Kennett, James P; Houtz, Robert E (2005): Smear slide analysis of Hole 29-281 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230562
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
DSDP (1989): Data from the Deep Sea Drilling Project. Sediment, hard rock and reference files. National Geophysical Data Center, National Environmental Satellite, Data and Information Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1, CD-ROM
Perch-Nielsen, Katharina; Ovenshine, A Thomas; Margolis, Stanley V; Jenkins, D Graham; Hampton, Monty A; Hajos, Marta; Gostin, Victor A; Edwards, Anthony R; Andrews, Peter B; Kennett, James P; Houtz, Robert E (1975): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXIX, 999 pp, https://doi.org/10.2973/dsdp.proc.29.1975
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -47.997300 * Longitude: 147.764200
Date/Time Start: 1973-03-31T00:00:00 * Date/Time End: 1973-03-31T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 159.10 m
Event(s):
29-281 * Latitude: -47.997300 * Longitude: 147.764200 * Date/Time: 1973-03-31T00:00:00 * Elevation: -1591.0 m * Penetration: 169 m * Recovery: 101.9 m * Location: Antarctic Ocean/Tasman Sea/CONT RISE * Campaign: Leg29 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 14 cores; 133 m cored; 36 m drilled; 76.6 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Sand | Sand | % | Smear slide analysis | ||
4 | Silt | Silt | % | Smear slide analysis | ||
5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
6 | Stratigraphy | Stratigraphy | Smear slide analysis | |||
7 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
8 | Comment | Comment | Smear slide analysis | |||
9 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Dolomite | Dol | % | Smear slide analysis | ||
11 | Nannofossils | Nannos | % | Smear slide analysis | ||
12 | Foraminifera | Foram | % | Smear slide analysis | ||
13 | Ostracoda | Ostrac | % | Smear slide analysis | ||
14 | Siliceous microfossils | Silic foss | % | Smear slide analysis | ||
15 | Radiolarians | Rad | % | Smear slide analysis | ||
16 | Diatoms | Diatoms | % | Smear slide analysis | ||
17 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
18 | Spiculae | Spiculae | % | Smear slide analysis | ||
19 | Minerals, other | Min other | % | Smear slide analysis | ||
20 | Quartz | Qz | % | Smear slide analysis | ||
21 | Feldspar | Fsp | % | Smear slide analysis | ||
22 | Mica | Mica | % | Smear slide analysis | ||
23 | Biotite | Bt | % | Smear slide analysis | ||
24 | Clay minerals | Clay min | % | Smear slide analysis | ||
25 | Glauconite | Glt | % | Smear slide analysis | ||
26 | Opaque minerals | Opaque | % | Smear slide analysis | ||
27 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
28 | Heavy minerals | HM | % | Smear slide analysis | ||
29 | Zircon | Zrn | % | Smear slide analysis | ||
30 | Tourmaline | Tur | % | Smear slide analysis | ||
31 | Hornblende | Hbl | % | Smear slide analysis | ||
32 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
33 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus | |
34 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1122 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Carb [%] | 10 Dol [%] | 11 Nannos [%] | 12 Foram [%] | 13 Ostrac [%] | 14 Silic foss [%] | 15 Rad [%] | 16 Diatoms [%] | 17 Silicoflag [%] | 18 Spiculae [%] | 19 Min other [%] | 20 Qz [%] | 21 Fsp [%] | 22 Mica [%] | 23 Bt [%] | 24 Clay min [%] | 25 Glt [%] | 26 Opaque [%] | 27 Py [%] | 28 HM [%] | 29 Zrn [%] | 30 Tur [%] | 31 Hbl [%] | 32 Volc glass [%] | 33 Terr [%] | 34 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.10 | 29-281-1-CC,0 | 0 | 0 | 0 | Upper pleistocene | NANNO RICH FORAM OOZE | Dominat lithology; relative abundance | 0 | 0 | 23 | 75 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
