Orogens and fold-and-thrust belts (FTB) commonly present
along-strike changes like changes in the structural architecture and/or
different deformation styles. The generation and evolution of the geological
architecture is primarily controlled by the presence of pre-existing structures
and/or stratigraphy horizontal changes. With the idea to keep advancing in the
knowledge of how this factors affect, we study the central-south Taiwan FTB.
Taiwan is an oblique Arc-continental collision between the
Luzon Arc, striking N-S, and the Eurasian continental margin, striking in south
Taiwan roughly E-W. This margin presents several extensional basins that now
are involved in the Taiwan FTB
In this study we combine surface geology and balanced cross
sections, which will help to understand the FTB, with seismic tomography and
seismicity, that are used to trace structures from the continental margin
offshore western Taiwan into the FTB. We use a Vp of 5.2 km/s as a proxy for
the basement-cover interface
We found that the FTB includes significant along strike
changes in structure and stratigraphy. Major N to S changes in seismic
velocities are interpreted as basement highs and lows and these correlate with
areas were changes in the structural grain of the FTB take place, including
some localized variation in the strike of thrusts and folds that are evident on
the map. Several seismicity clusters align along the borders of these basement
blocks. We interpret this to be related with reactivation of basement
structures.
Figure 1: a) Tomography
of 6km depth slice showing with grey transparent rectangles the main areas with
velocity changes. b) Tomography E-W sections with seismicity and main geologic
structures. c) Geological map showing with grey transparent rectangles the main
areas were structural and stratigraphic changes are present. d) N-S tomography
section with seismicity showing a seismicity cluster at the south of a basement
high. e) Block diagram showing roughly the possible structure of the basement
on the fold-and-thrust belt, with gray transparent rectangles showing the areas
were structural, stratigraphic, velocity and seismicity changes are.
This work is supervised by Joaquina
Álvarez-Marrón and Dennis Brown (ICTJA-CSIC). Economic support has been
provided through CGL2014-4377-P project funded by the Spanish Ministry of
Science and Innovation. We acknowledge National Geographic Institute for
providing the seismic data for the study.
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