ライフサイエンスコーパス: eruption

1 owed for the successful forecast of its 2015 eruption.

2 the time interval duration from the previous eruption.

3 quired for normal bone development and tooth eruption.

4 es in advance of changing hazards during the eruption.

5 such as high bone mass and failure of tooth eruption.

6 hours of collection during the 2018 Kilauea eruption.

7 fraction was withdrawn before the end of the eruption.

8 calization at conduit margins, and explosive eruption.

9 ound 0.5 degrees C for a few years after the eruption.

10 ted by the injection of fresh magma prior to eruption.

11 etween the waxing and waning portions of the eruption.

12 cause most magmas are strongly degassed upon eruption.

13 onent into the magma reservoir just prior to eruption.

14 reported on entecavir induced lichenoid drug eruption.

15 as malocclusions and delayed or failed tooth eruption.

16 uninhabitable for years to decades after the eruption.

17 es it appear after the outsized 1257 Samalas eruption.

18 genetic disorder exclusively affecting tooth eruption.

19 extending the surface cooling caused by the eruption.

20 ental impact of the Thera/Santorini volcanic eruption.

21 the depth of their source and the timing of eruption.

22 ce and severity change over time after tooth eruption.

23 redicted timing of through-going failure and eruption.

24 ke intrusion and ultimately facilitating the eruption.

25 Samalas eruption.

26 eft shoulder and developed systemic pruritic eruptions.

27 vesicles between the samples from the three eruptions.

28 in the seismic energy generation during the eruptions.

29 tigating the dynamics and timing of volcanic eruptions.

30 ever and self-limiting vesiculopustular skin eruptions.

31 rence of volcanic lightning during explosive eruptions.

32 has impacts analogous to those from volcanic eruptions.

33 as temperature, that are inherent in natural eruptions.

34 tion in the upper crust before many volcanic eruptions.

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

36 is likely to occur in all explosive volcanic eruptions.

37 art of the millennia between successive nova eruptions.

38 bution of magma mingling to highly explosive eruptions.

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

40 can be a key process during highly explosive eruptions.

41 beneath Sinabung and is being tapped during eruptions.

42 ment outcomes of patients with purpuric drug eruptions.

43 etic breakout is a universal model for solar eruptions.

44 ent occurrence of lightning during explosive eruptions.

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

46 re forced by orbital variations and volcanic eruptions.

47 seismicity and other precursors of dyke-fed eruptions.

48 characterize electrical activity in volcanic eruptions.

49 s adverse reactions, most commonly acne-like eruptions.

50 cts caused by historic droughts and volcanic eruptions.

51 characterized by recurrent and pruritic skin eruptions.

52 a white dwarf star ignites a classical nova eruption(1,2)-a thermonuclear runaway in the accumulated

53 Skin symptoms included papular eruptions (100%), sclerodermoid features (91%), and leon

54 volcanic area; (iii) the time since the last eruption (70 ka) exceeds the average recurrence interval

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

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

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

58 the periodontal ligament (PDL) include tooth eruption and anchorage, force absorption, and provision

59 nced its largest lower East Rift Zone (LERZ) eruption and caldera collapse in at least 200 years.

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

61 ks in physiological conditions such as tooth eruption and movement and also for periodontal diseases.

62 genitor cell populations that regulate tooth eruption and tooth root formation are beginning to be un

63 w normal during the 2 y period following the eruption and unusually wet conditions.

64 years of research, the drivers of population eruptions and crashes are still not fully understood and

65 lly to the timing and frequency of Kilauea's eruptions and intrusions.

66 Vesicular, urticarial, and maculopapular eruptions and livedo, necrosis, and other vasculitis for

67 lation between some continental flood basalt eruptions and mass extinctions has been proposed to indi

68 s the main external forcings (i.e., volcanic eruptions and solar activity) on NAO variability which,

69 gma volume flowing out of the chamber during eruptions and the volume of the chamber.

70 eruption, the ~650-y-old Deadman Creek Dome eruption, and several mafic subvolcanic orbicules and pl

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

72 ce of GS etiologies, such as altered passive eruption (APE) and hypermobile upper lip (HUL), has not

73 Individuals with altered passive eruption (APE) are assumed to be more susceptible to per

74 ronmental and climatic impacts of this large eruption are not well known because the eruption magnitu

75 Eruptions are also followed by socioeconomic stress with

76 Caldera-forming eruptions are among Earth's most hazardous natural pheno

77 These eruptions are associated with fast spectral transitions

78 Eruptions are associated with revolt onset against elite

79 cause of these extinctions, the Deccan Traps eruptions are believed to have contributed to extinction

80 The skin eruptions are classically diffuse, symmetric maculopapul

81 Large-volume pyroclastic eruptions are not known from the basalt-dominated Britis

82 Explosive volcanic eruptions are the largest non-anthropogenic perturbation

83 Volcanic eruptions are thought to be a key driver of rapid climat

84 , crystallization depths of magmas that feed eruptions are thought to be less than nine kilometres(2)

85 recent models of volcano unrest suggest that eruptions are triggered when conditions of critical stre

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

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

88 d such as asteroid impacts and supervolcanic eruptions, as well as risks that remain unknown.

