Kennett, James P; Houtz, Robert E (2005): Smear slide analysis of Hole 29-283 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230565
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:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -43.910000 * Longitude: 154.282700
Date/Time Start: 1973-04-10T00:00:00 * Date/Time End: 1973-04-10T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 578.10 m
Event(s):
29-283 * Latitude: -43.910000 * Longitude: 154.282700 * Date/Time: 1973-04-10T00:00:00 * Elevation: -4729.0 m * Penetration: 592 m * Recovery: 61.1 m * Location: Antarctic Ocean/Tasman Sea * Campaign: Leg29 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 136.5 m cored; 19.5 m drilled; 44.8 % 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 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Collophane | Collophane | % | Smear slide analysis | ||
18 | Quartz | Qz | % | Smear slide analysis | ||
19 | Feldspar | Fsp | % | Smear slide analysis | ||
20 | Zeolite | Zeo | % | Smear slide analysis | ||
21 | Mica | Mica | % | Smear slide analysis | ||
22 | Clay minerals | Clay min | % | Smear slide analysis | ||
23 | Glauconite | Glt | % | Smear slide analysis | ||
24 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
25 | Iron | Fe | % | Smear slide analysis | ||
26 | Heavy minerals | HM | % | Smear slide analysis | ||
27 | Tourmaline | Tur | % | Smear slide analysis | ||
28 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
29 | Palagonite | Palagonite | % | Smear slide analysis | ||
30 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus | |
31 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1020 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 Rad [%] | 14 Diatoms [%] | 15 Silicoflag [%] | 16 Spiculae [%] | 17 Collophane [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Clay min [%] | 23 Glt [%] | 24 Py [%] | 25 Fe [%] | 26 HM [%] | 27 Tur [%] | 28 Volc glass [%] | 29 Palagonite [%] | 30 Terr [%] | 31 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.10 | 29-283-1-CC,0 | 0 | 0 | 0 | Cenozoic | DETRITAL CLAY RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 49 | 15 | 0 | 2 | 0 | 1 | 0 | 8 | 0 | 8 | 0 | 10 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 1 |
10.45 | 29-283-2-1,45 | 20 | 15 | 65 | Neogene | DETRITAL SILTY SAND RICH CLAY ZEOLITE OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 45 | 1 | 37 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 3 |
12.70 | 29-283-2-21,120 | 10 | 20 | 70 | Neogene | DETRITAL SILTY SAND RICH CLAY ZEOLITE OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 1 | 45 | 2 | 40 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 10 | 4 |
12.95 | 29-283-2-21,145 | 2 | 25 | 73 | Neogene | DETRITAL QUARTZ SILT RICH AUTHIGENIC CLAY | Dominat lithology; relative abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 5 | 55 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 35 | 0 |
16.10 | 29-283-2-CC,0 | 5 | 5 | 90 | Neogene | DETRITAL SILT AND SAND BEARING ZEOLITE CLAY OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 7 | 1 | 40 | 1 | 44 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 3 |
30.60 | 29-283-3-CC,0 | 20 | 50 | 30 | Upper eocene | DETRITAL QUARTZ RICH DIATOM OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 63 | 1 | 10 | 0 | 20 | 2 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 |
57.60 | 29-283-4-CC,0 | 15 | 45 | 40 | Upper eocene | DETRITAL QUARTZ SILT RICH DIATOM OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 10 | 60 | 0 | 10 | 0 | 15 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
86.08 | 29-283-5-1,8 | 20 | 40 | 40 | Upper eocene | DETRITAL SILT AND SPONGE SPICULE BEARING AUTHIGENIC CLAY RICH DIATOM OOZ | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 5 | 49 | 4 | 8 | 0 | 5 | 0 | 10 | 1 | 15 | 1 | 0 | 0 | 1 | 0 | 2 | 0 | 7 | 0 |
89.10 | 29-283-5-CC,0 | 5 | 35 | 60 | Upper eocene | SILICEOUS (RED DIATOM) OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 15 | 60 | 5 | 10 | 0 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
125.42 | 29-283-6-11,142 | 0 | 1 | 0 | Upper eocene | DIATOM OOZE | Dominat lithology; relative abundance | 0 | 0 | 4 | 0 | 5 | 75 | 5 | 5 | 0 | 1 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 1 |
126.05 | 29-283-6-2,55 | 5 | 25 | 70 | Upper eocene | SPICULE AND RAD BEARING DIATOM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 45 | 0 | 10 | 25 | 5 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
