Hsü, Kenneth J; LaBrecque, John L (2005): Smear slide analysis of Hole 73-524 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.231029
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
Weissert, Helmut J; Tucker, Peter; Tauxe, Lisa; Schreiber, Edward; Poore, Richard Z; Pisciotto, Kenneth A; Peterson, Nikolai P; Percival, Stephen F Jr; McKenzie, Judith A; Karpoff, Anne Marie; Gombos, Andrew M; Carman, M F; Hsü, Kenneth J; LaBrecque, John L (1984): Initial Reports of the Deep Sea Drilling Project. U.S. Government Printing Office, LXXIII, 798 pp, https://doi.org/10.2973/dsdp.proc.73.1984
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -29.484200 * Longitude: 3.512300
Date/Time Start: 1980-05-21T00:00:00 * Date/Time End: 1980-05-21T00:00:00
Minimum DEPTH, sediment/rock: 10.36 m * Maximum DEPTH, sediment/rock: 285.94 m
Event(s):
73-524 * Latitude: -29.484200 * Longitude: 3.512300 * Date/Time: 1980-05-21T00:00:00 * Elevation: -4796.0 m * Penetration: 348.5 m * Recovery: 200.3 m * Location: South Atlantic/CANYON * Campaign: Leg73 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 35 cores; 306.5 m cored; 0 m drilled; 65.3 % 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 | Nannofossils | Nannos | % | Smear slide analysis | ||
11 | Foraminifera | Foram | % | Smear slide analysis | ||
12 | Siliceous microfossils | Silic foss | % | Smear slide analysis | other siliceous material | |
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Quartz | Qz | % | Smear slide analysis | ||
17 | Feldspar | Fsp | % | Smear slide analysis | ||
18 | Clay minerals | Clay min | % | Smear slide analysis | ||
19 | Glauconite | Glt | % | Smear slide analysis | ||
20 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
21 | Iron | Fe | % | Smear slide analysis | ||
22 | Heavy minerals | HM | % | Smear slide analysis | ||
23 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
24 | Palagonite | Palagonite | % | Smear slide analysis | ||
25 | Fragments | Fragm | % | Smear slide analysis | calcareous material | |
26 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus | |
27 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1781 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 Nannos [%] | 11 Foram [%] | 12 Silic foss [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Spiculae [%] | 16 Qz [%] | 17 Fsp [%] | 18 Clay min [%] | 19 Glt [%] | 20 Py [%] | 21 Fe [%] | 22 HM [%] | 23 Volc glass [%] | 24 Palagonite [%] | 25 Fragm [%] | 26 Terr [%] | 27 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
10.36 | 73-524-2-1,86 | 0 | 95 | 5 | Lower eocene | NANNO OOZE | Dominat lithology; relative abundance | 10 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
11.39 | 73-524-2-2,39 | 0 | 85 | 15 | Lower eocene | MARLY NANNO OOZE | Minor lithology; relative abundance | 10 | 65 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 5 |
29.39 | 73-524-3-1,89 | 5 | 90 | 5 | Lower eocene | NANNOFOSSIL OOZE | numerical abundance | 10 | 80 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
31.65 | 73-524-3-3,15 | 40 | 50 | 10 | Lower eocene | FORAM NANNO OOZE | Minor lithology; relative abundance | 0 | 50 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 |
32.39 | 73-524-3-3,89 | 5 | 90 | 5 | Lower eocene | NANNOFOSSIL OOZE | relative abundance | 10 | 80 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
50.31 | 73-524-4-21,131 | 0 | 100 | 0 | NANNO OOZE | Dominat lithology; relative abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
52.06 | 73-524-4-4,6 | 0 | 95 | 5 | GREENISH NANNO OOZE | Minor lithology; numerical abundance | 0 | 91 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | |
52.45 | 73-524-4-4,45 | 0 | 90 | 10 | BROWNISH SILICEOUS NANNO OOZE | Dominat lithology; numerical abundance | 10 | 45 | 0 | 0 | 10 | 5 | 10 | 0 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
