ライフサイエンスコーパス: eruptive

1 y help explain large uplift unaccompanied by eruptive activity at other volcanoes.

2 Here we show that much of the eruptive activity can be explained by broad, curtain-lik

3 Long-term eruptive activity has produced an unusual chemical envir

4 Here, we use infrasound data recorded during eruptive activity in June 2021 at Mt.

5 The persistent eruptive activity of mild Strombolian explosions is occa

6 Eruptive activity shapes volcanic edifices.

7 e conclude that the waning/extinguishment of eruptive activity shifted progressively from NW to SE, f

8 one million years of semi-continuous Deccan eruptive activity spanned the Cretaceous-Paleogene bound

9 a major lateral collapse during a period of eruptive activity that began in June.

10 lcano, blocking subsequent dykes and causing eruptive activity to migrate.

11 ominant volcanic processes controlling their eruptive activity, with different characteristic times a

12 de emissions remained high despite low-level eruptive activity.

13 king place within the plumbing system before eruptive activity.

14 allows interpreting temporal modulations in eruptive activity.

15 the African armyworm Spodoptera exempta, an eruptive agricultural pest and its endemic dsDNA virus (

16 ilica igneous rocks and is resistant to post-eruptive alteration, thus offering a reliable record of

17 Climate change has amplified eruptive bark beetle outbreaks over recent decades, incl

18 a supply and confirmed that Axial Seamount's eruptive behavior is inflation-predictable, probably tri

19 Changes in magma chemistry that affect eruptive behavior occur during many volcanic eruptions,

20 modelling, reveal that abrupt transitions in eruptive behaviour - from lava fountaining to low-energy

21 findings should help identify transitions in eruptive behaviour at other mafic volcanoes worldwide.

22 lation between melt structure, viscosity and eruptive behaviour holds despite the variable water cont

23 llapse of the caldera roof and the long-term eruptive behaviour of the volcano.

24 e these break-up instabilities to changes in eruptive behaviour, the associated natural hazard and ul

25 complex relationship between deformation and eruptive behaviour.

26 mergencies is responding to rapid changes in eruptive behaviour.

27 the currently observed larger variability of eruptive behaviour.

28 eir magmatic systems, leading to predictable eruptive behaviour.

29 disorganization of their nucleus followed by eruptive cell death.

30 w that most of the 30 investigated volcanic (eruptive) centers are linked to contractional wrinkle ri

31 lastic flows that travelled >170 km from the eruptive centre and entrained blocks up to approximately

32 estimation of the potential reach of distant eruptive centres.

33 iterature describing the association between eruptive cherry hemangiomatosis and MCD.

34 Eruptive cherry hemangiomatosis, which involves the sudd

35 Quantifying changes in both eruptive column dynamics and aerosol lifecycle is theref

36 rewer-Dobson circulation, and an increase in eruptive column height.

37 future tropopause height rise and unchanged eruptive column height.

38 We combine an eruptive column model with an aerosol-climate model to s

39 cted from the vent and the maximum height of eruptive columns.

40 A major knowledge gap exists on how eruptive compositions of a single martian volcanic provi

41 today is lower than typical estimates of pre-eruptive conditions for rhyolites(1,10,11), and measurem

42 e and thus provide strong constraints on pre-eruptive conditions, which are of utmost importance for

43 volcano experienced one of the most violent eruptive crises in the last hundred years.

44 vesicle flattening due to gas escape and syn-eruptive cristobalite precipitation.

45 Syn-eruptive crystallisation of nanolites and their interact

46 plumes moderate cooling, allowing 20-30% syn-eruptive crystallization, and thus reduce the distinctio

47 y covers volcanoes globally throughout their eruptive cycles, independent of ground-based monitoring,

48 es in WT embryos the nuclear instability and eruptive death of neutrophils seen in Wdr1-deficient emb

49 oth mortality hazard during the first 4 post-eruptive decades was bathtub-shaped and that it varied c

50 Over the first 4 post-eruptive decades, the tooth mortality risks (excluding o

51 on period and show evidence of inflation, co-eruptive deflation and shallow dyke intrusion.

