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首页> 外文期刊>Journal of South American earth sciences >Reinterpretation of the suture zone between the Itabuna-Salvador-Curaca and Jequie blocks, of the Sao Francisco Craton, Bahia, Brazil, using structural and geophysical data
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Reinterpretation of the suture zone between the Itabuna-Salvador-Curaca and Jequie blocks, of the Sao Francisco Craton, Bahia, Brazil, using structural and geophysical data

机译:使用结构和地球物理数据重新解释巴西巴伊亚州圣弗朗西斯科克拉顿的Itabuna-Salvador-Curaca和Jequie区块之间的缝合带

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摘要

The study area is located in the central portion of the Sao Francisco Craton (SFC), between two of the main blocks that compose this feature: the Jequie and the Itabuna-Salvador-Curaca blocks. The main objective of this study was to reevaluate the transition zone between both blocks, employing airborne geophysical, geologic and structural data. The geophysical data are represented by gamma-ray spectrometry and magnetic surveys, which showed the structure of the lithotypes mapped and helped in the identification of their limits. The analysis of these images established five radiometric domains and six magnetic zones. The geophysical data interpreted along with mapping survey, with macroscopic description and structural data, allowed better identification of the suture zone between the referred blocks. The structural analysis identified four deformation phases, characteristic of a transpressional zone, uplifting the ISCB onto JB. The present study proposes the modification of the limits between these blocks to a more southern location and updates the regional geotectonic understanding of the central region of the state of Bahia.
机译:研究区域位于圣弗朗西斯科·克拉顿(SFC)的中部,构成此功能的两个主要街区之间:Jequie和Itabuna-Salvador-Curaca街区。这项研究的主要目的是利用机载地球物理,地质和结构数据重新评估两个区块之间的过渡带。地球物理数据由伽马射线能谱仪和磁测图表示,这些图显示了标绘的岩石类型的结构,并有助于确定其界限。这些图像的分析建立了五个辐射域和六个磁区。地球物理数据与制图勘测一起解释,具有宏观描述和结构数据,可以更好地识别参考区块之间的缝合带。结构分析确定了四个变形阶段,这是一个超压带特征,将ISCB抬升到JB上。本研究建议将这些区块之间的界限修改为更南部的位置,并更新对巴伊亚州中部地区的区域大地构造认识。

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