57.52 | 73-524-5-1,52 | 75 | 15 | 10 | VOLCANIC ASH | numerical abundance | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 10 | 65 | 0 | 0 | 0 | |
59.37 | 73-524-5-2,87 | 15 | 65 | 20 | CALCAREOUS CHALK | relative abundance | 25 | 35 | 0 | 0 | 2 | 0 | 5 | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 0 | |
59.84 | 73-524-5-21,134 | 25 | 55 | 20 | (CALCAREOUS) VOLCANIC RICH CHALK | relative abundance | 25 | 15 | 2 | 0 | 2 | 0 | 5 | 5 | 0 | 20 | 0 | 0 | 0 | 0 | 25 | 5 | 0 | 0 | 0 | |
61.14 | 73-524-5-31,114 | 5 | 70 | 25 | NANNOFOSSIL OOZE | relative abundance | 10 | 70 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | |
63.73 | 73-524-5-5,73 | 5 | 75 | 20 | NANNOFOSSIL OOZE | relative abundance | 10 | 60 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | |
64.00 | 73-524-5-51,100 | 20 | 70 | 10 | CALCAREOUS OOZE (CHALK) | relative abundance | 40 | 40 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 5 | 0 | 0 | 2 | 0 | 10 | 2 | 0 | 0 | 0 | |
64.02 | 73-524-5-51,102 | 40 | 40 | 20 | GLAUCONITIC FORAMINIFER CHALK | numerical abundance | 10 | 30 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | |
76.56 | 73-524-7-1,56 | 15 | 60 | 25 | Upper paleocene | VOLCANIC RICH CALCAREOUS OOZE (CHALK) | relative abundance | 10 | 30 | 0 | 0 | 0 | 2 | 5 | 10 | 0 | 15 | 0 | 0 | 2 | 0 | 25 | 5 | 0 | 0 | 0 |
77.63 | 73-524-7-2,13 | 30 | 40 | 30 | Upper paleocene | CALCAREOUS VOLCANIC RICH MUD | relative abundance | 15 | 15 | 2 | 0 | 0 | 0 | 5 | 10 | 0 | 20 | 10 | 0 | 2 | 0 | 15 | 10 | 0 | 0 | 0 |
78.13 | 73-524-7-2,63 | 30 | 40 | 30 | Upper paleocene | CALCAREOUS VOLCANIC-RICH MUD | relative abundance | 15 | 20 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 20 | 5 | 0 | 2 | 0 | 20 | 5 | 0 | 0 | 2 |
88.90 | 73-524-8-3,40 | 25 | 55 | 20 | Upper paleocene | CALCAREOUS VOLCANIC SAND (ASH LAYER) | relative abundance | 15 | 10 | 0 | 0 | 0 | 0 | 2 | 15 | 0 | 10 | 10 | 0 | 2 | 0 | 30 | 10 | 0 | 0 | 0 |
90.19 | 73-524-8-4,19 | 15 | 70 | 15 | Upper paleocene | VOLCANIC RICH CALCAREOUS OOZE (CHALK) | relative abundance | 5 | 20 | 20 | 0 | 0 | 0 | 2 | 5 | 0 | 15 | 0 | 0 | 2 | 0 | 10 | 5 | 0 | 0 | 0 |
95.31 | 73-524-9-1,31 | 5 | 80 | 15 | Upper paleocene | CALCAREOUS OOZE (CHALK) | relative abundance | 15 | 60 | 10 | 0 | 2 | 0 | 2 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 2 |
100.51 | 73-524-9-41,101 | 70 | 20 | 10 | Upper paleocene | VOLCANO CLASTIC CALCAREOUS SAND | numerical abundance | 60 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
100.54 | 73-524-9-41,104 | 80 | 0 | 20 | Upper paleocene | GLAUCONITIC VOLCANOCLASTIC CARB SAND | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 20 | 40 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
105.84 | 73-524-10-11,134 | 60 | 0 | 0 | Upper paleocene | CALCAREOUS VOLCANOCLASTIC SANDSTONE | numerical abundance | 40 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 20 | 10 | 5 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
107.73 | 73-524-10-3,23 | 40 | 40 | 20 | Upper paleocene | VOLCANIC CALCAREOUS SANDSTONE | Minor lithology; relative abundance | 50 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 30 | 10 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
110.40 | 73-524-10-41,140 | 0 | 70 | 30 | Upper paleocene | MARLY NANNO OOZE | Dominat lithology; numerical abundance | 40 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
115.37 | 73-524-11-11,137 | 0 | 80 | 20 | Upper paleocene | VOLCANIC CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 90 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
122.41 | 73-524-11-CC,0 | 0 | 0 | 60 | Upper paleocene | NANNO MARL | numerical abundance | 10 | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 48 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
