Produção Científica

**Apresentação**

Uma formulaÃ§Ã£o Bayesiana para inversÃ£o conjunta de AVO de dados PP e PSSÃ©rgio Adriano Moura Oliveira, Fernando SÃ©rgio de Moraes, Anderson Franco e JosÃ© Caparica. 1Âº Workshop do INCT-GP (2011) |

**Apresentação**

Medidas de coerÃªncia para anÃ¡lise de velocidade na migraÃ§Ã£o em tempo.Jonathas da S. Maciel, JessÃ© C. Costa e JÃ¶rg Schleicher. 1Âº Workshop do INCT-GP (2011) |

**Apresentação**

Results for three simple sea bed logging antenna modelsAllen Q. Howard. JR. 1Âº Workshop do INCT-GP (2011) |

**Apresentação**

RecuperaÃ§Ã£o de contornos nÃ£o convexos de corpos anÃ´malos na tomografia poÃ§o a poÃ§o em funÃ§Ã£o da presenÃ§a de ruÃdoWalter EugÃªnio de Medeiros, Roberto Hugo Bielschowsky. 1Âº Workshop do INCT-GP (2011) |

**Apresentação**

High-order pseudo-analytical method for acoustic wave modelingReynam Pestana, Chunlei Chu and Paul L. Stoffa. 1Âº Workshop do INCT-GP (2011) |

**Apresentação**

Modelagem Bidimensional do MÃ©todo EletromagnÃ©tico a MultifrequÃªncia.ValdelÃrio da Silva e Silva, CÃcero Roberto Teixeira RÃ©gis e Carlos Alberto Dias. 1Âº Workshop do INCT-GP (2011) |

**Apresentação**

Fast estimation of common-reflection-surface parameters using local slopesLÃºcio Santos, JÃ¶rg Schleicher, JessÃ© C. Costa, and AmÃ©lia Novais. 1Âº Workshop do INCT-GP (2011) |

**Apresentação**

3D complex PadÃ© FFD migration: A comparison of splitting techniquesJessÃ© C. Costa, DÃ©bora Mondini, JÃ¶rg Schleicher, and AmÃ©lia Novais SEG Expanded Abstracts 30, 4420-4424 (2011) SUMMARY Three-dimensional wave-equation migration techniques are quite expensive because of the huge matrices that need to be inverted. Many techniques have been proposed to reduce this cost by splitting the 3D problem into a sequence of 2D problems. We compare the performance of splitting techniques for stable 3D Fourier Finite-Difference (FFD) migration techniques in terms of image quality and computational cost. The FFD methods are complex Pade FFD and FFD plus interpolation, and the compared splitting techniques are two and fourway splitting as well as alternating four-way splitting, i.e., splitting into the coordinate directions at one depth and the diagonal directions at the next level. From numerical examples in homogeneous and inhomogeneous media, we conclude that alternate four-way splitting yields results of the same quality as full four-way splitting at the cost of two-way splitting. |

**Apresentação**

Diffraction imaging point of common-offset gather: GPR data exampleJ. J. S. de Figueiredo, F. Oliveira, E. Esmi, L. Freitas, S. Green, A. Novais, and J. Schleicher SEG Expanded Abstracts 30, 4399-4403 (2011) SUMMARY Hydrocarbon traps are generally located beneath complex geological structures. Such areas contain many seismic diffractors that carry detailed structure information in the order of the seismic wavelength. Therefore, the development of computational resources capable of detecting diffractor points with a good resolution is desirable, but has been a challenge in the area of seismic processing. In this work, we present a method for the detection of diffractor points in the common-offset gathers domain. In our approach, the diffraction imaging is based on the diffraction operator, which can be used in both the time and depth domains, in accordance with the complexity of the area. This method, which does not require any knowledge apart from the migration velocity field (i.e., rms velocities or interval velocities) applies pattern recognition to the amplitudes along the diffraction operator. Numerical examples using synthetic and real data demonstrate the feasibility of the technique. |

**Apresentação**

Coherence measures in automatic time migration velocity analysisJonathas S. Maciel, JessÃ© C. Costa (UFPA & INCT-GP, Brazil) and JÃ¶rg Schleicher (Unicamp & INCT-GP, Brazil) SUMMARY Time-migration velocity analysis can be carried out automatically by evaluating the coherence of the migrated seismic events in the common-image gathers (CIGs). The performance of gradient methods for automatic time-migration velocity analysis depends on the coherence measures used in the objective function. We compare the results of four different coherence measures, being conventional semblance, differential semblance, an extended differential semblance using more neighboring traces, and the product of the latter with conventional semblance. In our numerical experiments, the objective functions based on conventional semblance and on the product of conventional semblance with extended differential semblance provided the best velocity models, as evaluated by the flatness of the resulting common-image gathers. The method can be easily extended to anisotropic media. |

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