ライフサイエンスコーパス: geophysical

1 Recent geophysical analyses suggest the presence of a late Pale

2 l on ice flow have not been characterized by geophysical analysis.

3 and Ranging) spacecraft and the NASA Goddard Geophysical and Astronomical Observatory (GGAO).

4 responsible for shaping Earth's distinctive geophysical and chemical properties and generating pathw

5 thermally or compositionally driven flows in geophysical and engineering systems.

6 urbulent dynamical systems are ubiquitous in geophysical and engineering turbulence.

7 The temporal relationships between these geophysical and eruptive time series were studied.

8 Here we report new geophysical and fluid geochemical data for high-temperat

9 over the weaker underlying mantle, although geophysical and geochemical constraints on the exact thi

10 Geophysical and geochemical data support the removal of

11 We use multiparameter geophysical and geochemical data to show that the 110-sq

12 requires greater quantitative comparison of geophysical and geochemical data, linked through sets of

13 Integrating geophysical and geochemical data, we estimate that 1.3 G

14 Co-located geophysical and geochemical datasets in the borehole sho

15 ailability limitations rising from different geophysical and geochemical dynamics at pore-scale.

16 Here, we provide geophysical and geochemical evidence that the salt chimn

17 hat significantly influenced the geological, geophysical and geochemical evolution of the planet, inc

18 ssential, though challenging, as traditional geophysical and geochemical methods for tracking volcani

19 also affects current interpretations of the geophysical and geochemical models using extrapolated or

20 These elements are key components in geophysical and geochemical models.

21 However, geophysical and geochemical observations suggest slab su

22 Such combined geophysical and geochemical observations will help const

23 stitution of the Earth's mantle dictates the geophysical and geochemical properties of this region.

24 rease of the hydrothermal system controlling geophysical and geochemical signals at the caldera.

25 Such processes produce geophysical and geochemical signals that may be detected

26 The formation of Earth's core left behind geophysical and geochemical signatures in both the core

27 iron core may be responsible for the unusual geophysical and geochemical signatures observed at the b

28 Our results demonstrate that high-resolution geophysical and geological observations can yield unprec

29 We present geophysical and geological observations from the west Ib

30 INDEPTH geophysical and geological observations imply that a par

31 S) as part of an integrated approach for the geophysical and geotechnical assessment of the shallow s

32 sive failure, which concerns a wide range of geophysical and geotechnical situations.

33 ed, despite the importance of these flows in geophysical and industrial systems.

34 formation of the Haumea family can match all geophysical and orbital characteristics of the family wi

35 However, this trend has scatter because geophysical and physicochemical parameters can vary, suc

36 Geological, geophysical, and geochemical data support a theory that

37 lications, including industrial, biological, geophysical, and medical settings.

38 g an integrated set of global environmental, geophysical, and social indicators.

39 eling the interaction between lake climatic, geophysical, and socioeconomic features and their stabil

40 100-km length scale is significant for many geophysical applications including mapping of crustal ma

41 r flow, posing an obstacle in industrial and geophysical applications.

42 of EOS data from nanosecond experiments for geophysical applications.

43 temporal patterns of genetic variation with geophysical aspects of the environment can best be attri

44 d decrease losses, as it happens in numerous geophysical, astrophysical flows and in tokamaks.

45 ecology, recent discussions have focused on geophysical attributes, and it is recognized that dynami

46 al land use, vegetation characteristics, and geophysical attributes.

47 e identify a nested evolutionary sequence of geophysical, biophysical, sociocultural, and sociotechni

48 Geophysical borehole measurements and chemical weatherin

49 ions are important sources of uncertainty in geophysical calculations of the AOD-to-PM2.5 relationshi

50 The present increase, whose geophysical cause(s) are uncertain, thus signifies a lar

51 These geophysical changes go along with widespread ecosystem d

52 However, numerical studies of how projected geophysical changes in sea ice will realistically impact

53 sociated with El Nino events and longer term geophysical changes, may thus have far-reaching impacts

54 Geophysical characterization of calderas is fundamental

55 Here we present the first geophysical characterization of serpentinite carbonation

56 )-saturated DIW for 49 days while monitoring geophysical, chemical, and hydrodynamic parameters.

57 buoyancy remains actively debated within the geophysical community.

58 ate services, given subnational geographical/geophysical complexity, attention is focused on lessons

59 cal evolution of ice sheets to ascertain the geophysical conditions that allow liquid water to be pro

60 s is consistent with existing geological and geophysical constraints, including Pleistocene glacio-is

61 et characteristics that describes platinum's geophysical constraints, institutional efficiency, and d

62 5) composition is compatible with a range of geophysical constraints.