125.16 | 73-524-12-2,16 | 60 | 20 | 20 | CARBONATE SAND | numerical abundance | 0 | 10 | 50 | 0 | 0 | 0 | 0 | 5 | 5 | 20 | 0 | 5 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | |
127.98 | 73-524-12-31,148 | 5 | 60 | 35 | NANNOFOSSIL MARL | numerical abundance | 20 | 45 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | |
138.83 | 73-524-13-41,133 | 10 | 60 | 30 | NANNOFOSSIL MARL | numerical abundance | 20 | 55 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
143.72 | 73-524-14-11,122 | 1 | 95 | 4 | Lower paleocene | NANNO CHALK | Dominat lithology; numerical abundance | 0 | 94 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
146.36 | 73-524-14-3,86 | 30 | 30 | 40 | Lower paleocene | VOLCANIC CLAY | Minor lithology; numerical abundance | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 40 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 0 | 0 |
146.41 | 73-524-14-3,91 | 0 | 50 | 50 | Lower paleocene | NANNO MARL | Minor lithology; relative abundance | 49 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 50 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 1 |
154.97 | 73-524-15-21,147 | 15 | 50 | 35 | Lower paleocene | CALCAREOUS MUD (MARL) | numerical abundance | 10 | 25 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 30 | 5 | 0 | 5 | 0 | 10 | 0 | 0 | 0 | 0 |
157.86 | 73-524-15-41,136 | 35 | 40 | 25 | Lower paleocene | SANDY CALCAREOUS MUD (MARL) | relative abundance | 10 | 20 | 5 | 0 | 0 | 0 | 2 | 5 | 0 | 25 | 5 | 0 | 0 | 2 | 20 | 5 | 0 | 0 | 5 |
171.43 | 73-524-17-1,43 | 0 | 80 | 20 | Lower paleocene | VOLC. ASH CLAYSTONE | relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 |
171.84 | 73-524-17-1,84 | 5 | 65 | 30 | Lower paleocene | NANNOFOSSIL MARL | relative abundance | 10 | 60 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 20 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 |
171.98 | 73-524-17-1,98 | 40 | 30 | 30 | Lower paleocene | CARBONATE SAND | numerical abundance | 10 | 30 | 30 | 0 | 0 | 0 | 0 | 0 | 5 | 20 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
181.10 | 73-524-18-1,60 | 70 | 20 | 10 | Lower paleocene | CALC SANDSTONE | Dominat lithology; relative abundance | 70 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
186.80 | 73-524-18-5,30 | 0 | 20 | 80 | Lower paleocene | REDDISH BROWN CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 2 |
200.14 | 73-524-20-1,64 | 15 | 40 | 45 | Maestrichtian | CALCAREOUS MUD (MUDSTONE) | relative abundance | 20 | 5 | 15 | 0 | 0 | 0 | 2 | 5 | 2 | 40 | 0 | 0 | 0 | 2 | 10 | 5 | 0 | 0 | 2 |
200.22 | 73-524-20-1,72 | 0 | 20 | 80 | Maestrichtian | SILICEOUS MUD | relative abundance | 2 | 2 | 0 | 55 | 0 | 0 | 5 | 15 | 2 | 10 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
200.97 | 73-524-20-11,147 | 10 | 40 | 50 | Maestrichtian | VOLCANIC SAND IRON RICH CLAYSTONE | numerical abundance | 0 | 5 | 0 | 5 | 0 | 0 | 5 | 10 | 0 | 20 | 0 | 0 | 20 | 0 | 20 | 10 | 0 | 0 | 5 |
202.17 | 73-524-20-21,117 | 10 | 30 | 60 | Maestrichtian | VOLCANICS RICH CLAYSTONE | numerical abundance | 5 | 5 | 0 | 10 | 0 | 0 | 0 | 5 | 0 | 40 | 0 | 0 | 5 | 0 | 20 | 5 | 0 | 0 | 5 |
203.80 | 73-524-20-31,130 | 0 | 0 | 0 | Maestrichtian | CALCAREOUS MUD (MARL) | relative abundance | 20 | 40 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 2 |
211.39 | 73-524-21-2,89 | 0 | 20 | 80 | Maestrichtian | CLAYSTONE | numerical abundance | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 75 | 0 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 |
213.79 | 73-524-21-4,29 | 5 | 40 | 55 | Maestrichtian | NANNOFOSSIL MARL | numerical abundance | 30 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 32 | 0 | 0 | 5 | 0 | 2 | 1 | 0 | 0 | 0 |
216.16 | 73-524-21-51,116 | 25 | 10 | 65 | Maestrichtian | MARL | numerical abundance | 15 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 55 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 0 |
