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Proceedings of the 16th International Congress of the Brazilian Geophysical Society&Expogef最新文献

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Status of salt interpretation for velocity model building in Brazilian basins 巴西盆地速度模型建立中的盐解释研究现状
F. Marpeau, V. Belz
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引用次数: 0
Full-wave inversion (FWI) to a 2D-ocean-bottom node (OBN) dataset after offset-continuation-trajectory (OCT) data regularization 偏移-连续轨迹(OCT)数据正则化后的二维海底节点(OBN)数据全波反演(FWI)
A. Camargo, J. Ribeiro, T. Coimbra, G. Ignácio, M. Tygel
The estimation of geophysical attributes for a better understanding of subsurface geological structures is essential in many stages of seismic exploration and production. As a powerful seismic inversion tool, the full waveform inversion (FWI) has been widely used to estimate many of such attributes (e.g., seismic velocities) with high resolution. In many cases, however, real acquisitions are unable to provide the quantity and density of traces required for optimal inversion results. As a consequence, schemes to produce (simulate) new traces by interpolation/extrapolation of neighboring available traces, play a crucial role. In this paper, we use the offset-continuation-trajectory (OCT) stacking method to generate new (non-recorded) traces and include them in an ocean-bottom node (OBN) acquisition. We next test the FWI inversion on the enhanced dataset and analyze the results. As proof-of-concept, our approach is applied to the synthetic dataset obtained for an OBN acquisition carried out on the 2D Marmousi model for which several additional traces, simulated by the OCT procedure, have been included. In spite of the recognized complexities of the Marmousi model, we have obtained very encouraging results.
为了更好地了解地下地质构造,地球物理属性的估计在地震勘探和生产的许多阶段都是必不可少的。作为一种功能强大的地震反演工具,全波形反演(FWI)已被广泛用于高分辨率地估计许多此类属性(如地震速度)。然而,在许多情况下,实际采集无法提供最佳反演结果所需的道的数量和密度。因此,通过邻近可用迹线的插值/外推来产生(模拟)新迹线的方案起着至关重要的作用。在本文中,我们使用偏移-连续-轨迹(OCT)叠加方法来生成新的(未记录的)轨迹,并将它们包含在海底节点(OBN)采集中。接下来,我们在增强数据集上测试FWI反演并分析结果。作为概念验证,我们的方法被应用于在二维Marmousi模型上进行OBN采集获得的合成数据集,其中包括通过OCT程序模拟的几个附加迹线。尽管公认的马尔穆西模型的复杂性,我们已经获得了非常令人鼓舞的结果。
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引用次数: 0
Um Tutorial de Implementação da FWI e Avaliação da Influência do Uso da Diagonal da Pseudo-Hessiana 实现FWI的教程和使用伪hessian对角线的影响评估
Rafael Siqueira, Leandro Di Bartolo, B. Souza
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引用次数: 0
Modeling HTEM Data Anomalies for Mineral Exploration in the Quadrilatero Ferrifero Ferrifero区域矿产勘探HTEM数据异常建模
Gabriela Serejo de Oliveira, J. Porsani, M. Couto
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引用次数: 0
Resitividade Elétrica Aplicada à Mineralizações Manganesíferas em Castanheira, MT 电电阻率在卡斯坦海拉锰矿化中的应用
Moara de Matos, W. R. Borges, V. Pinto, Ciro Calachibete, Maria Clara Lopes Paula, I. Almeida
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引用次数: 0
Refining Structural Interpretation by Using the Composite Map of the Vertical Derivatives of Aeromagnetic Anomaly Data 利用航磁异常资料垂直导数复合图改进构造解释
B. C. Araújo, Maria da Gama, Flávio Junior, Tatiane do Nascimento, Luis Fernando da Silva, Guilherme dos Santos, L. Borghi, M. A. Braga, J. Figueiredo
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引用次数: 0
Thermomagnetic Features of Central Brazil, between regions of Trans-Brazilian Lineament (TBL) and São Francisco Craton (SFC) 巴西中部跨巴西构造(TBL)与<s:1>弗朗西斯科克拉通(SFC)之间的热磁特征
S. Guimarães, F. P. Vieira, V. Hamza
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引用次数: 0
Brazilian geomagnetic observatories - recent improvements and data availability 巴西地磁观测站——最近的改进和数据的可用性
G. Soares, K. Pinheiro, J. Matzka, A. Morschhauser, Cristiano Martins
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引用次数: 0
The influence of microporosity on porosity-permeability correlation in carbonate rocks 碳酸盐岩微孔隙度对孔渗对比的影响
Grazielle Oliveira, M. Ceia, R. Misságia, I. L. Neto, V. Santos
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引用次数: 0
Fissuras no pavimento da rodovia ERS-149 - Geofísica aplicada como auxílio na caracterização do terreno ERS-149公路路面裂缝-应用地球物理辅助地形表征
M. M. Zago, Maximilian Fries, I. Clemente, A. Nummer, R. Pinheiro
Geophysics is widely recognized tool in indirect subsurface and non-invasive investigation. It is applied in different near-surface and geotechnical studies. As an example, we can mention ground investigations for structures, cables, fractures, cavities and water infiltration. In geotechnics, lithologies heterogeneities, fault/joints and basement rocks soil (altered zone) investigations have been producing significant results with low costs, less time and simple logistics. This study proposes the use of direct current resistivity profiles to detect and characterize altered rocks layers limits (regolith), water saturated areas and depth as an auxiliary aid to characterize a collapsed asphalt paved road (ERS-149). The area is located between Faxinal do Soturno and Nova Palma cities, Rio Grande do Sul State, Brazil. Locally, on the road side, several cracks occurred due the ground instability leading to an asphalt and material below collapse. We performed two DC-resistivity profiles perpendicular to the road integrated with a high-resolution digital elevation model. The results presented a large amount of unconsolidated material (soil and rocks fragments) and a significant inpore water filling zones. These features, associated with the gravitational action in the area are interpreted as the main sliding, cracking and collapsing causes. The use of geophysics in this context was a valuable and effective method as an aid to conduct and locate direct subsurface investigations as detail geological and soil mapping and drill-holes to better describes the lithology/materials refining the subsurface modeling.
地球物理是一种被广泛认可的非侵入性地下间接勘探工具。它被应用于不同的近地表和岩土工程研究。例如,我们可以提到对结构、电缆、裂缝、空腔和水渗透的地面调查。在岩土工程中,岩性非均质性、断层/节理和基底岩石-土壤(蚀变带)的研究已经取得了显著的成果,而且成本低、时间短、物流简单。本研究建议使用直流电阻率剖面来检测和表征蚀变岩层极限(风化层)、水饱和面积和深度,作为表征坍塌沥青路面的辅助手段(ERS-149)。该地区位于巴西南里奥格兰德州法克斯纳尔和诺瓦帕尔马市之间。在当地,在道路一侧,由于地面不稳定,导致沥青和下面的材料倒塌,出现了几条裂缝。我们进行了两个垂直于道路的直流电阻率剖面,并结合了高分辨率数字高程模型。结果表明:该地区存在大量的松散物质(土和岩石碎块)和明显的孔隙充水带。这些特征与该地区的重力作用有关,被解释为主要的滑动、开裂和塌陷原因。在这种情况下,使用地球物理是一种有价值和有效的方法,可以帮助进行和定位直接的地下调查,如详细的地质和土壤测绘,以及钻孔,以更好地描述岩性/材料,完善地下建模。
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引用次数: 0
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Proceedings of the 16th International Congress of the Brazilian Geophysical Society&Expogef
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