FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2010223894> ?p ?o ?g. }

• W2010223894 endingPage "91" @default.
• W2010223894 startingPage "75" @default.
• W2010223894 abstract "Significant changes in carbonate mineralogy, texture, and stable isotope composition occur at the transition from the Wilkins Peak Member to the Laney Member in the Eocene Green River Formation, Bridger Basin, Wyoming, which reflect evolution of inflow waters, lake waters, and paleoenvironments. The top of the Wilkins Peak Member contains heterogeneous laminae of calcite and dolomite. Evaporites associated with these layers suggest deposition in hypersaline lakes. Diagenetic carbonate mineral textures include euhedral cement overgrowths and interlocking mosaics of calcite and dolomite crystals, 20–70 μm in size. Electron microprobe analyses indicate diagenetic overgrowth of Fe-rich dolomite on cloudy Fe-poor cores. δ18O values of carbonate laminae in the upper Wilkins Peak Member vary by ~ 6‰ with no depth dependent or mineralogic trends, which also suggests diagenetic overprinting. Alternating organic-rich and primary aragonite, calcite, and dolomite laminae were identified from the lower Laney Member. Primary lacustrine aragonite consists of well sorted, prismatic crystals 5–10 μm in length, with micro-lamination defined by crystal size variation. Primary precipitated calcite and dolomite laminae are monominerallic, with well sorted polyhedral crystals, ~ 10 μm in size. Primary mineralogy of the lower Laney Member changes from calcite to aragonite and dolomite stratigraphically upward. Along the same 15 m thick stratigraphic interval, δ18O values decrease upward by ~ 3‰, all of which suggests (1) lake waters underwent evaporative concentration, which together with calcite precipitation increased the lake water Mg/Ca ratios and led to formation of aragonite and dolomite, (2) source waters became lower in δ18O, possibly as inflow changed to higher altitude foreland rivers. The results from this study show that understanding the primary lacustrine versus diagenetic origin of Green River carbonate minerals is essential for paleoenvironmental and paleoclimate interpretations." @default.
• W2010223894 created "2016-06-24" @default.
• W2010223894 creator A5006827140 @default.
• W2010223894 creator A5031060451 @default.
• W2010223894 creator A5059792787 @default.
• W2010223894 date "2014-12-01" @default.
• W2010223894 modified "2023-10-06" @default.
• W2010223894 title "Preservation of primary lake signatures in alkaline earth carbonates of the Eocene Green River Wilkins Peak-Laney Member transition zone" @default.
• W2010223894 cites W1450611364 @default.
• W2010223894 cites W1487996665 @default.
• W2010223894 cites W1491851109 @default.
• W2010223894 cites W1529529414 @default.
• W2010223894 cites W1537519627 @default.
• W2010223894 cites W1824516414 @default.
• W2010223894 cites W1964178556 @default.
• W2010223894 cites W1967628674 @default.
• W2010223894 cites W1968540330 @default.
• W2010223894 cites W1972070875 @default.
• W2010223894 cites W1972635099 @default.
• W2010223894 cites W1979862655 @default.
• W2010223894 cites W1981161040 @default.
• W2010223894 cites W1983272995 @default.
• W2010223894 cites W1989783267 @default.
• W2010223894 cites W1998260793 @default.
• W2010223894 cites W2002006624 @default.
• W2010223894 cites W2004361138 @default.
• W2010223894 cites W2006090307 @default.
• W2010223894 cites W2007460213 @default.
• W2010223894 cites W2007933701 @default.
• W2010223894 cites W2008281306 @default.
• W2010223894 cites W2009537421 @default.
• W2010223894 cites W2016411821 @default.
• W2010223894 cites W2017887575 @default.
• W2010223894 cites W2017913935 @default.
• W2010223894 cites W2024654077 @default.
• W2010223894 cites W2030300681 @default.
• W2010223894 cites W2032478816 @default.
• W2010223894 cites W2038557901 @default.
• W2010223894 cites W2040322819 @default.
• W2010223894 cites W2040843117 @default.
• W2010223894 cites W2043795917 @default.
• W2010223894 cites W2046736223 @default.
• W2010223894 cites W2047438189 @default.
• W2010223894 cites W2064251711 @default.
• W2010223894 cites W2065456918 @default.
• W2010223894 cites W2066161385 @default.
• W2010223894 cites W2067709398 @default.
• W2010223894 cites W2068168634 @default.
• W2010223894 cites W2068171707 @default.
• W2010223894 cites W2071184501 @default.
• W2010223894 cites W2072959158 @default.
• W2010223894 cites W2073480393 @default.
• W2010223894 cites W2074981976 @default.
• W2010223894 cites W2088988432 @default.
• W2010223894 cites W2096129028 @default.
• W2010223894 cites W2102790100 @default.
• W2010223894 cites W2113327033 @default.
• W2010223894 cites W2117586485 @default.
• W2010223894 cites W2118575573 @default.
• W2010223894 cites W2118931596 @default.
• W2010223894 cites W2121562238 @default.
• W2010223894 cites W2122325899 @default.
• W2010223894 cites W2127694256 @default.
• W2010223894 cites W2128907222 @default.
• W2010223894 cites W2132216432 @default.
• W2010223894 cites W2143539806 @default.
• W2010223894 cites W2146483033 @default.
• W2010223894 cites W2149736100 @default.
• W2010223894 cites W2149957944 @default.
• W2010223894 cites W2151476104 @default.
• W2010223894 cites W2158556931 @default.
• W2010223894 cites W2160219350 @default.
• W2010223894 cites W2163519046 @default.
• W2010223894 cites W2163608510 @default.
• W2010223894 cites W2168225982 @default.
• W2010223894 cites W2172583075 @default.
• W2010223894 cites W223703772 @default.
• W2010223894 cites W2275584307 @default.
• W2010223894 cites W2317325823 @default.
• W2010223894 cites W2471795074 @default.
• W2010223894 cites W4211032951 @default.
• W2010223894 cites W60834526 @default.
• W2010223894 doi "https://doi.org/10.1016/j.sedgeo.2014.09.005" @default.
• W2010223894 hasPublicationYear "2014" @default.
• W2010223894 type Work @default.
• W2010223894 sameAs 2010223894 @default.
• W2010223894 citedByCount "28" @default.
• W2010223894 countsByYear W20102238942015 @default.
• W2010223894 countsByYear W20102238942016 @default.
• W2010223894 countsByYear W20102238942017 @default.
• W2010223894 countsByYear W20102238942018 @default.
• W2010223894 countsByYear W20102238942019 @default.
• W2010223894 countsByYear W20102238942020 @default.
• W2010223894 countsByYear W20102238942021 @default.
• W2010223894 countsByYear W20102238942022 @default.
• W2010223894 countsByYear W20102238942023 @default.
• W2010223894 crossrefType "journal-article" @default.
• W2010223894 hasAuthorship W2010223894A5006827140 @default.

• next