 r for the entry of water molecules and large slip lengths inside graphene capillaries.

171 illary pressures (about 1,000 bar) and large slip lengths.

172 ated under cyclic loading to move in a stick-slip manner.

173 The unique cross-slip mechanism is governed by common features of the gen

174 rack in the CG Cu was blunted by dislocation-slip mediated plastic deformation, while the cracks in t

175 Using the distributed slip model obtained by a linear solution, we estimated t

176 We propose a magnetic "stick-slip" model to explain this peculiar feature, which was

177 However, in general, the slip models derived from tsunami wave modeling and seism

178 Stochastic slip models, which can be computed rapidly, are used to

179 he relative preferences among the identified slip modes are examined using a mean-field crystal plast

180 h shearing on nine distinct crystallographic slip modes in the hexagonal omega-Zr crystal are calcula

181 Further, the coupled and stick-slip motion was confirmed for a sliding water droplet on

182 tact angle and provide a mechanism for stick-slip motion when a drop is forced strongly: the contact

183 Intermittent sliding (stick-slip motion) between solids is commonplace (e.g., squeak

184 onsidering a single patch with a homogeneous slip motion.

185 n as against the traditional staggered stick-slip motion.

186 The mechanism that results in such large slip near the surface is poorly understood as shallow pa

187 mic rupture simulations reproduced the large slip near the trench observed in the 2011 Tohoku-oki ear

188 We also demonstrate that phase slips occur deterministically as the barrier separating

189 ates at specific distances where sharp local slips occur.

190 igorite, unstable fault slip (that is, stick-slip) occurred during dehydration reactions in the lawso

191 Within the model, slip occurs in discrete slip events exclusively by indiv

192 In northeastern Japan, aseismic slip occurs in the form of decelerating afterslip after

193 Most aseismic slip occurs within the fluid-pressurized zone and obeys

194 a linear solution, we estimated that a peak slip of approximately 1.7 m occurred around 4 km depth f

195 ake and predicted the possibility of a large slip of over 30 m for the impending megaquake at the Nan

196 e solution of emitters on a microscope cover slip of silicate based glass (such as quartz).

197 planes, but the structure, motion, and cross-slip of the associated [Formula: see text] dislocations

198 a fracture through the physis with resultant slip of the epiphysis, is the most common hip abnormalit

199 midal I and II planes, which occurs by cross-slip of the individual partial dislocations.

200 ht femoral head, with a medial and posterior slip of the right femoral head.

201 w that, within our resolution of ca. 0.1 nm, slip of the surfaces is not correlated with any dilation

202 ion electron microscopy to occur through the slip of {111} layers, induces morphological changes from

203 n contact lines, hence inducing a collective slipping of the colony across the surface.

204 associated with local, tip-induced 2pi phase slips of the CDW, and that dissipation maxima arise from

205 The subsequent outcome devaluation and 'slip-of-action' tests allowed evaluation of the particip

206 Shallow slip offshore Sumatra appears driven by diagenetic stren

207 ructures, such as NaCl and HfC predominately slip on 110{110}, the ISF here is believed to facilitate

208 ry slip, and the propensity for simultaneous slip on multiple slip systems.

209 alized plasticity requires the activation of slip on pyramidal planes, but the structure, motion, and

210 The temporal evolution of slip on surface ruptures during an earthquake is importa

211 We combine 'on-fault' trench observations of slip on the Polochic fault (North America-Caribbean plat

212 of the visual surround, which suppress image slip on the retina for visual acuity.

213 110}, the ISF here is believed to facilitate slip on the {111} planes for this B1 HfN phase.

214 ich is the partial dislocation direction for slip on these close packed planes.

215 erplate earthquakes and as relatively steady slip on uncoupled areas of the subduction thrust.

216 s, and propagate into adjacent Cu layers via slips on {111} plane non-parallel to the interface.

217 CR-pMHC-II catch-slip bonds for agonists but slip-only bonds for antagonists, thereby amplifying the

218 RhoA switches the actin catch-slip bonds to slip-only bonds.

219 The smooth slip onset, indicating a large (~5-meter) slip-weakening

220 We investigate how the choice of either no-slip or stress-free boundary conditions affects numerica

221 s, and the earth all deform via intermittent slips or "quakes".

222 me, but some cells evade this checkpoint and slip out of mitosis.

223 peed, the processes that underlie slow fault slip phenomena, including recent discoveries of tremor,

224 ations that illuminate the mechanics of slow-slip phenomena.

225 ted types of compounds by introducing active slip planes in structures via different noninterfering s

226 me fraction of strengthening precipitates on slip planes, increase in vacancy diffusion barrier, redu

227 y (shape synthons), reliably form low energy slip planes, thus facilitating an impressive mechanical

228 with two pairs of bendable faces but without slip planes.

229 Although principally a strike-slip plate boundary, the faulted margins of the Gulf dis

230 a new approach to assessing the near-trench slip potential quantitatively by integrating laboratory-

231 olding time of 10 s at room temperature, the slip process evolves as a self-similar random process wi

232 le (nanofriction) is often governed by stick-slip processes.

233 behavior, allowing for modeling of realistic slip profiles for use in seismic hazard assessment and p

234 lyze high-resolution along-strike co-seismic slip profiles of the 1992 Mw = 7.3 Landers and 1999 Mw =

235 crometer-thick layers can facilitate seismic slip propagation during earthquakes in continental domai

236 Seismic slip propagation is facilitated by along-fault low dynam

237 , where pelagic clays participate in seismic slip propagation.

