ライフサイエンスコーパス: eruption

1 etween the waxing and waning portions of the eruption.

2 stic processes until the completion of tooth eruption.

3 its central district by about 3 m without an eruption.

4 e region of partial melt feeding the massive eruption.

5 ontent reductions in the years following the eruption.

6 and acute generalized exanthematous pustular eruption.

7 he mechanical interplay between collapse and eruption.

8 rapid attrition of Irf6-cKO molars following eruption.

9 R system during root morphogenesis and tooth eruption.

10 e rate and the intensity of the 180-day-long eruption.

11 th the recovery from the El Chichon volcanic eruption.

12 -duration quasi-static evolution to its fast eruption.

13 ctober ozone hole occurred after the Calbuco eruption.

14 nal magnetic reconnection which triggers the eruption.

15 l inferred prior to the violent 1914 Plinian eruption.

16 xia and mass extinctions shortly after their eruption.

17 ass enough magma to feed a future 1914-sized eruption.

18 cause most magmas are strongly degassed upon eruption.

19 neath volcanoes is likely a sign of imminent eruption.

20 onent into the magma reservoir just prior to eruption.

21 aggregation from a well-characterized 'wet' eruption.

22 ulation (AMOC) 15 years after the 1963 Agung eruption.

23 y tapped during the paroxysmal phase of this eruption.

24 vour an El Nino within 2 years following the eruption.

25 arine sediments coeval with the Deccan Traps eruptions.

26 g vapour injected into the atmosphere during eruptions.

27 stallization and gas exsolution for basaltic eruptions.

28 previously reported to cause lichenoid drug eruptions.

29 volatiles that can be released during these eruptions.

30 the excess sulfur released during explosive eruptions.

31 tion in the upper crust before many volcanic eruptions.

32 ing of volcanic CO2 fluxes helps to forecast eruptions.

33 e Reunion hot spot at the time of the Deccan eruptions.

34 nstrains potential vent locations for future eruptions.

35 solar activity and strong tropical volcanic eruptions.

36 amber dynamics and the triggers for volcanic eruptions.

37 be reconciled with, and sustain, long-lived eruptions.

38 ed crystal abundances for different basaltic eruptions.

39 present with other, more common erythematous eruptions.

40 t in the aftermath of invasions and volcanic eruptions.

41 has a long history of catastrophic explosive eruptions.

42 face reservoirs that are drained by volcanic eruptions.

43 iew is that intrusions must precede and feed eruptions.

44 s extruded in more massive and more episodic eruptions.

45 has impacts analogous to those from volcanic eruptions.

46 is likely to occur in all explosive volcanic eruptions.

47 art of the millennia between successive nova eruptions.

48 bution of magma mingling to highly explosive eruptions.

49 as temperature, that are inherent in natural eruptions.

50 n of ash sourced from high-latitude volcanic eruptions.

51 can be a key process during highly explosive eruptions.

52 beneath Sinabung and is being tapped during eruptions.

53 ment outcomes of patients with purpuric drug eruptions.

54 etic breakout is a universal model for solar eruptions.

55 ent occurrence of lightning during explosive eruptions.

56 -nova event, the system exhibited dwarf-nova eruptions.

57 use rupture, dyke injection, and a potential eruption?

58 he outset of the Puyehue-Cordon Caulle (PCC) eruption (~1 km(3)) in southern Chile which commenced on

59 st common cutaneous AEs were macular papular eruption (24 [29%]), pruritus (10 [12%]), and hypopigmen

60 ase or a decrease in precipitation following eruptions - a significant (p<0.1) decrease in streamflow

61 nding is that barring another major volcanic eruption, a detectable acceleration is likely to emerge

62 esis of population spread versus independent eruption, a model of spot formation by dispersing beetle

63 nd the potential impacts of a similar future eruption, a thorough physical understanding of the YWAS

64 es, likely the most representative of the BT eruption age, yield a weighted mean of 764.8 +/- 0.3/0.6

65 ovae display nova shells, but lack firm post-eruption ages, and are also dwarf novae at present.

