FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2131134554> ?p ?o ?g. }

• W2131134554 endingPage "257" @default.
• W2131134554 startingPage "241" @default.
• W2131134554 abstract "The Lower Cretaceous (Berriasian) Valdeprado Formation (Cameros Basin, northern Spain) contains more than 900 m of laminated carbonates and pseudomorphs after sulfates. Traditionally, many sedimentary packages of different ages and lithologies have been interpreted as deep-water deposits based essentially on the abundance of laminations and the absence of subaerial exposure features. In contrast, the Valdeprado Formation provides an example of a shallow-water deposit dominated by laminations with scarce evidence of subaerial exposure, and gives criteria to solve the challenge of distinguishingshallow-water and deep-water, ancient laminated deposits.The two most abundant facies all along the Valdeprado Formation are: a) parallel-laminated limestone, formed byalternating carbonate mudstone and calcite and quartz pseudomorphs after displacive gypsum, and b) graded-laminated limestone, consisting of quartz, mica, ostracodes, and pseudomorphs after detrital gypsum grains at the base, which changes gradually upwards to carbonate mudstone. Parallel-laminated limestone and graded-laminated limestone could have been deposited in either deep or shallow environments as a result of salinity fluctuations driven by alternation of flooding andevaporation and by sediment resuspension processes, respectively. Subaerial exposure features, such as desiccation mudcracks, are scarce in most of the succession, except in a few meter-scale stratigraphic intervals where they are very abundant. Interestingly, in these intervals desiccation cracks are present at the tops of several successive laminae (up to 25 mudcrackedlaminae per meter of deposit), indicating that, at least during those periods of time, deposition occurred in shallow water bodies that were desiccated frequently. In the upper part of the stratigraphic section, parallel-laminated and graded-laminated limestones are associated with current-ripple and wave-ripple cross-laminated arenites, and ostracode mudstone to wackestone with centimeter-size pseudomorphs after lenticular gypsum, and abundant desiccation mudcracks and tepees, which also suggestsedimentation in shallow-water environments. Moreover, the laminated carbonates display continuous, parallel layering, and the same facies along the 40-km-long outcropping area. These deposits are directly interbedded with, and pass laterally to, siliciclastic sandy–muddy flat deposits in the western area of the basin, without clinoforms, slump structures, or slide masses in between. All of these features suggest deposition in shallow, perennial carbonate–sulfate water bodies and their peripheral mudflats, developed in a flat-bottomed basin with no marked gradients." @default.
• W2131134554 created "2016-06-24" @default.
• W2131134554 creator A5000322983 @default.
• W2131134554 creator A5016160373 @default.
• W2131134554 creator A5048364933 @default.
• W2131134554 creator A5090270117 @default.
• W2131134554 date "2013-04-09" @default.
• W2131134554 modified "2023-10-18" @default.
• W2131134554 title "Depositional Depth of Laminated Carbonate Deposits: Insights From the Lower Cretaceous Valdeprado Formation (Cameros Basin, Northern Spain)" @default.
• W2131134554 cites W1040261480 @default.
• W2131134554 cites W1482550205 @default.
• W2131134554 cites W1496187190 @default.
• W2131134554 cites W1523297324 @default.
• W2131134554 cites W1554623503 @default.
• W2131134554 cites W1564076024 @default.
• W2131134554 cites W1573350472 @default.
• W2131134554 cites W1589316101 @default.
• W2131134554 cites W1606487280 @default.
• W2131134554 cites W1673688546 @default.
• W2131134554 cites W1824516414 @default.
• W2131134554 cites W1909795750 @default.
• W2131134554 cites W196508073 @default.
• W2131134554 cites W1968939426 @default.
• W2131134554 cites W1973307821 @default.
• W2131134554 cites W1974957281 @default.
• W2131134554 cites W1979800212 @default.
• W2131134554 cites W1981161040 @default.
• W2131134554 cites W1981748068 @default.
• W2131134554 cites W1981768333 @default.
• W2131134554 cites W1982187447 @default.
• W2131134554 cites W1983353696 @default.
• W2131134554 cites W1988754874 @default.
• W2131134554 cites W1992324899 @default.
• W2131134554 cites W1999626549 @default.
• W2131134554 cites W1999772449 @default.
• W2131134554 cites W2003216251 @default.
• W2131134554 cites W2010572118 @default.
• W2131134554 cites W2010919560 @default.
• W2131134554 cites W2018906472 @default.
• W2131134554 cites W2019671085 @default.
• W2131134554 cites W2026190235 @default.
• W2131134554 cites W2030087278 @default.
• W2131134554 cites W2035492077 @default.
• W2131134554 cites W2035718784 @default.
• W2131134554 cites W2036482356 @default.
• W2131134554 cites W2040087078 @default.
• W2131134554 cites W2045376179 @default.
• W2131134554 cites W2050568010 @default.
• W2131134554 cites W2051512258 @default.
• W2131134554 cites W2056672338 @default.
• W2131134554 cites W2065093349 @default.
• W2131134554 cites W206868555 @default.
• W2131134554 cites W2069719632 @default.
• W2131134554 cites W2074981976 @default.
• W2131134554 cites W2075127416 @default.
• W2131134554 cites W2081842181 @default.
• W2131134554 cites W2084199524 @default.
• W2131134554 cites W2088179139 @default.
• W2131134554 cites W2091974041 @default.
• W2131134554 cites W2106136177 @default.
• W2131134554 cites W2107364199 @default.
• W2131134554 cites W2109989023 @default.
• W2131134554 cites W2112523979 @default.
• W2131134554 cites W2114819910 @default.
• W2131134554 cites W2123876944 @default.
• W2131134554 cites W2132614854 @default.
• W2131134554 cites W2135341036 @default.
• W2131134554 cites W2137723516 @default.
• W2131134554 cites W2140765420 @default.
• W2131134554 cites W2145794341 @default.
• W2131134554 cites W2147767331 @default.
• W2131134554 cites W2149736100 @default.
• W2131134554 cites W2150772200 @default.
• W2131134554 cites W2156781874 @default.
• W2131134554 cites W2159100105 @default.
• W2131134554 cites W2159348598 @default.
• W2131134554 cites W2160219350 @default.
• W2131134554 cites W2162497332 @default.
• W2131134554 cites W2164162148 @default.
• W2131134554 cites W2168045244 @default.
• W2131134554 cites W2170327774 @default.
• W2131134554 cites W2266359591 @default.
• W2131134554 cites W2321066180 @default.
• W2131134554 cites W2326049910 @default.
• W2131134554 cites W2625955089 @default.
• W2131134554 cites W629685990 @default.
• W2131134554 cites W90548151 @default.
• W2131134554 cites W981087750 @default.
• W2131134554 cites W2492656256 @default.
• W2131134554 doi "https://doi.org/10.2110/jsr.2013.23" @default.
• W2131134554 hasPublicationYear "2013" @default.
• W2131134554 type Work @default.
• W2131134554 sameAs 2131134554 @default.
• W2131134554 citedByCount "20" @default.
• W2131134554 countsByYear W21311345542014 @default.
• W2131134554 countsByYear W21311345542015 @default.
• W2131134554 countsByYear W21311345542016 @default.
• W2131134554 countsByYear W21311345542018 @default.

• next