63 ring many optical devices in the seismic and geophysical context.

64 l tropical N cycle by examining climatic and geophysical controls of surface soil N content and stabl

65 ctively the daily, seasonal, lunar and tidal geophysical cycles regulate much of the temporal biology

66 sing isolation of human societies from these geophysical cycles, as a result of improved living condi

67 Here, using sea-floor geophysical data and marine sediment cores, we resolve t

68 From geophysical data and modeling analyses, we evaluate gas

69 Marine geophysical data collected in 2006 reveal a large, arcua

70 The geophysical data define a 2,500-km-long rift system in E

71 , we interpret petrographic, geochemical and geophysical data from drill holes in a modern SMS deposi

72 deling, as well as obtaining samples and new geophysical data from other planets (Venus, Mars, or Mer

73 Here we show, using marine geological and geophysical data from the continental shelf seaward of t

74 ep to derive eruption source parameters from geophysical data in real-time.

75 Geophysical data indicate that deep magma influx beneath

76 These combined geochemical and geophysical data indicate that the structure and hydrati

77 Deriving eruption source parameters from geophysical data is critical for volcano hazard mitigati

78 Most of the geophysical data provide global information that cannot

79 erical simulations and fine-tuned with small geophysical data sets for potential applications to faul

80 oil clay content, while temporal analysis of geophysical data showed the impact of soil moisture and

81 effective coupling of UAV data products with geophysical data to extract critical information for far

82 ent times range from 10's-100's of years and geophysical data typically exist for only a portion of a

83 Here, we assimilate geophysical data with modelling of the Eurasian Ice Shee

84 d magnetic susceptibility models of airborne geophysical data(5,6).

85 es on a watershed scale, by linking borehole geophysical data, near-surface geophysics, and remote se

86 w that this structure is compatible with all geophysical data, notably (1) deep reflected and diffrac

87 c mode, constrained by satellite and in situ geophysical data, we identify the nature of this potenti

88 actorily explain the available structural or geophysical data.

89 ed on more than one million hours of diverse geophysical data.

90 le structural changes that are detectable in geophysical data.

91 storage" model is generally applicable, then geophysical detection of melt beneath volcanoes is likel

92 Geophysical detection of subducted mid-ocean ridge basal

93 The geophysical detection of such a layer has, however, prov

94 and Amazonian forest, to assess climatic and geophysical determinants of LES traits and their interre

95 's magnetosphere is therefore likely to be a geophysical effect associated with fluctuating boundary

96 As a result, the analysis of geophysical events and the performance of largely empiri

97 small-scale experiments and the larger-scale geophysical events, a rather good agreement is found bet

98 est in the absence of robust geochemical and geophysical evidence for a mantle source.

99 However, the geophysical evidence for such large early emissions is e

100 We find geological and geophysical evidence for this process in the Tasmanides

101 However, a range of geophysical evidence indicates that compositionally dist

102 ing these results with geochemical and other geophysical evidence reveals highly symmetric lower-crus

103 Geophysical evidence strongly supports the complete isol

104 Petrological, geochemical, and geophysical evidence suggests that the MTZ may host subd

105 dates are based on several morphological and geophysical evidences and analogies: (i) the dimensions

106 cological dynamics to planetary change, with geophysical evolution determining the relevant time scal

107 connects polar volatiles to the geologic and geophysical evolution of the Moon and the bombardment hi

108 ents, planetary geological, geochemical, and geophysical evolution, orbital dynamics of bodies in the

109 nclusions and show that new opportunities in geophysical exploration and characterization could arise

110 nclusions suggest a rigorous new approach in geophysical exploration for mineral deposits.

111 Geophysical exploration of the seabed is typically done

112 demonstrating the method's effectiveness for geophysical exploration.

113 ossible thermophysical effects; however, the geophysical expressions of these effects are unknown.

114 2013, and whether lake-specific or regional geophysical factors were related to the observed changes

115 Multiple additional climatic and geophysical factors were secondary determinants of plant

116 bitats and find patterns with bioclimate and geophysical factors, as well as land use, host phylogeny

117 s well as how seasonal differences vary with geophysical factors.

118 This geophysical feature, clearly more evident than the ones

119 Among the geophysical features shown in the map, the important Sil

120 data a dictionary of local, or small-scale, geophysical features.

121 r the extrapolation of laboratory results to geophysical field scales.