66 e model simulations of both the 1815 Tambora eruption and a hypothetical analogous future eruption ar

67 e we use observations from Mount Etna's 2001 eruption and a magma ascent model to constrain timescale

68 hra thickness could affect attempts to infer eruption and dispersion parameters.

69 eland immediately after the Eyjafjallajokull eruption and had a vertical thickness of ~200 m, a width

70 ificance of the combined influence of the CI eruption and Heinrich Event 4 on European climate and po

71 olving towards conditions more favourable to eruption and identify field tests for predictions on how

72 Also, PTHLH, a hormone involved in tooth eruption and invasive growth, was one of the most differ

73 urface deformation preceding the Monte Nuovo eruption and investigate the shallow magma transfer.

74 ring fault accommodated deflation during the eruption and provided a pathway for a dike that propagat

75 phra deposits result from explosive volcanic eruption and serve as indirect probes into fragmentation

76 PR) in these progenitors leads to failure of eruption and significantly truncated roots lacking perio

77 elated serious adverse events (atypical drug eruption and thrombocytopenia) and two in the tenofovir

78 ntracontinental rhyolitic calderas formed on eruption and weathering of lithium-enriched magmas have

79 with approaches to criticality for volcanic eruptions and creep failure.

80 ailure scenarios both in the field (volcanic eruptions and landslides) and in the laboratory (rock an

81 ric gravity oscillations induced by volcanic eruptions and recorded by pressure sensors can be modele

82 ghts the inherent problem of under-reporting eruptions and the dangers of underestimating the long-te

83 , as reflected by post-caldera effusive lava eruptions and uplifted lake sediment.

84 --such as those associated with mastication, eruption, and orthodontic tooth movement-does the tissue

85 Tube growth, eruption, and shuffling droplets are subsequently observ

86 ect implications for the style of a possible eruption, and thus on the associated risk of any crisis

87 of anaphylaxis, 26 of nonimmediate cutaneous eruptions, and 17 of bronchospasm related to ASA/nonster

88 ent large-volume (>10 km(3)) caldera-forming eruptions, and eruptive fluxes were elevated five times

89 Ground deformation often precedes volcanic eruptions, and results from complex interactions between

90 bon reserves, magma build-up before volcanic eruptions, and subterranean tunnels.

91 eruption and a hypothetical analogous future eruption are examined, the latter occurring in 2085 assu

92 Eruptions are also followed by socioeconomic stress with

93 Eruptions are associated with revolt onset against elite

94 Accurate and precise ages of large silicic eruptions are critical to calibrating the geologic times

95 Multiple energetic pre-supernova eruptions are expected to occur in stars of 95 to 130 so

96 Magmatic intrusions and volcanic eruptions are intimately related phenomena.

97 focus on strong volcanic forcing since large eruptions are known to be a dominant mechanism in natura

98 tiger stripe terrain, while suggesting that eruptions are maintained over geological timescales.

99 In addition, the NH volcanic eruptions are more efficient in reducing the NH monsoon

100 Such eruptions are thought to recur on timescales of ten thou

101 The atmospheric sulfur yields of eruptions are variable and not well correlated with erup

102 Solar eruptions are well-recognized as major drivers of space

103 rix are surprisingly common in low intensity eruptions around the world, yet their origin is poorly u

104 Here we employ the 75 ka Toba super-eruption as a case study to show that quartz can resolve

105 Limitations in using major volcanic eruptions as a constraint on cloud feedbacks are also fo

106 ic observations to show that the most recent eruption at the fast-spreading East Pacific Rise just No

107 osols from large tropical explosive volcanic eruptions backscatter shortwave radiation and reduce the

108 Five years post-eruption, bacterial 16S rRNA gene and fungal internal tr

109 ssible reduction in seasonality after Deccan eruptions began, continuing through the meteorite event.

