2-D Inversion of magnetic data and gravity modelling of the transition zone between the Pernambuco-Alagoas domain and the northern portion of the Sergipano Belt (NE, Brazil)

Priscilla Alvarez, A. Dutra
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Abstract

Two-dimensional magnetic inversions were performed with the purpose to obtain information about the magnetic susceptibility, depth and volume of true magnetic sources located in the basement adjacent to the Sergipe-Alagoas basin, in the transition zone between the Pernambuco-Alagoas Domain and the northern portion of the Sergipano Belt (Borborema Province, NE Brazil) and to delineate its geometries. The magnetic data processing was performed to interpret geological contacts, source’s edge boundaries and mapping of folds and shear zones. In the results of the magnetic inversion, a source was found in the Rio Coruripe domain between 9 and 21 km in depth with a magnetic susceptibility of 0.0079 (SI) and another in the Pernambuco-Alagoas domain between 7.5 and 9 km with a magnetic susceptibility of 0.0077 (SI). The basement’s depth was obtained through spectral analysis, whose base was found at 37.7 km. In addition, gravity models were created with the purpose to verify the information obtained by the magnetic inversion and spectral analysis, which was useful to understand how these sources interfere in the structure of the basement and how it affected its tectonic model.
巴西东北部Pernambuco-Alagoas域与Sergipano带北部过渡带的二维磁资料反演及重力模拟
在Pernambuco-Alagoas域与Sergipano带北部(borborrema省,巴西东北部)之间的过渡带上,在Sergipe-Alagoas盆地附近的基底进行了二维磁反演,目的是获得真实磁源的磁化率、深度和体积信息,并描绘其几何形状。进行了磁资料处理,解释了地质接触面、震源边缘边界以及褶皱和剪切带的填图。在磁反演结果中,在Rio Coruripe域9 ~ 21 km处发现了一个磁化率为0.0079 (SI)的震源,在Pernambuco-Alagoas域7.5 ~ 9 km处发现了一个磁化率为0.0077 (SI)的震源。通过光谱分析得到基底深度,基底深度为37.7 km。此外,还建立了重力模型,对地磁反演和波谱分析得到的信息进行验证,有助于了解这些源对基底结构的干扰及其对构造模式的影响。
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