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

Larson, Roger L; Fisher, Andrew T; Jarrard, Richard D; Becker, Keir; ODP Leg 144 Shipboard Scientific Pary (1993): Interval transmissivities and permeabilities in ODP Hole 129-801C (Table 2) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.715254, Supplement to: Larson, RL et al. (1993): Highly permeable and layered Jurassic oceanic crust in the western Pacific. Earth and Planetary Science Letters, 119(1-2), 71-83, https://doi.org/10.1016/0012-821X(93)90007-V

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

Published: 1993 (exact date unknown)DOI registered: 2009-06-16

RIS CitationBibTeX Citation ShareShow MapGoogle Earth

Abstract:
Bulk permeability was determined from drillstring packer measurements in ODP Hole 801C in Jurassic oceanic crust in the western Pacific. The values average 8 * 10**-14 m**2 over 93 m of open hole, or 4 * 10**-13 m**2 if the permeable interval is confined to an 18 m thick hydrothermal zone within oceanic basement. These values are about 1-10 times higher than those reported for the upper sections of Holes 395A, 504B and 735B in 3.7, 5.9 and 11 Ma old oceanic crust respectively. The discovery that 160 Ma old oceanic crust contains a zone with extremely high permeability is not predicted by any model of ocean crustal evolution. The high permeability interval appears to be associated with the burial by off-ridge volcanism of a zone of hydrothermal precipitates and altered basalts. The generality of this result may depend on the generality of off-ridge volcanism necessary to create and preserve such zones of high permeability within the ocean crustal section. Although the crustal and permeability structures detected at Hole 801C may not fit easily into currently accepted models of crustal accretion and aging, the generality of off-ridge volcanism suggests that these structures could actually be typical of large portions of the world's oceanic crust.
Project(s):
Coverage:
Latitude: 18.642300 * Longitude: 156.359800
Date/Time Start: 1990-01-06T11:48:00 * Date/Time End: 1990-01-16T07:15:00
Minimum DEPTH, sediment/rock: 519.0 m * Maximum DEPTH, sediment/rock: 547.5 m
Event(s):
129-801C * Latitude: 18.642300 * Longitude: 156.359800 * Date/Time Start: 1990-01-06T11:48:00 * Date/Time End: 1990-01-16T07:15:00 * Elevation: -5685.0 m * Penetration: 594.3 m * Recovery: 60.6 m * Location: North Pacific Ocean * Campaign: Leg129 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 12 cores; 100.6 m cored; 0 m drilled; 60.2 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Depth, top/minDepth topmLarson, Roger L
Depth, bottom/maxDepth botmLarson, Roger L
Sample commentSample commentLarson, Roger LTest
Flow rateFlow ratel/minLarson, Roger L
Permeability (earth science)k10-12 m2Larson, Roger L
TransmissivityTransmism2/sLarson, Roger L
Size:
44 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth sed [m]

Depth top [m]

Depth bot [m]

Sample comment

Flow rate [l/min]

k [10-12 m2]

Transmis [m2/s]
547.5501594Inject 19450.0980.00052
547.5501594Shut-in 10.0920.00049
547.5501594Inject 214180.0640.00034
547.5501594Shut-in 20.0820.00041
519.0510528Inject 19450.5000.00052
519.0510528Shut-in 10.4800.00049
519.0510528Inject 214180.3200.00034
519.0510528Shut-in 20.4200.00041