2024-03-29T11:15:19Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:63412021-09-30T10:24:14ZDOIDBDOIDB.FID
10.5880/fidgeo.2017.019
Trippetta, Fabio
Fabio
Trippetta
0000-0001-8336-2194
Dipartimento di Scienze della Terra, Sapienza Università di Roma
Carpenter, Brett M
Brett M
Carpenter
0000-0002-3451-2528
School of Geology and Geophysics, University of Oklahoma, Norman, OK, USA
Mollo, Silvio
Silvio
Mollo
0000-0002-1448-0282
Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy
Scuderi, Marco M.
Marco M.
Scuderi
0000-0001-5232-0792
Dipartimento di Scienze della Terra, Sapienza Università di Roma
Scarlato, Piergiorgio
Piergiorgio
Scarlato
0000-0003-1933-0192
Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy
Collettini, Cristiano
Cristiano
Collettini
0000-0002-4828-2516
Dipartimento di Scienze della Terra, Sapienza Università di Roma
Dataset of Physical and Transport Property Variations Within the Carbonate-Bearing Fault Zones of the Monte Maggio Fault (Central Italy)
GFZ Data Services
2017
Sesmic Waves
Carbonates
Permeability
Physical properties
Elastic properties
Borehole sonic logs
Vp
Vs
Vp/Vs Ratio
Critical Rupture Length
EPOS
Multi-scale laboratories
rock and melt physical properties
Trippetta, Fabio
Fabio
Trippetta
0000-0001-8336-2194
Dipartimento di Scienze della Terra, Sapienza Università di Roma
Trippetta, Fabio
Fabio
Trippetta
0000-0001-8336-2194
Dipartimento di Scienze della Terra, Sapienza Università di Roma
Trippetta, Fabio
Fabio
Trippetta
0000-0001-8336-2194
Dipartimento di Scienze della Terra, Sapienza Università di Roma
Trippetta, Fabio
Fabio
Trippetta
0000-0001-8336-2194
Dipartimento di Scienze della Terra, Sapienza Università di Roma
HP-HT Laboratory of Experimental Volcanolgy and Geophysics (INGV, Italy)
INGV, Italy
2017-11-03
en
10.1002/2017GC007097
10.1029/2011JB008352
19556 Bytes
1 Files
application/x-zip-compressed
CC BY 4.0
Here we report the raw data of the physical properties of carbonate samples collected along the Monte Maggio normal Fault (MMF), a regional structure (length ~10 km and displacement ~500 m) located within the active system of the Apennines (Italy). In particular, we report results coming from large cores (100 mm in diameter and up to 20 cm long) drilled perpendicular to the fault plane made of Calcare Massiccio (massive limestone) and Bugarone fm (limestone with 8.3 % of clay).
From these large cores, we obtained smaller cores, 38 mm in diameter both parallel and perpendicular to the fault plane, that have been used for experiments. We have divided the rock samples in four categories following the fault architecture. The four structural domains of the fault are:1) the hangingwall (HW) made of Bugarone fm that is still preserved in some portions of the fault, 2) a Cemented Cataclasite (CC) and 3) a Fault Breccia (FB) that characterize the cataclastic damage zones and 4) the correspondent undeformed protolith of the footwall block made of Calcare Massiccio.
Raw data reported here are those used for drawing Figures 5, 6, 8 and 9 of the paper “Physical and transport property variations within carbonate- bearing fault zones: Insights from the Monte Maggio Fault (central Italy)”, http://doi.org/10.1002/ 2017GC007097 by Trippetta et al.
Dataset_Fig05.txt reports P- and S-wave velocities (in km/s) of the described samples at pressure from 0.1 MPa (ambient pressure) up to 100 MPa at ambient temperature in dry conditions and the corresponding Vp/Vs ratio. Experiments have been performed by using the permeameter at the HP-HT Laboratory of experimental Volcanology and Geophysics at INGV (Rome).
Dataset_Fig06.txt reports permeability data (in m^2) on the same type of samples of fig05 for the same range of confining pressure at ambient temperature. Pore pressure values athletes each confining pressure step are indicated in the file. Data have been again acquired with the permeameter.
Dataset_Fig08.txt reports P-wave velocity data (in km/s) vs depth (in m), recorded on the portion that crossed the Calare Massiccio fm of three boreholes drilled in the Apennines: Varoni 1, Monte Civitello 1 and Daniel1. Data have been obtained by digitalizing each pdf file of the boreholes mentioned above, that are available at http://unmig.sviluppoeconomico.gov.it/videpi/videpi.asp. Once digitalized, respect to the original pdf file, velocity data have been simply converted from um/f to km/s.
Dataset_Fig09.txt reports values of the maximum, minimum and average values of Critical fault nucleation length (in m) at each corresponding depth (in m) and applied confining pressure (in MPa). Critical nucleation lengths have been calculated by using the equations described in the text of the Trippetta et al paper and by using the elastic parameters calculated from data reported here. Data on earthquakes-depth distribution of the 2009 L'Aquila sequence can be found on Chiaraluce et al. (2011).
12.927989959716797
12.952194213867188
42.75823057701311
42.781543233362996
Sapienza Università di Roma
http://doi.org/10.13039/501100004271
From small to large, to very large: a multiscale study of the influence of fractures on physical properties of carbonate rocks