110 If magmas are vapour-saturated before eruption, bubbles cause the magma to become more compres

111 is insufficient as an indicator of imminent eruption, but instead represents the normal state of mag

112 open to the sea during the main phase of the eruption, but was flooded once the eruption had finished

113 ound that some jets are driven by base-field eruptions, but only one such study, of only one jet, pro

114 Nino tends to follow 2 years after volcanic eruptions, but the physical mechanism behind this phenom

115 ybrid events are used empirically to predict eruptions, but their ambiguous physical origin limits th

116 Here we show that explosive eruptions can also cause magma intrusion.

117 Volcanic eruptions can impact the mass balance of ice sheets thro

118 lfur released during large silicic explosive eruptions can induce global cooling.

119 Volcanic ash from explosive eruptions can provide iron (Fe) to oceanic regions where

120 Further, rhyolitic eruptions can switch repeatedly between effusive and exp

121 To characterize purpuric skin eruptions caused by epidermal growth factor receptor inh

122 Purpuric drug eruptions caused by epidermal growth factor receptor inh

123 ant biotic recovery did not begin until CAMP eruptions ceased.

124 lyses using microsatellites revealed no post-eruption changes in genetic variation in C. haigi, but a

125 duction which, in turn, has consequences for eruption column stability, tephra dispersal, aggregation

126 r knowledge, this is a previously unreported eruption comprising 2 distinct components: an eczematous

127 del simulations to show that a Pinatubo-like eruption cools tropical Africa and drives westerly wind

128 r elucidate these associations with detailed eruption data and examine the implications of this varia

129 The tempo and magnitude of these eruptions depends on the physical conditions under which

130 ening the SH monsoon, because the equatorial eruptions, despite reducing moisture content, have weake

131 We conclude that sustained high-eruption discharge and long-lived high-pore pressure in

132 eds of approximately 5-20 m s(-1), fed by an eruption discharging magma at rates up to approximately

133 Here, we show that the 1815 eruption drove strong responses in both the ocean and cr

134 f thousands of years or more with punctuated eruptions during these periods.

135 d exsolution plays a key role in controlling eruption dynamics in basaltic volcanism.

136 decisive in determining the mobilization and eruption dynamics of Earth's largest volcanic systems, r

137 n rate and help to refine interpretations of eruption dynamics.

138 gmas is of great importance for interpreting eruption dynamics.

139 Unrest at large calderas rarely ends in eruption, encouraging vulnerable communities to perceive

140 iated with submarine volcanoes, following an eruption event, plays an important role in the supply of

141 mately 192-y series of halogen-rich volcanic eruptions exactly at the start of accelerated deglaciati

142 ucleation and growth and could have enhanced eruption explosivity.

143 tems such as the Earth's climate to volcanic eruptions, extreme events or geoengineering.

144 rvoirs are rarely molten and only capable of eruption for durations as brief as 1,000 years following

145 "seasons", which include enhanced bursts of eruptions for several months, followed by quiet periods.

146 lly significant reductions in flow following eruptions for the Amazon, Congo, Nile, Orange, Ob, Yenis

147 aldera centre, that has been feeding lateral eruptions for the last ~5 ka.

148 ell studied examples of largely crystal-poor eruptions (for example, Katmai, Taupo and Minoan) often

149 These new inferences are important for eruption forecasting and risk mitigation, and have signi

150 Despite their importance for eruption forecasting the causes of seismic rupture proce

151 uch a nearly realistic simulation of a solar eruption from origin to onset can provide important insi

152 Observations show eruptions from "tiger stripe" fissures that are sustaine

153 atic reservoirs, often associated with large eruptions from long-lived magmatic systems.

154 olony expansion were abruptly ended by large eruptions from the Deception Island volcano, resulting i

155 The eruption generated strong tremor that was recorded by se

156 se of the eruption, but was flooded once the eruption had finished.

157 Extensive fallout from these massive eruptions has been found >2,800 km from Mount Takahe.

158 Although its presence after solar eruptions has been verified by spacecraft measurements n

159 ransfer changes prior, during and after nova eruptions has not hitherto been found.

