@Article{AlvesRossValeAndr:2019:EvLaQu,
author = "Alves, F{\'a}bio Corr{\^e}a and Rossetti, Dilce de F{\'a}tima
and Valeriano, M{\'a}rcio de Morisson and Andrades Filho,
Cl{\'o}dis de Oliveira",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Universidade Estadual do Rio
Grande do Sul (UERGS)}",
title = "Neotectonics in the South American passive margin: Evidence of
late quaternary uplifting in the northern Paraiba Basin (NE
Brazil)",
journal = "Geomorphology",
year = "2019",
volume = "325",
pages = "1--16",
month = "Jan.",
keywords = "Digital elevation model, Uplifting, Late Quaternary, South
American passive margin.",
abstract = "The relief evolution of several areas of northeastern Brazil has
been increasingly related to tectonic events. This is the case for
the Paraiba Basin, where an abundance of faults and folds were
recorded in Neogene and even Late Pleistocene-Holocene deposits.
We tested whether dome-like morphologies in the northern sector of
this basin, where geological exposures are scarce, were also
formed by tectonic deformation. The work combined limited
geological data with qualitative and quantitative analyses of the
relief applying the 1 arc-second digital elevation model provided
by the Shuttle Radar Topography Mission. The geomorphic indices of
basin asymmetry factor (AF), swath topographic profiles, enhanced
transverse hypsometry index (THi*) and normalized river
long-profiles were used for validating a neotectonic origin for
the dome-like morphologies. This interpretation was also supported
by other morphological evidence of the dome relief, including:
recurving channels featured in radial to recurved trellis
patterns; tectonically-controlled drainage sub-basins; high
relative relief values related to increased fluvial incision; and
anomalous river long-profiles indicative of ungraded rivers. The
domic structures were attributed to fault- and fold-related
strike-slip deformation during the late Quaternary. This record
supports the proposal that the South American passive margin
remained under tectonic stress long after the main rifting in the
late Jurassic-early Cretaceous.",
doi = "10.1016/j.geomorph.2018.09.028",
url = "http://dx.doi.org/10.1016/j.geomorph.2018.09.028",
issn = "0169-555X",
language = "en",
targetfile = "alves_neotectonics.pdf",
urlaccessdate = "20 maio 2024"
}