Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Raimundo Almeida-Filho"'
Publikováno v:
Revista Brasileira de Cartografia, Vol 68, Iss 5 (2016)
This article estimates for the ï¬rst time the extents of the landscape changes in the Anavilhanas Archipelago, as registered by satellite images acquired during the flood peak and drought events ever recorded in the Negro River (in Portuguese,
Externí odkaz:
https://doaj.org/article/dc44e8257d4e48d28f528d8ec2d12063
Publikováno v:
Acta Amazonica, Vol 41, Iss 1, Pp 47-56 (2011)
Este estudo apresenta um mapa da cobertura vegetal da planície de inundação do Rio Amazonas entre as cidades de Parintins (AM) e Almeirim (PA), com base em imagens Landsat-MSS adquiridas entre 1975 e 1981. O processamento digital dessas imagens en
Externí odkaz:
https://doaj.org/article/0371c0d4fe5e4b4f9b3283a348cc02b8
Autor:
Ramon Morais de Freitas, Raimundo Almeida Filho, Tatiana Mora Kuplich, Yosio Edemir Shimabukuro
Publikováno v:
Revista Ambiente & Água, Vol 3, Iss 1, Pp 18-25 (2008)
This paper discusses the use of a Landsat Thematic Mapper (TM) and JERS-1 Synthetic Aperture Radar (SAR) time-series for mapping and monitoring land cover types in a test site in the region of Corumbiara, Rondônia State, western Brazilian Amazônia.
Publikováno v:
Revista Brasileira de Geociências. 798:798-811
Publikováno v:
Revista Brasileira de Geociências. 33:183-190
Publikováno v:
Revista Brasileira de Geociências. 29:203-206
Publikováno v:
Remote Sensing of Environment. 67:181-193
The consequences of shifting the spectral location of narrow and broad red (R) and near-infrared (NIR) bands on measurements of the normalized difference vegetation index (NDVI) of Brazilian savannas were investigated for different plant communities
Publikováno v:
Revista Brasileira de Geociências. 27:207-210
Publikováno v:
Geocarto International. 11:61-69
The Tin Province of Goias, in central Brazil, includes several granitoids with greisenized‐albitized facies, which occupy the apical parts of the massifs. Stanniferous mineralizations (cassiterite) frequently occur associated with these metasomatka
Publikováno v:
Boletim Paranaense de Geociências. 52
O complexo máfico/ultramáfico Campo Formoso, no estado da Bahia, é constituído por rochas metamórficas de alto grau, derivadas de peridotitos e piroxenitos do Proterozóico Inferior. Em superfície, ele estende-se por cerca de 40 km, com largura