89 of ~5 x 10(6) kg/s for the initial explosive eruption associated with a flank collapse.

90 Models consistently predict eruption at a reservoir pressure threshold of 12-14 MPa

91 show that in December 2018 an intra-caldera eruption at Ambrym preceded normal faulting with >2 m of

92 Processes related to eruptions at arc volcanoes are linked by structures that

93 , lending support to the interpretation that eruptions at Axial Seamount are triggered by reservoir o

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

95 ccurrence of several closely spaced volcanic eruptions between 1108 and 1110 CE.

96 ent with the forced response to low-latitude eruptions but further, that this warming is a response t

97 volcanic seismicity that sometimes precedes eruptions but mostly occurs at quiescent volcanoes.

98 n El Nino-like response in the year after an eruption, but this response is not statistically signifi

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

100 eruptive behavior occur during many volcanic eruptions, but typical analytical techniques are too slo

101 mantle melts and the triggering of volcanic eruptions by supply of magma from greater depth.

102 Volcanic eruptions can affect global climate through changes in a

103 ion columns are developed; meaning that such eruptions can generate extensive tephra-fall and pyrocla

104 Nevertheless, occasional more intense eruptions can present a serious danger.

105 Such eruptions cause a strong asymmetrical hemispheric coolin

106 The delay between intense unrest and eruption caused considerable challenges to emergency res

107 Purpuric drug eruptions caused by epidermal growth factor receptor inh

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

109 and 82 km(3) of magma was dispersed from an eruption coignimbrite column that rose to ~45 km by mode

110 Large Igneous Province eruptions coincide with many major Phanerozoic mass exti

111 one deposits, moderate to intense, unstable, eruption columns are developed; meaning that such erupti

112 sponse to large volcanic eruptions: Volcanic eruptions cool the surface, thus masking the relative El

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

114 mount has exhibited an inflation predictable eruption cycle, which allowed for the successful forecas

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

116 Her eruption did not result in lichenification and was not f

117 Finally, our analysis suggests that volcanic eruptions do not lead to an overall global reduction in

118 1477) claimed that large volcanic eruptions do not produce a detectable El Nino response.

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

120 gmas is of great importance for interpreting eruption dynamics.

121 The comparison with Pele's hair of similar eruptions elsewhere demonstrates that there is no univoc

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

123 ses, suggest that magmatic rejuvenation (and eruption) events, as reflected in crystal growth times,

124 The eruption evolved, and its impact expanded, as a sequence

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

126 ion of 14 +/- 2 Tg S associated with the TBJ eruption, exceeding those of the historic eruption of Pi

127 nearity between magma decompression rate and eruption explosivity.

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

129 Eruption forecasting is inherently challenging in cascad

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

131 c deformation, crustal stress evolution, and eruption forecasts.

132 The Tierra Blanca Joven (TBJ) eruption from Ilopango volcano deposited thick ash over

133 re work is needed to confirm that a volcanic eruption from Mt.

134 attributed in previous studies to a volcanic eruption from the submarine Kuwae caldera in Vanuatu.

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

136 report observations of quasi-periodic X-ray eruptions from the nucleus of GSN 069 over the course of

137 Under slow decompression typical of effusive eruptions, gas extraction is promoted, whereas under rap

138 The eruption generated strong tremor that was recorded by se

139 vations suggest that, rather than portending eruptions, global DLP activity may more commonly be indi

140 lance, the response of the Southern Ocean to eruptions has yet to be understood.

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

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

143 o reveal a previously unknown major tropical eruption in 1108 CE.

144 Kelut eruption in 2014, stratospheric ash-rich aerosols were o

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

146 rence during the 3 June 2018 Volcan de Fuego eruption in Guatemala.

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

148 essentially recapitulate primary failure of eruption in humans, a rare genetic disorder exclusively

149 ying ultramafic nodules from the Borgarhraun eruption in Iceland.

150 ooth root malformation, and failure of tooth eruption in molars, which essentially recapitulate prima

151 erturbs the fields, triggering their surface-eruption in the form of new cycle spots.

152 hing the lava lakes, and feeding a submarine eruption in the rift edge.