127.10 | 29-283-6-CC,0 | 0 | 0 | 0 | Upper eocene | RAD AND SPONGE SPICULE BEARING SILICOFLAGILLATE RICH DIATOM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 30 | 0 | 10 | 25 | 15 | 10 | 0 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
153.76 | 29-283-7-11,126 | 10 | 30 | 60 | Upper eocene | NANNO RICH DIATOM OOZE | Dominat lithology; relative abundance | 0 | 0 | 15 | 0 | 2 | 65 | 0 | 8 | 0 | 4 | 0 | 0 | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
161.60 | 29-283-7-CC,0 | 0 | 0 | 0 | Upper eocene | DIATOM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 5 | 25 | 5 | 5 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
191.25 | 29-283-8-1,75 | 10 | 40 | 50 | Eocene | SPONGE SPICULE AND DIATOM RICH DETRITAL QUARTZ SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 5 | 25 | 3 | 15 | 0 | 20 | 2 | 0 | 2 | 30 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 52 | 2 |
194.50 | 29-283-8-31,100 | 10 | 30 | 60 | Eocene | SPONGE SPICULE AND DIATOM RICH DETRITAL QUARTZ SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 5 | 20 | 5 | 15 | 0 | 20 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
195.10 | 29-283-8-CC,0 | 15 | 35 | 50 | Eocene | QUARTZ SILT AND SPONGE SPICULE RICH DETRITAL CLAY | relative abundance | 0 | 2 | 0 | 0 | 2 | 10 | 0 | 25 | 0 | 20 | 0 | 0 | 5 | 36 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
221.10 | 29-283-9-2,60 | 15 | 40 | 45 | Eocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 5 | 5 | 50 | 0 | 0 | 0 | 2 | 0 | 5 | 2 | 90 | 5 |
226.60 | 29-283-9-CC,0 | 5 | 20 | 75 | Eocene | QUARTZ SILT RICH CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 22 | 0 | 0 | 1 | 70 | 5 | 0 | 0 | 1 | 0 | 1 | 0 | 20 | 2 |
238.10 | 29-283-10-CC,0 | 0 | 20 | 80 | Eocene | DETRITAL SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 15 | 0 | 0 | 0 | 89 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 97 | 0 |
280.60 | 29-283-11-CC,0 | 5 | 15 | 80 | Middle eocene | SILTY CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 1 | 2 | 2 | 2 | 0 | 5 | 0 | 5 | 2 | 80 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 87 | 2 |
324.70 | 29-283-12-11,120 | 10 | 30 | 60 | Lower tertiary | QUARTZ RICH SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 2 | 0 | 30 | 0 | 2 | 2 | 55 | 0 | 0 | 2 | 0 | 0 | 1 | 5 | 0 | 5 |
326.60 | 29-283-12-CC,0 | 10 | 40 | 50 | Paleocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 2 | 0 | 2 | 69 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 96 | 3 |
374.94 | 29-283-13-3,94 | 1 | 21 | 78 | Paleocene | MICRONODULE BEARING SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 18 | 2 | 2 | 1 | 80 | 1 | 0 | 0 | 2 | 0 | 2 | 0 | 90 | 5 |
378.60 | 29-283-13-CC,0 | 5 | 35 | 60 | Paleocene | QUARTZ RICH SILTY CLAY | Dominat lithology; numerical abundance | 0 | 2 | 0 | 0 | 1 | 3 | 0 | 1 | 0 | 30 | 2 | 1 | 5 | 44 | 2 | 0 | 0 | 1 | 0 | 2 | 1 | 0 | 5 |
433.48 | 29-283-14-4,98 | 2 | 10 | 80 | Paleocene | DETRITAL CLAY BEARING DOLOMITE | relative abundance | 0 | 78 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 20 | 1 |
433.80 | 29-283-14-41,130 | 20 | 50 | 50 | Paleocene | GLAUCONITE BEARING SANDY AND SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 2 | 0 | 1 | 59 | 8 | 1 | 0 | 2 | 0 | 1 | 1 | 84 | 5 |
434.10 | 29-283-14-CC,0 | 0 | 0 | 0 | Paleocene | MICRONODULE BEARING SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 80 | 1 | 0 | 0 | 2 | 2 | 2 | 2 | 92 | 5 |
489.77 | 29-283-15-4,27 | 15 | 35 | 50 | Paleocene | GLAUCONITE BEARING DETRITAL QUARTZ SILTY CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 5 | 50 | 4 | 2 | 2 | 3 | 0 | 5 | 3 | 84 | 5 |
491.10 | 29-283-15-CC,0 | 2 | 15 | 83 | Paleocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 15 | 0 | 0 | 1 | 77 | 1 | 0 | 0 | 1 | 0 | 0 | 2 | 94 | 1 |
546.60 | 29-283-16-CC,0 | 0 | 5 | 95 | Paleocene | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 1 | 88 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 94 | 5 |
576.30 | 29-283-17-41,130 | 5 | 40 | 55 | Paleocene | QUARTZ RICH SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 2 | 69 | 2 | 1 | 0 | 1 | 0 | 5 | 2 | 87 | 5 |
578.10 | 29-283-17-CC,0 | 0 | 30 | 55 | Paleocene | SILTY CLAY | Dominat lithology; numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 2 | 2 | 2 | 48 | 0 | 0 | 2 | 2 | 0 | 3 | 5 | 84 | 10 |
578.10 | 29-283-17-CC,0 | 5 | 40 | 70 | Paleocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 2 | 0 | 5 | 71 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 90 | 5 |