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期刊论文 [7]
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Glacier elevation change in the Western Qilian mountains as observed by TerraSAR-X/TanDEM-X images
[期刊论文]
GEOCARTO INTERNATIONAL, 2019-01-01,
Zhang, Qibing
;
Kang, Shichang
View/Download:1/0
Subsidence at Cerro Prieto Geothermal Field and postseismic slip along the Indiviso fault from 2011 to 2016 RADARSAT-2 DInSAR time series analysis
[期刊论文]
Geophysical Research Letters, 2017-01-01, 44 (6
Samsonov S.V.
;
Feng W.
;
Fialko Y.
View/Download:10/0
Polarimetric differential SAR interferometry in an arid natural environment
[期刊论文]
International Journal of Applied Earth Observation and Geoinformation, 2017-01-01, 59
Mullissa A
;
G
;
, Tolpekin V
;
, Stein A
;
, Perissin D
View/Download:0/0
Evidence of a shallow persistent magmatic reservoir from joint inversion of gravity and ground deformation data: The 25-26 October 2013 Etna lava fountaining event
[期刊论文]
Geophysical Research Letters, 2016-01-01, 43 (7
Greco F.
;
Currenti G.
;
Palano M.
;
Pepe A.
;
Pepe S.
View/Download:19/0
Ground deformation and source geometry of the 24 August 2016 Amatrice earthquake (Central Italy) investigated through analytical and numerical modeling of DInSAR measurements and structural-geological data
[期刊论文]
Geophysical Research Letters, 2016-01-01, 43 (24
Lavecchia G.
;
Castaldo R.
;
de Nardis R.
;
De Novellis V.
;
Ferrarini F.
;
Pepe S.
;
Brozzetti F.
;
Solaro G.
;
Cirillo D.
;
Bonano M.
;
Boncio P.
;
Casu F.
;
De Luca C.
;
Lanari R.
;
Manunta M.
;
Manzo M.
;
Pepe A.
;
Zinno I.
;
Tizzani P.
View/Download:28/0
Very shallow dyke intrusion and potential slope failure imaged by ground deformation: The 28 December 2014 eruption on Mount Etna
[期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (8
Bonforte A.
;
Guglielmino F.
View/Download:0/0
Lithology-controlled subsidence and seasonal aquifer response in the Bandung basin, Indonesia, observed by synthetic aperture radar interferometry
[期刊论文]
International Journal of Applied Earth Observation and Geoinformation, 2014-01-01, 32 (1
Khakim M
;
Y
;
N
;
, Tsuji T
;
, Matsuoka T
View/Download:0/0
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