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 de emissions remained high despite low-level eruptive activity.

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

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

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

8 complex relationship between deformation and eruptive behaviour.

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

10 estimation of the potential reach of distant eruptive centres.

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

12 Eruptive cherry hemangiomatosis, which involves the sudd

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

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

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

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

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

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

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

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

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

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

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

24 inins persisted regionally across this major eruptive event.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

41 Generalized eruptive histiocytosis in association with a myeloid neo

42 Eruptive hypomelanosis is a novel viral exanthem.

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

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

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

46 years), experienced pembrolizumab-associated eruptive KAs.

47 mbrolizumab-treated cancer who all developed eruptive KAs.

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

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

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

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

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

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

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

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

56 Eruptive melanocytic nevi (EMN) are characterized by the

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

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

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

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

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

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

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

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

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

66 isode are considered pertinent to evaluating eruptive potential.

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

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

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

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

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

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

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

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

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

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

77 lain the correlation between composition and eruptive style.

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

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

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

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

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

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

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

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

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

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