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- W4280494590 abstract "Abstract The Viggiano Mt. platform carbonates form a layered succession cross-cut by a dense array of pressure solution seams, and five sets of fractures and veins, which together form a sub-seismic structural network associated with polyphasic tectonic evolution. To assess the influence exerted by depositional and diagenetic heterogeneities on fracture geometry, distribution and multiscale properties, we present the results of stratigraphic, petrographic, mineralogical and mesoscale structural analyses conducted at the Viggiano Mountain, southern Italy. Based on rock textures and fossil associations, we documented that the Sinemurian–Pleinsbachian carbonates were deposited in a low-energy open lagoon, the Toarcian carbonates in a ramp setting rimmed by sand shoals, and the Cenomanian carbonates in a medium- to high-energy, lagoonal–tidal setting. Fracture-density (P20) and intensity (P21) values computed after circular scanline measurements show similar trends in both Sinemurian–Pleinsbachian and Toarcian carbonates, consistent with the bed and bed-package heterogeneities acting as efficient mechanical interfaces during incipient faulting. On the other hand, P20 and P21 do not show very similar variations throughout the Cenomanian carbonates due to pronounced bed amalgamation. Throughout the study area, the aforementioned parameters do not vary in proportion to the bed thickness, and show higher values within the coarse-grained carbonate beds. This conclusion is confirmed by results of linear scanline measurements, which focus on the P10 properties of the most common diffuse fracture set. The original results reported in this work are consistent with burial-related, physical–chemical compaction and cementation processes affecting the fracture stratigraphy of the Mesozoic platform carbonates." @default.
- W4280494590 created "2022-05-22" @default.
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- W4280494590 creator A5072945902 @default.
- W4280494590 date "2022-05-19" @default.
- W4280494590 modified "2023-10-18" @default.
- W4280494590 title "Fracture stratigraphy of Mesozoic platform carbonates, Agri Valley, southern Italy" @default.
- W4280494590 cites W1496646338 @default.
- W4280494590 cites W1639626886 @default.
- W4280494590 cites W1961220440 @default.
- W4280494590 cites W1967436979 @default.
- W4280494590 cites W1973555167 @default.
- W4280494590 cites W1974370779 @default.
- W4280494590 cites W1976970169 @default.
- W4280494590 cites W1977428438 @default.
- W4280494590 cites W1980291244 @default.
- W4280494590 cites W1981009026 @default.
- W4280494590 cites W1984116629 @default.
- W4280494590 cites W1985812645 @default.
- W4280494590 cites W1989769473 @default.
- W4280494590 cites W1990270818 @default.
- W4280494590 cites W1991818708 @default.
- W4280494590 cites W1992121998 @default.
- W4280494590 cites W1992601320 @default.
- W4280494590 cites W1999305528 @default.
- W4280494590 cites W2001205080 @default.
- W4280494590 cites W2005203918 @default.
- W4280494590 cites W2005268633 @default.
- W4280494590 cites W2007748096 @default.
- W4280494590 cites W2008458017 @default.
- W4280494590 cites W2011272671 @default.
- W4280494590 cites W2014491351 @default.
- W4280494590 cites W2015112602 @default.
- W4280494590 cites W2015889059 @default.
- W4280494590 cites W2020847161 @default.
- W4280494590 cites W2021096449 @default.
- W4280494590 cites W2023869153 @default.
- W4280494590 cites W2026804472 @default.
- W4280494590 cites W2028684055 @default.
- W4280494590 cites W2032773424 @default.
- W4280494590 cites W2033867961 @default.
- W4280494590 cites W2034892466 @default.
- W4280494590 cites W2037415830 @default.
- W4280494590 cites W2039761922 @default.
- W4280494590 cites W2040015450 @default.
- W4280494590 cites W2043252277 @default.
- W4280494590 cites W2043408739 @default.
- W4280494590 cites W2047997104 @default.
- W4280494590 cites W2049071194 @default.
- W4280494590 cites W2050569300 @default.
- W4280494590 cites W2051527466 @default.
- W4280494590 cites W2051737686 @default.
- W4280494590 cites W2051875053 @default.
- W4280494590 cites W2055639186 @default.
- W4280494590 cites W2055944292 @default.
- W4280494590 cites W2056390919 @default.
- W4280494590 cites W2069626853 @default.
- W4280494590 cites W2069682007 @default.
- W4280494590 cites W2076098565 @default.
- W4280494590 cites W2077351841 @default.
- W4280494590 cites W2078206416 @default.
- W4280494590 cites W2080714679 @default.
- W4280494590 cites W2083824245 @default.
- W4280494590 cites W2085932537 @default.
- W4280494590 cites W2087246217 @default.
- W4280494590 cites W2089458442 @default.
- W4280494590 cites W2090276952 @default.
- W4280494590 cites W2091028913 @default.
- W4280494590 cites W2092273609 @default.
- W4280494590 cites W2095442334 @default.
- W4280494590 cites W2097033875 @default.
- W4280494590 cites W2097304923 @default.
- W4280494590 cites W2116033899 @default.
- W4280494590 cites W2120285078 @default.
- W4280494590 cites W2122685419 @default.
- W4280494590 cites W2131616329 @default.
- W4280494590 cites W2133338925 @default.
- W4280494590 cites W2133477667 @default.
- W4280494590 cites W2140319746 @default.
- W4280494590 cites W2151490301 @default.
- W4280494590 cites W2163475804 @default.
- W4280494590 cites W2167662102 @default.
- W4280494590 cites W2258982263 @default.
- W4280494590 cites W2300828436 @default.
- W4280494590 cites W2332707452 @default.
- W4280494590 cites W2338358517 @default.
- W4280494590 cites W2407190894 @default.
- W4280494590 cites W2462063280 @default.
- W4280494590 cites W2515763494 @default.
- W4280494590 cites W2552932169 @default.
- W4280494590 cites W2626723595 @default.
- W4280494590 cites W2749992262 @default.
- W4280494590 cites W2755813755 @default.
- W4280494590 cites W2767185858 @default.
- W4280494590 cites W2791857910 @default.