Miller, D Jay; Iturrino, Gerardo J; McGuire, Jennifer C (2003): (Table T1) Orientation estimates for oxide-bearing lithologies of ODP Hole 179-1105A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.787243, Supplement to: Miller, DJ et al. (2003): Core-log correlations in oceanic basement from Hole 1105A on the Southwest Indian Ridge. In: Casey, JF; Miller, DJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 179, 1-29, https://doi.org/10.2973/odp.proc.sr.179.016.2003
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Published: 2003 (exact date unknown) • DOI registered: 2012-09-07
Abstract:
During a lull in hammer drill testing during Ocean Drilling Program Leg 179, Hole 1105A was cored to 158 mbsf on the Southwest Indian Ridge within ~1.3 km of Hole 735B. This coring operation resulted in not only high recovery (in excess of 80%) but in the collection of a suite of continuous downhole logging data. This combination allows the rare opportunity to demonstrate the utility of logging in hard rock environments. By using the core as a reference, we have been able to recognize specific Formation MicroScanner (FMS) image characteristics that represent different structural aspects of the core. Gabbro with disseminated oxide has a mottled appearance in the FMS images, and in foliated intervals, the attitude of the foliation can be determined from FMS orientation. We also present evidence of decreased and poorer quality core recovery from intervals that have resistivity characteristics indicative of intense fracturing and that certain lithologic units can have markedly different characteristics in the FMS record, improving estimates of interval thickness. This study shows that, at least for this expedition, the material sampled is consistently (albeit not universally) from the top of the cored interval, which varies in lithologic character on scales as small as a few centimeters. Therefore, the core recovered does not necessarily proportionally represent the cored interval. Reorientation of structural data measured on cores and on FMS images to paleomagnetic data indicates the direction of principle stress during the crystallization and deformation history of the Atlantis Bank was parallel to the Southwest Indian Ridge axis.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -32.718910 * Longitude: 57.277530
Date/Time Start: 1998-05-02T06:50:00 * Date/Time End: 1998-05-10T15:50:00
Minimum DEPTH, sediment/rock: 31.10 m * Maximum DEPTH, sediment/rock: 152.70 m
Event(s):
179-1105A * Latitude: -32.718910 * Longitude: 57.277530 * Date/Time Start: 1998-05-02T06:50:00 * Date/Time End: 1998-05-10T15:50:00 * Elevation: 0.0 m * Penetration: 158 m * Recovery: 118.43 m * Location: Indian Ocean * Campaign: Leg179 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 30 cores; 143 m cored; 15 m drilled; 82.8 % recovery
Comment:
DEPTH, sediment is curated depth (mbsf).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Miller, D Jay | DSDP/ODP/IODP sample designation | only top of interval given | |
| 2 | Piece | Piece | Miller, D Jay | |||
| 3 | Sample comment | Sample comment | Miller, D Jay | oriented Y = yes, N = no | ||
