ライフサイエンスコーパス: rift

1 erferometric Fourier transform spectroscopy (RIFTS).

2 luvial floodplain in Ethiopia's western Afar rift.

3 ruded basalts flow more than 100 km from the rift.

4 icroplates partly separated by the Hess Deep rift.

5 o other major rift systems such as the Kenya rift.

6 e-shear rifting mechanism for the Rio Grande rift.

7 dike propagated along the extensional north rift.

8 ated Ocean Drilling Program at the Hess Deep rift.

9 tonic processes that formed the East African Rift.

10 cally found at ocean islands and continental rifts.

11 les to both mid-ocean ridges and continental rifts.

12 e settings, but are divergent in continental rifts.

13 yr ago) and Cretaceous (roughly 100 Myr ago) rifting.

14 lization in a zone of narrow, magma-assisted rifting.

15 ick lithosphere during the initial stages of rifting.

16 he mantle initiates early during continental rifting.

17 subsequent vertical motions associated with rifting.

18 km-long Dabbahu magmatic segment of the Afar rift, a nascent seafloor spreading centre in stretched c

19 sely dated 25.2-Myr-old stratum in the Rukwa Rift, a segment of the western branch of the East Africa

20 we show that the extensive magmatism during rifting along the southern Red Sea rift in Afar, a uniqu

21 ary process, periodic shear stress along the rifts also generates heat along their lengths, which has

22 temperature, account for the observed robust rift and post-rift magmatism.

23 ts, during the initial stages of continental rifting and before significant crustal thinning.

24 ntal material into the shallow mantle during rifting and breakup of Gondwana, or contamination of the

25 tern Africa preserve a record of continental rifting and contain important fossil assemblages for int

26 Rifting and magmatism are fundamental geological process

27 olution of the Gamburtsevs demonstrates that rifting and preserved orogenic roots can produce broad r

28 ough lithospheric faults caused by incipient rifting and the collapse of the accretionary wedge.

29 Investigations of a variety of continental rifts and margins worldwide have revealed that a conside

30 ted to be the frozen remnants of lava-filled rifts and the underlying feeder dykes that served as the

31 eak dynamic Coulomb stress is similar on the rifts and transforms.

32 ultiple sub-chambers are a common feature of rift- and hotspot related supervolcanoes.

33 Recent investigations of rift architecture have suggested that multiphase deforma

34 On the other hand, continental rifts are segmented by large offset normal faults, and m

35 r Desert is best explained by magma-assisted rifting associated with Plio-Pleistocene volcanism.

36 ing 200 mW/m(2) consistent with hypothesized rift-associated magmatic migration and volcanism.

37 atic change in splitting parameters into the rift axis from the increased density of dyke-induced fau

38 , have a consistent age-progression from the rift axis outwards, indicating that axial dyke intrusion

39 trate how, given appropriate geohydrology, a rift basin and its catchment can buffer vegetation respo

40 in the Ischigualasto-Villa Union continental rift basin of Argentina.

41 ous notosuchian crocodyliform from the Rukwa Rift Basin of southwestern Tanzania.

42 ror in sedimentary rocks from early Mesozoic rift basins in North America, Greenland, and Europe.

43 We conclude that rift basins that cut across the WAIS margin can rapidly

44 steered back to the ice-sheet interior along rift basins.

45 Continental rifts begin and develop through repeated episodes of fau

46 argins and the magmatism resulting from such rifting can help refine our understanding of the strengt

47 of rift-related volcanics in the Rio Grande rift compared to other major rift systems such as the Ke

48 Constraints on the structure of rifted continental margins and the magmatism resulting f

49 tretching and break-up of tectonic plates by rifting control the evolution of continents and oceans,

50 These rifting crises are rarely observed in thick lithosphere

51 Numerical modelling of rift development shows that when breakup occurs at the s

52 nd dominant mechanisms of melt generation in rifting environments is impeded by a paucity of direct o

53 imensional deformation field for the Dabbahu rifting episode derived from satellite radar data, which

54 Discrete rifting episodes have been observed along two subaerial

55 tween faulting and magmatism during discrete rifting episodes remains poorly documented.

