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- W2487188314 abstract "The Gran Sasso range shows two kinds of late Triassic successions: one, in the west, referable to a carbonate platform environment (Dolomia Principale fm), the other, to the east, deposited in an anoxic basin (Bituminous Dolostones fm). The Bituminous Dolostones lie on a thrust surface and they are very deformed. In spite of this, they preserve many sedimentary structures, described in this paper. Bituminous Dolostones are fine-grained and they consist of thin-bedded bituminous dolostones (often with planar lamination), solid bitumen layers and massive dolostones. Wave ripples were found just in one place. Plastic deformation structures, such as microslumps, slumps and convolute laminations, are frequent. Intraformational breccias usually consist of mud-supported flat granules of bitumen and, more rarely, of grain-supported clasts of bituminous dolostone and bitumen; both are interpreted as products of sliding that involved lithified or partially lithified sediments. Lithifaction occurred under shallow burial and preceded the bitumen maturation; it is evidenced also by normal faults and microfaults, bounded by undeformed beds and with a small throw. The sedimentary environment was characterized by the fall-out of fine-grained material with large amounts of organic matter. The periodically anoxic sea-bottom was rarely reached by the largest storm waves. The connection with the adjacent platform is interpreted as a gentle ramp." @default.
- W2487188314 created "2016-08-23" @default.
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- W2487188314 date "2005-01-01" @default.
- W2487188314 modified "2023-09-26" @default.
- W2487188314 title "Sedimentary structures in the Triassic bituminous dolostones of the eastern Gran Sasso Range (Italy)" @default.
- W2487188314 hasPublicationYear "2005" @default.
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