Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
about
Geophysics. Monitoring volcanoes.Continuous deflation of the Askja caldera, Iceland, during the 1983-1998 noneruptive periodDeep magma storage at Hekla volcano, Iceland, revealed by InSAR time series analysisInelastic compaction and permeability evolution in volcanic rockDeformation due to a pressurized horizontal circular crack in an elastic half-space, with applications to volcano geodesyDynamic deformation of Etna Volcano observed by satellite radar interferometry
P2860
Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
description
article publié dans la revue scientifique Nature
@fr
scientific article published in Nature
@en
wetenschappelijk artikel
@nl
наукова стаття, опублікована в Nature в жовтні 1993
@uk
name
Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
@en
Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
@nl
type
label
Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
@en
Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
@nl
prefLabel
Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
@en
Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
@nl
P2093
P356
P1433
P1476
Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
@en
P2093
Alan T. Linde
I. Selwyn Sacks
Kristjan Agustsson
Ragnar Stefansson
P2888
P304
P356
10.1038/365737A0
P407
P577
1993-10-01T00:00:00Z
P6179
1017035042