56 y performing a statistical analysis of these rifting episodes, we demonstrate that dike intrusions ob

57 nts dropped by two-thirds, while the rate of rift events increased eightfold.

58 periods also coincide with the magmatism and rifting events in South China.

59 Previous models of rifting events indicate either lateral dyke growth away

60 ype topography is a significant milestone in rift evolution as it signifies the localization of crust

61 ential requirement to reproduce the observed rift evolution.

62 As continental rifts evolve towards mid-ocean ridges, strain is accommo

63 nce to suggest that a 200 km-long segment of rift experienced a major pulse of explosive volcanic act

64 ol structural evolution and magmatism during rifting (extension rate, mantle potential temperature an

65 Our models show that the combination of rift-flank uplift, root buoyancy and the isostatic respo

66 olcanic dikes during the SCR-Northern Nevada Rift flood basalt event both in space and time.

67 o Laurasia and Gondwanaland; in turn, Africa rifted from Gondwanaland.

68 tidal stress open and close the tiger-stripe rifts, governing the timing of eruptions.

69 Here we present evidence that the 'incipient rift' has also rifted towards the east and opens anticlo

70 temperature but, to a similar degree, on the rift history.

71 tain in their architecture a record of their rift history.

72 After initial rifting, however, the displacement on normal faults obse

73 p-sea hydrothermal vents along the Galapagos Rift in 1977, numerous vent sites and endemic faunal ass

74 sm during rifting along the southern Red Sea rift in Afar, a unique region of sub-aerial transition f

75 and the Manda-Hararo segment of the Red Sea Rift in Ethiopia.

76 nt of the western branch of the East African Rift in Tanzania.

77 e in the Gulf of Mexico, a major propagating rift in the South Atlantic Ocean, abyssal hill fabric on

78 Sustained magmatic activity during rifting in Afar thus requires persistently high mantle t

79 and ecological changes driven by geological rifting in Eastern Africa.

80 g with minor synchronous magmatism to narrow rifting in magmatically robust segments.

81 bservations of the south pole revealed large rifts in the crust, informally called 'tiger stripes', w

82 the Saturnian moon Enceladus revealed large rifts in the south-polar terrain, informally called 'tig

83 ting lithospheric structures, at the time of rift initiation.

84 The Northern Ethiopian Rift is an ideal place to test break-up models because i

85 ocalized thinning and melt focusing when the rift is narrow.

86 metric extension to localized and asymmetric rifting is directly controlled by the existence of a str

87 Elevated melt production during continental rifting is likely due to localized thinning and melt foc

88 When continents break apart, the rifting is sometimes accompanied by the production of la

89 een transform faults, seafloor spreading and rifting is well established in several basins.

90 An important structural classification of rifts is by width, with narrow rifts thought to form as

91 se of voluminous melt production at volcanic rifts is primarily increased mantle temperature or plate

92 erial transition from continental to oceanic rifting, is driven by deep melting of hotter-than-normal

93 ding crust located adjacent to the Hess Deep rift, it is imaged significantly above the sheeted dykes

94 nt Bellamya species (n = 4) from the African Rift Lake Malawi that provides an unusual opportunity to

95 volcanic margins with almost no rift or post-rift magmatism.

96 ccount for the observed robust rift and post-rift magmatism.

97 Our model challenges conventional ideas of rifted margin evolution, as it implies that during rift

98 gest an ancient juvenile magmatism along the rifting margin of the southern Gondwana prior to the ope

99 rctica: Neodymium isotopes of Neoproterozoic rift-margin strata are similar; hafnium isotopes of appr

100 rpentinites have been detected at magma-poor rifted margins and above subduction zones, where they ar

101 tension velocity control the architecture of rifted margins and their temporal evolution.

102 observed variations in volcanic activity at rifted margins in terms of the mantle temperature at the

103 Rifted margins mark a transition from continents to ocea

104 ctural evolution and complex architecture of rifted margins through fault interaction processes, here

105 etailed observations have been made at other rifted margins worldwide, the validity of this interpret

106 nsional deformation, suggesting a pure-shear rifting mechanism for the Rio Grande rift.