52 CO(2)/y (11.7 x 10(11) mol CO(2)/y) for non-eruptive degassing and 1.8 +/- 0.9 Tg/y for eruptive deg

53 -eruptive degassing and 1.8 +/- 0.9 Tg/y for eruptive degassing during the period from 2005 to 2015.

54 a silicic conduit system connected to upper eruptive deposits provides support for the 'cryptic frag

55 manufactured through milling and sieving of eruptive deposits with different bulk compositions and m

56 show that volcanic gases captured during an eruptive episode at Oldoinyo Lengai are indistinguishabl

57 its application to constrain the ages of key eruptive episodes of the volcanic history of Deception I

58 es of the scaling factors in five out of six eruptive episodes, which can be considered as a promisin

59 s, occurred before the beginning of the main eruptive episodes.

60 or up to ten years after some of the largest eruptive episodes.

61 at the volcano was probably poised in a near-eruptive equilibrium state long before the onset of the

62 ough the detection of other types of stellar eruptive event(6-9).

63 inins persisted regionally across this major eruptive event.

64 ed to the surface in only one high-magnitude eruptive event.

65 opes measured in olivine samples of the main eruptive events (pre-, syn- and post caldera) offer insi

66 ew avenue in understanding the properties of eruptive events and their impact on exoplanetary environ

67 hat many large- to small-scale, point-source eruptive events can be fed by multiple melt bodies rathe

68 dence of age- and compositionally-equivalent eruptive events in regional volcanic stratigraphies.

69 The Sun sporadically produces eruptive events leading to intense fluxes of solar energ

70 However, as recently reported in Nature, eruptive events like coronal mass ejections and solar fl

71 erge from the solar interior and where major eruptive events occur.

72 Seafloor diking-eruptive events represent the irreducible, quantum event

73 olcanic sequence with at least four discrete eruptive events spanning 93 +/- 12 Ma (1416 +/- 7 Ma to

74 These diking-eruptive events trigger a sequence of related, rapidly e

75 acific Rise captures the known 1991 and 1992 eruptive events, documents several additional events bet

76 ng a complex carbon system response to large eruptive events.

77 iconic intrusions can thus be interpreted as eruptive features that pose unique and previously unreco

78 surface energy needed to open the 6-7 August eruptive fissure.

79 rn caldera wall connecting the MMR roof with eruptive fissures are imaged.

80 Eruptive fissures opened in the LERZ on 3 May, eventuall

81 and troughs vertically aligned with seafloor eruptive fissures that we interpret as remnant dike root

82 st EUV wavefront associated with an adjacent eruptive flare propagates laterally through a neighborin

83 e (>10 km(3)) caldera-forming eruptions, and eruptive fluxes were elevated five times above the avera

84 upported teeth under masticatory loading and eruptive forces, 2 additional mechanical conditions were

85 can serve as a blueprint for tackling other eruptive forest insects.

86 ge and catastrophic eruptions, yet their low eruptive frequency makes it challenging to interpret the

87 y, numerical modeling of mineral zoning, syn-eruptive gas plume measurements, the distribution and fr

88 At these pressures, the maximum pre-eruptive H2O contents for the different magma compositio

89 Generalized eruptive histiocytosis (GEH) is a rare non-Langerhans ce

90 Generalized eruptive histiocytosis in association with a myeloid neo

91 cts, are used to reconstruct and compare the eruptive histories of the Monti Sabatini and Colli Alban

92 The model satisfactorily fits the eruptive history of the three active volcanoes in the Ne

93 dredge sites that considerably improve OJP's eruptive history.

94 ments proximal to the CAMP flows due to post-eruptive hydrothermal activity.

95 Eruptive hypomelanosis is a novel viral exanthem.

96 This novel clinical presentation, eruptive hypomelanosis, may represent a paraviral exanth

97 secutive patients with pembrolizumab-induced eruptive KAs and their management.

98 olizumab therapy may also be associated with eruptive KAs with characteristic dermal inflammation, wh

99 years), experienced pembrolizumab-associated eruptive KAs.

100 mbrolizumab-treated cancer who all developed eruptive KAs.

