@Article{AlmeidaFoRoMiFeSiBe:2009:QuReBa,
author = "Almeida Filho, Raimundo and Rossetti, Dilce de F{\'a}tima and
Miranda, Fernando Pellon de and Ferreira, Francisco J F and Silva,
Clauzionor and Beisl, Carlos Henrique",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and Petrobras Research and
Development Center-CENPES, Rio de Janeiro, RJ, Brazil and Federal
University of Paran{\'a}-UFPR, Curitiba, PR, Brazil and Federal
University of Amazonas, UFAM, Manaus, AM, Brazil and Federal
University of Rio de Janeiro-UFRJ, Rio de Janeiro, RJ, Brazil",
title = "Quaternary reactivation of a basement structure in the
Barreirinhas Basin, Brazilian Equatorial Margin",
journal = "Quaternary Research",
year = "2009",
volume = "72",
number = "1",
pages = "103--110",
month = "Jul.",
keywords = "geophysical method, landscape, lineament, luminescence dating,
Miocene, morphology, Pleistocene, Quaternary, remote sensing,
structural control.",
abstract = "The Pirapemas Lineament is a remarkable 200-km-long, NE-SW
trending structure in the Barreirinhas Basin, one of the several
Brazilian coastal basins. This lineament splits the study area in
two sectors of distinctive morphology, drainage patterns, and
sedimentary covers. Terrain northward of the lineament presents a
smooth topography with sub-parallel to sub-dendritic drainage
patterns, whereas a dissected plateau characterized by incised
valleys and rectangular drainage pattern occurs southward,
suggesting a structural control by joints and faults. Geological
field data, crossed with thermal luminescence (TL) and optically
stimulated luminescence (OSL) dating, revealed that the surface
southward of the lineament consists mostly of Miocene and late
Pleistocene sedimentary deposits, represented by the Barreiras
Formation and the Post-Barreiras sediments, respectively. In
contrast, relatively younger sands mantle most of the northward
terrain, as indicated by well-preserved paleodune deposits that
grade into active aeolian dunes of the Lencois Maranhenses
National Park. Geomorphological and geological data analysis
suggests that the northern sector is under the effect of
subsidence, proving that the Pirapemas Lineament is an active
agent modeling the landscape in the region. Geophysical data
(gravity and seismic) confirm that such a structural feature is
the surface expression of an active deep-seated basement fault.",
doi = "10.1016/j.yqres.2009.02.010",
url = "http://dx.doi.org/10.1016/j.yqres.2009.02.010",
issn = "0033-5894",
label = "lattes: 4856245127929080 1 Almeida-FoRoMiFeSiBe:2009:QuReBa",
language = "en",
targetfile = "beisel.pdf",
urlaccessdate = "27 abr. 2024"
}