ライフサイエンスコーパス: rift

1 erferometric Fourier transform spectroscopy (RIFTS).

2 dike propagated along the extensional north rift.

3 ated Ocean Drilling Program at the Hess Deep rift.

4 tonic processes that formed the East African Rift.

5 view of the flexural deformation across the rift.

6 and character of sediment delivered into the rift.

7 aline rhyolite caldera in the Main Ethiopian Rift.

8 pisodic volcanic activity along the Terceira Rift.

9 e settings, but are divergent in continental rifts.

10 cally found at ocean islands and continental rifts.

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

12 overlapping tips of the Ethiopian and Kenyan rifts.

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

14 he mantle initiates early during continental rifting.

15 subsequent vertical motions associated with rifting.

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

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

18 ion with new numerical models indicates that rift abandonment resulted from progressive focusing of t

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

20 ds the transition between a wide continental rift and highly extended (<15 km) continental margin.

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

22 Rifting and magmatism are fundamental geological process

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

24 e lacking, leaving unanswered a link between rifting and slope instability.

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

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

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

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

29 It utilizes the cutting-edge Oculus Rift, and Leap Motion hand detection, resulting in intui

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

31 Recent investigations of rift architecture have suggested that multiphase deforma

32 Continental rifts are important sources of mantle carbon dioxide (CO

33 Young rifts are shaped by combined tectonic and surface proces

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

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

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

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

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

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

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

41 e processes over an extended period of early rift-basin development.

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

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

44 ong periods in the lithospheric mantle(4-6), rift CO(2) flux depends on lithospheric processes that c

45 and paleoenvironmental changes when a young rift connects to the global oceans.

46 0 to 169,000 km(3) beneath the South Georgia Rift, consistent with moderately elevated mantle potenti

47 during emplacement flexed down a previously rifted continental margin thereby contributing to subsid

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

49 m in the South Georgia Rift is caused by syn-rift decompression melting of a warm, enriched mantle.

50 and breaks up, forming either wide or narrow rifts depending on the thermo-mechanical state of the ex

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

52 ension and transform 'encroachment' into the rift domain.

53 m the southward propagation of the Ethiopian rift during the Pliocene but this propagation was short-

54 kes, and feeding a submarine eruption in the rift edge.

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

56 Discrete rifting episodes have been observed along two subaerial

57 Recurring rifting episodes, favored by stress induced by the D'Ent

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

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

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

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

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

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

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

65 ion of the Azores Plateau along the Terceira Rift exposes a lava sequence on the steep northern flank

66 m-affinity faults reactivated to accommodate rift extension and transform 'encroachment' into the rif

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

68 ged marine terraces associated with flexural rift-flank uplift.

69 glacials drove higher sediment flux from the rift flanks.

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

71 We show that the Ririba rift formed from the southward propagation of the Ethiop

72 wanan relatives when the Indian subcontinent rifted from Gondwana in the Late Jurassic, and colonized

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

74 isional coastwise transport of arc fragments rifted from the Congo/Tanzania cratonic nucleus in a man

75 In the Corinth Rift (Greece), the unique record of onshore and offshore

76 ay increase CO(2) fluxes in some continental rifts, helping to control the production and location of

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

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

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

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

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

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

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

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

85 Tanzania, indicating that plateau uplift and rifting in East Africa triggered large and potentially t

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

87 he early-mid Miocene is coeval with cratonic rifting in Tanzania, indicating that plateau uplift and

88 vik-Flatey Fault (HFF) dextral transform and rifting in the Northern Volcanic Zone.

89 hing a consensus regarding the long-standing rifts in the field.

90 strikingly similar to the broad continental rifts in the North American Cordillera and in the Aegean

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

92 This process impacts many aspects of rifting including rift morphology at breakup, and eventu

93 East African rift, the Kenyan and Ethiopian rifts, interact.

94 The May 2018 rift intrusion and eruption of Kilauea Volcano, Hawai'i,

95 est that CAMP magmatism in the South Georgia Rift is caused by syn-rift decompression melting of a wa

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

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

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

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

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

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

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

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

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

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

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

107 Rifted margins mark a transition from continents to ocea

108 d topographic uplift that were active on the rifted margins of the North Atlantic during the formatio

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

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

111 ides an outstanding possibility to constrain rift mechanics over a range of timescales.

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

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

114 argin asymmetry are produced by steady state rift migration.

115 ss impacts many aspects of rifting including rift morphology at breakup, and eventual ocean-ridge seg

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

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

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

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

120 lithospheric uplift, in which globe-spanning rifting occurs as a consequence of horizontal extension.

121 Our results suggest that rifting of oceanic lithosphere alternates between magmat

122 Rifting of the continents leading to plate rupture occur

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

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

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

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

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

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

129 This rifting phase was followed by alkaline volcanism at D.

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

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

132 calities, reflecting the influence of active rift processes on the palaeolandscape.

133 mosaic of Precambrian provinces affected by rifting processes.