101 edge, there have been no previous reports of eruptive keratoacanthomas (KAs) in patients receiving pe

102 lapse ending on August 2, 2018 and lower ERZ eruptive lava activity ending by 4 September 2018.

103 it, followed by a steady decrease toward pre-eruptive levels over the subsequent 300 thousand years,

104 t otherwise be erroneously attributed to pre-eruptive magma mixing.

105 , together, imply that water contents of pre-eruptive magma on Mars could have been up to 1.8%.

106 tive alkaline basalt, an analogue of the pre-eruptive magma that likely feeds the Campi Flegrei Volca

107 This is the first reconstruction of pre-eruptive magma transfer at Campi Flegrei and corroborate

108 Although co-eruptive magma withdrawal resulted in 8.5 m of subsidenc

109 on near-edge structure spectroscopy, and pre-eruptive magmatic H2O contents of a global sampling of p

110 rovides a novel approach to constraining pre-eruptive magmatic processes and greatly increases our un

111 Constraining the timescales of pre-eruptive magmatic processes in active volcanic systems i

112 Crater (Arizona) ca. 1085 AD by undetermined eruptive mechanisms.

113 Eruptive melanocytic nevi (EMN) are characterized by the

114 manner, we argue that commonly observed pre-eruptive microtextures caused by disequilibrium crystall

115 phenomenon that can occur in the setting of eruptive nevi or epidermotropic melanoma metastases.

116 g to nevogenesis, benign "nevic" metastases, eruptive nevi, and epidermotropic metastatic melanoma.

117 Our results show how the pre-eruptive noble gas signals of volcanic activity is an im

118 contextualised through a combination of syn-eruptive observations and detailed post-eruption field i

119 relationship between geophysical signals and eruptive parameters measured during six explosive episod

120 ts, and numerical simulations to analyze the eruptive patterns leading to the paroxysmal explosions.

121 However, the pre-eruptive patterns of deformation and seismicity vary wid

122 successful simulated application to the pre-eruptive period of May 2008, at Mount Etna (Italy).

123 geochronology and resolved four high-volume eruptive periods.

124 ults of this study show: (i) The most recent eruptive phase occurred between 100 ka and 70 ka; (ii) t

125 During the co-eruptive phase of the seismic activity, hypocenters dept

126 warmth of the early Eocene, likely linked to eruptive phases of the North Atlantic Igneous Province.

127 the existing magma was evacuated by the main eruptive phases, enough to trigger caldera collapse.

128 These can be used to explain post-eruptive phenomena and hazards to the local population,

129 plosively, and it is responsible for various eruptive phenomena in the universe.

130 ate tsunamis by the interaction of different eruptive phenomena with the sea.

131 y into the solar system via flares and other eruptive phenomena.

132 the most sophisticate atmospheric models and eruptive plume dynamics require input parameters such as

133 Numerical modelling suggests Martian plinian eruptive plumes moderate cooling, allowing 20-30% syn-er

134 eral life-history traits are associated with eruptive population dynamics, e.g., neoteny of females,

135 crystal-poor magmas has implications for the eruptive potential of such magmas, and is the likely sou

136 isode are considered pertinent to evaluating eruptive potential.

137 to FU Orionis- or EX Lupi-type outbursts of eruptive pre-main-sequence stars.

138 f magmas is critical to our understanding of eruptive processes and their deep Earth cycling essentia

139 nto account the non-isothermal nature of pre-eruptive processes, deconstructing the main core-rim dif

140 Earliest eruptive products ((187)Os/(188)Os <= 0.188, platinum (P

141 The eruptive products are commonly very crystal-poor and hig

142 exploration because lithium leached from the eruptive products by meteoric and hydrothermal fluids be

143 oximately twice the melt volume as the total eruptive products of all three volcanoes combined.

144 The conventional approach to dating these eruptive products using the (40)Ar/(39)Ar method is to f

145 observations, textural and chemical data of eruptive products, and numerical simulations to analyze

146 p is stronger for LIPs with higher estimated eruptive rates and for stage boundaries with higher exti

147 ates have insufficient resolution to confirm eruptive rates required to induce major climate perturba

148 matic volatile release in Iceland and global eruptive records.

