Heezen, Bruce C; MacGregor, Ian D (2005): Smear slide analysis of Hole 20-194 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230453
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
Ruef, Michael R; Okada, Hakuyu; Krasheninnikov, Valery A; Kaneps, Ansis G; Jones, E J W; Hoskins, R; Hesse, Reinhard; Hekel, H; Forristall, G; Foreman, H P; Heezen, Bruce C; MacGregor, Ian D (1973): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XX, 958 pp, https://doi.org/10.2973/dsdp.proc.20.1973
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 33.978000 * Longitude: 148.810700
Date/Time Start: 1971-09-19T00:00:00 * Date/Time End: 1971-09-19T00:00:00
Minimum DEPTH, sediment/rock: 38.22 m * Maximum DEPTH, sediment/rock: 149.17 m
Event(s):
20-194 * Latitude: 33.978000 * Longitude: 148.810700 * Date/Time: 1971-09-19T00:00:00 * Elevation: -5754.0 m * Penetration: 248 m * Recovery: 15 m * Location: North Pacific/ABYSSAL FLOOR * Campaign: Leg20 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 2 cores; 19 m cored; 20.5 m drilled; 78.9 % 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 | Radiolarians | Rad | % | Smear slide analysis | ||
11 | Diatoms | Diatoms | % | Smear slide analysis | ||
12 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
13 | Spiculae | Spiculae | % | Smear slide analysis | ||
14 | Minerals, other | Min other | % | Smear slide analysis | ||
15 | Quartz | Qz | % | Smear slide analysis | ||
16 | Feldspar | Fsp | % | Smear slide analysis | ||
17 | Zeolite | Zeo | % | Smear slide analysis | ||
18 | Mica | Mica | % | Smear slide analysis | ||
19 | Clay minerals | Clay min | % | Smear slide analysis | ||
20 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
21 | Iron | Fe | % | Smear slide analysis | ||
22 | Limonite | Lm | % | Smear slide analysis | ||
23 | Heavy minerals | HM | % | Smear slide analysis | ||
24 | Hornblende | Hbl | % | Smear slide analysis | ||
25 | Amphibole | Amp | % | Smear slide analysis | ||
26 | Pyroxene | Pyrox | % | Smear slide analysis | ||
27 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
28 | Palagonite | Palagonite | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1053 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 Rad [%] | 11 Diatoms [%] | 12 Silicoflag [%] | 13 Spiculae [%] | 14 Min other [%] | 15 Qz [%] | 16 Fsp [%] | 17 Zeo [%] | 18 Mica [%] | 19 Clay min [%] | 20 Py [%] | 21 Fe [%] | 22 Lm [%] | 23 HM [%] | 24 Hbl [%] | 25 Amp [%] | 26 Pyrox [%] | 27 Volc glass [%] | 28 Palagonite [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
38.22 | 20-194-1-1,72 | 0 | 30 | 70 | Lower pleistocene | RAD DIATOM BEARING SILTY CLAY | Dominat lithology; numerical abundance | 0 | 5 | 5 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
38.46 | 20-194-1-1,96 | 0 | 5 | 95 | Lower pleistocene | ALTERED VOLCANIC GLASS | Minor lithology; numerical abundance | 0 | 0 | 1 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
38.90 | 20-194-1-11,140 | 0 | 95 | 5 | Lower pleistocene | RAD DIATOM BEARING CLAYEY ASH | Dominat lithology; numerical abundance | 0 | 2 | 2 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 90 | 0 |
39.38 | 20-194-1-2,38 | 0 | 60 | 40 | Lower pleistocene | CLAYEY ASH RICH IN RADIOLARIAN | Minor lithology; numerical abundance | 0 | 10 | 0 | 0 | 0 | 10 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 70 | 0 |