122 ause both processes generate seismic energy, geophysical field studies of volcanic processes are ofte

123 Our results reveal nested climatic and geophysical filtering of LES traits and their interrelat

124 ) and fundamentally altering the behavior of geophysical flows (landslides, debris flows, pyroclastic

125 Waves observed in geophysical flows are also robust to perturbations, whic

126 r small-amplitude, abrupt reorganizations of geophysical flows at forcing levels lower than the criti

127 Turbulence in geophysical flows tends to organize itself so that the m

128 itable discrete numerical approximations for geophysical flows with many conserved quantities as a nu

129 ments are presented here for these truncated geophysical flows with topography in a suitable regime.

130 d atoms to metamaterials, active matter, and geophysical flows.

131 deep sea, the sense of time is dependent on geophysical fluctuations, such as internal tides and atm

132 and tropospheric sulfate aerosols) from the Geophysical Fluid Dynamics Laboratory and Hadley Centre

133 Using the Geophysical Fluid Dynamics Laboratory comprehensive Eart

134 changing climate (A2 and B1 IPCC emissions; Geophysical Fluid Dynamics Laboratory General Circulatio

135 Here, we use an earth system model from the Geophysical Fluid Dynamics Laboratory to investigate reg

136 value in data assimilation, for example, in geophysical fluid dynamics.

137 rizing slow-fast interactions are central to geophysical fluid dynamics.

138 e (as found in oceans, atmospheres and other geophysical fluids) and those of SOC.

139 in turbulence, combustion, nonlinear optics, geophysical fluids, and neuroscience.

140 Integration of geophysical, geochemical, and geological evidence suppor

141 on high-resolution aeromagnetic imaging and geophysical-geodetic observations.

142 s than the upper convecting mantle underpins geophysical, geodynamic and geochemical models of Earth'

143 add to sounds of biological (biophonic) and geophysical (geophonic) origin, with human contributions

144 er species distributions in conjunction with geophysical habitat alterations, such as changes to land

145 resulted from the complex environmental and geophysical history of the region.

146 aleomagnetic record is an archive of Earth's geophysical history, informing reconstructions of ancien

147 Geophysical hotspots have been attributed to partially m

148 cs of subduction zones(4,6); however, direct geophysical imaging of the complex fracture networks pro

149 been little corroboration from crustal scale geophysical imaging.

150 Here, we couple geophysical induced polarization (IP) measurements in H(

151 ows with rigid boundaries, occurring in many geophysical, industrial and biophysical flows.

152 Geophysical inferences of the viscosity structure, howev

153 Several lines of geophysical inquiry now suggest that a change in the loc

154 Seafloor geophysical instrumentation is challenging to deploy and

155 es worldwide are continuously monitored with geophysical instrumentation.

156 m methods to image small-scale structures of geophysical interest buried within the Earth requires th

157 nstrates significant potential for improving geophysical interpretation in complex geological environ

158 structure of the landing site to aid in situ geophysical investigations.

159 o their passive mode-overseen by the typical geophysical investigations.

160 The chemical and geophysical issues that have to be solved to interpret i

161 Drill cores and geophysical logs from International Ocean Discovery Prog

162 The use of a geophysical mapping system during the submarine SCICEX e

163 highlighting that H(2)O can be a high-energy geophysical material.

164 nts from a radiometer and a radar, producing geophysical measurements at a finer spatial resolution t

165 e than the surrounding rocks, and electrical geophysical measurements can be used to map these zones.

166 nally, high-resolution multitemporal surface geophysical measurements of apparent soil electrical con

167 from basalt major-element barometers(7) and geophysical measurements of lithospheric thickness(8).

168 ECa) maps deriving from on-site near-surface geophysical measurements of vineyard soils obtained by a

169 Expanded geophysical measurements onshore and offshore in these s

170 Geophysical measurements, however, suggest that melts of

171 Magnetotellurics, a geophysical method measuring subsurface electrical resis

172 eous aquifer sediment, using the noninvasive geophysical method spectral induced polarization (SIP).

173 f complex electrical conductivity imaging, a geophysical method, to monitor the high-pressure injecti

174 Geophysical methods are even further limited at frequent

175 nd are studied intensively, particularly, by geophysical methods sensitive to active and/or visible s

176 otelluric and geomagnetic depth sounding are geophysical methods sensitive to mantle melt.

177 he effectiveness of chemical, hydraulic, and geophysical methods to monitor microbial activity, gel f

178 rust are still not accurately resolved using geophysical methods.

179 rgin using new shallow water electromagnetic geophysical methods.