153 er, identification of stratospheric volcanic eruptions in the geological record and their causal link

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

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

156 During eruptions, inelastic processes including magma mush eros

157 show that immediately before and during the eruption, infiltration of rainfall into Kilauea Volcano'

158 Tooth eruption is a continuous biological process with dynamic

159 Tooth eruption is a unique biological process by which highly

160 Pinatubo eruption is consistent with the forced response to low-l

161 magma volume leaving the chamber during each eruption is estimated at 0.064 km(3).

162 from any single classical or recurrent nova eruption is known(8-10), but thousands of successive rec

163 as the time of 70 kyr elapsed since the last eruption is of the same order of the longest dormancies

164 e and slower recovery from the 1991 Pinatubo eruption lead to later signal detection (between 1997 an

165 ive forcing from this massive, high-latitude eruption led to pronounced changes in hydroclimate, incl

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

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

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

169 re climatic anomalies following the proposed eruptions, likely providing the environmental preconditi

170 arge eruption are not well known because the eruption magnitude and date are not well constrained.

171 gest that warming induced by future volcanic eruptions may further enhance the vulnerability of the i

172 ars ago suggests that stratospheric volcanic eruptions may have contributed to synergetic environment

173 cal surface cooling caused by large volcanic eruptions may mask El Nino warming at our central Pacifi

174 Within a given eruption, melt inclusions trapped in primitive olivine c

175 irst months of Paricutin volcano monogenetic eruption (Mexico, 1943-1952) record fast growth and larg

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

177 magma reservoir pressure threshold at which eruptions occur, and as such, an overpressure eruption t

178 Asama, whose largest Holocene eruption occurred in August 1108 CE and is credibly docu

179 In 2018, a highly destructive eruption occurred on the lower flank of Kilauea Volcano,

180 The new date confirms the eruption occurred within the Early Classic phase when Ma

181 Moreover, statistical analysis of historic eruption occurrence suggests that rainfall patterns cont

182 to investigate the impact of strong volcanic eruptions occurring in the tropical Northern (NH) and So

183 reak-up, both in our experiments and natural eruptions, occurs by both viscous and capillary instabil

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

185 older, stored magma-including the unexpected eruption of andesite-and hotter magma delivered during d

186 Failed eruption of canines or second molars in affected persons

187 From June to August 2018, the eruption of Kilauea volcano on the island of Hawai'i inj

188 The 2018 summit and flank eruption of Kilauea Volcano was one of the largest volca

189 The May 2018 rift intrusion and eruption of Kilauea Volcano, Hawai'i, represented one of

190 ced tsunami since the catastrophic explosive eruption of Krakatau in 1883 and the sector collapse of

191 ustal hydrothermal alteration related to the eruption of large igneous provinces is poorly known and

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

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

194 Random eruption of locally endemic populations was tested using

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

196 The 1257 CE eruption of Mount Samalas (Indonesia) is the source of t

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

198 BJ eruption, exceeding those of the historic eruption of Pinatubo in 1991.

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

200 as well as the extinctions are linked to the eruption of the Central Atlantic Magmatic Province (CAMP

201 er, we provide a date for the youngest known eruption of the MSVD and assess the timing of the most r

202 interval and the time elapsed since the last eruption of the MSVD.

203 rt a surface air temperature response to the eruption of the order of -1 degrees C, performing well a

204 climate change coincide temporally with the eruption of the smallest DT phases, suggesting that eith

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

206 ts exploration as a potential marker for the eruption of Thera.

207 previously speculated that a large volcanic eruption of unknown origin was the most likely cause.

208 industry is found at Dhaba spanning the Toba eruption of ~74 ka (i.e., the Youngest Toba Tuff, YTT) b

209 We extend these findings to caldera-forming eruptions of crystal-rich magma where large overpressure

210 several days before the onset of voluminous eruptions of fast-moving flows that destroyed hundreds o

211 of Pele's hair formed during three different eruptions of Kilauea volcano have been investigated: fou

212 Caldera-forming eruptions of mushy silicic magma are among the most cata

213 up of severe skin disorders characterized by eruptions of neutrophil-filled pustules.

214 of aerosols and/or ash particles during the eruptions of the CAMP basalts.

215 E) is associated with a rise in CO(2) due to eruptions of the Central Atlantic Magmatic Province (CAM

216 c to gauge ENSO's response to large volcanic eruptions of the last millennium.