39.40 | 20-194-1-2,40 | 0 | 70 | 30 | Lower pleistocene | RADIOLARIAN BEARING ASH | Minor lithology; numerical abundance | 0 | 3 | 0 | 0 | 0 | 5 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 |
40.40 | 20-194-1-21,140 | 0 | 30 | 70 | Lower pleistocene | SILTY CLAY RICH IN DIATOMS, RADS, SPONGE | Dominat lithology; numerical abundance | 0 | 20 | 20 | 0 | 15 | 0 | 0 | 5 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
41.13 | 20-194-1-3,63 | 0 | 20 | 80 | Lower pleistocene | SILTY CLAYEY ASH WITH SOME RADS | Dominat lithology; relative abundance | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 40 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 |
41.22 | 20-194-1-3,72 | 0 | 40 | 60 | Lower pleistocene | CLAY.MINS 30 | Dominat lithology; numerical abundance | 0 | 50 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
42.14 | 20-194-1-4,14 | 0 | 10 | 90 | Lower pleistocene | RAD RICH SILTY CLAY | Dominat lithology; relative abundance | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 3 | 0 |
42.34 | 20-194-1-4,34 | 0 | 20 | 80 | Lower pleistocene | RAD RICH SILTY CLAY | Dominat lithology; numerical abundance | 0 | 20 | 0 | 0 | 0 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
42.68 | 20-194-1-4,68 | 0 | 70 | 30 | Lower pleistocene | CLAYEY ASH WITH GLASS AND RADS | Dominat lithology; numerical abundance | 0 | 1 | 0 | 0 | 0 | 10 | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 |
43.00 | 20-194-1-41,100 | 20 | 70 | 10 | Lower pleistocene | ASH OF MOSTLY VOLCANIC GLASS | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 |
43.60 | 20-194-1-5,10 | 20 | 70 | 10 | Lower pleistocene | ASH MOSTLY GLASS | Minor lithology; numerical abundance | 0 | 2 | 2 | 0 | 0 | 0 | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 60 | 0 |
43.77 | 20-194-1-5,27 | 10 | 30 | 60 | Lower pleistocene | SILTY CLAY RICH IN VOLCANIC GLASS, RADS | Dominat lithology; numerical abundance | 0 | 20 | 5 | 0 | 0 | 0 | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 |
43.97 | 20-194-1-5,47 | 30 | 50 | 10 | Lower pleistocene | ASH WITH GLASS, QTZ, FEL, PYROX | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 85 | 0 |
44.80 | 20-194-1-51,130 | 30 | 50 | 20 | Lower pleistocene | RAD DIATOM BEARING CLAYEY SANDY SILT | Dominat lithology; numerical abundance | 0 | 5 | 5 | 0 | 0 | 0 | 5 | 30 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 5 | 0 |
44.83 | 20-194-1-51,133 | 30 | 60 | 10 | Lower pleistocene | ASH, POORLY SORTED | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 95 | 0 |
45.08 | 20-194-1-6,8 | 30 | 70 | 1 | Lower pleistocene | FEL BEARING SANDY GLASS SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 10 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 71 | 0 |
45.19 | 20-194-1-6,19 | 0 | 40 | 60 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 3 | 5 | 0 | 2 | 5 | 0 | 3 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 30 | 0 |
143.16 | 20-194-2-11,116 | 10 | 60 | 30 | Lower miocene | SANDY CLAYEY GLASS SILT | Minor lithology; numerical abundance | 0 | 10 | 30 | 2 | 3 | 30 | 0 | 5 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 50 | 0 |
143.25 | 20-194-2-11,125 | 0 | 40 | 60 | Lower miocene | RAD DIATOM BEARING SILTY CLAY | Dominat lithology; numerical abundance | 8 | 5 | 10 | 0 | 0 | 2 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 1 |
143.39 | 20-194-2-11,139 | 2 | 88 | 10 | Lower miocene | SILTY ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 |