107 We demonstrate that rift migration is accomplished by sequential, oceanward-

108 margin evolution, as it implies that during rift migration large amounts of material are transferred

109 argin asymmetry are produced by steady state rift migration.

110 Our rift model is based on numerical experiments constrained

111 al stretching, supporting the magma-assisted rifting model in this area of initially cold, thick cont

112 ind subduction zones progresses from initial rifting near the volcanic arc to seafloor spreading.

113 d asthenosphere, and concentrated extension (rift necking) near the central TAM range front but with

114 he Loma Blanca normal fault zone, Rio Grande rift, New Mexico, United States, that constrain earthqua

115 porally resolved contexts in Ethiopia's Afar Rift, now illuminates earlier hominid paleobiology and a

116 past six million years, Baja California has rifted obliquely apart from North America, opening up th

117 plopia Game (Vivid Vision) run in the Oculus Rift OC DK2 virtual reality head mounted display (Oculus

118 The rifting of continents and evolution of ocean basins is a

119 Rifting of the continents leading to plate rupture occur

120 ely cool fluid-dominated metasomatism during rifting of the southern shelf of the Zimbabwe Craton.

121 mained a mystery, the broad synchronicity of rifting of the supercontinent Rodinia, the emplacement o

122 re, are higher on the transforms than on the rifts, opposite to the observations.

123 odels to non-volcanic margins with almost no rift or post-rift magmatism.

124 tive small-scale mantle convection under the rift or the presence of fertile mantle at the time of co

125 gnetic and gravity measurements to propose a rift origin for the basin in association with the wider

126 The Ferrigno rift, overdeepened by glacial erosion, is a conduit whic

127 The lack of rift-perpendicular anisotropy in the lithosphere, and co

128 It is unclear when during the rifting process the segmented nature of magma supply typ

129 provides evidence of self-similarity in the rifting process.

130 mosaic of Precambrian provinces affected by rifting processes.

131 cent Basin and Range province and Rio Grande rift province underwent Cenozoic shortening followed by

132 ervations of the magmatism that results from rifting range from volcanic margins with two to three ti

133 passive seismic experiment in the Rio Grande rift region of the southwestern United States has produc

134 terally abrupt lithospheric thinning beneath rifted regions suggests efficient strain localization.

135 We show that the volume of rift-related magmatism generated, both in the northwest

136 , usually occurring within intra-continental rift-related settings, have strong light rare earth elem

137 ed mantle upwelling may explain a deficit of rift-related volcanics in the Rio Grande rift compared t

138 es the localization of crustal extension and rift-related volcanism.

139 ion-Range of Impaired Functioning Tool (LIFE-RIFT) (relationships, satisfaction with activities, work

140 phere deforms and accommodates strain during rifting remain enigmatic.

141 ed over a region four times the width of the rift's surface expression.

142 conclude that hydrothermal heating of young rift sediments alter deep-ocean budgets of bioavailable

143 Our results suggest that as this rift segment has formed, in thinned and intruded contine

144 farther from static Coulomb failure and the rift segments approximately 0.2 bar closer to static fai

145 nd present crustal-scale images across three rift segments.

146 nd trace-element differentiation patterns in rift settings suggest higher water content in plutonic m

147 ctic Mountains (TAM) are the world's longest rift shoulder but the source of their high elevation is

148 ch orbit, every portion of each tiger stripe rift spends about half the time in tension, which allows

149 l distances, we observe large differences in rifting style and magmatism--from wide rifting with mino

150 t segmented zones of melt supply beneath the rift, suggesting that buoyancy-driven active upwelling o

151 upper thermo-mechanical boundary layer in a rift system approaching the point of plate rupture.

152 ce ~200 ka along part of the on-land Red Sea rift system in Afar, Ethiopia, have a consistent age-pro

153 The geophysical data define a 2,500-km-long rift system in East Antarctica surrounding the Gamburtse

154 graphic barriers associated with the African Rift System in shaping population genetic patterns, as w

155 hin the low topography of the West Antarctic Rift System where geothermal fluxes are expected to be h

156 ophyletic lineages on each side of the Great Rift System, high genetic exclusivity, and restricted ge

157 gnized tectonic activity in the East African rift system.