16.60 | 29-281-2-CC,0 | 0 | 0 | 0 | Upper pliocene | NANNO BEARING FORAM OOZE | Dominat lithology; numerical abundance | 0 | 0 | 10 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
20.10 | 29-281-3-3,10 | 0 | 0 | 0 | Upper pliocene | FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 73 | 25 | 0 | 0 | 0 | 5 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 1 | 1 | 2 | 0 |
20.30 | 29-281-3-3,30 | 0 | 0 | 0 | Upper pliocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 50 | 45 | 0 | 0 | 1 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
26.10 | 29-281-3-CC,0 | 0 | 0 | 0 | Upper pliocene | MICARB BEARING FORAM NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 35 | 60 | 0 | 0 | 0 | 30 | 0 | 30 | 0 | 1 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
26.10 | 29-281-3-CC,0 | 1 | 30 | 0 | Upper pliocene | MICARB BEARING FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
26.60 | 29-281-4-CC,0 | 0 | 0 | 0 | Lower pliocene | DETRITAL BEARING NANNO FORAM OOZE | Dominat lithology; relative abundance | 0 | 0 | 35 | 60 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 3 | 0 |
40.60 | 29-281-5-CC,0 | 0 | 0 | 0 | Upper miocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 1 | 0 | 35 | 65 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
54.60 | 29-281-6-CC,0 | 0 | 0 | 0 | Upper miocene | SILICIOUS BEARING NANNO FORAM OOZE | Dominat lithology; relative abundance | 0 | 0 | 35 | 55 | 0 | 0 | 1 | 1 | 5 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 |
64.10 | 29-281-7-CC,0 | 0 | 0 | 0 | Upper miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 59 | 40 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
64.60 | 29-281-8-CC,0 | 0 | 0 | 0 | Upper miocene | SPICULE BEARING FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 25 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
83.10 | 29-281-9-CC,0 | 0 | 0 | 0 | Middle miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 55 | 40 | 1 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
92.60 | 29-281-10-CC,0 | 0 | 0 | 0 | Middle miocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 0 | 0 | 35 | 60 | 1 | 0 | 0 | 0 | 1 | 2 | 0 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
102.10 | 29-281-11-CC,0 | 50 | 0 | 0 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 64 | 35 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
111.60 | 29-281-12-CC,0 | 0 | 0 | 0 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 35 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
114.70 | 29-281-13-21,120 | 0 | 0 | 0 | Lower miocene | GLAUCONITE BEARING NANNO FORAM OOZE | Dominat lithology; numerical abundance | 0 | 0 | 30 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
116.40 | 29-281-13-31,140 | 70 | 10 | 0 | Lower miocene | DETRITAL SAND AND GLAUCONITE BEARING FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 66 | 20 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 7 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 |
117.25 | 29-281-13-4,75 | 90 | 0 | 0 | Lower miocene | FORAM OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 40 | 41 | 2 | 1 | 0 | 0 | 0 | 0 | 7 | 1 | 0 | 1 | 0 | 100 | 0 |
117.75 | 29-281-13-41,125 | 70 | 30 | 0 | Lower oligocene | NANNO AND FORAM BEARING GLAUCONITE DETRITAL SAND | Dominat lithology; relative abundance | 2 | 0 | 4 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 42 | 5 | 2 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 24 | 0 |
119.33 | 29-281-13-51,133 | 80 | 20 | 1 | Lower oligocene | DOLOMITE AND FORAM BEARING GLAUCONITE AND NANNO RICH DETRITAL SAND | Dominat lithology; relative abundance | 1 | 4 | 15 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 10 | 1 | 0 | 0 | 15 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 60 | 0 |