160 focused on tropical eruptions; high-latitude eruptions have drawn less attention because their impact

161 Volcanic eruptions have episodically interfered with healing, par

162 howed that over the last 110 years, volcanic eruptions have influenced ASM variations on an inter-dec

163 These eruptions have the potential to influence global climate

164 es of Earth's magnetic field following Solar eruptions, have been proposed as one such trigger.

165 Most studies have focused on tropical eruptions; high-latitude eruptions have drawn less atten

166 The spatially random eruption hypothesis was found to be highly improbable.

167 Europe, recognition of ash from the Oruanui eruption in Antarctica dramatically increases the reach

168 e we show that the massive 2014-2015 fissure eruption in Holuhraun, Iceland, reduced the size of liqu

169 ithium abundance in zircons from a rhyolitic eruption in New Zealand reflected short-lived residence

170 Hepatitis C patients suffering from drug eruptions in association with administration of pegylate

171 ends to peak during the year following large eruptions in simulations of the Fifth Coupled Model Inte

172 which cover between two and 6 major volcanic eruptions in the 20(th) and late 19(th) century.

173 e is presented of explosive Late Pleistocene eruptions in the Pacific Arc, currently undocumented in

174 marker to identify the imprint of the Deccan eruptions in the stratigraphic record and is evidence of

175 nds and then by using the number of volcanic eruptions in the world.

176 the magnitude and timing of large explosive eruptions in this region is poor.

177 n than the equatorial ones, and so do the SH eruptions in weakening the SH monsoon, because the equat

178 e pathogenesis of psoriasis-related pustular eruptions including generalized pustular psoriasis, palm

179 Observations following major volcanic eruptions indicate that aerosol enhancements confined to

180 ian dust and of ash from occasional volcanic eruptions, indicating that metallurgic production during

181 owever, during the Last Glacial, the initial eruption-induced climate response was prolonged by NH gl

182 idable natural events such as major volcanic eruptions interact with anthropogenic warming unforeseen

183 brief vigorous outward flow of fluid (named 'eruptions') into the tumour interstitial space.

184 Here we show how an eruption is initiated in a non-potential magnetic flux-e

185 from a magma reservoir to the surface before eruptions is a major challenge.

186 ant (p<0.1) decrease in streamflow following eruptions is detected in northern South American, centra

187 rial failure and broadly applied to volcanic eruptions, landslides and other phenomena.

188 eased surface UV radiation indicate that the eruptions led to stratospheric ozone depletion.

189 posed that a decreasing pressure of volcanic eruptions led to the oxygenation of the atmosphere.

190 es again-with accretion returning to the pre-eruption level and leading to a new nova explosion.

191 lated adverse events including maculopapular eruption, lichenoid reactions, pruritus, and vitiligo ha

192 ns are variable and not well correlated with eruption magnitude and for many eruptions the volume of

193 ive interference caused by the Pinatubo 1991 eruption may have damped the observed decreasing trend o

194 These stochastic eruptions may explain the enhanced extravasation of nano

195 Our results show that explosive eruptions may rapidly force significant quantities of ma

196 Pozzuoli to the location of the last caldera eruption (Mt.

197 rowth was slowed down by an effusive fissure eruption near the end of the dyke.

198 Furthermore, transposon eruptions occurring in the p53(-) germline were incited

199 he binary star underlying the classical nova eruption of 11 March AD 1437, and independently confirm

200 s volcanic activity, in particular the great eruption of AD 79, on all of the ancient cities of the B

201 emplaced laccolith during the 2011 rhyolite eruption of Cordon Caulle, Chile.

202 ietal impact of the April/May 2010 Icelandic eruption of Eyjafjallajokull generated renewed interest

203 YWAS) has been widely attributed to the 1815 eruption of Indonesia's Mt.

204 history by ubiquitous and sustained massive eruption of lava, forming several enormous igneous plate

205 response to magma ascension and is loaded by eruption of lavas.

206 Random eruption of locally endemic populations was tested using

207 ing teeth were systematically accompanied by eruption of molars faster than permanent premolars.

208 ned climate model simulations shows the 1991 eruption of Mt Pinatubo to likely have masked the accele

209 w in the two springs after the 1991 volcanic eruption of Mt.Pinatubo.