219.43 | 73-524-22-1,93 | 0 | 25 | 75 | Maestrichtian | REDDISH BROWN CLAYSTONE | relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 75 | 0 | 0 | 10 | 2 | 3 | 0 | 0 | 0 | 0 |
220.95 | 73-524-22-2,95 | 2 | 70 | 28 | Maestrichtian | CALC/NANNOS MARL | Minor lithology; numerical abundance | 40 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 28 | 0 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 |
221.99 | 73-524-22-3,49 | 10 | 70 | 20 | Maestrichtian | ALTERED VOLCANIC CLASTIC | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 20 | 0 | 0 | 10 | 0 | 70 | 0 | 0 | 0 | 0 |
235.10 | 73-524-23-51,110 | 20 | 70 | 10 | Maestrichtian | TUFFACEOUS SANDSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 25 | 2 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 |
237.74 | 73-524-24-1,24 | 0 | 10 | 90 | Maestrichtian | BROWN CLAYSTONE | Dominat lithology; numerical abundance | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 80 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 5 |
238.71 | 73-524-24-11,121 | 0 | 20 | 80 | Maestrichtian | GRAYISH CALCAREOUS CLAYSTONE | Dominat lithology; numerical abundance | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 80 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
238.80 | 73-524-24-11,130 | 0 | 10 | 90 | Maestrichtian | BRIGHT REDDISH BROWN CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 90 | 0 | 0 | 5 | 0 | 3 | 0 | 0 | 0 | 0 |
249.67 | 73-524-25-21,117 | 10 | 40 | 50 | Maestrichtian | CALCAREOUS MUD | relative abundance | 20 | 20 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 30 | 0 | 0 | 2 | 0 | 15 | 5 | 0 | 0 | 2 |
250.98 | 73-524-25-3,98 | 0 | 30 | 70 | Maestrichtian | VOLCANOCLASTIC MUDSTONE | relative abundance | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 2 | 65 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 5 |
252.44 | 73-524-25-4,94 | 0 | 20 | 80 | Maestrichtian | VOLCANIC RICH CLAYSTONE | relative abundance | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 70 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 0 | 0 |
253.07 | 73-524-25-5,7 | 10 | 30 | 60 | Maestrichtian | CLAYSTONE | relative abundance | 10 | 5 | 0 | 0 | 0 | 0 | 2 | 10 | 2 | 65 | 0 | 0 | 0 | 0 | 10 | 10 | 0 | 0 | 2 |
256.90 | 73-524-26-1,40 | 15 | 10 | 75 | Maestrichtian | VOLCANOCLASTIC MUDSTONE | relative abundance | 5 | 2 | 0 | 0 | 0 | 0 | 2 | 5 | 5 | 70 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 2 |
258.11 | 73-524-26-2,11 | 0 | 0 | 0 | Maestrichtian | VOLCANICLASTIC CLAYSTONE | numerical abundance | 5 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
266.51 | 73-524-27-1,51 | 10 | 20 | 70 | Maestrichtian | VOLCANOCLASTIC CLAY (CLAYSTONE) | relative abundance | 5 | 5 | 0 | 0 | 0 | 0 | 2 | 10 | 5 | 55 | 0 | 0 | 0 | 0 | 15 | 5 | 0 | 0 | 2 |
268.44 | 73-524-27-2,94 | 0 | 20 | 80 | Maestrichtian | VOLCANOCLASTIC CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 75 | 0 | 0 | 0 | 5 | 3 | 2 | 0 | 0 | 2 |
268.81 | 73-524-27-21,131 | 0 | 10 | 90 | Maestrichtian | CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 85 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 |
270.97 | 73-524-27-4,47 | 5 | 25 | 70 | Maestrichtian | CLAYSTONE | relative abundance | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 70 | 0 | 0 | 0 | 5 | 5 | 5 | 0 | 0 | 2 |
276.34 | 73-524-28-1,84 | 0 | 30 | 70 | Maestrichtian | CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 5 |
276.58 | 73-524-28-11,108 | 0 | 0 | 0 | Maestrichtian | CALCAREOUS CLAYSTONE (MARL?) | Dominat lithology; numerical abundance | 40 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 38 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
285.94 | 73-524-29-1,94 | 10 | 10 | 80 | Maestrichtian | CALCAREOUS CLAYSTONE | numerical abundance | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |