FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4205684997> ?p ?o ?g. }

• W4205684997 endingPage "24" @default.
• W4205684997 startingPage "24" @default.
• W4205684997 abstract "In this study, six basic Quaternary landform series (LFS) and their sedimentary deposits (LFS1 aeolian, LFS 2.1 to 2.2 mass wasting, LFS 3 cryogenic-glacial, LFS 4.1 to 4.6 fluvial, LFS 5.1 to 5.2 coastal-marine, LFS 6.1 to 6.3 lacustrine) are subdivided into subtypes and examined with regard to their sedimentological parameters and their mineralogical and chemical compositions. Emphasis is placed on the textural (related to transport and deposition), compositional (sediment load/weight, Eh and pH) and geodynamic maturity of the sedimentary deposits which are influenced by the parent lithology and bedrock tectonic and by the climate during the last 2 Ma. To constrain the development of the LFS and their sediments, composite trend-line diagrams are designed combining sedimentological (x-axis) and chemical/mineralogical dataset (y-axis): (1) sorting vs. heavy mineral content; (2) sphericity of grains vs. silica/carbonate contents; and (3) median vs. Ti/Fe ratios. In addition, the x-y plots showing the log SiO2/Al2O3 vs. log Na2O/K2O are amended by a dataset of the three most common clay minerals, i.e., kaolinite-, mica-, and smectite-group clay minerals. Such joint sedimentological-chemical-mineralogical investigations focused on the depositional environment of unconsolidated clastic sediments of Quaternary age can be used to describe the economic geology and environmental geology of mineral deposits in the pre-Quaternary sedimentary series according to the phrase: “The Present is the key to the Past”. Both trend diagrams and compositional x-y plots can contribute to constraining the development of the full transect of landform series from the fluvial incision and slope retreat to reef islands fringing the coastal zone towards the open sea as far as they are built up of clastic sedimentary deposits enriched in siliceous and/or carbonate minerals. Climate zonation and crustal maturity are the exogenous and endogenous “drivers”, as can be deduced from the compositional (mineralogy and chemistry) and physical (transport and deposition) variations observed in the Quaternary sediments. The current study bridges the gap between a review only based on literature and a hybrid manual generated by practical field studies devoted to applied geosciences in economic and environmental geology (“E & E issue”)." @default.
• W4205684997 created "2022-01-25" @default.
• W4205684997 creator A5014655086 @default.
• W4205684997 date "2022-01-06" @default.
• W4205684997 modified "2023-09-26" @default.
• W4205684997 title "Trends and Composition—A Sedimentological-Chemical-Mineralogical Approach to Constrain the Origin of Quaternary Deposits and Landforms—From a Review to a Manual" @default.
• W4205684997 cites W1485321927 @default.
• W4205684997 cites W1522680740 @default.
• W4205684997 cites W1587288524 @default.
• W4205684997 cites W1882205371 @default.
• W4205684997 cites W1906506370 @default.
• W4205684997 cites W1963584854 @default.
• W4205684997 cites W1963915811 @default.
• W4205684997 cites W1964253975 @default.
• W4205684997 cites W1969367528 @default.
• W4205684997 cites W1972604732 @default.
• W4205684997 cites W1974741654 @default.
• W4205684997 cites W1975921996 @default.
• W4205684997 cites W1982241772 @default.
• W4205684997 cites W1982258379 @default.
• W4205684997 cites W1982809901 @default.
• W4205684997 cites W1984077034 @default.
• W4205684997 cites W1984752020 @default.
• W4205684997 cites W1985733246 @default.
• W4205684997 cites W1985772392 @default.
• W4205684997 cites W1987075673 @default.
• W4205684997 cites W1987223324 @default.
• W4205684997 cites W1987867969 @default.
• W4205684997 cites W1988674279 @default.
• W4205684997 cites W1993859923 @default.
• W4205684997 cites W1994612790 @default.
• W4205684997 cites W1994958984 @default.
• W4205684997 cites W1995026670 @default.
• W4205684997 cites W1996902893 @default.
• W4205684997 cites W1997930364 @default.
• W4205684997 cites W1998450920 @default.
• W4205684997 cites W1998480190 @default.
• W4205684997 cites W1998835213 @default.
• W4205684997 cites W2001817815 @default.
• W4205684997 cites W2004529964 @default.
• W4205684997 cites W2006630397 @default.
• W4205684997 cites W2006994988 @default.
• W4205684997 cites W2009440314 @default.
• W4205684997 cites W2011651911 @default.
• W4205684997 cites W2012560032 @default.
• W4205684997 cites W2013724465 @default.
• W4205684997 cites W2017761260 @default.
• W4205684997 cites W2017844359 @default.
• W4205684997 cites W2017985414 @default.
• W4205684997 cites W2019365398 @default.
• W4205684997 cites W2023008226 @default.
• W4205684997 cites W2028361215 @default.
• W4205684997 cites W2028630457 @default.
• W4205684997 cites W2029783452 @default.
• W4205684997 cites W2031473613 @default.
• W4205684997 cites W2032226859 @default.
• W4205684997 cites W2032979417 @default.
• W4205684997 cites W2033356481 @default.
• W4205684997 cites W2034458246 @default.
• W4205684997 cites W2035321369 @default.
• W4205684997 cites W2037350614 @default.
• W4205684997 cites W2041080687 @default.
• W4205684997 cites W2042637615 @default.
• W4205684997 cites W2044636155 @default.
• W4205684997 cites W2046593598 @default.
• W4205684997 cites W2047729922 @default.
• W4205684997 cites W2047926728 @default.
• W4205684997 cites W2050487135 @default.
• W4205684997 cites W2050670879 @default.
• W4205684997 cites W2051584572 @default.
• W4205684997 cites W2052010649 @default.
• W4205684997 cites W2053320451 @default.
• W4205684997 cites W2054635427 @default.
• W4205684997 cites W2055452600 @default.
• W4205684997 cites W2056235941 @default.
• W4205684997 cites W2057117045 @default.
• W4205684997 cites W2059247071 @default.
• W4205684997 cites W2062081352 @default.
• W4205684997 cites W2065135402 @default.
• W4205684997 cites W2067396672 @default.
• W4205684997 cites W2067825499 @default.
• W4205684997 cites W2071391858 @default.
• W4205684997 cites W2076958925 @default.
• W4205684997 cites W2077089956 @default.
• W4205684997 cites W2078117752 @default.
• W4205684997 cites W2087192329 @default.
• W4205684997 cites W2088477088 @default.
• W4205684997 cites W2089284596 @default.
• W4205684997 cites W2090578644 @default.
• W4205684997 cites W2092309739 @default.
• W4205684997 cites W2092651219 @default.
• W4205684997 cites W2093701286 @default.
• W4205684997 cites W2097319335 @default.
• W4205684997 cites W2097996280 @default.
• W4205684997 cites W2101108516 @default.
• W4205684997 cites W2111660321 @default.
• W4205684997 cites W2113803257 @default.
• W4205684997 cites W2115100090 @default.

• next