149 n of organometallic complexes following post-eruptive redistribution.

150 des an updated assessment of possible future eruptive scenarios for the city of Rome.

151 The protracted eruptive sequence has implications for the emplacement d

152 ano, Hawai'i, USA, over the 2008-2018 summit eruptive sequence, encoded by "very-long-period" seismic

153 i, represented one of its most extraordinary eruptive sequences in at least 200 years, yet the trigge

154 Pre-eruptive spatiotemporal magma dynamics are examined for

155 Thus, eruptive Spitz nevus is a striking example of benign met

156 he Fagradalsfjall Fires in 2021 involved pre-eruptive stalling, fractional crystallization and crusta

157 the key transition from the pre-eruptive to eruptive state is due to the establishment of a positive

158 he mechanisms by which cavities evolve to an eruptive state remain poorly understood.

159 nclusions are commonly used to determine pre-eruptive storage conditions.

160 from an over-pressured chamber roof to a pre-eruptive storage pool near the brittle-ductile transitio

161 transports from a deep reservoir(s) to a pre-eruptive storage pool with eruptible magma remains elusi

162 ive estimates of magma conditions during pre-eruptive storage.

163 The olivine zoning patterns change with the eruptive stratigraphy, and record a transition towards a

164 Dome-forming eruption is a frequent eruptive style and a major hazard on numerous volcanoes

165 roposed here can help forecast shifts in the eruptive style and especially the onset of flank eruptio

166 there is no univocal correspondence between eruptive style and Pele's hair texture.

167 Transitions in eruptive style during volcanic eruptions strongly depend

168 within the magma, was characteristic of the eruptive style.

169 impacts magma rheology, ascent dynamics, and eruptive style.

170 lain the correlation between composition and eruptive style.

171 plications for magma degassing processes and eruptive styles.

172 eological formations indicates that mild pre-eruptive subsidence took place in the Wallowa Mountains,

173 in Montserrat, West Indies, to constrain pre-eruptive subsurface initial conditions and to compare wi

174 and progressive magma recharge maximized pre-eruptive sulfur accumulation at Samalas.

175 When normalized by OM levels, post-eruptive surfaces with OM inputs had the highest beta-gl

176 stal-rich and crystal-free silicic magmas at eruptive temperatures, extending the range of known cond

177 relationships between these geophysical and eruptive time series were studied.

178 and power laws, linking seismo-acoustic and eruptive time series.

179 this event, the key transition from the pre-eruptive to eruptive state is due to the establishment o

180 constraints on recognising and responding to eruptive transitions in a resource-constrained setting,

181 onally distinct basanitic to alkali basaltic eruptive units.

182 ly to a shallow reservoir drove 6.5 m of pre-eruptive uplift and seismicity over thirteen years, incl

183 ce in the Wallowa Mountains, followed by syn-eruptive uplift of several hundred metres and a long-ter

184 ollapse, revealing that small differences in eruptive vent elevation can lead to major differences in

185 form plumes rising several kilometers above eruptive vents, which can pose serious risk on human hea

186 ntributed to extreme differentiation and pre-eruptive volatile build-up.

187 Here we report the undersaturated pre-eruptive volatile content for a suite of mid-ocean-ridge

188 as been proposed to indicate causality, with eruptive volatile release driving environmental degradat

189 The influence of noneruptive and eruptive volcanic activity on glacier mass balance is pr

190 e that is one to four times greater than the eruptive volume of the largest past caldera-forming erup

191 Caldera, has a storage volume similar to the eruptive volume of Yellowstone's smallest caldera-formin

192 e-modifying gases is not directly related to eruptive volume or DT volcanism was not the source of La

193 agma flux decreases, resulting in changes in eruptive volume, style, and composition.

194 Although the pre-eruptive water content of the lunar volcanic glasses can

195 ll paroxysms at Stromboli share a common pre-eruptive weeks-to months-long unrest phase, marking the

196 tures as abdominal pain, acute pancreatitis, eruptive xanthomas, and lipemia retinalis.

197 macrophages, leading to the clinical finding eruptive xanthomas.

198 ay that might be responsible for creation of eruptive xanthomas.