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Tartarotti, Paola; Crispini, Laura; Einaudi, Florence; Campari, E (2006): (Table T1) Natural structures measured at ODP Hole 206-1256D with respect to the ODP reference frame and reorientation results [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.775780, Supplement to: Tartarotti, P et al. (2006): Data report: Reoriented structures in the East Pacific Rise basaltic crust from ODP Hole 1256D, Leg 206: integration of core measurements and electrical-acoustic images. In: Teagle, DAH; Wilson, DS; Acton, GD; Vanko, DA (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 206, 1-26, https://doi.org/10.2973/odp.proc.sr.206.004.2006

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Published: 2006 (exact date unknown)DOI registered: 2012-03-08

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Abstract:
Brittle structures (open fractures and veins) from basaltic oceanic crust drilled at Ocean Drilling Program (ODP) Site 1256 (Guatemala Basin, Pacific Ocean) during Leg 206 were reoriented to the geographic coordinates by (1) correlating structures observed on the core with unoriented images of the exterior of the core and (2) correlating core structures and unoriented images with oriented borehole images. The images of the exterior of the core were obtained by scanning whole-core pieces with the Deutsche Montan Technologie Digital Color Core-Scan system. In the unrolled core images, nonhorizontal planar structures (e.g., veins, faults, or fractures) produce sinusoidal-shaped curves. These can be matched to similar-shaped features imaged along the borehole wall. The borehole images were obtained by the Formation MicroScanner (FMS)-sonic (Dipole Sonic Imager) tool string and the Ultrasonic Borehole Imager (UBI). The FMS provides high-resolution electrical resistivity-based images of borehole walls. FMS images are oriented to magnetic north using the General Purpose Inclinometer Tool. This allows the dip and azimuth of geological features intersecting the hole to be measured from the processed FMS image. The UBI features a high-resolution transducer that provides acoustic images of the borehole wall. The UBI was used in hard rocks for the first time in the history of the ODP during Leg 206.
Related to:
Wilson, Douglas S; Teagle, Damon A H; Acton, Gary D; et al. (2003): Proceedings of the Ocean Drilling Program, 206 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 206, online, https://doi.org/10.2973/odp.proc.ir.206.2003
Project(s):
Coverage:
Latitude: 0.736050 * Longitude: -91.934350
Date/Time Start: 2002-11-23T03:45:00 * Date/Time End: 2002-11-23T03:45:00
Minimum DEPTH, sediment/rock: 30.00 m * Maximum DEPTH, sediment/rock: 352.85 m
Event(s):
206-1256D * Latitude: 0.736050 * Longitude: -91.934350 * Date/Time: 2002-11-23T03:45:00 * Elevation: -3634.7 m * Penetration: 752 m * Recovery: 227.3 m * Location: North Pacific Ocean * Campaign: Leg206 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 73 cores; 475.9 m cored; 276.1 m drilled; 47.8 % recovery
Comment:
Depth in sediment given as corrected depth of section top [mbsf].
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelTartarotti, Paola
2PiecePieceTartarotti, Paola
3StructureStructureTartarotti, Paola
4DEPTH, sediment/rockDepth sedmGeocode
5Depth, top/minDepth topmTartarotti, Paolaof the measured structure
6Depth, bottom/maxDepth botmTartarotti, Paolaof the measured structure
7Standard errorStd e±Tartarotti, Paolaof the core depth when compared with curated depth
8StrikeStrikedegTartarotti, Paolareal and calculated
9Bed dip directionBed dip direcdegTartarotti, Paolareal and calculated
10Bed dipDipdegTartarotti, Paolareal and calculated
11Depth, referenceDepth refmTartarotti, PaolaWilson et al. (2003)
12Bed dip directionBed dip direcdegTartarotti, PaolaFormation microscanner (FMS)and Ultrasonic Borehole Imager; recognized during ODP Leg 206 (Wilson et al., 2003)
13Bed dipDipdegTartarotti, PaolaFormation microscanner (FMS)and Ultrasonic Borehole Imager; recognized during ODP Leg 206 (Wilson et al., 2003)
14Angle of rotationAngle rotateddegTartarotti, Paolacalculated, negative if rotation is counterclockwise
15Angle of rotationAngle rotateddegTartarotti, Paolautilized, negative if rotation is counterclockwise
16Depth, reconstructedReconstr depthmTartarotti, Paolaaverage depth of reoriented structures
Size:
5838 data points

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