210 The March 2016 eruption of Pavlof Volcano, Alaska, produced an ash plum

211 The caldera-forming eruption of Santorini in the Late Bronze Age is known to

212 at circa 252 Ma and has been linked with the eruption of the basaltic Siberian Traps large igneous pr

213 Triassic mass extinction overlapped with the eruption of the Central Atlantic Magmatic Province (CAMP

214 The eruption of the Central Atlantic Magmatic Province (CAMP

215 f two closely timed potential causal events: eruption of the Deccan Traps volcanic province and impac

216 y, therefore, is to assess the potential for eruption of the large volumes of crystal-poor, silicic m

217 e Chicxulub asteroid impact (Mexico) and the eruption of the massive Deccan volcanic province (India)

218 ydrodynamic nature of the phenomenon ensures eruption of the nanoclusters towards a much colder regio

219 tained before and immediately after the 2011 eruption of the Puyehue-Cordon Caulle volcanic complex i

220 tic conduits widely believed to have fed the eruption of the SLIP basalts.

221 ntroduction of Ni into the atmosphere during eruption of the SLIP lavas.

222 istory of individual zircon crystals from an eruption of the Taupo Volcanic Zone, New Zealand.

223 y influenced by vegetation recovery after an eruption of the Tianchi volcano in 1702.

224 r whether the new spots are spatially random eruptions of a locally endemic population or a mode of M

225 Caldera-forming eruptions of island volcanoes generate tsunamis by the i

226 ication of this method to the main explosive eruptions of Mount Somma-Vesuvius highlights two main ma

227 Explosive volcanic super-eruptions of several hundred cubic kilometres or more ge

228 Large-volume caldera-forming eruptions of silicic magmas are an important feature of

229 Coronal mass ejections (CMEs) are episodic eruptions of solar plasma and magnetic flux that travel

230 Ptolemaic vulnerability to volcanic eruptions offers a caution for all monsoon-dependent agr

231 Large volcanic eruptions on Earth commonly occur with a collapse of the

232 ous volcanic melts and the largest explosive eruptions on our planet consist of calcalkaline rhyolite

233 Magnetically driven eruptions on the Sun, from stellar-scale coronal mass ej

234 igma analytical/full uncertainty) indicating eruption only approximately 7 ky following the Matuyama-

235 sing indicates that an intrusion began after eruption onset and caused severe (>200 m) uplift over 1

236 s and can be strongly influenced by volcanic eruptions or anthropogenic emissions.

237 variability coinciding with either volcanic eruptions or possible wild fire activity.

238 ometrically-dated Tambora-sized or larger NH eruptions over the interval 30 to 80 ka BP are associate

239 ed on the variations in crown height, dental eruption pattern, and associated body mass of 69 notoung

240 pared with that during the inactive volcanic eruption period (1936-1962).

241 During the active volcanic eruption periods (1901-1935 and 1963-1993), significantl

242 We found that during active volcanic eruption periods, which correspond to a negative AMO sta

243 the presence of a diffuse papular descending eruption, petechiae on the palate, and hyperemic sclerae

244 va Centauri 2009) covering its pre- and post-eruption phases and precisely documenting its evolution.

245 st continental flood basalt provinces, whose eruption played a role in the Cretaceous-Paleogene extin

246 Silicic volcanic eruptions pose considerable hazards, yet the processes l

247 ing can impact magmatic fO2 before or during eruption, potentially obscuring relationships between th

248 to remove the residual signal from volcanic eruptions present in the OMI data.

249 degassing trends suggests that a decrease in eruption pressure would not produce this effect.

250 Large volcanic eruptions produce sulfur dioxide, which in turn produces

251 l kinship with Toba, and zircons from recent eruption products suggest Toba's climactic magma reservo

252 Volcanic eruptions provide tests of human and natural system sens

253 vents will improve (lower) estimates of mass eruption rate and help to refine interpretations of erup

254 s were elevated five times above the average eruption rate for the past 700 ka.

