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

MacLeod, Christopher J; Parson, Lindsey M; Sager, William W (1994): (Table 1) Examples for core reorientations of ODP Hole 135-841B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.792845, Supplement to: MacLeod, CJ et al. (1994): Reorientation of cores using the formation microscanner and borehole televiewer: application to structural and paleomagnetic studies with the Ocean Drilling Program. In: Hawkins, J; Parson, L; Allan, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 135, 301-311, https://doi.org/10.2973/odp.proc.sr.135.160.1994

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

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Structural and paleomagnetic studies of Ocean Drilling Program (ODP) cores are severely hampered by the fact that the recovered cores can rarely be reoriented with any degree of confidence. Although several techniques for orienting cores have been used, none is without limitations. Core orientation devices used during drilling are expensive to operate and are usually unreliable. A common alternative, used when no core orientation tools are available, is to assume that the horizontal component of the magnetization direction of the core pointed north, and thus that features may be oriented relative to this direction. However, this neglects the effects of secular variations in the Earth's magnetic field and of later tectonic rotation on the sample.
In this paper we outline a technique for core reorientation that matches distinctive inclined planar features measured on the core with their images on Formation MicroScanner and Borehole Televiewer wireline logs. It allows reorientation of structural and magnetic data, and hence the possibility of detecting vertical axis tectonic rotations using Paleomagnetism. Its methodology is described and an example, from ODP Leg 135, presented to illustrate its application.
Project(s):
Coverage:
Latitude: -23.346000 * Longitude: -175.297000
Date/Time Start: 1991-02-02T15:40:00 * Date/Time End: 1991-02-10T20:30:00
Minimum DEPTH, sediment/rock: 491.37 m * Maximum DEPTH, sediment/rock: 548.23 m
Event(s):
135-841B * Latitude: -23.346000 * Longitude: -175.297000 * Date/Time Start: 1991-02-02T15:40:00 * Date/Time End: 1991-02-10T20:30:00 * Elevation: -4821.0 m * Penetration: 834.2 m * Recovery: 182.54 m * Location: South Pacific Ocean * Campaign: Leg135 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 70 cores; 664.4 m cored; 0 m drilled; 27.5 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelMacLeod, Christopher JDSDP/ODP/IODP sample designation
2DEPTH, sediment/rockDepth sedmGeocode – mbsf
3DipDipdegMacLeod, Christopher Jcore, apparent, 1
4DirectionDirectiondegMacLeod, Christopher Jcore, apparent dip direction toward the tempirary core-liner coordinates, 1
5DipDipdegMacLeod, Christopher Jcore, apparent, 2
6DirectionDirectiondegMacLeod, Christopher Jcore, apparent dip direction toward the tempirary core-liner coordinates, 1
7StrikeStrikedegMacLeod, Christopher Jcore, apparent
8DipDipdegMacLeod, Christopher Jcore, auxiliary (recombined)
9DirectionDirectiondegMacLeod, Christopher Jcore, dip direction of sedimentary bedding (relative to the core-liner)
10DeclinationDecldegMacLeod, Christopher Jcore, sample magnetization vector
11InclinationIncldegMacLeod, Christopher Jcore, sample magnetization vector
12DirectionDirectiondegMacLeod, Christopher JFormation microscanner (FMS)dip direction
13DeclinationDecldegMacLeod, Christopher Jgeographical, sample magnetization vector
14InclinationIncldegMacLeod, Christopher Jgeographical, sample magnetization vector
Size:
187 data points

Download Data

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

View dataset as HTML