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- W2000443558 abstract "In this paper the structural setting of the Umbria-Marche fold belt is briefly described. The basement-cover relationships and the primary or secondary origin of the arcuate shape are also discussed. Mainly on the basis of structural data, it is suggested that the Umbria-Marche fold belt can hardly be the result of a thin-skinned tectonics under little overburden, but one or more deep-seated detachment levels must have worked (thick-skinned tectonics) during the Mio-Pliocene transpressional phase. Furthermore, an orocline origin for the arcuate shape of the fold belt, resulting from a progressive history of oblique right-lateral shearing, is suggested. During the first deformative stage (stage 1a, Late Miocene) the cover, detached from the basement, is deformed by a NW-SE trending linear fold belt, whilst the basement is deformed by oblique right-lateral shear. Then (stage 1b), the linear fold belt is progressively bent, by right-lateral dragging in correspondence with the deep-seated shear zones. During the second deformative stage (stage 2, Early Piocene), the cover deforms in connection with the basement: the northern and the central sectors of Umbria-Marche Apennines undergo a prevailing shortening accomodated by NW-SE, NNW-SSE dip-slip thrusting; the southern sector undergoes a prevailing right-lateral shearing, accommodated by NNE-SSW oblique thrusting." @default.
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- W2000443558 date "1988-01-01" @default.
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- W2000443558 title "The Umbria-Marche arcuate fold belt (Italy)" @default.
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- W2000443558 doi "https://doi.org/10.1016/0040-1951(88)90086-8" @default.
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