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author Markov, Yu D
Mozherovsky, A V
Barinov, N N
Derkachev, A N
Utkin, I V
Sereda, N A
author_facet Markov, Yu D
Mozherovsky, A V
Barinov, N N
Derkachev, A N
Utkin, I V
Sereda, N A
collection Datos científicos de ciencias marinas y ambientales
contents Mineral and chemical compositions of highly ferruginous layered silicates (HLS) of glauconite sands occurred on the East Korean Rise outside volcanic structures and on an unnamed volcano and the Chentsov Volcano have been studied. The use of cluster and discriminant analyses has resulted to more objectively distinguished groups among HLS, and the use of factor analysis - to illustrate correlations between chemical elements in different groups. It has been found that green mineral assemblages of the East Korean Rise are heterogeneous in terms of morphology, composition and origin, and their formation is a complex multistage process including both neoformation and degradation.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_745243
institution PANGAEA
language en
publishDate 2005
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Chemical composition of Fe-rich layered silicates from the East Korean Rise, Japan Sea
Markov, Yu D
Mozherovsky, A V
Barinov, N N
Derkachev, A N
Utkin, I V
Sereda, N A
Aluminium oxide; Archive of Ocean Data; ARCOD; Area/locality; Calcium oxide; Calculated; Event label; Grab; GRAB; Iron oxide, Fe2O3; Iron oxide, FeO; Japan Sea; Japan Sea, Chentsov Volcano; Japan Sea, Korean Rise; Latitude of event; Longitude of event; Loss of ignition analysis; Loss on ignition; Magnesium oxide; Manganese oxide; Phosphorus pentoxide; Potassium oxide; Sample code/label; Sample comment; Silicon dioxide; Sodium oxide; Sum; Titanium dioxide; TOI-1307; TOI-1308; TOI-1618; TOI-1875; TOI-1876; TOI-2260; TOI-2270; TOI-2287; TOI-2290; TOI-2331; TOI-2397; TOI-2398; TOI-2400; TOI-2402; TOI-2415; TOI-2416A; TOI-2425; TOI-6219; Wet chemistry
Mineral and chemical compositions of highly ferruginous layered silicates (HLS) of glauconite sands occurred on the East Korean Rise outside volcanic structures and on an unnamed volcano and the Chentsov Volcano have been studied. The use of cluster and discriminant analyses has resulted to more objectively distinguished groups among HLS, and the use of factor analysis - to illustrate correlations between chemical elements in different groups. It has been found that green mineral assemblages of the East Korean Rise are heterogeneous in terms of morphology, composition and origin, and their formation is a complex multistage process including both neoformation and degradation.
title (Table 1) Chemical composition of Fe-rich layered silicates from the East Korean Rise, Japan Sea
topic Aluminium oxide; Archive of Ocean Data; ARCOD; Area/locality; Calcium oxide; Calculated; Event label; Grab; GRAB; Iron oxide, Fe2O3; Iron oxide, FeO; Japan Sea; Japan Sea, Chentsov Volcano; Japan Sea, Korean Rise; Latitude of event; Longitude of event; Loss of ignition analysis; Loss on ignition; Magnesium oxide; Manganese oxide; Phosphorus pentoxide; Potassium oxide; Sample code/label; Sample comment; Silicon dioxide; Sodium oxide; Sum; Titanium dioxide; TOI-1307; TOI-1308; TOI-1618; TOI-1875; TOI-1876; TOI-2260; TOI-2270; TOI-2287; TOI-2290; TOI-2331; TOI-2397; TOI-2398; TOI-2400; TOI-2402; TOI-2415; TOI-2416A; TOI-2425; TOI-6219; Wet chemistry
url https://doi.org/10.1594/PANGAEA.745243