コーパス検索結果 (1語後でソート)
通し番号をクリックするとPubMedの該当ページを表示します
1 d applications, including prediction of deep seismic activity and immobilization of nuclear waste in
2 ses and that, despite low deformation rates, seismic activity in the zone is not decaying with time.
9 ons, and high-intensity acoustic inputs from seismic airgun arrays or natural sources (e.g., earthqua
13 alternative interpretation for the origin of seismic and geochemical anomalies in the deep lower mant
16 across the spin transition can help explain seismic and mineralogical models of the lower-mantle inc
17 generated strong tremor that was recorded by seismic and remote low-frequency acoustic (infrasound) s
21 n believed to be one potential source of the seismic anisotropic layer at the bottom of the lower man
24 the lower mantle that reconcile the observed seismic anisotropy beneath the Tonga slab (V(SH)>V(SV))
28 lived geochemical reservoirs and the lack of seismic anisotropy in the majority of the lower mantle e
30 nes, however, where regional observations of seismic anisotropy suggest that the direction of mantle
31 this anisotropy and show how an analysis of seismic anisotropy that incorporates measured ray path g
33 arth's mantle-known as D''-shows significant seismic anisotropy, the variation of seismic wave speed
35 lso provides a strong mechanism for creating seismic anomalies in the inner core itself, much stronge
36 the robustness and distribution of positive seismic anomalies, inferred as subducted slabs, we creat
37 uring the 2011 typhoon season, we deployed a seismic array along the Chishan River in the mountain ar
40 se data recorded by the WOMBAT transportable seismic array to constrain a detailed (20 km resolution
41 ted spatiotemporal resolutions because dense seismic arrays are rarely sufficiently affordable for su
44 g to weak interaction regimes in a system of seismic asperities embedded in a ductile fault zone matr
45 dary is parallel to the top of the plate and seismic attributes indicate a P-wave speed decrease of a
46 hese data provide insight into the long-term seismic behavior of the Loma Blanca fault and, by infere
50 pe composition of calcite formed during this seismic cluster records rapid degassing of CO2, suggesti
59 e available geomorphological, geological and seismic data in the literatures show that this model is
60 ls poking through shallow gas pockets in 3-D seismic data of the CNS indicating that about one-third
61 ic analysis of this doublet, we use regional seismic data providing robust two-point source models, f
62 e sensing and analyses of limited Apollo-era seismic data, deficiencies remain in our understanding o
63 ower-mantle bridgmanite is required to match seismic data, implying the presence of metallic iron in
64 Here using, high-resolution active-source seismic data, we show that Mount St Helens sits atop a s
65 l also makes a testable prediction of a post-seismic decrease of seismic velocity in the shallow crus
67 uation domain controls the largest monitored seismic, deformation, and geochemical unrest at the cald
68 ies in the drill core coincide with regional seismic discontinuities and reflect transient expansion
69 inverse scattering of SS waves the depths to seismic discontinuities below the Central Pacific, which
72 by residual upper mantle, producing a sharp seismic discontinuity at depths of around 38 to 42 kilom
73 We present a novel record of near-field co-seismic displacement, measured with 1-second temporal re
80 ur results suggest that detection of abiotic seismic events are biologically relevant and widespread
81 fective in the lower and middle crust, where seismic events are rare and resolution is generally poor
85 of glacial earthquakes, globally detectable seismic events whose proper interpretation will allow re
87 Earth's inner core boundary, here we present seismic evidence for a localized 4-8 km thick zone acros
94 eismic body wave images from dense broadband seismic experiments that show higher than expected volum
95 graphic model, derived from on- and offshore seismic experiments, that reveals a strong low-velocity
99 s observation has implications for enigmatic seismic features beyond ~2000 kilometers depth and sugge
104 ximately 550 ka-the longest direct record of seismic frequency documented for any fault to date.
110 ve important implications for assessments of seismic hazard and our understanding of how faults inter
111 , they have been excluded from probabilistic seismic hazard assessment and aftershock hazard notices.
112 deling of realistic slip profiles for use in seismic hazard assessment and paleoseismology studies.