217 c ice cores that one of the largest volcanic eruptions of the past 2,500 y occurred in early 43 BCE,

218 e Phanerozoic, has been widely attributed to eruptions of the Siberian Traps Large Igneous Province,

219 t and very cold conditions from this massive eruption on the opposite side of Earth probably resulted

220 The main magma source for eruptions on Etna (Italy) is poorly constrained.

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

222 The effect of the volcanic eruptions on the ITCZ and hence on TC activity lasts for

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

224 ) from a stellar companion leads to frequent eruptions on timescales of years(4,5) to decades(6).

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

226 layed manner as different forms of cutaneous eruptions or liver injury consistent with priming of an

227 ral drivers such as large explosive volcanic eruptions or multidecadal cycles in ocean circulation oc

228 catastrophic events such as phreato-magmatic eruptions or volcano destabilizations.

229 er the solar flare, including the associated eruption, particle acceleration, and plasma heating.

230 The inflation predictable eruption pattern suggests a magma reservoir pressure thr

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

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

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

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

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

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

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

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

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

240 on these estimates it is likely that the TBJ eruption produced a cooling of around 0.5 degrees C for

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

242 acement mode of CAMP magmas, favouring rapid eruption pulses (a few centuries each).

243 The results provide a clear link between eruption rate fluctuations and their driving processes i

244 munities on active volcanoes, and volumetric eruption rate is one of the primary factors controlling

245 The time scales and driving forces of eruption rate variability, however, remain poorly unders

246 According to this model, maximum eruption rates occurred before and after the K-Pg extinc

247 he primary vent exhibited substantial cyclic eruption rates on both short (minutes) and long (tens of

248 We estimated Deccan eruption rates with uranium-lead (U-Pb) zircon geochrono

249 However, because of eruption-related degassing of sulfur (S) and the composi

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

251 Forecasting explosive eruptions relies on using monitoring data to interpret t

252 The dynamics of peralkaline rhyolite eruptions remain elusive with no direct observations rec

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

254 The sources of these eruptions remain unknown, but we propose that Mt.

255 Determining whether magma fragments during eruption remains a seminal challenge in volcanology.

256 wever, the exact triggering mechanism of its eruptions remains ambiguous.

257 gh quality records of stratospheric volcanic eruptions, required to model past climate variability, h

258 nd likely not a large stratospheric tropical eruption, requires revision of the stratospheric sulfate

259 , but thousands of successive recurrent nova eruptions should be capable of generating shells hundred

260 anomaly of sulfate for the largest volcanic eruptions, showing a further change in atmospheric chemi

261 plumbing system at the long-lived Pu'u 'O'o eruption site caused widespread pressurization in the vo

262 be considered as a promising step to derive eruption source parameters from geophysical data in real

263 Deriving eruption source parameters from geophysical data is crit

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

265 may not be suitable for the investigation of eruption-specific processes, they record timescales of c

266 o detectors aimed at earthquake and volcanic eruption studies, and monitoring of nuclear sites.

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

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

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

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

271 ings reveal important characteristics of the eruptions that gave rise to them: that despite the relat

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

273 crysts from the 1915 Mount Lassen rhyodacite eruption, the ~650-y-old Deadman Creek Dome eruption, an

274 During these eruptions, the X-ray count rate increases by up to two o

275 The discovery, which presages the eruption there by more than eight months, suggests that

276 d the product of the 1104 CE Hekla (Iceland) eruption, this event can now be associated with substant

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

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

279 ceted study we have resolved the date of the eruption to 431 +/- 2 CE by identifying the ash layer in

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

281 wo distinct periods of lightning during this eruption totaling 75 unique lightning flash occurrences

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

283 A precipitation-induced eruption trigger is consistent with the lack of precurso

284 ruptions occur, and as such, an overpressure eruption triggering mechanism.

285 We test hypotheses of eruption triggering using 3-dimensional finite element m

286 ndamental climate response to large volcanic eruptions: Volcanic eruptions cool the surface, thus mas

287 A reconstructed eruption volume of >=5km(3) DRE is derived, suggesting a

288 t, it may be difficult to forecast the final eruption volume; pressure in a magma body may drop well

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

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

291 ction of new nutrient sources, but not tooth eruption, was associated with increasing complexity.

292 phases and the time elapsed between the last eruptions, we conclude that the waning/extinguishment of

293 This, combined with observations of the 1963 eruption which caused more than thousand fatalities, sug

294 he fine-scale plasma structure of very small eruptions, which are frequently ejected from the Sun.

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

296 Pinatubo eruption with the Last Millennium Ensemble (850-1850) co

297 The most intense explosive eruptions with accompanying rapid lava effusion occurred

298 Large volume effusive eruptions with relatively minor observed precursory sign

299 urse conversation about child's future tooth eruption, with advice given to visit a general dental pr

300 on Earth, capable of large and catastrophic eruptions, yet their low eruptive frequency makes it cha