Clay mineral assemblage, major element composition and carbonate content of core GIK18383-3 in the southern South China Sea during SONNE cruise SO140A

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Auteur principal: Liu, Zhifei
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2019
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author Liu, Zhifei
author_facet Liu, Zhifei
collection Datos científicos de ciencias marinas y ambientales
contents This data set includes clay mineral assemblage, major element composition and carbonate content of Core SO18383-3 retrieved in the southern South China Sea during the cruise SO140 on R/V SONNE. The Core SO18383-3 is located at 7º38.54'N, 109º29.15'E, and is 710.6 m water depth and 9.44 m long. The clay mineral assemblage (237 samples, 4 cm resolution) was analyzed by X-ray diffraction (XRD) using a PANalytical X'Pert PRO diffractometer on oriented mounts of non-calcareous, clay-sized particles. The major element composition (166 samples, 4-8 cm resolutions) was analyzed by X-ray fluorescence (XRF) using a PANalytical Axios MAX Spectrometer on bulk sediments. The carbonate content was analyzed by the gasometric method on bulk sediments.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_905089
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Clay mineral assemblage, major element composition and carbonate content of core GIK18383-3 in the southern South China Sea during SONNE cruise SO140A
Liu, Zhifei
carbonate contents; Clay minerals; Core SO18383-3; GIK18383-3; Gravity corer (Kiel type); major elements; SL; SO140A; Sonne; South China Sea; SÜDMEER III
This data set includes clay mineral assemblage, major element composition and carbonate content of Core SO18383-3 retrieved in the southern South China Sea during the cruise SO140 on R/V SONNE. The Core SO18383-3 is located at 7º38.54'N, 109º29.15'E, and is 710.6 m water depth and 9.44 m long. The clay mineral assemblage (237 samples, 4 cm resolution) was analyzed by X-ray diffraction (XRD) using a PANalytical X'Pert PRO diffractometer on oriented mounts of non-calcareous, clay-sized particles. The major element composition (166 samples, 4-8 cm resolutions) was analyzed by X-ray fluorescence (XRF) using a PANalytical Axios MAX Spectrometer on bulk sediments. The carbonate content was analyzed by the gasometric method on bulk sediments.
title Clay mineral assemblage, major element composition and carbonate content of core GIK18383-3 in the southern South China Sea during SONNE cruise SO140A
topic carbonate contents; Clay minerals; Core SO18383-3; GIK18383-3; Gravity corer (Kiel type); major elements; SL; SO140A; Sonne; South China Sea; SÜDMEER III
url https://doi.org/10.1594/PANGAEA.905089