@InProceedings{VenezianiSantBettOkid:2005:MaTeRe,
               author = "Veneziani, Paulo and Santos, Athos Ribeiro dos and Bettencourt, 
                         Jorge Silva and Okida, Rosana",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)} and {Universidade de 
                         S{\~a}o Paulo (USP). Instituto de Geoci{\^e}ncias.} and 
                         {GEOAMBIENTE – Sensoriamento Remoto S/C Ltda.}",
                title = "Mapa tectono-estratigr{\'a}fico da regi{\~a}o centro-sul do 
                         Estado de Rond{\^o}nia baseado em dados integrados de sensores 
                         remotos e gamaespectrom{\'e}tricos",
            booktitle = "Anais...",
                 year = "2005",
               editor = "Epiphanio, Jos{\'e} Carlos Neves and Fonseca, Leila Maria 
                         Garcia",
                pages = "1923--1932",
         organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 12. (SBSR)",
            publisher = "INPE",
              address = "S{\~a}o Jos{\'e} dos Campos",
             keywords = "tectonic-stratigraphic map, Caraj{\'a}s, optical, SAR and gamma 
                         TC data, digital fusion.",
             abstract = "Significant advances in understanding the tectonic stratigraphic 
                         evolution of the central - southern region in the Rond{\^o}nia 
                         State were acquired by using the following: 1- spaceborne optical 
                         (Landsat TM) imagery; 2- aerial side looking radar (GEMS) imagery; 
                         3- digital integrated products Landsat TM/aerial gammaspectrometry 
                         and; 4- field work along previous selected profiles. This region 
                         is part of an Intraplate Strike Slip Belt with 
                         Paleo/Neoproterozoic ages, characterised by three ductile and 
                         brittle transpression phases, locally transtensive, and extensive 
                         reactivations with pulses at the end of the Proterozoic and 
                         beginning of the Paleozoic, at the Mesozoic and the Tertiary. The 
                         area is well known due to its mineral potential specially Sn ore. 
                         From the tectonic - stratigraphic viewpoint the region is 
                         problematic due to several drawbacks such as physiographic 
                         complexity, high contrast between tropical rainforest and 
                         intensive land use and large areas without outcrop. The objectives 
                         of this work were: 1- to show methodological criteria to obtain 
                         geological information by using remote sensing imageries and 
                         integrated products Landsat TM/aerial gammaspectrometry and; 2- to 
                         show the Tectonic -Stratigraphic Map of the studied area.",
  conference-location = "Goi{\^a}nia",
      conference-year = "16-21 abr. 2005",
                 isbn = "85-17-00018-8",
             language = "Portugu{\^e}s",
         organisation = "Instituto Nacional de Pesquisas Espaciais",
                  ibi = "ltid.inpe.br/sbsr/2004/11.17.11.00",
                  url = "http://urlib.net/ibi/ltid.inpe.br/sbsr/2004/11.17.11.00",
           targetfile = "1923.pdf",
                 type = "Geologia",
        urlaccessdate = "11 maio 2024"
}