158 the wider development of the West Antarctic rift system.

159 enetic variation structured across the Great Rift System.

160 t anisotropic axis follows trends of ancient rift systems older than 350 million years, suggesting "f

161 the Rio Grande rift compared to other major rift systems such as the Kenya rift.

162 seismic crisis in the weakly extended Natron rift, Tanzania, was released aseismically.

163 as a slowly diverging, westward propagating rift, tapering towards the East Pacific Rise.

164 In highly evolved rifts, tensile stresses from far-field plate motions acc

165 extreme geologic youth, and narrow tectonic rifts that exhibit coarse-grained ice and coincide with

166 nt--'Amasia'--will form either where Pangaea rifted (the 'introversion' model) or on the opposite sid

167 The 'incipient rift' then bounds a second microplate, north of the cloc

168 sification of rifts is by width, with narrow rifts thought to form as necking instabilities (where ex

169 on rates outpace thermal diffusion) and wide rifts thought to require a mechanism to inhibit localiza

170 t half the time in tension, which allows the rift to open, exposing volatiles, and allowing eruptions

171 he underlying mantle and the transition from rifting to seafloor spreading.

172 evidence that the 'incipient rift' has also rifted towards the east and opens anticlockwise about a

173 ke altered seismicity in the Andaman backarc rift-transform system.

174 ly present there during this period, and the Rift Valley did not present an impenetrable barrier to c

175 ives of Pan were present in the East African Rift Valley during the Middle Pleistocene, where they we

176 The emergence of Rift Valley fever (RVF) in the Middle East, and its cont

177 Rift Valley fever (RVF) is a mosquito-borne viral diseas

178 Rift Valley fever (RVF) is a mosquito-borne zoonotic dis

179 Rift Valley fever (RVF) is a mosquito-transmitted viral

180 Rift Valley fever (RVF) is a vector-borne viral disease

181 Rift Valley fever (RVF) is a veterinary and human diseas

182 Rift Valley fever (RVF) is a zoonotic and vector-borne d

183 Rift Valley fever (RVF) is a zoonotic disease endemic in

184 Rift Valley fever (RVF) is endemic to Africa, and the mo

185 ) or 1 x 10(5) plaque-forming units (pfu) of Rift Valley fever (RVF) MP-12 vaccine by oral, intranasa

186 A Rift Valley fever (RVF) risk mapping model using these c

187 Rift Valley fever (RVF) virus (RVFV) can cause severe hu

188 Rift Valley fever (RVF) virus historically has caused wi

189 Rift Valley fever (RVF) virus is a mosquito-borne human

190 Rift Valley fever (RVF) virus is a mosquito-borne RNA vi

191 Rift Valley fever (RVF) virus is a mosquito-borne virus

192 Rift Valley fever (RVF), an emerging mosquito-borne zoon

193 addition, some well-known bunyaviruses like Rift Valley fever and Crimean-Congo haemorrhagic fever v

194 Rift Valley fever and Toscana viruses are human pathogen

195 To test safety and efficacy of the Rift Valley fever MP-12 (RVF MP-12) vaccine, 9 healthy a

196 Rift Valley fever phlebovirus (RVFV) is a clinically and

197 ease caused by the related highly pathogenic Rift Valley fever phlebovirus in humans and domesticated