| 4 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 5 | Depth, logging | Depth log | m | Miller, D Jay | ||
| 6 | Feature | Feature | Miller, D Jay | type | ||
| 7 | Bed dip | Dip | deg | Miller, D Jay | ||
| 8 | Azimuth | Azim | deg | Miller, D Jay |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
497 data points
Data
| 1 Sample label | 2 Piece | 3 Sample comment | 4 Depth sed [m] | 5 Depth log [m] | 6 Feature | 7 Dip [deg] | 8 Azim [deg] |
|---|---|---|---|---|---|---|---|
| 179-1105A-3R-2,120 | 12 | Y | 31.10 | 31.6 | Steep-dipping oxide veins | 60 | 255 |
| 179-1105A-4R-4,25 | 4 | Y | 37.70 | 38.3 | Top of dipping oxide layer | 45 | 230 |
| 179-1105A-5R-1,120 | 8 | Y | 39.50 | 39.9 | Oxide-gabbro/gneissic oxide gabbro | 45 | 120 |
| 179-1105A-5R-1,36 | 2 | Y | 38.70 | 39.1 | Base crystal-plastic foliation and oxide out | 25 | 161 |
| 179-1105A-7R-1,40 | 1 | Y | 48.20 | 48.7 | Top of oxide gabbro | 45 | 200 |
| 179-1105A-7R-1,70 | 5 | Y | 48.50 | 49.0 | Base of oxide gabbro | 45 | 205 |
| 179-1105A-7R-1,135 | 10 | Y | 49.15 | 49.6 | Top of gneissic oxide gabbro | 25 | 180 |
| 179-1105A-7R-2,25 | 2 | Y | 49.40 | 49.8 | Base of gneissic oxide gabbro | 55 | 200 |
| 179-1105A-7R-2,80 | 5 | Y | 49.90 | 50.1 | Increase in oxide abundance | 45 | 205 |
| 179-1105A-7R-3,1 | 3 | Y | 51.40 | 51.9 | Base of gneissic oxide gabbro | 70 | 170 |
| 179-1105A-8R-2,47 | 4 | Y | 53.90 | 54.5 | Top of oxide gabbro | 30 | 265 |
| 179-1105A-8R-2,133 | 8 | Y | 54.10 | 54.7 | Base of oxide gabbro | 30 | 285 |
| 179-1105A-8R-3,20 | 1 | Y | 55.00 | 55.6 | Base of disseminated oxide gabbro | 15 | 330 |
| 179-1105A-8R-3,125 | 10 | Y | 56.10 | 56.5 | Top of oxide gabbro | 20 | 310 |
| 179-1105A-9R-1,34 | 2 | Y | 58.20 | 58.7 | Top of oxide gabbro | 30 | 210 |
| 179-1105A-9R-3,76 | 6 | Y | 61.20 | 61.7 | Base of oxide gabbro | 30 | 230 |
| 179-1105A-10R-1,20 | 2 | Y | 62.20 | 62.9 | Top of oxide gabbro | 30 | 200 |
| 179-1105A-10R-1,40 | 3 | Y | 62.40 | 63.2 | Base of oxide gabbro | 25 | 240 |
| 179-1105A-10R-1,70 | 3 | Y | 62.70 | 63.3 | Top of oxide gabbro | 35 | 250 |
| 179-1105A-10R-1,80 | 3 | Y | 62.80 | 63.4 | Base of oxide gabbro | 35 | 270 |
| 179-1105A-10R-2,30 | 4 | Y | 63.80 | 64.4 | Top oxide gabbro | 40 | 320 |
| 179-1105A-10R-2,90 | 8 | Y | 65.00 | 65.7 | Base oxide gabbro | 45 | 350 |
| 179-1105A-11R-1,45 | 5 | Y | 67.40 | 67.8 | Top of oxide gabbro | 50 | 345 |
| 179-1105A-11R-3,35 | 2 | Y | 69.90 | 70.2 | Decrease in oxide abundance | 55 | 355 |
| 179-1105A-12R-1,88 | 12 | N | 72.20 | 72.6 | Base of oxide gabbro | 40 | 110 |
| 179-1105A-13R-1,26 | 2 | Y | 76.50 | 76.8 | Top of oxide layer | 25 | 305 |
| 179-1105A-13R-1,35 | 2 | Y | 76.60 | 76.9 | Base of oxide layer | 25 | 295 |
| 179-1105A-13R-1,66 | 3C | Y | 77.00 | 77.2 | Top of oxide layer | 40 | 225 |
| 179-1105A-13R-1,85 | 3D | Y | 77.20 | 77.4 | Base of oxide layer | 35 | 230 |
| 179-1105A-13R-2,50 | 2 | Y | 78.10 | 78.5 | Top of oxide layer | 25 | 290 |
| 179-1105A-13R-2,60 | 2 | Y | 78.20 | 78.6 | Base of oxide layer | 30 | 280 |
| 179-1105A-13R-2,125 | 4 | Y | 78.80 | 79.2 | Top of oxide layer | 25 | 290 |
| 179-1105A-13R-3,25 | 3 | Y | 79.20 | 79.6 | Base of oxide layer | 35 | 320 |
