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• W4310571329 abstract "Structural studies carried out on mesoscopic scale of planar and linear brittle structures from quarries in Precambrian rocks of the central-southern portion of the Catarinense Shield led to a characterization of four main fault directions: NE-SW, NW-SE and some around N-S and E-W. The older dextral (~ N-S) and sinistral (~ E-W) strike-slip faults are explained through a paleostress field approximately NE-SW oriented. The younger dextral (NE-SW) and sinistral (NW) strike-slip faults are compatible with an approximately E-W oriented paleostress field. The oldest event fits between the Cretaceous and Cenozoic and the younger event fits between the Neogene and Quaternary." @default.
• W4310571329 created "2022-12-12" @default.
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• W4310571329 date "2022-01-01" @default.
• W4310571329 modified "2023-09-26" @default.
• W4310571329 title "Mesozoic/cenozoic strike-slip tectonics in the catarinense shield and its correlation with structures associated with the continental rift in southeastern Brazil" @default.
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• W4310571329 doi "https://doi.org/10.1590/0001-3765202220211033" @default.
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