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

135 t and food for many species in the Albertine Rift region.

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

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

138 ngest (after 10 Ma) phase of widespread EARS rift-related magmatism where it extends into the Indian

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

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

141 bduction initiation, suggesting that simpler rifting-related processes can more simply explain the av

142 phere deforms and accommodates strain during rifting remain enigmatic.

143 near pure extension directly connecting the rift sectors.

144 of basin infill will likely influence early rift sedimentary and faulting processes, potentially inc

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

146 Yet, rift segment growth and interaction remain enigmatic.

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

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

149 rift systems form by propagation of isolated rift segments that interact, and eventually evolve into

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

151 me fault pattern observed in the Barents Sea rift-shear margin.

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

153 Program (IODP) Expedition 381 in the Corinth Rift show 10s-100s of kyr cyclic variations in basin pal

154 gical data from the poorly documented Ririba rift (South Ethiopia) that reveals how two major sectors

155 aulting processes, potentially including syn-rift stratigraphy, sediment burial rates, and organic ca

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

157 nomaly (superplume) beneath the East African Rift System (EARS).

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

159 oncile competing ideas on the opening of the rift system by highlighting differences in orientation o

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

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

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

163 ern and Western Branches of the East African Rift System is one of the largest continental microplate

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

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

166 nsively along the flanks of the East African Rift System, including an offshore branch in the western

167 deep carbon below parts of the East African Rift System.

168 gnized tectonic activity in the East African rift system.

169 the wider development of the West Antarctic rift system.

170 enetic variation structured across the Great Rift System.

171 rain the mechanical behaviour of continental rift systems as well as the related seismic hazards.

172 Continental rift systems form by propagation of isolated rift segmen

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

174 ismic data across the Triassic South Georgia Rift that formed shortly before CAMP.

175 me that superplume mantle exists beneath the rift the length of Africa from the Red Sea to the Indian

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

177 ls how two major sectors of the East African rift, the Kenyan and Ethiopian rifts, interact.

178 e evolutionary process from wide continental rift to continental breakup remains enigmatic due to the

179 omain, and reflects the transition from wide rift to continental breakup.

180 Rift-transform interactions in this natural laboratory h

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

182 tle CO(2) flux and (3)He/(4)He ratios as the rift transitions from Archaean (cratonic) to Proterozoic

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

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

185 Rift Valley fever (RVF) is a mosquito-borne viral zoonos

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

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

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

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

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

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

192 Rift Valley fever (RVF) is an emerging, zoonotic, arbovi

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

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

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

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

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

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

199 Rift Valley fever and Toscana viruses are human pathogen

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

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

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

203 titis virus (VSV) (Rhabdoviridae family) and Rift Valley fever virus (RVFV) (Phenuiviridae family).

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

205 The method was validated using the zoonotic Rift Valley fever virus (RVFV) and Schmallenberg virus (

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

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

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

209 Rift Valley Fever virus (RVFV) causes recurrent outbreak

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

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

212 The increasing risk of Rift Valley fever virus (RVFV) infection as a global vet

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

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

215 Rift Valley fever virus (RVFV) is a mosquito-borne patho

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

245 mines in the replication of the bunyaviruses Rift Valley fever virus (vaccine strain MP-12) and La Cr

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

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

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

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

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

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

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

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

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

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

256 viruses, including influenza A virus, HIV-1, Rift Valley fever virus, and dengue virus, were unaffect

257 te was also observed for La Crosse virus and Rift Valley fever virus, highlighting the importance of

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 two other bunyaviruses, La Crosse virus and Rift Valley fever virus.

261 Louis Encephalitis, Sindbis, and Rift Valley Fever viruses), most with substantial transm

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

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

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

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

266 h concern including chikungunya, hantavirus, Rift Valley fever, cholera, plague, and Zika.

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

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

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

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

273 hot springs in the semi-arid southern Kenya Rift Valley.

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

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

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

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

278 Wide continental rifts, which can reach 1,000 km across, have been extens

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

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

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

282 apse of the Pu'u O'o Vent on the middle East Rift Zone (ERZ) of Kilauea Volcano, active since 1983.

283 a Volcano experienced its largest lower East Rift Zone (LERZ) eruption and caldera collapse in at lea

284 >2 m of associated uplift along the eastern rift zone and 2.5 m of caldera-wide subsidence.

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

286 Lake Baikal, lying in a rift zone in southeastern Siberia, is the world's oldest

287 matic activity into an oblique, throughgoing rift zone of near pure extension directly connecting the

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

289 uitive, convergent margin systems can induce rift zone volcanism and subsequent caldera subsidence.

290 n of >0.4 cubic kilometers of magma into the rift zone, extinguishing the lava lakes, and feeding a s

291 riven by changes in pore pressure within the rift zone, prompting opportunistic dyke intrusion and ul

292 n people currently living within this active rift zone.

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

294 the forceful intrusion of new magma into the rift zone.

295 latile-rich magmas typically associated with rift zones and extensional settings.

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,