143.71 | 20-194-2-2,21 | 0 | 40 | 60 | Lower miocene | RAD BEARING DIATOM RICH SILTY CLAY | Dominat lithology; numerical abundance | 5 | 5 | 20 | 0 | 0 | 5 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 |
143.81 | 20-194-2-2,31 | 0 | 0 | 50 | Lower miocene | ALTERED PUMICE TAKEN FROM A PEBBLE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 6 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 20 |
143.86 | 20-194-2-2,36 | 0 | 100 | 0 | Lower miocene | VOLCANIC GLASS SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 90 | 0 |
144.30 | 20-194-2-2,80 | 0 | 3 | 10 | Lower miocene | CLAY NANNO OOZE | Minor lithology; numerical abundance | 0 | 5 | 60 | 10 | 15 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
144.56 | 20-194-2-21,106 | 0 | 0 | 50 | Lower miocene | RAD AND DIATOM BEARING CLAY | Dominat lithology; relative abundance | 0 | 10 | 10 | 0 | 5 | 0 | 5 | 8 | 1 | 0 | 50 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 7 | 0 |
145.80 | 20-194-2-3,80 | 0 | 45 | 55 | Lower miocene | RAD RICH DIATOM SILTY CLAY | Dominat lithology; relative abundance | 0 | 15 | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 2 |
146.27 | 20-194-2-31,127 | 0 | 30 | 70 | Lower miocene | SILTY CLAY | Dominat lithology; numerical abundance | 30 | 5 | 1 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 |
146.80 | 20-194-2-4,30 | 0 | 30 | 60 | Lower miocene | DIATOMS, RADS, SPON RICH CLAY | Dominat lithology; numerical abundance | 0 | 10 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
147.13 | 20-194-2-4,63 | 0 | 80 | 20 | Lower miocene | CALCISILTITE | Minor lithology; numerical abundance | 70 | 0 | 0 | 0 | 0 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 20 | 0 |
147.18 | 20-194-2-4,68 | 0 | 5 | 95 | Lower miocene | RADIOLARIAN CLAYEY ASH | Dominat lithology; numerical abundance | 0 | 15 | 2 | 0 | 0 | 0 | 10 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 15 | 0 |
147.50 | 20-194-2-41,100 | 0 | 5 | 95 | Lower miocene | RAD OOZE MINOR AMOUNTS OF CLAYEY ASH | Dominat lithology; numerical abundance | 0 | 70 | 5 | 0 | 0 | 0 | 10 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 |
148.90 | 20-194-2-5,90 | 0 | 60 | 40 | Lower miocene | RAD RICH VOLCANIC ASH LAYER | Dominat lithology; numerical abundance | 0 | 15 | 2 | 0 | 0 | 0 | 10 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 30 | 0 |
149.11 | 20-194-2-51,111 | 0 | 95 | 0 | Lower miocene | LIGHT BROWN PALE ASH | Minor lithology; numerical abundance | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 88 | 1 |
149.12 | 20-194-2-51,112 | 5 | 75 | 20 | Lower miocene | BROWN RAD RICH DIATOMACEOUS CLAY | Dominat lithology; numerical abundance | 0 | 15 | 30 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 32 | 0 |
149.17 | 20-194-2-51,117 | 0 | 10 | 40 | Lower miocene | ASHEY CLAY RICH IN RADIOLARIA | Dominat lithology; numerical abundance | 0 | 1 | 2 | 0 | 0 | 3 | 3 | 3 | 0 | 3 | 75 | 0 | 1 | 1 | 0 | 0 | 0 | 1 | 11 | 0 |
149.17 | 20-194-2-51,117 | 0 | 15 | 85 | Lower miocene | GLASS BEARING GRAY CLAY | Dominat lithology; numerical abundance | 0 | 1 | 2 | 0 | 0 | 0 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 20 | 0 |
149.17 | 20-194-2-51,117 | 0 | 60 | 90 | Lower miocene | RAD TRACE DIATOM BEARING CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 15 | 3 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 |