Sensitivity Analysis of FWI Applied to OVSP Synthetic Data for Fault Detection and Characterization in Crystalline Rocks

We have performed several sensitivity studies to assess the ability of the Full Wave Inversion method to detect, delineate and characterize faults in a crystalline geothermal reservoir from OVSP data. The distant goal is to apply the method to the Soultz-sous-Forêts site (France). Our approach consi...

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Autores principales: Yassine Abdelfettah, Christophe Barnes
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Lenguaje:EN
Publicado: MDPI AG 2021
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EGS
Acceso en línea:https://doaj.org/article/29650f9d5fdb4edbab03c4b6cf8e40b5
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spelling oai:doaj.org-article:29650f9d5fdb4edbab03c4b6cf8e40b52021-11-25T17:42:45ZSensitivity Analysis of FWI Applied to OVSP Synthetic Data for Fault Detection and Characterization in Crystalline Rocks10.3390/geosciences111104422076-3263https://doaj.org/article/29650f9d5fdb4edbab03c4b6cf8e40b52021-10-01T00:00:00Zhttps://www.mdpi.com/2076-3263/11/11/442https://doaj.org/toc/2076-3263We have performed several sensitivity studies to assess the ability of the Full Wave Inversion method to detect, delineate and characterize faults in a crystalline geothermal reservoir from OVSP data. The distant goal is to apply the method to the Soultz-sous-Forêts site (France). Our approach consists of performing synthetic Full Wave 2D Inversion experiments using offset vertical seismic and comparing the estimated fields provided by the inversion, i.e., the estimated underground images, to the initial reference model including the fault target. We first tuned the inversion algorithmic parameters in order to adapt the FWI software, originally dedicated to a sedimentary context, to a crystalline context. In a second step, we studied the sensitivity of the FWI fault imaging results as a function of the acquisition geometry parameters, namely, the number of shots, the intershot distance, the maximum offset and also the antenna length and well deviation. From this study, we suggest rules to design the acquisition geometry in order to improve the fault detection, delineation and characterization. In a third step, we studied the sensitivity of the FWI fault imaging results as a function of the fault or the fault zone characteristics, namely, the fault dip, thickness and the contrast of physical parameters between the fault materials and the surrounding fresh rocks. We have shown that a fault with high dip, between 60 and 90° as thin as 10 m (i.e. lower than a tenth of the seismic wavelength of 120 m for Vp and 70 m for Vs) can be imaged by FWI, even in the presence of additive gaussian noise. In summary, for a crystalline geological context, and dealing with acceptable S/N ratio data, the FWI show a high potential for accurately detecting, delineating and characterizing the fault zones.Yassine AbdelfettahChristophe BarnesMDPI AGarticlegeothermalOVSPwell seismic datafaultfractureEGSGeologyQE1-996.5ENGeosciences, Vol 11, Iss 442, p 442 (2021)
institution DOAJ
collection DOAJ
language EN
topic geothermal
OVSP
well seismic data
fault
fracture
EGS
Geology
QE1-996.5
spellingShingle geothermal
OVSP
well seismic data
fault
fracture
EGS
Geology
QE1-996.5
Yassine Abdelfettah
Christophe Barnes
Sensitivity Analysis of FWI Applied to OVSP Synthetic Data for Fault Detection and Characterization in Crystalline Rocks
description We have performed several sensitivity studies to assess the ability of the Full Wave Inversion method to detect, delineate and characterize faults in a crystalline geothermal reservoir from OVSP data. The distant goal is to apply the method to the Soultz-sous-Forêts site (France). Our approach consists of performing synthetic Full Wave 2D Inversion experiments using offset vertical seismic and comparing the estimated fields provided by the inversion, i.e., the estimated underground images, to the initial reference model including the fault target. We first tuned the inversion algorithmic parameters in order to adapt the FWI software, originally dedicated to a sedimentary context, to a crystalline context. In a second step, we studied the sensitivity of the FWI fault imaging results as a function of the acquisition geometry parameters, namely, the number of shots, the intershot distance, the maximum offset and also the antenna length and well deviation. From this study, we suggest rules to design the acquisition geometry in order to improve the fault detection, delineation and characterization. In a third step, we studied the sensitivity of the FWI fault imaging results as a function of the fault or the fault zone characteristics, namely, the fault dip, thickness and the contrast of physical parameters between the fault materials and the surrounding fresh rocks. We have shown that a fault with high dip, between 60 and 90° as thin as 10 m (i.e. lower than a tenth of the seismic wavelength of 120 m for Vp and 70 m for Vs) can be imaged by FWI, even in the presence of additive gaussian noise. In summary, for a crystalline geological context, and dealing with acceptable S/N ratio data, the FWI show a high potential for accurately detecting, delineating and characterizing the fault zones.
format article
author Yassine Abdelfettah
Christophe Barnes
author_facet Yassine Abdelfettah
Christophe Barnes
author_sort Yassine Abdelfettah
title Sensitivity Analysis of FWI Applied to OVSP Synthetic Data for Fault Detection and Characterization in Crystalline Rocks
title_short Sensitivity Analysis of FWI Applied to OVSP Synthetic Data for Fault Detection and Characterization in Crystalline Rocks
title_full Sensitivity Analysis of FWI Applied to OVSP Synthetic Data for Fault Detection and Characterization in Crystalline Rocks
title_fullStr Sensitivity Analysis of FWI Applied to OVSP Synthetic Data for Fault Detection and Characterization in Crystalline Rocks
title_full_unstemmed Sensitivity Analysis of FWI Applied to OVSP Synthetic Data for Fault Detection and Characterization in Crystalline Rocks
title_sort sensitivity analysis of fwi applied to ovsp synthetic data for fault detection and characterization in crystalline rocks
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/29650f9d5fdb4edbab03c4b6cf8e40b5
work_keys_str_mv AT yassineabdelfettah sensitivityanalysisoffwiappliedtoovspsyntheticdataforfaultdetectionandcharacterizationincrystallinerocks
AT christophebarnes sensitivityanalysisoffwiappliedtoovspsyntheticdataforfaultdetectionandcharacterizationincrystallinerocks
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