198 The NSm nonstructural protein of Rift Valley fever virus (family Bunyaviridae, genus Phle

199 Rift Valley fever virus (RVFV) (genus Phlebovirus, famil

200 Rift Valley fever virus (RVFV) (genus Phlebovirus, famil

201 Rift Valley fever virus (RVFV) (genus Phlebovirus, famil

202 Replication of infectious Rift Valley fever virus (RVFV) and cowpox virus (CPXV) w

203 Rift Valley fever virus (RVFV) causes major outbreaks am

204 Rift Valley fever virus (RVFV) causes outbreaks of sever

205 Rift Valley fever virus (RVFV) causes outbreaks of sever

206 Rift Valley fever virus (RVFV) causes recurrent insect-b

207 Rift Valley Fever virus (RVFV) causes recurrent outbreak

208 Rift Valley fever virus (RVFV) has been expanding its ge

209 Although the NSs of Rift Valley fever virus (RVFV) has been identified as an

210 Rift Valley fever virus (RVFV) is a highly pathogenic ar

211 Rift Valley fever virus (RVFV) is a member of the Bunyav

212 Rift Valley fever virus (RVFV) is a member of the genus

213 Rift Valley fever virus (RVFV) is a mosquito-borne human

214 Rift Valley fever virus (RVFV) is a mosquito-borne zoono

215 Rift Valley fever virus (RVFV) is a negative-sense RNA v

216 Rift Valley fever virus (RVFV) is a single-stranded RNA

217 Rift Valley fever virus (RVFV) is a zoonotic pathogen ca

218 Rift Valley fever virus (RVFV) is an arbovirus that is c

219 Rift Valley fever virus (RVFV) is an arbovirus within th

220 Rift Valley fever virus (RVFV) is an emerging pathogen t

221 Rift Valley fever virus (RVFV) is an emerging RNA virus

222 Analysis of purified Rift Valley fever virus (RVFV) particles demonstrated th

223 n the February 20 issue of Cell, report that Rift Valley Fever Virus (RVFV) targets cellular transcri

224 an Peninsula caused by the highly infectious Rift Valley fever virus (RVFV) that can be lethal to hum

225 ger the epidemics: They only modulated local Rift Valley fever virus (RVFV) transmission in ruminants

226 Rift Valley fever virus (RVFV), a member in the Phlebovi

227 Rift Valley fever virus (RVFV), a mosquito-borne phlebov

228 d in flies and mammals during infection with Rift Valley fever virus (RVFV), a mosquito-borne virus t

229 r the DEAD-box helicase DDX17 in restricting Rift Valley fever virus (RVFV), a mosquito-transmitted v

230 Rift Valley fever virus (RVFV), an ambisense member of t

231 Rift Valley fever virus (RVFV), belonging to the genus P

232 Rift Valley fever virus (RVFV), belongs to genus Phlebov

233 The mosquito-transmitted bunyavirus, Rift Valley fever virus (RVFV), is a highly successful p

234 embers of the Bunyaviridae family, including Rift Valley fever virus (RVFV), La Crosse virus, Andes v

235 Rift Valley fever virus (RVFV), like many other Bunyavir

236 the severe human hemorrhagic fever caused by Rift Valley fever virus (RVFV), thus providing an animal

237 viruses, including Zaire ebolavirus (EBOV), Rift Valley fever virus (RVFV), Venezuelan equine enceph

238 Rift Valley fever virus (RVFV), which belongs to the gen

239 c development to combat infections caused by Rift Valley fever virus (RVFV), which causes devastating

240 are vaccines against Dengue virus (DENV) and Rift Valley fever virus (RVFV), which recently have seen

241 zoonotic pathogens West Nile virus (WNV) and Rift Valley fever virus (RVFV).

242 Rift Valley fever virus (RVFV, family Bunyaviridae, genu

243 Rift Valley fever virus (RVFV; family Bunyaviridae) is a

244 Rift Valley fever virus (RVFV; family Bunyaviridae, genu

245 Rift Valley fever virus (RVFV; family Bunyaviridae, genu

246 RVF is caused by Rift Valley fever virus (RVFV; family Bunyaviridae, genu

247 time course tissue culture infections using Rift Valley fever virus and Francisella tularensis.