180 ct detection in the deep Earth possible with geophysical methods.

181 nthesis of the mammalian fossil record and a geophysical model of topographic evolution of the Basin

182 core conditions are essential input for the geophysical modelling but are poorly constrained experim

183 hermal conductivity at odds with traditional geophysical models and direct evidence for a primordial

184 Likewise, our findings suggest that geophysical models of Uranus and Neptune require reasses

185 rom beneath Enceladus' surface at times when geophysical models predict its fissures should be under

186 l signatures to salt volume fraction through geophysical models, and (iii) increases of porosity (by

187 A goal of subsurface geophysical monitoring is the detection and characteriza

188 e first time, ten years of multidisciplinary geophysical monitoring of simulated clandestine graves u

189 y be injected into the subsurface to enhance geophysical monitoring tools used to track fluids and ma

190 tonomy(1), provide remote time standards for geophysical monitoring(2) and distributed coherent sensi

191 n about this storage because geochemical and geophysical observations are limited to pits, boreholes,

192 Reconciling contradictory geochemical and geophysical observations at ocean ridges requires a bett

193 These findings align with geophysical observations from caldera systems, emphasizi

194 Using geophysical observations from offshore Svalbard to const

195 ere, we investigate this elusive phase using geophysical observations from the 2004 moment magnitude

196 Geophysical observations from the 2011 moment magnitude

197 al experiments constrained by geological and geophysical observations from the Alpine Tethys and Iber

198 On Mars, geophysical observations have confirmed that the core is

199 In the past decade, marine geophysical observations have led to the discovery of th

200 ical discontinuities are predicted and match geophysical observations in a consistent petrological an

201 Geophysical observations indicate that melting beneath r

202 igh-frequency seismic attenuation with other geophysical observations is a powerful tool for understa

203 tectonic plates, but have been challenged by geophysical observations of asymmetric upwelling that su

204 1)) are presented to support geochemical and geophysical observations of Campi Flegrei as a critical

205 loor spreading is thus inferred largely from geophysical observations of spreading events on land at

206 Reconciling geophysical observations of the melting regime beneath t

207 It is unclear if these geophysical observations represent a true picture of the

208 More fundamentally, experimental studies and geophysical observations show that the core is under-sat

209 simulations of Chicxulub-scale impacts with geophysical observations suggests that the Chicxulub cra

210 ever, this assumption has been questioned by geophysical observations(2,3) and by the identification

211 aints of [Formula: see text] K inferred from geophysical observations, while a plausible scenario for

212 of the mineral matrix, which may explain the geophysical observations.

213 lly satisfy geochemical constraints, but not geophysical observations.

214 of the lower mantle could partly explain the geophysical observations.

215 s, potentially unveiling ongoing activity of geophysical or biological origin.

216 ng cracks that have been postulated to solve geophysical paradoxes about heat generated by earthquake

217 relate spatial variations in geochemical and geophysical parameters at the Earth's surface.

218 Both instruments, sensitive to the geophysical parameters in the swath, provided independen

219 for the exploration of condensed phases and geophysical phenomena(1).

220 with tectonics, influences a broad array of geophysical phenomena.

221 composition, perhaps associated with recent geophysical phenomena.

222 eal short time scale and large spatial scale geophysical phenomenon, which is necessarily human in or

223 gh rates of kinetic energy extraction may be geophysical possible.

224 the water-bearing capacity of these phases, geophysical probes such as electrical conductivity have

225 ion can take place by natural selection if a geophysical process is capable of heterotrophic formatio

226 interpret the petrological, geochemical, and geophysical processes associated with subduction zones.

227 st unexpected strong connections between the geophysical processes in Earth's deep interior, the surf

228 Radon is useful as a tracer of certain geophysical processes in marine and aquatic environments

229 s alone, it is not possible to determine the geophysical processes responsible for the observed eleva

230 The two fluxes are critically dependent on geophysical processes that determine mixed-layer depth,

231 ul indicators of a wide variety of planetary geophysical processes, and for Mars they reveal the reco

232 dment of the Stafford Act to include gradual geophysical processes, such as erosion, in the statutory

233 This article discusses a few basic geophysical processes, which collectively indicate that

234 h, economic activity, ecosystem function and geophysical processes.

235 nt in many industrial, civil engineering and geophysical processes.

236 namely the roles of fungi in geochemical and geophysical processes.

237 r analyses of a wide range of industrial and geophysical processes.

238 s, with implications for many industrial and geophysical processes.

239 eep carbon cycle and related geochemical and geophysical processes.