| 179-1105A-16R-1,60 | 13 | Y | 91.20 | 91.9 | Bottom of strong foliation | 65 | 220 |
| 179-1105A-16R-1,30 | 4 | Y | 90.90 | 91.6 | Top of strong foliation | 10 | 270 |
| 179-1105A-16R-2,10 | 2 | Y | 92.00 | 92.5 | Steep-dipping oxide layer | 10 | 270 |
| 179-1105A-17R-1,47 | 3 | Y | 96.10 | 96.4 | Top of dipping oxide gabbro | 25 | 200 |
| 179-1105A-17R-1,70 | 6 | Y | 96.30 | 96.5 | Base of dipping oxide gabbro | 25 | 210 |
| 179-1105A-17R-3,147 | 18 | Y | 99.70 | 100.0 | Top of foliated oxide layer | 25 | 270 |
| 179-1105A-17R-4,50 | 4 | Y | 100.30 | 100.6 | Base of foliated oxide gabbro | 25 | 270 |
| 179-1105A-18R-1,117 | 11 | Y | 101.30 | 102.3 | Base of foliated oxide gabbro | 45 | 300 |
| 179-1105A-18R-1,35 | 4 | Y | 100.50 | 101.5 | Top of oxide gabbro | 45 | 300 |
| 179-1105A-19R-1,50 | 5 | Y | 105.70 | 106.1 | Top of oxide gabbro | 25 | 10 |
| 179-1105A-19R-1,120 | 6 | Y | 106.30 | 106.7 | Top of oxide gabbro | 25 | 270 |
| 179-1105A-19R-1,110 | 6 | Y | 106.10 | 106.5 | Base of oxide gabbro | 25 | 290 |
| 179-1105A-19R-3,20 | 2 | Y | 108.10 | 108.4 | Base of oxide gabbro | 25 | 300 |
| 179-1105A-19R-4,1 | 1 | Y | 109.20 | 109.5 | Top of oxide gabbro | 25 | 320 |
| 179-1105A-21R-1,90 | 8A | Y | 111.70 | 111.9 | Oxide gabbro | 25 | 30 |
| 179-1105A-22R-2,66 | 4 | Y | 117.10 | 117.2 | Base of foliated oxide gabbro | 30 | 75 |
| 179-1105A-22R-3,70 | 4 | Y | 118.30 | 118.4 | Base of oxide gabbro | 30 | 355 |
| 179-1105A-23R-1,70 | 7 | Y | 120.10 | 120.1 | Top of oxide gabbro | 30 | 240 |
| 179-1105A-23R-1,90 | 8 | Y | 120.30 | 120.3 | Base of oxide gabbro | 30 | 240 |
| 179-1105A-24R-1,150 | 6 | Y | 125.30 | 125.7 | Foliated oxide gabbro | 20 | 170 |
| 179-1105A-24R-2,53 | 7 | Y | 126.20 | 126.6 | Crosscutting fracture | 30 | 260 |
| 179-1105A-24R-3,45 | 4 | Y | 127.20 | 127.4 | Base of oxide gabbro | 55 | 350 |
| 179-1105A-25R-1,7 | 1 | Y | 129.10 | 129.3 | Top of strongly foliated oxide gabbro | 25 | 55 |
| 179-1105A-25R-2,20 | 1 | Y | 130.60 | 130.8 | Base of strongly foliated oxide gabbro | 35 | 190 |
| 179-1105A-25R-2,132 | 4 | Y | 131.70 | 131.9 | Top of foliated oxide gabbro | 30 | 200 |
| 179-1105A-25R-3,57 | 6 | Y | 132.30 | 132.5 | Base of foliated oxide gabbro | 20 | 230 |
| 179-1105A-26R-1,75 | 2 | Y | 134.70 | 134.9 | Base of oxide gabbro | 35 | 320 |
| 179-1105A-26R-2,2 | 1 | Y | 135.30 | 135.4 | Top of oxide gabbro | 50 | 320 |
| 179-1105A-26R-2,20 | 1 | Y | 135.50 | 135.6 | Base of oxide gabbro | 15 | 355 |
| 179-1105A-27R-1,47 | 1 | Y | 139.10 | 139.8 | Top of oxide gabbro | 20 | 50 |
| 179-1105A-27R-1,95 | 3 | Y | 139.70 | 140.5 | Base of oxide gabbro | 20 | 50 |
| 179-1105A-28R-1,104 | 3 | Y | 144.70 | 144.7 | Top of oxide gabbro | 15 | 225 |
| 179-1105A-28R-2,4 | 1 | Y | 144.80 | 144.8 | Base of oxide gabbro | 30 | 270 |
| 179-1105A-28R-3,140 | 2 | Y | 147.00 | 147.0 | Subhorizontal fracture | 30 | 270 |
| 179-1105A-29R-1,100 | 4 | Y | 149.40 | 149.8 | Top of foliated oxide gabbro | 20 | 170 |
| 179-1105A-29R-2,94 | 3 | Y | 150.60 | 151.1 | Oxide gabbro pod | 45 | 210 |
| 179-1105A-29R-3,40 | 4 | Y | 151.30 | 151.7 | Top of strongly foliated oxide gabbro | 45 | 210 |
| 179-1105A-29R-4,40 | 2 | Y | 152.70 | 153.1 | Base of strongly foliated oxide gabbro | 45 | 280 |