首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Robust geophysical integration through structure-coupled joint inversion and multispectral fusion of seismic reflection, magnetotelluric, magnetic, and gravity images: Example from Santos Basin, offshore Brazil
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Robust geophysical integration through structure-coupled joint inversion and multispectral fusion of seismic reflection, magnetotelluric, magnetic, and gravity images: Example from Santos Basin, offshore Brazil

机译:通过结构耦合的联合反演和地震反射,大地电磁,磁场和重力图像的多光谱融合进行稳健的地球物理整合:来自巴西近海桑托斯盆地的示例

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摘要

We have applied a crossgradient joint inversion and geospectral visualization method to marine seismic reflection, magnetotelluric, gravity, and magnetic data sets acquired along a 162 km profile across a segment of Santos Basin oil province in the continental margin of southeast Brazil. The main exploration targets are the top of the fractured Precambrian crystalline basement and any concealed basement grabens, the overlying presalt and salt/carbonate deposits, and the postsalt cover deposits. The results of joint inversion clearly mapped the various units and are a significant improvement over previous models derived from separate 2D seismic reflection processing and 2D magnetotelluric imaging. Additionally, multispectral fusion of these models resulted in a single image that permits highly constrained geologic interpretations enabling a better understanding of basin architecture. We suggest that joint inversion and image fusion is the way forward for effective geophysical integration.
机译:我们将跨梯度联合反演和地球光谱可视化方法应用于在巴西东南部大陆边界的Santos盆地石油省一段沿162 km剖面采集的海洋地震反射,大地电磁,重力和磁数据集。主要勘探目标是断裂的前寒武纪晶体基底的顶部和任何隐蔽的基底grab陷,上覆的盐前和盐/碳酸盐矿床以及后盐盖层矿床。联合反演的结果清楚地映射了各个单位,并且相对于以前的模型进行了重大改进,该模型是从单独的2D地震反射处理和2D大地电磁成像获得的。此外,这些模型的多光谱融合产生了一张图像,该图像允许高度受限的地质解释,从而可以更好地了解盆地构造。我们建议,联合反演和图像融合是有效地球物理整合的前进方向。

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