{"id":2243,"date":"2010-08-19T21:53:25","date_gmt":"2010-08-20T00:53:25","guid":{"rendered":"https:\/\/giruenf.org\/?p=2243"},"modified":"2018-12-26T14:38:52","modified_gmt":"2018-12-26T16:38:52","slug":"time-frequency-spectral-signature-of-pelotas-basin-deep-water-gas-hydrates-system","status":"publish","type":"post","link":"https:\/\/giruenf.org\/?p=2243","title":{"rendered":"Time\u2013frequency spectral signature of Pelotas Basin deep water gas hydrates system"},"content":{"rendered":"

Time\u2013frequency spectral signature of Pelotas Basin deep water gas hydrates system<\/h3>\n<\/div>
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Revista: Marine Geophysical Researches, 2010, 31, 89-97<\/strong><\/p>\n

Abstract:\u00a0Pelotas 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 km2. In this work we apply spectral decomposition technique in order to better understand a gas hydrate deep water system, performing a continuous time\u2013frequency 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.<\/p>\n

\u00a0http:\/\/link.springer.com\/article\/10.1007%2Fs11001-010-9085-x<\/a><\/p>\n<\/div>

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