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GEOMORPHIC INDEXES APPLIED TO TECTONIC DEFORMATION STUDY: A REVIEW

dc.contributor.authorSantos, Marcilene dos [UNESP]
dc.contributor.authorBernardes Ladeira, Francisco Sergio
dc.contributor.authorBatezelli, Alessandro
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionUniversidade Estadual de Campinas (UNICAMP)
dc.date.accessioned2019-10-04T12:37:50Z
dc.date.available2019-10-04T12:37:50Z
dc.date.issued2019-04-01
dc.description.abstractThis work gathers and discusses the major techniques of geomorphic indexes developed by several researchers over time, and currently applied to tectonics/neotectonics/active tectonic deformation study. Drainage is the most sensitive feature to relief changes, especially those related to tectonics and/or climate change, sea level oscillations, or anthropic action. The river sensitivity to relief changes reflects not only their rapid morphological/morphometric and sedimentary response but also the quick adjustment to a near-equilibrium stage in short geological time. It allows inferring recent tectonic activity by identifying regions in erosional disequilibrium in large areas, regardless of geological or geomorphic provinces. Such unique river feature strengthens the significance of identifying anomalous behaviors in studies of tectonic activity, and the evolution of modern environments or paleogeographic reconstitution. Thus, the present review considers the indexes related to quantitative relief features, such as altimetry, hypsometry and slope. And gives special attention to those indexes related to geomorphic and sedimentary responses of rivers to tectonic deformation (deflections, piracy and beheading, avulsion and combing, channel pattern adjustment, longitudinal profile adjustment and SL index, asymmetry factor and basin shape index, sinuosity of rivers and channel pattern, mountain front sinuosity (S-mf), index of active tectonics (I-at), sediment load and flow, etc.). For this purpose, the present study involved a bibliographic review and analysis of such techniques, as well as some cases from more recent works, presenting some indexes applied to the Aiuruoca river (Mantiqueira Hill, State of Minas Gerais) and the Cinzas and Laranjinha rivers, (Cinzas River watershed, State of Parana). The present work aims to support the studying strategy and the process of choosing the existing techniques, as well as to improve understanding and careful application of such current techniques.en
dc.description.affiliationUniv Estadual Paulista, Campus Ourinhos,Av Renato da Costa Lima 451, BR-19903302 Ourinhos, SP, Brazil
dc.description.affiliationUniv Estadual Campinas, Inst Geociencias, Rua Carlos Gomes 250, BR-13083855 Campinas, SP, Brazil
dc.description.affiliationUnespUniv Estadual Paulista, Campus Ourinhos,Av Renato da Costa Lima 451, BR-19903302 Ourinhos, SP, Brazil
dc.format.extent287-316
dc.identifierhttp://dx.doi.org/10.20502/rbg.v20i2.1564
dc.identifier.citationRevista Brasileira De Geomorfologia. Uberlandia, Brazil: Uniao Geomorfologia Brasileira, v. 20, n. 2, p. 287-316, 2019.
dc.identifier.doi10.20502/rbg.v20i2.1564
dc.identifier.issn1519-1540
dc.identifier.lattes8695585354475745
dc.identifier.orcid0000-0002-4883-1511
dc.identifier.urihttp://hdl.handle.net/11449/185702
dc.identifier.wosWOS:000467332000005
dc.language.isospa
dc.publisherUniao Geomorfologia Brasileira
dc.relation.ispartofRevista Brasileira De Geomorfologia
dc.rights.accessRightsAcesso restrito
dc.sourceWeb of Science
dc.subjectGeomorphic indexes
dc.subjectTectonics
dc.subjectRivers
dc.titleGEOMORPHIC INDEXES APPLIED TO TECTONIC DEFORMATION STUDY: A REVIEWen
dc.typeResenha
dcterms.rightsHolderUniao Geomorfologia Brasileira
dspace.entity.typePublication
unesp.author.lattes8695585354475745[1]
unesp.author.orcid8695585354475745[1]
unesp.departmentGeografia - FCTEpt

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