238 ar data to model the earthquake rupture as a slip pulse ~20 kilometers in width, ~6 seconds in durati

239 The repeat intervals of the slow slip range from 1 to 6 years and often coincide with or

240 The periodicity in the slow-slip rate has the potential to help refine time-dependen

241 otary shear experiments conducted at seismic slip rates (1 ms(-1)) show that phyllosilicates can faci

242 experiments, we demonstrate that, at seismic slip rates (1 ms(-1)), similar calcite gouges with pre-e

243 arated by similar length time intervals when slip-rates are much lower, and activity shifts between f

244 We constrain fault slip-rates since 18 ka using variations in cosmogenic (

245 rate were increased there was a stable wall slip regime followed by an evolving wall slip regime, wh

246 all slip regime followed by an evolving wall slip regime, which is finally followed by the onset of e

247 peratures the system enters a multiple phase-slip regime.

248 vely to enhanced trans-grain and inter-grain slip resistance, and hence, increased strength.

249 Analysis of motor slipping reveals that the force resisting packaging rema

250 ositive feedbacks between processes of fault slip, rock fracturing and alteration, and landscape deve

251 red-cubic silver nanocrystals, where crystal slip serves as a stimulus to surface diffusional creep.

252 Using a duplicate copy of the pipo slip site region fused into a different genomic location

253 all show the same scaling behavior for their slip size distributions and other statistical properties

254 It predicts the observed slip-size distributions and the observed stress-dependen

255 ctamethylcyclotetrasiloxane) varies in stick-slip sliding between atomically smooth surfaces during t

256 roller are long enough, these molecules can "slip-stack" in the solid state, leading to high crystall

257 In contrast, when the TDI molecules are slip-stacked along their N-N axes in films of 2, fsTA sh

258 6-31+G(d,p)] reveal that the dimers prefer a slip-stacked geometry and feature elongated bonds.

259 their singlet fission dynamics and find that slip stacking leads to rapid, subpicosecond singlet fiss

260 range ordering of the dyes in staircase-like slipped stacks with J-type excitonic coupling favors cha

261 ches in both systems, and show that both the slip statistics and dynamics are independent of the scal

262 the claim of universality includes only the slip statistics or also the slip dynamics.

263 lipping weak spots and predicts the observed slip statistics, stress-strain curves, and their depende

264 Slipped-strand mispairing during replication is likely t

265 Catastrophic failure occurs only when the slip surface is characterized by rate-weakening friction

266 ature regimes and 110{110} to be a secondary slip system activated at elevated temperature.

267 scopy (TEM) revealed 110{111} as the primary slip system in both temperature regimes and 110{110} to

268 The dislocation slip system in each of the forty crystal grains adjacent

269 We identify four possible slip systems of bridgmanite in the lower mantle that rec

270 xperiences successive reorganizations of the slip systems.

271 propensity for simultaneous slip on multiple slip systems.

272 t the last 480 years included a component of slip that was aseismic, or associated with very light se

273 Notably, these two earthquakes had a maximum slip that was very close to the surface.

274 owly strained solids deform via intermittent slips that exhibit a material-independent critical size

275 tes, HEAs deform in a jerky way, with sudden slips that make it difficult to precisely control the de

276 similar tests on antigorite, unstable fault slip (that is, stick-slip) occurred during dehydration r

277 In the first 5 mm of slip the shear stress was reduced up to 30% and CO2 was

278 n the axle of a singly threaded rotaxane can slip through a macrocycle that is sufficiently large to

279 produced in diesel engines and that they can slip through a modern aftertreatment system (ATS) at low

280 Alphaproteobacteria, can evade filtration by slipping through the mucous nets of both pelagic and ben

281 In this state the plastron allows slip to occur across the surface which results in a drag

282 , p62) mediated association of ubiquitinated SLiPs to the autophagy gene product LC3.

283 the tumour was passed from animal to animal, slipping under the radar of the immune system.

284 of slippery liquid-infused porous surfaces (SLIPS) using nanoporous and chemically reactive polymer

285 We show that the wavelength and amplitude of slip variability correlates to the spatial distribution

286 ted rapidly, are used to explore the natural slip variability; however, they generally do not deal sp

287 l under gravity demonstrates that asymmetric slip via collapse of the hanging wall is a natural conse

288 Here we provide new insight into strike-slip volcano-tectonic relations by analysing Bouguer gra

289 low fronts is potentially as generic as slow slip, we anticipate that it might occur in the wide rang

290 model explains these slips as avalanches of slipping weak spots and predicts the observed slip stati

291 A simple mean field model for avalanches of slipping weak spots explains the agreement across scales

292 th slip onset, indicating a large (~5-meter) slip-weakening distance, caused moderate ground shaking

293 with flash heating but not with widely used slip-weakening friction laws.

294 llites with a mirror-image lattice form) and slip (whereby lattice dislocations are generated and mov

295 escribe the Strain Library Imaging Protocol (SLIP), which is a high-throughput, automated microscopy

296 tions of the order parameter, known as phase slips, which cause the decay of persistent current in su

297 Beyond this critical strain, layers begin to slip with respect to each other.

298 es that other mechanisms, such as intralayer slip within the lubricant film, or at its interface with

299 SLIP yields rich data sets on cell morphology and gene e

300 on electron microscopy investigations of the slipping zones reveal the presence of calcite nanograins