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Time–frequency spectral signature of Pelotas Basin deep water gas hydrates system
by
Vilhena, Odilla
, da Costa, Emanuel
, Oliveira, Sérgio
in
Deep water
/ Earth and Environmental Science
/ Earth Sciences
/ Frequencies
/ Frequency analysis
/ Gas hydrates
/ Gases
/ Geological structures
/ Geophysics/Geodesy
/ Hydrates
/ Lithology
/ Marine
/ Oceanography
/ Offshore Engineering
/ Original Research Paper
/ River basins
/ Seismic waves
/ Seismology
/ Spectrum analysis
2010
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Time–frequency spectral signature of Pelotas Basin deep water gas hydrates system
by
Vilhena, Odilla
, da Costa, Emanuel
, Oliveira, Sérgio
in
Deep water
/ Earth and Environmental Science
/ Earth Sciences
/ Frequencies
/ Frequency analysis
/ Gas hydrates
/ Gases
/ Geological structures
/ Geophysics/Geodesy
/ Hydrates
/ Lithology
/ Marine
/ Oceanography
/ Offshore Engineering
/ Original Research Paper
/ River basins
/ Seismic waves
/ Seismology
/ Spectrum analysis
2010
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While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Time–frequency spectral signature of Pelotas Basin deep water gas hydrates system
by
Vilhena, Odilla
, da Costa, Emanuel
, Oliveira, Sérgio
in
Deep water
/ Earth and Environmental Science
/ Earth Sciences
/ Frequencies
/ Frequency analysis
/ Gas hydrates
/ Gases
/ Geological structures
/ Geophysics/Geodesy
/ Hydrates
/ Lithology
/ Marine
/ Oceanography
/ Offshore Engineering
/ Original Research Paper
/ River basins
/ Seismic waves
/ Seismology
/ Spectrum analysis
2010
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Time–frequency spectral signature of Pelotas Basin deep water gas hydrates system
Journal Article
Time–frequency spectral signature of Pelotas Basin deep water gas hydrates system
2010
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Overview
Pelotas Basin has the largest gas hydrate occurrence of the Brazilian coast. The reserves are estimated in 780 trillion cubic feet, covering an area of 45,000 km
2
. In this work we apply spectral decomposition technique in order to better understand a gas hydrate deep water system, performing a continuous time–frequency analysis of seismic trace, where frequency spectrum is the output for each time sample of the seismic trace. This allows a continuous analysis on the effects of the geologic structures and lithology over frequency content of the seismic wave. Spectral anomalies found were interpreted as variations of hydrates concentration inside the Gas Hydrate Stability Zone (GHSZ), as well free gas accumulations beneath and Below the GHSZ and gas chimneys. We concluded that this technique has a good potential to assist seismic study of structures associated with gas hydrates accumulations.
Publisher
Springer Netherlands,Springer Nature B.V
Subject
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