000061557 001__ 61557
000061557 005__ 20190709135449.0
000061557 0247_ $$2doi$$a10.5038/1827-806X.46.2.2064
000061557 0248_ $$2sideral$$a99241
000061557 037__ $$aART-2017-99241
000061557 041__ $$aeng
000061557 100__ $$0(orcid)0000-0002-1460-1590$$aPueyo Anchuela, Óscar$$uUniversidad de Zaragoza
000061557 245__ $$aIntegrated approach for sinkhole evaluation and evolution prediction in the Central Ebro Basin (NE Spain)
000061557 260__ $$c2017
000061557 5060_ $$aAccess copy available to the general public$$fUnrestricted
000061557 5203_ $$aEvaluation of karst hazards benefits from the integration of different techniques, methodologies and approaches. Each one presents a different signature and is sensitive to certain indicators related to karst hazards. In some cases, detailed analysis permits the evaluation of representativeness either from isolated approaches or by means of integrated analyses. In this study, we present the evaluation of an area with high density of karstic collapses at different evolutionary stages through the integration of surficial, historical, geomorphological and geophysical data in order to finally define the evolutionary model for karst activity development. The obtained dataset permits to identify different steps in sinkhole evolution: (i) cavities and open sinkholes, (ii) filling of these cavities, with materials having different signatures, (iii) the progression from collapses to subsidence sinkholes and (iv) enlargement through collapses in marginal areas of previous sinkholes. The presence of different stages of this evolutionary model permits to determine their own signatures that can be of application in contexts where analysis cannot be so systematic and also to evaluate the definition of the marginal areas of previous sinkholes as the most hazardous sectors.
000061557 536__ $$9info:eu-repo/grantAgreement/ES/DGA/PI-030-08$$9info:eu-repo/grantAgreement/ES/DGA/GEOTRANSFER RESEARCH GROUP$$9info:eu-repo/grantAgreement/ES/DGA/GA-LC-026-2009
000061557 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc$$uhttp://creativecommons.org/licenses/by-nc/3.0/es/
000061557 590__ $$a1.392$$b2017
000061557 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b132 / 189 = 0.698$$c2017$$dQ3$$eT3
000061557 592__ $$a0.693$$b2017
000061557 593__ $$aGeology$$c2017$$dQ2
000061557 593__ $$aEarth-Surface Processes$$c2017$$dQ2
000061557 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000061557 700__ $$0(orcid)0000-0003-3197-4177$$aPocoví Juan, Andrés$$uUniversidad de Zaragoza
000061557 700__ $$0(orcid)0000-0003-3652-3527$$aCasas Sainz, Antonio M.$$uUniversidad de Zaragoza
000061557 700__ $$aGracia Abadías, Javier
000061557 700__ $$0(orcid)0000-0002-9130-117X$$aLiesa Carrera, Carlos L.$$uUniversidad de Zaragoza
000061557 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000061557 7102_ $$12000$$2428$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Interna
000061557 773__ $$g46, 2 (2017), 237-249$$pInt. j. speleol.$$tINTERNATIONAL JOURNAL OF SPELEOLOGY$$x0392-6672
000061557 8564_ $$s9198011$$uhttps://zaguan.unizar.es/record/61557/files/texto_completo.pdf$$yVersión publicada
000061557 8564_ $$s130091$$uhttps://zaguan.unizar.es/record/61557/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000061557 909CO $$ooai:zaguan.unizar.es:61557$$particulos$$pdriver
000061557 951__ $$a2019-07-09-11:39:32
000061557 980__ $$aARTICLE