Matches in SemOpenAlex for { <https://semopenalex.org/work/W4220994671> ?p ?o ?g. }
- W4220994671 endingPage "105673" @default.
- W4220994671 startingPage "105673" @default.
- W4220994671 abstract "Soft-sediment deformation structures (SSDSs) are ubiquitous in several depositional sedimentary environments and can be triggered by autogenic- and allogenic-related mechanisms. SSDSs identification in the geological record is more frequent in siliciclastic deposits, from which the most accepted models were developed. Given the fact that carbonate rocks have rapid diagenesis, which results in changes in the rheological behavior of deformational processes in short time, these are excellent facies for exploring past deformational mechanisms in a given sedimentary basin. Here, we describe distinct SSDSs developed in mixed carbonate-siliciclastic successions deposited in an Early Cretaceous lacustrine depositional system (carbonate-dominated) subjected to recurrent epicontinental marine ingressions (siliciclastic-dominated). Deformation occur in some siliciclastic intervals but it is more common in carbonate beds. Facies associations analysis combined with detailed outcrop description of the SSDSs allowed the recognition of seismic- and non-seismic-generated structures. Two km-scale, laterally continuous carbonate beds, characterized by deformation-bearing horizons, are interpreted to be the result of seismic shocks. Conversely, most of the recognized SSDSs cannot be confidentially interpreted as seismites. Autogenic triggers and criteria for accessing the origin of deformation mechanisms in both carbonate- and siliciclastic-dominated settings are alternatively proposed. Assessing such criteria is fundamental for differentiatte the timing and range of deformation and are here discussed in the context of the offshore petroleum reservoirs in the Brazilian Pre-Salt successions, where lacustrine carbonates were probably subjected to a similiar superposition of syn-sedimentary seismicity and later events of salt-tectonics and hydrotermalism." @default.
- W4220994671 created "2022-04-03" @default.
- W4220994671 creator A5009085965 @default.
- W4220994671 creator A5042608269 @default.
- W4220994671 creator A5042851364 @default.
- W4220994671 creator A5047909621 @default.
- W4220994671 creator A5053215574 @default.
- W4220994671 creator A5061809739 @default.
- W4220994671 creator A5075312461 @default.
- W4220994671 date "2022-06-01" @default.
- W4220994671 modified "2023-10-15" @default.
- W4220994671 title "Evaluation of distinct soft-sediment deformation triggers in mixed carbonate-siliciclastic systems: Lessons from the Brazilian Pre-Salt analogue Crato Formation (Araripe Basin, NE Brazil)" @default.
- W4220994671 cites W1508694051 @default.
- W4220994671 cites W1833718078 @default.
- W4220994671 cites W1965015674 @default.
- W4220994671 cites W1965514731 @default.
- W4220994671 cites W1974695842 @default.
- W4220994671 cites W1978105150 @default.
- W4220994671 cites W1978251637 @default.
- W4220994671 cites W1982454684 @default.
- W4220994671 cites W1986297985 @default.
- W4220994671 cites W1993477453 @default.
- W4220994671 cites W1993610346 @default.
- W4220994671 cites W1997606857 @default.
- W4220994671 cites W2003449785 @default.
- W4220994671 cites W2007527244 @default.
- W4220994671 cites W2020631733 @default.
- W4220994671 cites W2022139345 @default.
- W4220994671 cites W2023910092 @default.
- W4220994671 cites W2024361351 @default.
- W4220994671 cites W2026799494 @default.
- W4220994671 cites W2033191509 @default.
- W4220994671 cites W2033765758 @default.
- W4220994671 cites W2034743106 @default.
- W4220994671 cites W2040834673 @default.
- W4220994671 cites W2047711976 @default.
- W4220994671 cites W2048770598 @default.
- W4220994671 cites W2055068542 @default.
- W4220994671 cites W2056435215 @default.
- W4220994671 cites W2056645750 @default.
- W4220994671 cites W2056892988 @default.
- W4220994671 cites W2062461656 @default.
- W4220994671 cites W2065093349 @default.
- W4220994671 cites W2067637061 @default.
- W4220994671 cites W2072471257 @default.
- W4220994671 cites W2072766643 @default.
- W4220994671 cites W2073480393 @default.
- W4220994671 cites W2075013000 @default.
- W4220994671 cites W2078333278 @default.
- W4220994671 cites W2099889411 @default.
- W4220994671 cites W2100920322 @default.
- W4220994671 cites W2101798675 @default.
- W4220994671 cites W2105166733 @default.
- W4220994671 cites W2109345399 @default.
- W4220994671 cites W2117249545 @default.
- W4220994671 cites W2125235146 @default.
- W4220994671 cites W2136729612 @default.
- W4220994671 cites W2143187817 @default.
- W4220994671 cites W2144964641 @default.
- W4220994671 cites W2155171122 @default.
- W4220994671 cites W2156339033 @default.
- W4220994671 cites W2168369208 @default.
- W4220994671 cites W2169857923 @default.
- W4220994671 cites W2171167339 @default.
- W4220994671 cites W2216371600 @default.
- W4220994671 cites W2268825196 @default.
- W4220994671 cites W2318182075 @default.
- W4220994671 cites W2392752597 @default.
- W4220994671 cites W2403014497 @default.
- W4220994671 cites W2415516716 @default.
- W4220994671 cites W2421790818 @default.
- W4220994671 cites W2465953013 @default.
- W4220994671 cites W2471623583 @default.
- W4220994671 cites W2539311635 @default.
- W4220994671 cites W2543354053 @default.
- W4220994671 cites W2555175070 @default.
- W4220994671 cites W2737535442 @default.
- W4220994671 cites W2741460040 @default.
- W4220994671 cites W2743780973 @default.
- W4220994671 cites W2753923995 @default.
- W4220994671 cites W2763696473 @default.
- W4220994671 cites W2775262878 @default.
- W4220994671 cites W2883187987 @default.
- W4220994671 cites W2885965268 @default.
- W4220994671 cites W2891303491 @default.
- W4220994671 cites W2895679661 @default.
- W4220994671 cites W2902296922 @default.
- W4220994671 cites W2904022903 @default.
- W4220994671 cites W2913387978 @default.
- W4220994671 cites W2914852198 @default.
- W4220994671 cites W2922569569 @default.
- W4220994671 cites W2924216826 @default.
- W4220994671 cites W2940329898 @default.
- W4220994671 cites W2941195061 @default.
- W4220994671 cites W2941978054 @default.
- W4220994671 cites W2946303985 @default.
- W4220994671 cites W2957127511 @default.
- W4220994671 cites W2959367486 @default.