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- W2000532407 abstract "Abstract The gravity models of the Finnish rapakivi granites show a remarkable similarity both of shape and depth values. The models resemble enormous, asymmetric laccoliths, the depth of the root part being 18–20 km. The formation of the rapakivi-sandstone-complex in Satakunta is apparently closely connected with a Pre-Cambrian, NW—SE-striking zone of weakness." @default.
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- W2000532407 date "1970-03-31" @default.
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- W2000532407 title "An Interpretation of the Negative Gravity Anomalies Associated with the Rapakivi Granites and the Jotnian Sandstone in Southern Finland" @default.
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- W2000532407 doi "https://doi.org/10.1080/11035897009451912" @default.
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