@InProceedings{MarquesAssuPadiPádu:2018:AsSoAm,
author = "Marques, Haroldo Antonio and Assump{\c{c}}{\~a}o, Marcelo and
Padilha, Ant{\^o}nio Lopes and P{\'a}dua, Marcelo Banik de",
affiliation = "{Instituto Militar de Engenharia (IME)} and {Universidade de
S{\~a}o Paulo (USP)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)}",
title = "Assessment of South America mid-plate strain rates through GNSS
velocities estimated from SIRGAS-C time series",
year = "2018",
organization = "AGU Fall Meeting",
abstract = "We are investigating terrain deformations of long range and
persistence that take place on continental scale over the stable
shield of continental South America. The crustal deformation is
being investigated by correlating with velocities and directions
obtained from time series of approximately 60 GNSS stations
deployed in Brazil and neighboring countries that take part of the
Continuous network of the Geocentric Reference System for the
Americas (SIRGAS-C). We attempt to estimate velocities and
mid-plate strain rates using the best GNSS stations located in the
stable South America mid-plate. The velocities have been estimated
by Least Square Estimation (LSE) using SIRGAS weekly time series
with a stochastic model composed of white noise plus flicker or
random walk noises. Variance Component Estimation (VCE;
Amiri-Simkooei et al., 2007) has been applied to classify the type
of noise and compose the time series stochastic model. In
addition, the time series breaks and offsets are taken into
account in the LSE. The noises were classified as white plus
flicker noise in approximately 70% of the horizontal component and
most of random walk appears for stations located in the Amazon and
Pantanal basins or near the coastal zones. The estimated formal
precision reach about 0.10 mm/year with RMS of residual near 1.5
and 4.5 mm respectively for horizontal and vertical velocities.
The estimated velocities by LSE were also computed by using the
MIDAs code (Blewit et al 2015) and the results show an agreement
of the order of 0.30 mm/y. The computed strain rates in the
central part of Brazil indicate shortening, consistent with the
predominance of reverse faulting mechanisms. When a station pair
includes one station near the coast, the linear strain rates
indicate extension. However, strain rates do not clearly indicate
a preferred principal direction and do not seem compatible with
the stress patterns derived from the focal mechanisms. In
addition, the rate of seismic moment release indicates strain
rates from earthquake occurrence two to three orders of magnitude
lower than the observed strain rates from the geodetic network.
Assessment of South America linear strain rates computed through
estimated GNSS velocities will be discussed.",
conference-location = "Washington, D. C.",
conference-year = "10-14 dec.",
language = "en",
ibi = "8JMKD3MGP3W34R/3SB3DDH",
url = "http://urlib.net/ibi/8JMKD3MGP3W34R/3SB3DDH",
targetfile = "marques_assessment.pdf",
urlaccessdate = "27 abr. 2024"
}