240 Geophysical properties of acoustic, seismic, electric, a

241 to the heat required to produce the observed geophysical properties of the crust.

242 um composition should affect geochemical and geophysical properties of the deep interior.

243 Due to their potential role in the peculiar geophysical properties of the ice giants Neptune and Ura

244 atiles to the exosphere, and geochemical and geophysical properties of the mantle.

245 ve methods of imaging and mapping of surface geophysical properties with many important applications

246 able time-series analysis of geochemical and geophysical properties, providing constraints on mantle

247 amounts of iron (Fe) with effects on various geophysical properties.

248 e that has not been documented in the modern geophysical record.

249 f salt precipitation can be achieved through geophysical remote sensing.

250 the top-shaped rubble-pile asteroid Bennu's geophysical response to spinup is highly sensitive to it

251 ught together to design a metasurface at the geophysical scale, the resonant metawedge, to control se

252 tance in both infrastructure engineering and geophysical science.

253 ngineering and have enjoyed great success in geophysical sciences, because they allow for computation

254 al and geochemical models constrained by the geophysical setting, rather than direct observations.

255 ments and multiple resilient examples of all geophysical settings in every ecoregion, it could form t

256 implications for coastal hazards in similar geophysical settings, suggesting a currently neglected s

257 habitats that instantiate aspects of Earth's geophysical signals (appropriately timed light exposure,

258 Accelerating rates of geophysical signals (e.g., seismicity and deformation) p

259 e explored the temporal relationship between geophysical signals and eruptive parameters measured dur

260 .5% decrease in wave velocities, linking the geophysical signatures to salt volume fraction through g

261 duced salt precipitation leads to detectable geophysical signatures.

262 maging and interpretation of their preserved geophysical signatures.

263 Our new results and their broad geophysical significance could be considered when planni

264 of the D'' region raises questions about its geophysical significance.

265 t, a 550 km-long transect of magnetotelluric geophysical soundings spanning the central TAM was acqui

266 Beyond geophysical stressors and responses, it is critical to a

267 method to obtain high-resolution subsurface geophysical structure in Long Beach, CA, from seismic no

268 s show promise for LST in obtaining detailed geophysical structure in travel time tomography studies.

269 tion of the lower crust are based largely on geophysical studies and ancient analogues (ophiolites) t

270 Recent geophysical studies suggest its persistence with down-go

271 Z) and the mid-crustal lens, consistent with geophysical studies that suggest the presence of melt wi

272 Previous geophysical studies typically analyzed individual episod

273 s inferred from seismic tomography and other geophysical studies.

274 agement and development to geomechanical and geophysical studies.

275 applied rigorous analytical procedures to a geophysical study with enormous implications for humanit

276 Observations from geophysical surveys and long-term oceanographic instrume

277 High-resolution geophysical surveys and underwater SCUBA diving reconnai

278 Marine geophysical surveys were carried out along the floating

279 often intricate and below the resolution of geophysical surveys.

280 s will significantly improve flow models for geophysical suspensions such as hyperconcentrated flows

281 more comprehensive understanding of complex geophysical systems such as large lakes.

282 cesses in biological, social, financial, and geophysical systems, little is known about contagion beh

283 ing inertia in political, technological, and geophysical systems.

284 complex nonlinear dynamical systems such as geophysical systems.

285 Geophysical techniques are also not very effective in th

286 the most recent to be recorded using modern geophysical techniques.

287 ture the imagination because of their tie to geophysical time, and tools are now in hand to analyse t

288 ally coordinate physiology and align it with geophysical time, which enables diverse life-forms to an

289 how environmental signals entrain clocks to geophysical time.

290 fficult test suite of prototype problems for geophysical turbulence with waves, jets, and vortices, w

291 a new conceptual foundation for the study of geophysical turbulence, an explanation for the mixing ef

292 Efficient computation of geophysical turbulence, such as occurs in the atmosphere

293 This hybrid approach combined the geophysical understanding and global applicability intri

294 sits, thus highlighting one of many possible geophysical uses of the marine cable network.

295 ome more than just another correlation among geophysical variables.

296 (flooding), meteorological (hurricanes), and geophysical (volcanic activity, tsunamis).

297 ar real time that synthesizes petrologic and geophysical volcano monitoring approaches.

298 Of these, only geophysical warming commitment has been quantified.

299 s, seafloor bathymetry, sediment properties, geophysical well logs, and drilling data to assess the g

300 he moment when funding for the International Geophysical Year enabled him to design and build a CO(2)