113 ly understood, and our ability to assess the seismic hazard associated with geothermal energy or unco
120 d physical models provide new ways to assess seismic hazards and forecast seismicity response to pert
121 s of the lower-mantle would exhibit enhanced seismic heterogeneities due to the occurrence of the mix
122 of the lower-mantle including the origin of seismic heterogeneities in the middle to lowermost parts
126 Here we describe the use of a whole-mantle seismic imaging technique--combining accurate wavefield
127 field modelling is a key component of modern seismic imaging techniques, such as reverse-time migrati
128 w, we document our belief that Rothman had a seismic impact on moving investigative dermatology from
130 oint local and teleseismic earthquake P-wave seismic inversion, we revealed a basaltic lower-crustal
131 ), incipient melts probably trigger both the seismic low velocities and the high electrical conductiv
133 locity to mean that hot plumes-which exhibit seismic low-velocity anomalies at depths of 200 kilometr
134 pot buoyancy fluxes and overlie regions with seismic low-velocity anomalies in the upper mantle, unli
136 nsities and velocities in accord with radial seismic models, and leaves behind a silicate mantle that
137 rgest strike-slip earthquakes ever recorded (seismic moment magnitude M(w) 8.7) occurred about 100-20
140 dy demonstrates the efficacy of near-surface seismic monitoring using DAS-recorded ambient noise.
142 from the Italian Strong Motion and National Seismic networks, and field measurements of surface rupt
145 fish exposed to playbacks of pile-driving or seismic noise for 12 weeks no longer responded with an e
146 e hysteresis in the high-frequency (5-15 Hz) seismic noise level relative to the associated hydrologi
147 and seismometers is challenged by background seismic noise, its robust detection with gravity gradiom
149 thod for detecting changes in gas flux using seismic observations and provides a new tool for monitor
153 istence has been used to explain a number of seismic observations, such as the D'' reflector and the
156 s are ubiquitous at interfaces with optical, seismic or acoustic waves, and also with electron, neutr
158 oratory experiments, numerical modeling, and seismic P-to-S conversions recorded by a dense seismic a
159 s, we find a relatively strong late-arriving seismic phase (dubbed Dam-forming phase or D-phase) reco
160 ault can slip in a single earthquake and the seismic potential of a partially coupled megathrust inte
161 ween our mineral physics predictions and the seismic Preliminary Reference Earth Model down to at lea
162 Mountains and available data from both deep seismic profiles and surface structural deformation.
164 wellhead pressure data, marine multichannel seismic profiles, seafloor and water-column sonar survey
165 together with bathymetry and high-resolution seismic profiles, were used to identify suitable samplin
166 boundary beneath southwest Okhotsk Sea with seismic properties intermediate between those of the inn
171 hich indicate that energetic, high-frequency seismic radiation originates from locations that are dis
172 oportionately large amount of high-frequency seismic radiation to be produced during fault rupture.
173 i earthquake was deficient in high-frequency seismic radiation--a difference that we attribute to its
174 loped to accurately describe and predict the seismic rainbow effect; allowing the metawedge to be des
175 es or reflect the Rayleigh waves creating a "seismic rainbow" effect analogous to the optical rainbow
176 of rocks at slip velocities approaching the seismic range ( approximately 0.1-1 m s(-1)), and at mod
177 e is highly-anisotropic and depending on the seismic ray path, its properties can be very difficult t
178 ropose a seismic metabarrier able to convert seismic Rayleigh waves into shear bulk waves that propag
182 Based on spectral characteristics of the seismic records, we also detected 20 landslide/debris fl
183 ts (DFLEs) in near real-time using broadband seismic records, which can provide timely warnings of th
184 ied iceberg scours seen in three-dimensional seismic reflection images from the mid-Norwegian slope.
190 Similar hysteresis has been observed between seismic river noise and discharge during storms, suggest
191 effectively defining the area of subsequent seismic rupture (rupture did not occur where slow slip w
192 eakening and promotes the propagation of the seismic rupture in carbonate-bearing fault patches.