255 evealing the timing, location, and volume of eruption-related magma movements.

256 ma and coal during the Siberian flood-basalt eruptions released large amounts of CO2 and CH4 into the

257 hazards, yet the processes leading to these eruptions remain poorly known.

258 timing of marine biotic recovery versus CAMP eruptions remains uncertain.

259 The skin eruption responded well to corticosteroids and did not r

260 Optical illusions in the curtain eruptions resulting from a combination of viewing direct

261 Extensive seismic activity preceding the eruption shows that inflation is accommodated by the rea

262 f volcanic emissions and characterization of eruption size and intensity.

263 feasibility of using gravity waves to derive eruption source parameters such as duration of the injec

264 Pleistocene Campanian Ignimbrite (CI) super-eruption (Southern Italy) is the largest known volcanic

265 Once north of the caldera, the eruption stepped westward, and a dike propagated along t

266 he hibernation hypothesis predicts that nova eruptions strongly affect the mass-transfer rate in the

267 le affects the dynamics of melting, volcanic eruption style and the evolution of Earth's atmosphere v

268 ch repeatedly between effusive and explosive eruption styles and this transition is difficult to attr

269 ctivity and the signaling network related to eruption, supporting and further extending the concept t

270 ransition ( 690 degrees C) to above inferred eruption temperatures (>1150 degrees C) for durations of

271 lations further emphasize that Pinatubo-like eruptions tend to shorten La Ninas, lengthen El Ninos an

272 April 2015, the seismic network captured an eruption that culminated in explosive acoustic signals w

273 cause it is impossible to forecast the solar eruptions that can cause these terrestrial events until

274 ay, and that it is caused either by episodic eruptions that emplace voluminous lava flows or by a cyc

275 related with eruption magnitude and for many eruptions the volume of erupted material is much greater

276 During the century before and after an eruption, the 'novalike' binary systems that give rise t

277 Monte Nuovo; this peripheral source fed the eruption through a shallower source, 0.4 +/- 0.3 km deep

278 imultaneously explain the persistence of the eruptions through the tidal cycle, the phase lag, and th

279 xide, which in turn produces aerosols; these eruptions thus represent a natural experiment through wh

280 hquakes, where we were able to calculate the eruption time and location to a satisfactory degree of a

281 ct hypothesis, the lack of a high-resolution eruption timeline for the Deccan basalts has prevented f

282 r Antarctica-plausibly link the Mount Takahe eruptions to the onset of accelerated Southern Hemispher

283 osits are correlated to known high-magnitude eruptions (Towada-H, Japan, ca 15 ka BP and Mount St Hel

284 Volcanic eruptions transfer huge amounts of gas to the atmosphere

285 altered roof material may represent a viable eruption trigger in large Toba-style magmatic systems.

286 contrary to the microsatellite analyses, the eruption was associated with a small but significant dec

287 six centuries CE have recorded how the AD 79 eruption was followed by a complete overhaul of Neapolis

288 Another possible eruption was recorded at the same position in 1954.

289 A 2015 eruption was successfully forecast on the basis of this

290 icic calderas form during explosive volcanic eruptions when magma withdrawal triggers collapse along

291 these clasts may be recycled from low level eruptions where they recrystallize by heating within the

292 is, acute generalized exanthematous pustular eruption), whereas hypomorphic mutations were identified

293 level) dating results for the age of the CI eruption, which substantially improve upon or augment pr

294 of the thermal history of magma feeding such eruptions, which largely controls crystallinity and ther

295 ze estimates, and studies conflating lack of eruption with impaction.

296 female and 2 male) and 18 with purpuric drug eruptions with pustules (mean [SD] age, 64 [11] years; 1

297 nclusions and Relevance: Papular and nodular eruptions with scale, as well as mucosal erosions, with

298 The most spectacular eruptions, with a ten-thousandfold increase in brightnes

299 ateral transfer of magma feeding non-central eruptions within the caldera.

300 Thirty-two patients, 14 with purpuric drug eruptions without pustules (mean [SD] age, 60 [11] years