G. Rossi, R. Caputo, D. Zuliani, P. Fabris, M. Maggini, P. Karvelis
{"title":"Analysis of global navigation satellite system data along the Southern Gas Corridor and estimate of the expected displacements","authors":"G. Rossi, R. Caputo, D. Zuliani, P. Fabris, M. Maggini, P. Karvelis","doi":"10.1306/eg.01222019023","DOIUrl":null,"url":null,"abstract":"In the present paper, we analyze the fi nal part of the Southern Gas Corridor, a route highlighted in the European energy security and energy union strategies. This route crosses one of the most seismically activezones of the Mediterranean with several recognized crustal-scale seismogenic sources. We focus on the possibility of identifying the areas where critical differential motions could be expected along the route, which will be occupied by the Trans Adriatic Pipeline, over the nominal pipeline life span of 50 yr. We analyze the available global navigation satellite system data and compare the results to the deformation patterns of the most signi fi cant faults affecting the area. We interpolated the sparsely available velocity vectors and calculated strain rate information, both considering the region as a continuum and by applying an original algorithm that allows the linear interpolation within individual blocks. The blocks are characterized by a relatively homogenous deformational behavior, or a speci fi c tectonic setting, independently upon the neighboring ones. The results of the two methods are then compared by calculating the maximum displacement that would cumulate in the next 50 yr of the pipeline lifespan and the differential displacements that could cause possible bending phenomena to the pipeline structure. The methodological approach followed in this research could be applied to other infrastructures to identify the segments prone to localized deformation because of interseismic tectonic loading.","PeriodicalId":11706,"journal":{"name":"Environmental Geosciences","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2020-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Environmental Geosciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1306/eg.01222019023","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 2
Abstract
In the present paper, we analyze the fi nal part of the Southern Gas Corridor, a route highlighted in the European energy security and energy union strategies. This route crosses one of the most seismically activezones of the Mediterranean with several recognized crustal-scale seismogenic sources. We focus on the possibility of identifying the areas where critical differential motions could be expected along the route, which will be occupied by the Trans Adriatic Pipeline, over the nominal pipeline life span of 50 yr. We analyze the available global navigation satellite system data and compare the results to the deformation patterns of the most signi fi cant faults affecting the area. We interpolated the sparsely available velocity vectors and calculated strain rate information, both considering the region as a continuum and by applying an original algorithm that allows the linear interpolation within individual blocks. The blocks are characterized by a relatively homogenous deformational behavior, or a speci fi c tectonic setting, independently upon the neighboring ones. The results of the two methods are then compared by calculating the maximum displacement that would cumulate in the next 50 yr of the pipeline lifespan and the differential displacements that could cause possible bending phenomena to the pipeline structure. The methodological approach followed in this research could be applied to other infrastructures to identify the segments prone to localized deformation because of interseismic tectonic loading.