248 Rift Valley fever virus is a mosquito-borne pathogen of

249 Rift Valley fever virus is a pathogen of humans and anim

250 Crystal structures of Rift Valley fever virus N-RNA complexes reconstituted wi

251 was demonstrated by using a highly efficient Rift Valley fever virus reverse genetics system to gener

252 he RNA elements involved in the packaging of Rift Valley fever virus RNA genome segments, L, M, and S

253 Rift Valley fever virus strain MP-12 was generated by se

254 ntravenously with 3 x 10(6) PFUs of virulent Rift Valley fever virus strain ZH-501 (RVFV ZH-501) at 1

255 t cell factors that are critically needed by Rift Valley fever virus to uphold its replication agains

256 ers of the Bunyaviridae (La Crosse virus and Rift Valley fever virus) also cause increased biting rat

257 inal portion of the nucleocapsid (N) mRNA of Rift Valley fever virus, a phlebovirus of the Bunyavirid

258 at of the prefusion structure of the related Rift Valley fever virus, we show that these changes invo

259 , Marburg, Nipah virus, o'nyong-nyong virus, Rift Valley fever virus, West Nile virus, and yellow fev

260 omes in other phleboviral infections such as Rift Valley fever virus.

261 Rift Valley fever viruses carrying mutations of the M ge

262 ented virus-induced mortality from Ebola and Rift Valley fever viruses.

263 renaviruses, yellow fever, Crimean-Congo and Rift Valley fever viruses.

264 ed in Drosophila cells against West Nile and Rift Valley Fever viruses.

265 halitis, Venezuelan equine encephalitis, and Rift Valley fever viruses; and urbanization, in which hu

266 genus Phlebovirus, is the causative agent of Rift Valley fever, an important zoonotic infection in Af

267 Ps with 6 different viruses (Machupo, Junin, Rift Valley Fever, Crimean-Congo Hemorrhagic Fever, Nipa

268 Human epidemics of Rift Valley fever, often initiated by contact with infec

269 RNAs in three diverse phleboviruses, namely, Rift Valley fever, sandfly Sicilian, and Toscana viruses

270 The Ethiopian Rift Valley hosts the longest record of human co-existen

271 The Rift Valley itself functions as an obstacle to chimpanze

272 a potential Vibrio cholerae reservoir in the Rift Valley lakes and the possible contribution of the l

273 Geochemical properties in the rift valley sediments exhibited strong centimeter-scale

274 Animal movements in the Kenya Rift Valley today are influenced by a combination of top

275 anganese concentration along 1,100 km of the rift valley, we identify hydrothermal plumes dispersing

276 il sites occur in the semi-arid East African Rift Valley.

277 Atlantic Ocean that suggest that passages in rift valleys and ridge-flank canyons provide the most en

278 Seismic hazard in continental rifts varies as a function of strain accommodation by te

279 y of hydrous silicate magmas relative to dry rift volcanics.

280 tes, formed probably during Mesozoic Tethyan rifting, were carried below the subduction system by pla

281 ales longer than decades, the sensitivity of rift wetlands to climate change has been stressed by som

282 continental crust entrained during Gondwana rifting, whereas the isotope signature of the Pacific up

283 Olorgesailie, a key site in the East African Rift with abundant evidence of large-mammal butchery bet

284 The metabolic rift with nature created by modern cities fueled largely

285 es in rifting style and magmatism--from wide rifting with minor synchronous magmatism to narrow rifti

286 an Spreading Centre, 13 km west of the axial rift, within a gabbro and peridotite basement.

287 aharan populations involve a sample from the rift zone (Uganda), suggesting that the progenitors of P

288 body at intermediate depth in the southwest rift zone during 2002 to 2005.

289 the Krafla segment of the Northern Volcanic Rift Zone in Iceland and the Manda-Hararo segment of the

290 ma accumulation occurred in a section of the rift zone that was unclamped by previous dikes and earth

291 aterial are transferred from one side of the rift zone to the other.

292 ismic anisotropy in the upper mantle of this rift zone using observations of shear-wave splitting.

293 n people currently living within this active rift zone.

294 rowth from cut ends into and across the stab rift zone.

295 ombination of shallow dike intrusions in the rift zones and earthquakes along the base of the volcano

296 The formation of these rift zones and the development of ocean-ridge type topog

297 es from observations that mountain belts and rift zones cyclically form at the same locations despite

298 As continental rift zones mature the tectonic and volcanic processes as

299 extension become confined to narrow magmatic rift zones, reminiscent of oceanic spreading ridges.

300 cattering of teleseismic shear waves beneath rifted zones and adjacent areas in Southern California,