193 tance for eruption forecasting the causes of seismic rupture processes during caldera unrest are stil
196 road range of engineering applications, from seismic shielding at low frequency to ultrasonic cloakin
198 'non-volcanic' tremor, a recently discovered seismic signal probably generated by shear slip on the d
199 ges in microseismic monitoring is that those seismic signals generated from micro seismicity have ext
201 ed together with high-frequency (HF, 1-3 Hz) seismic signals, we find a relatively strong late-arrivi
203 re-insulating D" layer, but the absence of a seismic signature suggests the transition does not contr
204 itically needed to evaluate the composition, seismic signatures, and geodynamics of the planet's remo
206 , the reason why, in continental domains, co-seismic slip along faults can propagate up to the Earth'
210 emonstrate that the observed variation of co-seismic slip is neither random nor artificial, but self-
211 We analyze high-resolution along-strike co-seismic slip profiles of the 1992 Mw = 7.3 Landers and 1
212 along micrometer-thick layers can facilitate seismic slip propagation during earthquakes in continent
215 cular, rotary shear experiments conducted at seismic slip rates (1 ms(-1)) show that phyllosilicates
216 riction experiments, we demonstrate that, at seismic slip rates (1 ms(-1)), similar calcite gouges wi
219 e we present high-resolution bathymetric and seismic sonar data sets of 10 morphologically similar dr
220 he geometry and the slip distribution of the seismic source and to compute the Coulomb Failure Functi
222 hese results suggest that interpretations of seismic structure in the deep mantle need to treat a bro
223 inental crust by calculating the density and seismic structure of two exposed sections of island arc
227 incorporating constraints from a collocated seismic study into the magnetotelluric inversion process
229 ts, we investigate the impact of exposure to seismic surveys on scallops, using measurements of physi
230 (playbacks of recordings of pile-driving and seismic surveys), but not to a more continuous additiona
231 g this hazard required analyses of 2D and 3D seismic surveys, seafloor bathymetry, sediment propertie
232 aseismic for two months just after the main seismic swarm (April 1, 1984) due to a SE-to-NW directed
239 se is coincident in depth with regions where seismic tomography has imaged slab stagnation, plume def
240 microplates close to the trench, but recent seismic tomography studies have revealed a high-velocity
241 l lithosphere 175 kilometers thick, whereas seismic tomography supports a much thicker root (>250 ki
243 we use joint active-source/local-earthquake seismic tomography to derive unprecedented constraints o
244 oscience community is increasingly utilizing seismic tomography to interpret mantle heterogeneity and
249 rupture geometry, demonstrated likelihood of seismic triggering, and high model temperatures in young
252 nated by linear abyssal hills, upper crustal seismic velocities abruptly increase by over 20%, and gr
256 l distribution of partial melt inferred from seismic velocities obtained from Rayleigh wave tomograph
257 nosphere is associated with a platewide high-seismic velocity "lid" overlying lowered velocities, con
258 drock fracture distributions, as revealed by seismic velocity and electrical resistivity surveys from
260 antle asthenosphere corresponds to an abrupt seismic velocity decrease and electrical conductivity in
261 composition layer suggested by an anomaly in seismic velocity in the 150 kilometres immediately above
262 ble prediction of a post-seismic decrease of seismic velocity in the shallow crust of the affected re
263 present a continuous high-resolution crustal seismic velocity model for an 800 km section of the act
265 flow measurements to estimate thickness and seismic velocity ratio, v(P)/v(S), of continental crust
266 and is characterized by a steady increase in seismic velocity similar to that observed in active arcs
267 topography-dependent tomographic scheme, the seismic velocity structure of the Eastern Tibetan Platea
268 s of the Earth is largely based on images of seismic velocity variations in the mantle obtained with
274 r function images to resolve a vertical high-seismic-velocity anomaly beneath the west-central platea
281 an approximately 15 degrees dipping, abrupt, seismic wave-speed transition (less than 1 kilometre thi
283 at the bottom of the mantle, leading to low seismic-wave velocities and high electrical conductivity
287 utations with information contained in whole seismic waveforms--that reveals the presence of broad (n
289 l earthquakes globally during passage of the seismic waves and during the following several hours to
298 icroearthquakes in the intraplate New Madrid Seismic Zone at annual and multi-annual timescales coinc
WebLSDに未収録の専門用語(用法)は "新規対訳" から投稿できます。