2024-03-28T09:51:46Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:66132020-09-26T12:02:23ZDOIDBDOIDB.FID
10.5880/fidgeo.2019.003
Corbi, Fabio
Fabio
Corbi
0000-0003-2662-3065
Universitá degli studi "Roma TRE", Rome, Italy
Xu, Wenbin
Wenbin
Xu
0000-0001-7294-8229
King Abdullah University of Science and Technology, , Thuwal, Saudi Arabia
University of California, Berkeley, California, USA
Rivalta, Eleonora
Eleonora
Rivalta
0000-0001-8245-0504
GFZ German Research Centre for Geosciences, Potsdam, Germany
Jonsson, Sigurjon
Sigurjon
Jonsson
0000-0001-5378-7079
King Abdullah University of Science and Technology, , Thuwal, Saudi Arabia
Supplement to: Graben formation and dike arrest during the 2009 Harrat Lunayyir dike intrusion in Saudi Arabia: Insights from InSAR, stress calculations and analog experiments
GFZ Data Services
2019
EPOS
multi-scale laboratories
analogue models of geologic processes
analogue modelling results
software tools
dike
Harrat Lunayyir
graben formation
dike-fault interaction
volcano deformation
EARTH SCIENCE > SOLID EARTH > TECTONICS > VOLCANIC ACTIVITY
graben
magmatic process > intrusion
magmatic process
fault
dike
volcanic features
Sand > Quartz Sand
Sandbox > Sandbox (cm scale)
Digital Image Correlation (DIC) / Particle Image Velocimetry (PIV) > MatPIV
SLR camera
Surface image
Corbi, Fabio
Fabio
Corbi
0000-0003-2662-3065
Universitá degli studi "Roma TRE", Rome, Italy
Laboratory of Experimental Tectonics (University of Roma TRE, Italy)
Universitá degli studi "Roma TRE", Rome, Italy
2015-07-14
eng
10.1002/2015JB012505
2 Files
application/octet-stream
application/octet-stream
CC BY 4.0
This dataset is supplementary material to the article by Xu et al. (2016) ‘Graben formation and dike arrest during the 2009 Harrat Lunayyir dike intrusion in Saudi Arabia: Insights from InSAR, stress calculations and analog experiments’. The Authors described the spatial and temporal effects of a propagating dike on crustal deformation, including the interaction with faulting, using a multidisciplinary approach. This supplementary material concerns the analog modelling part only. For a detailed description of the experimental procedure, set-up and materials used, please refer to the article of Xu et al. (2016; paragraph 5).
The data available in this supplementary publication are:
- A folder (2019-003_Corbi-et-al_Fig6.zip) containing: 1. top-view pictures (e.g. ‘lunayyr1_0025.JPG’) and displacement data obtained with MatPiv (e.g. ‘uun25.mat’ and ‘uvn25.mat’; dike parallel and orthogonal components; respectively) shown in figure 6 of Xu et al 2016. 2. a Matlab script (‘fig6_a_h.m’) that allows reproducing the same figure setup as in figure 6 panels a-h of Xu et al 2016. The thick red line highlights dike position. The background shading refers to dike orthogonal displacement.
- A folder (2019-003_Corbi-et-al_PIV_data.zip) containing: 1. surface deformation data obtained with MatPiv. Each file (‘vel_fine_piv#.mat’) contains 4 elements (x, y, u, v) representing the coordinates and horizontal and vertical component of incremental velocity field organized in a 143 x 215 matrix; 2. the run_movie.m Matlab script. Running it the user can visualize the space-time evolution of cumulative surface displacement. The background shading refers to dike orthogonal component of displacement. The thick red line highlights dike position.
- A folder (2019-003_Corbi-et-al_pictures.zip) containing the whole set of pictures from the experiment shown in Xu et al., 2016.
- A movie (2019-003_Corbi-et-al_graben formation.mp4) obtained using the whole set of pictures (96 photos). The thick red line highlights dike position. The amount of dike opening is reported as header.
- A movie (2019-003_Corbi-et-al_cum_displacement.mp4) showing the space-time evolution of cumulative surface displacement, where the background shading refers to dike orthogonal component of displacement. The thick red line highlights dike position.
37.43952519700963
38.20307500169713
24.871957649836745
25.394129841584835
European Union
ERC-StG
240583
CCMP-POMPEI