(Table T1) Density, porosity, void ratio and silica crystallinity index of ODP Site 185-1149 sediments

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Main Authors: Tanaka, Chihiro, Ogawa, Yujiro
Format: Dataset Open Access
Language:en
Published: PANGAEA 2006
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_version_ 1867170927901409280
author Tanaka, Chihiro
Ogawa, Yujiro
author_facet Tanaka, Chihiro
Ogawa, Yujiro
collection Datos científicos de ciencias marinas y ambientales
contents Siliceous pelagic sediments have been known to be crystallographically altered during burial diagenesis (e.g., Hesse, 1990; Behl and Smith, 1992, doi:10.2973/odp.proc.sr.129.112.1992). In order to know the systematic downhole change of silicification, sediments from Pacific Ocean crust obtained during Ocean Drilling Program Leg 185 Site 1149 (Plank, Ludden, Escutia, et al., 2000, doi:10.2973/odp.proc.ir.185.2000) were analyzed. For collected samples of Early Cretaceous age below the pelagic sediments, which are not as highly silicified, silica mineral crystallization in the siliceous sedimentary rocks is determined by X-ray diffraction (XRD), and the related textural change is shown by using scanning electron microscope (SEM).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_784110
institution PANGAEA
language en
publishDate 2006
publisher PANGAEA
record_format pangaea
spellingShingle (Table T1) Density, porosity, void ratio and silica crystallinity index of ODP Site 185-1149 sediments
Tanaka, Chihiro
Ogawa, Yujiro
185-1149A; 185-1149B; 185-1149C; 185-1149D; Density; DEPTH, sediment/rock; DRILL; Drilling/drill rig; d-spacing; Event label; Gamma-ray attenuation (GRA) densitometer; Index; Joides Resolution; Leg185; North Pacific Ocean; Ocean Drilling Program; ODP; Porosity; Sample code/label
Siliceous pelagic sediments have been known to be crystallographically altered during burial diagenesis (e.g., Hesse, 1990; Behl and Smith, 1992, doi:10.2973/odp.proc.sr.129.112.1992). In order to know the systematic downhole change of silicification, sediments from Pacific Ocean crust obtained during Ocean Drilling Program Leg 185 Site 1149 (Plank, Ludden, Escutia, et al., 2000, doi:10.2973/odp.proc.ir.185.2000) were analyzed. For collected samples of Early Cretaceous age below the pelagic sediments, which are not as highly silicified, silica mineral crystallization in the siliceous sedimentary rocks is determined by X-ray diffraction (XRD), and the related textural change is shown by using scanning electron microscope (SEM).
title (Table T1) Density, porosity, void ratio and silica crystallinity index of ODP Site 185-1149 sediments
topic 185-1149A; 185-1149B; 185-1149C; 185-1149D; Density; DEPTH, sediment/rock; DRILL; Drilling/drill rig; d-spacing; Event label; Gamma-ray attenuation (GRA) densitometer; Index; Joides Resolution; Leg185; North Pacific Ocean; Ocean Drilling Program; ODP; Porosity; Sample code/label
url https://doi.org/10.1594/PANGAEA.784110