A comportamento corrupto deve ser investigado a partir de diferentes níveis de análise. A nível intraindividual, a personalidade é uma variável relevante para sua compreensão. Objetivo. Na presente pesquisa, buscou-se analisar a influência dos traços de personalidade na intenção de comportamento corrupto a partir do modelo dos cinco grandes fatores da personalidade. Método. Participaram da pesquisa 286 indivíduos com idades entre 18 e 76 anos. Para coleta, foram utilizadas a Escala Reduzida dos cinco grandes fatores da personalidade, a Medida de Intenção de Corrupção e um questionário sociodemográfico. Resultados. Se encontraram correlações positivas entre a intenção de corrupção com as dimensões amabilidade, conscienciosidade e abertura à experiência. Porém, por meio de uma regressão linear múltipla, apenas a conscienciosidade teve efeito significativo. Implicações são discutidas.
e Barreirinhas Basin is located in northeast Brazil and is part of the Brazilian Equatorial Margin, a new exploration frontier with complex geology. is basin is characterized by a rugose water bottom, a fast carbonate platform, shallow gas pockets, and a complex channel network. All of these elements represent a signi cant challenge for velocity model building and imaging of the depositional system. From preprocessing to nal imaging, high-end technologies were required to meet the processing objectives. e 3D designature and 3D deghosting were crucial to remove bubble energy and ghosts related to canyon di ractions. e velocity model building exploited o set-dependent dip information in the nonlinear slope tomography-i.e., dip-constrained tomography (DCT)-to deal with small-scale lateral velocity variations. e full-waveform inversion, up to 20 Hz, was able to e ciently capture small velocity anomalies and resolve highspatial-resolution variations that DCT could not totally solve. Even with a detailed velocity model, some dim zones and amplitude variations were still observable in the depth-migrated image. Gas pockets, responsible for the absorption and phase distortion of the seismic signal (commonly denoted by the quality factor of attenuation, Q), were detected and delineated using volumetric Q tomography. e resultant interval Q model was consistent with the geology, and its use was bene cial in a Q-compensating Kirchho prestack depth migration.
Contents of this paper were reviewed by the Technical Committee of the 16 th International Congress of the Brazilian Geophysical Society and do not necessarily represent any position of the SBGf, its officers or members. Electronic reproduction or storage of any part of this paper for commercial purposes without the written consent of the Brazilian Geophysical Society is prohibited.
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