119.60 | 29-281-13-CC,0 | 70 | 25 | 5 | Lower oligocene | FELDSPAR RICH GLAUCONITE QUARTZ SAND | Dominat lithology; numerical abundance | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 52 | 18 | 0 | 0 | 0 | 26 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
121.58 | 29-281-14-1,8 | 50 | 50 | 0 | Upper eocene | GLAUCONITE FORAM RAD AND SPICULE BEARING DIATOM AND DETRITAL SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 1 | 3 | 0 | 0 | 3 | 16 | 0 | 6 | 0 | 46 | 13 | 3 | 0 | 0 | 3 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 50 | 0 |
123.75 | 29-281-14-2,75 | 30 | 30 | 45 | Upper eocene | RAD SPICULE AND GALUCONITE BEARING DETRITAL SANDY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 20 | 0 | 5 | 0 | 45 | 6 | 6 | 0 | 6 | 10 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 60 | 0 |
128.25 | 29-281-14-5,75 | 30 | 30 | 40 | Upper eocene | GLAUCONITE RAD AND FORAM BEARING SPICULE RICH DIATOM DETRITAL SAND SILT | Dominat lithology; relative abundance | 0 | 0 | 2 | 1 | 0 | 0 | 5 | 30 | 0 | 14 | 0 | 17 | 9 | 2 | 0 | 17 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 45 | 0 |
130.60 | 29-281-14-CC,0 | 20 | 50 | 30 | Upper eocene | GLAUCONITE RAD SPICULE BEARING DETRITAL SILT RICH FORAM DIATOM OOZE | Dominat lithology; relative abundance | 0 | 0 | 1 | 30 | 0 | 0 | 5 | 30 | 0 | 10 | 0 | 13 | 5 | 1 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 20 | 0 |
133.23 | 29-281-15-2,73 | 15 | 45 | 40 | Upper eocene | FORAM-NANNO-SPICULE BEARING DETRITAL CLAYEY SILT TO DIATOM OOZE | Dominat lithology; relative abundance | 2 | 0 | 5 | 5 | 0 | 0 | 1 | 30 | 0 | 11 | 0 | 23 | 0 | 3 | 0 | 22 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 |
133.44 | 29-281-15-2,94 | 80 | 20 | 0 | Upper eocene | FORAM NANNO SPONGE AND DETRITAL SAND RICH DIATOM OOZE | Dominat lithology; relative abundance | 0 | 0 | 15 | 10 | 0 | 0 | 1 | 54 | 1 | 10 | 0 | 8 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
135.60 | 29-281-15-CC,0 | 60 | 30 | 10 | Upper eocene | GLAUCONITE BEARING FORAM NANNO SPONGE SPICULE AND DETRITAL SILTY SAND RI | Dominat lithology; relative abundance | 0 | 0 | 20 | 10 | 0 | 0 | 1 | 35 | 2 | 15 | 0 | 1 | 1 | 2 | 1 | 1 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 15 | 0 |
149.32 | 29-281-16-61,107 | 90 | 8 | 2 | Upper eocene | DETRITAL SAND RICH NANNO DIATOM OOZE | Minor lithology; relative abundance | 0 | 2 | 35 | 2 | 0 | 0 | 0 | 40 | 1 | 5 | 0 | 1 | 0 | 1 | 0 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 15 | 0 |
149.70 | 29-281-16-61,145 | 15 | 35 | 50 | Upper eocene | NANNO BEARING SPICULE AND FORAM-RICH DETRITAL SILTY CLAY-DIATOM OOZE | Dominat lithology; relative abundance | 0 | 0 | 5 | 15 | 0 | 0 | 0 | 25 | 0 | 10 | 55 | 18 | 1 | 5 | 0 | 22 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 |
149.85 | 29-281-16-CC,0 | 67 | 33 | 0 | Upper eocene | RAD AND NANNO BEARING FORAM DETRITAL SAND AND SPICULE RICH DIATOM OOZE | Dominat lithology; relative abundance | 1 | 0 | 10 | 15 | 0 | 0 | 10 | 30 | 2 | 20 | 0 | 14 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
150.10 | 29-281-17-1,10 | 80 | 20 | 0 | Upper eocene | GLAUCONITE BEARING DETRITAL SAND-FORAM RICH NANNO CHALK | Dominat lithology; relative abundance | 0 | 1 | 52 | 15 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 25 | 1 | 1 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 20 | 2 |
157.79 | 29-281-17-6,29 | 30 | 30 | 40 | Upper eocene | SANDY SILTY CLAY | Dominat lithology; relative abundance | 0 | 1 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 65 | 25 | 0 | 0 | 0 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
159.10 | 29-281-17-CC,0 | 0 | 0 | 0 | Upper eocene | MUSCOVITE QUARTZ SCHIST | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |