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

Meissl, Sandra; Behrmann, Jan Hinrich; Franke, C (2011): (Table 1) Magnetic susceptibility from IODP Hole 308-U1322B. doi:10.1594/PANGAEA.787621,
Supplement to: Meissl, Sandra; Behrmann, Jan Hinrich; Franke, Christine (2011): Magnetic fabrics in Quaternary sediments, Ursa Basin, northern Gulf of Mexico record transport processes, compaction and submarine slumping. Marine Geology, 286(1-4), 51-64, doi:10.1016/j.margeo.2011.05.007

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

Show MapGoogle Earth RISBibTeX

Abstract:
The continental slope of the northern Gulf of Mexico seaward of the Mississippi Delta is characterized by very rapid Quaternary sedimentation. Thick sequences of underconsolidated muds and mudstones are present, which are severely overpressured. In the Ursa Basin, Site U1322 of the Integrated Ocean Drilling Program (IODP) provided an excellent coring record of interleaved fine-grained turbidites and hemipelagic sediments, in part severely affected by submarine slumping and sliding after deposition. Cores were continuously sampled and analyzed for anisotropy of magnetic susceptibility (AMS), to elucidate the effects of different transport mechanisms and degree of settling and consolidation on magnetic fabric properties. Generally AMS ellipticity increases with depth irrespective of transport mode, due to loss of porosity. Samples from slumped mass transport deposits (MTD), however, have higher AMS if compared to immediately overlying nonslumped material. MTD samples dominantly show triaxial magnetic fabrics whereas those found in nonslumped sediments are much more oblate. Long axes of the fabric ellipsoid reflect the direction of eastward to southward suspension transport in samples not overprinted by sliding or slumping. Short ellipsoid axes in non-slumped material are vertical, and thus parallel to the axis of maximum uniaxial shortening. In the MTD samples, many short ellipsoid axes are inclined, reflecting an overprint of the uniaxial shortening by bedparallel shearing induced by the slumping. Shear and MTD transport direction deduced from the fabrics is top to- SE, downslope along the morphological axis of Ursa Basin. Generally we show that magnetic fabrics of muds and mudstones are sensitive recorders of sedimentary and tectonic processes, and can be used to reconstruct essential
Coverage:
Latitude: 28.001657 * Longitude: -89.000417
Minimum DEPTH, sediment/rock: 1.76 m * Maximum DEPTH, sediment/rock: 233.86 m
Event(s):
308-U1322B * Latitude: 28.001657 * Longitude: -89.000417 * Elevation: -1319.5 m * Recovery: 236.79 m * Campaign: Exp308 (Gulf of Mexico Hydrogeology) * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 29 cores; 234.5 m cored; 101 % recovered; 0 m drilled; 234.5 m penetrated
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethodComment
1Sample code/labelLabelMeissl, SandraODP sample designation
2DEPTH, sediment/rockDepthmGeocode – mbsf
3UnitUnitMeissl, Sandra
4Sample, optional label/labor noLab noMeissl, Sandra
5Magnetic tool face angleAgl MTFdegMeissl, Sandra
6SusceptibilitySusceptsensor valuesMeissl, SandraSusceptibility unit Kappabridge KLY-2
7Principle axes K1 of normalized anisotropy tensorK maxMeissl, SandraSusceptibility unit Kappabridge KLY-2
8Principle axes K2 of normalized anisotropy tensorK intMeissl, SandraSusceptibility unit Kappabridge KLY-2
9Principle axes K3 of normalized anisotropy tensorK minMeissl, SandraSusceptibility unit Kappabridge KLY-2
10Declination of principle axis K1D(Kmax)degMeissl, Sandracorrected
11Inclination of principle axis K1I(Kmax)degMeissl, Sandracorrected
12Declination of principle axis K2D(Kint)degMeissl, Sandracorrected
13Inclination of principle axis K2I(Kint)degMeissl, Sandracorrected
14Declination of principle axis K3D(Kmin)degMeissl, Sandracorrected
15Inclination of principle axis K3I(Kmin)degMeissl, Sandracorrected
16Anisotropy-magnetic susceptibility, factor L, lineationAMS factor LMeissl, SandraSusceptibility unit Kappabridge KLY-2k(max)/k(int)
17Anisotropy-magnetic susceptibility, factor F, foliationAMS factor FMeissl, SandraSusceptibility unit Kappabridge KLY-2k(int)/k(min)
18Anisotropy-magnetic susceptibility, factor P, anisotropy degreeAMS factor PMeissl, SandraSusceptibility unit Kappabridge KLY-2k(max)/k(min)
19Shape of susceptibilityTMeissl, SandraSusceptibility unit Kappabridge KLY-22*ln k(int)/k(min)/ln k(max)/k(min-1)
Size:
3564 data points

Download Data

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

View dataset as HTML (shows only first 2000 rows)