Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Chen, Min-Pen; Juang, Jeng-Shyan; Ladd, John W (1993): Physical properties, compressional-wave velocity and consolidation characteristics of ODP Holes 133-815B and 133-817B [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.786892, Supplement to: Chen, M-P et al. (1993): Physical properties, compressional-wave velocity, and consolidation characteristics of slope sediments, Townsville Trough, Northeast Australia. In: McKenzie, JA; Davies, PJ; Palmer-Julson, A; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 133, 625-632, https://doi.org/10.2973/odp.proc.sr.133.266.1993

Always quote citation above when using data! You can download the citation in several formats below.

Published: 1993 (exact date unknown) • DOI registered: 2012-08-30

RIS CitationBibTeX Citation ShareShow MapGoogle Earth

Abstract:
Sites 815 and 817 were drilled near the Townsville Trough during Leg 133 of the Ocean Drilling Program. The physical properties, compressional-wave velocity, and consolidation characteristics indicate that the periplatform carbonate sediments maintain more water content and lower compressional velocity near the Queensland Plateau than the clayey hemipelagic sediments, which have a clay content of up to 60%. Bulk density, void ratio or porosity, water content, and compressional-wave velocity are shown to have a linear relationship with burial depth. Between 3.5 and 5 Ma (about 100-500 mbsf), these physical properties maintained a constant rate vs. the depth in core because of the fast sedimentation-rate effect at Site 815. However, compressionalwave velocity still increases downward in this section. The clay content in this section causes an increase of bulk modulus and compaction effect. At Site 817, scarce terrigenous mud content and abundant carbonate content (88%-97%) cause a straight line relationship between physical properties and burial depth. During the consolidation test, we show that dominant micritic particles may cause faster acoustic velocity than sediments composed mainly of coccoliths. The bulk modulus ratio increasing rate in the clay-rich carbonate sediments is almost 4.5 times higher than in the clay-free periplatform carbonate sediments.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -18.654500 * Median Longitude: 149.875553 * South-bound Latitude: -19.151000 * West-bound Longitude: 149.758200 * North-bound Latitude: -18.158000 * East-bound Longitude: 149.993000
Date/Time Start: 1990-08-27T00:00:00 * Date/Time End: 1990-09-08T00:00:00
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3 datasets

Download Data

Download ZIP file containing all datasets as tab-delimited text — use the following character encoding:

Datasets listed in this publication series

  1. Chen, M-P; Juang, J-S; Ladd, JW (1993): (Table 1) Lithologic characteristics of samples from ODP Sites 113-815 and 133-817. https://doi.org/10.1594/PANGAEA.786889
  2. Chen, M-P; Juang, J-S; Ladd, JW (1993): (Table 3) Consolidation test results of samples from ODP Holes 113-815B and 133-817B. https://doi.org/10.1594/PANGAEA.786891
  3. Chen, M-P; Juang, J-S; Ladd, JW (1993): (Table 2) Grain size analysis of samples from ODP Holes 113-815B and 133-817B. https://doi.org/10.1594/PANGAEA.786890