Controle Neotectônico das Águas Subterrâneas

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dc.contributor.authorVALENTE, Cidney Rodrigues
dc.contributor.authorOLIVEIRA, Sérgio M. Azevedo de
dc.contributor.authorVENEZIANI, Paulo
dc.date.accessioned2013-12-19T16:34:19Z
dc.date.available2013-12-19T16:34:19Z
dc.date.issued2001
dc.description.abstractStructural lineaments interpretation from remote sensing products integrated with data of airborne geophysical data (magnetometry) had as objective to investigate and to define the hydrogeological local control in Rio de Janeiro State. Photogeological techniques were applied to the tectonic-structural analysis by using satellite imagery. Several thematic maps, such as structural lineament, joint zone traces and morphostructural were produced and analyzed. The vertical to subvertical fractures. (directions around N50E, N50W and N75E) are responsible for the recharge of the fissured aquifers in the structural highs. This fracture system, in connection with the subhorizontal fractures, works as groundwater conductors for the recharging
dc.identifier.citationVALENTE, Cidney Rodrigues; OLIVEIRA, Sérgio M. Azevedo de; VENEZIANI, Paulo. Controle Neotectônico das Águas Subterrâneas. In: SIMPÓSIO BRASILEIRO DE SENSORIAMENTO REMOTO, 10., 2001, Foz do Iguaçu. Anais [...]. São José dos Campos, SP: INPE, 2001. p. 367-373.
dc.identifier.urihttps://rigeo.sgb.gov.br/handle/doc/635
dc.language.isopor
dc.localFoz do Iguaçu, PR
dc.subjectHIDROGEOLOGIA
dc.subjectNEOTECTÔNICA
dc.subjectSENSORIAMENTO REMOTO
dc.subjectCONGRESSOS
dc.subjectBRASIL
dc.subjectRIO DE JANEIRO
dc.titleControle Neotectônico das Águas Subterrâneas
dc.typeWorking Paperpt_BR

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