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- W2611616219 abstract "The late Miocene was characterized by high global temperatures and partly to nearly complete desiccation of the Mediterranean Sea throughout the latter part of the Messinian age (the Messinian salinity crisis). The non-marine paleoenvironmental and paleoclimatic records from the Mediterranean area are highly limited in their spatial range. Late Miocene river flood-plain sediments in the Central Anatolian Volcanic Province (CAVP) of central Turkey consist of siliciclastic and pyroclastic sediments with paleosols and calcrete. Five lithofacies were identified as (A) massive conglomerate, (B) trough-cross-bedded sandstone, (C) massive mudstone, (D) disrupted mud, (E) and disrupted matrix-supported conglomerate. The paleosols were composed predominantly of smectite and illite with smaller amounts of feldspar, quartz, opal-A, pyroxene and amphibole, and the calcretes were composed mainly of calcite, with smaller amounts of feldspar, quartz and opal-A, and minor amounts of smectite, chlorite and illite. Authigenic clay minerals and micritic calcite coating on the detrital grains and soil peds and pendant cement in the calcrete and paleosol horizons were evidence of a vadose zone. In contrast, the large equant spar drusy mosaics were formed in phreatic environments. The weathering of ignimbrite and marble led to the depletion of SiO2, CaO, Al2O3, Fe2O3, TiO2, and K2O through the precipitation of smectite and illite in the paleosols, and CaO in the form of micrite and calcite in the calcrete horizons. Field observations, mineralogy, geochemistry and the results of δ18O and δ13C isotopic analysis reveal that alternating wet and dry periods resulted in an upward increase in precipitation of authigenic smectite and illite within the late Miocene sections, under the influence of geochemical and pH fluctuations in phreatic or vadose water within the river flood-plain paleoenvironment." @default.
- W2611616219 created "2017-05-12" @default.
- W2611616219 creator A5062849902 @default.
- W2611616219 date "2017-09-01" @default.
- W2611616219 modified "2023-10-16" @default.
- W2611616219 title "Geology, mineralogy, and geochemistry of late Miocene paleosol and calcrete in the western part of the Central Anatolian Volcanic Province (CAVP), Turkey" @default.
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- W2611616219 cites W1972740096 @default.
- W2611616219 cites W1973326864 @default.
- W2611616219 cites W1976153669 @default.
- W2611616219 cites W1979384525 @default.
- W2611616219 cites W1985278073 @default.
- W2611616219 cites W1990059612 @default.
- W2611616219 cites W1993391787 @default.
- W2611616219 cites W1993718789 @default.
- W2611616219 cites W1996208972 @default.
- W2611616219 cites W2002114726 @default.
- W2611616219 cites W2005517049 @default.
- W2611616219 cites W2006470649 @default.
- W2611616219 cites W2008401349 @default.
- W2611616219 cites W2020653555 @default.
- W2611616219 cites W2024901067 @default.
- W2611616219 cites W2026608718 @default.
- W2611616219 cites W2028141898 @default.
- W2611616219 cites W2028385080 @default.
- W2611616219 cites W2031164272 @default.
- W2611616219 cites W2033832891 @default.
- W2611616219 cites W2034635765 @default.
- W2611616219 cites W2034809195 @default.
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- W2611616219 cites W2070507230 @default.
- W2611616219 cites W2072010825 @default.
- W2611616219 cites W2075164170 @default.
- W2611616219 cites W2079836004 @default.
- W2611616219 cites W2082972472 @default.
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- W2611616219 cites W2111421094 @default.
- W2611616219 cites W2117249156 @default.
- W2611616219 cites W2118061256 @default.
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- W2611616219 cites W2163482249 @default.
- W2611616219 cites W2164267444 @default.
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- W2611616219 doi "https://doi.org/10.1016/j.geoderma.2017.04.016" @default.
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