de Graciansky, Pierre C; Poag, C Wylie (2005): Smear slide analysis of Hole 80-549 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.231087
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
Waples, Douglas W; Vaos, Staphanos P; Townsend, Hilary A; Snyder, Scott W; Sigal, Jacques; Reynolds, Leslie A; Otsuka, Kenichi; Müller, Carla; Montadert, Lucien; Mazzullo, James M; Masson, Douglas G; Cunningham, Robert; Loubere, Paul; de Graciansky, Pierre C; Poag, C Wylie (1985): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXXX, 679 pp + 1258 pp, https://doi.org/10.2973/dsdp.proc.80.1985
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 49.088000 * Longitude: -13.098000
Date/Time Start: 1981-06-15T00:00:00 * Date/Time End: 1981-06-15T00:00:00
Minimum DEPTH, sediment/rock: 0.22 m * Maximum DEPTH, sediment/rock: 940.08 m
Event(s):
80-549 * Latitude: 49.088000 * Longitude: -13.098000 * Date/Time: 1981-06-15T00:00:00 * Elevation: -2515.0 m * Penetration: 1001.5 m * Recovery: 370 m * Location: North Atlantic/SPUR * Campaign: Leg80 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 91 cores; 759.5 m cored; 53 m drilled; 48.7 % 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 | Nannofossils | Nannos | % | Smear slide analysis | ||
10 | Foraminifera | Foram | % | Smear slide analysis | ||
11 | Radiolarians | Rad | % | Smear slide analysis | ||
12 | Diatoms | Diatoms | % | Smear slide analysis | ||
13 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
14 | Spiculae | Spiculae | % | Smear slide analysis | ||
15 | Opaque minerals | Opaque | % | Smear slide analysis | ||
16 | Iron | Fe | % | Smear slide analysis | ||
17 | Organic matter | OM | % | Smear slide analysis | organic debris |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2235 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Nannos [%] | 10 Foram [%] | 11 Rad [%] | 12 Diatoms [%] | 13 Silicoflag [%] | 14 Spiculae [%] | 15 Opaque [%] | 16 Fe [%] | 17 OM [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.22 | 80-549-1-1,22 | 2 | 15 | 83 | Quaternary | (FORAMINIFERA BEARING) NANNO OOZE M TOT.DET 7,QTZ 2,CLAY 5,GLAUC TR,PYR | numerical abundance | 65 | 7 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
4.99 | 80-549-1-4,49 | 1 | 5 | 94 | Quaternary | MARLY NANNO OOZE M TOT.DET 28,QTZ 3,HVY.MINS TR/N HORNBLENDE, CLAY 25,GL | relative abundance | 45 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
8.67 | 80-549-1-61,117 | 2 | 20 | 78 | Quaternary | NANNOFOSSIL OOZE M TOT.DET 1,QTZ 1,CLAY 5,GLAUC TR,PYR 1,CARB 20 | numerical abundance | 68 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
10.40 | 80-549-H1-1,90 | 15 | 10 | 75 | Upper oligocene | SP SPIC FORAMS BEARING NANNO OOZE M TOT.DET 6,QTZ 1,CLAY 5,GLAUC TR,PYR | numerical abundance | 65 | 10 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
10.55 | 80-549-H1-11,105 | 15 | 5 | 80 | Upper oligocene | SP SPIC & FORAMS BEARING NANNO OOZE M TOT.DET 6,QTZ 1,CLAY 5,GLAUC TR,PY | numerical abundance | 56 | 7 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
11.49 | 80-549-H1-2,49 | 15 | 10 | 75 | Upper oligocene | NANNO OOZE (BEARING SP SPIC & FORAMS) M TOT.DET 4,QTZ 1,CLAY 3,GLAUC TR, | numerical abundance | 75 | 7 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
14.92 | 80-549-H1-4,92 | 0 | 0 | 0 | Upper oligocene | SP SPIC BEARING NANNOFOSSIL OOZE M TOT.DET 3,CLAY 3,PYR TR,CARB 5 | relative abundance | 84 | 3 | 0 | 2 | 0 | 5 | 0 | 0 | 0 |
96.02 | 80-549-H2-2,52 | 0 | 0 | 0 | Upper eocene | (SP SPIC BEARING) NANNOFOSSIL OOZE M TOT.DET 5,CLAY 5 | numerical abundance | 90 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
99.16 | 80-549-H2-4,66 | 0 | 0 | 0 | Upper eocene | NANNOFOSSIL OOZE M TOT.DET 5,CLAY 5 | relative abundance | 90 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
198.80 | 80-549-2-1,30 | 0 | 0 | 0 | Middle eocene | NANNO CHALK M VOLC.GLAS TR,CARB 10 | relative abundance | 70 | 5 | 2 | 2 | 0 | 5 | 0 | 0 | 0 |
199.60 | 80-549-2-11,110 | 10 | 45 | 45 | Middle eocene | SPICULE NANNO CHALK M VOLC.GLAS TR,CARB 5 | numerical abundance | 70 | 5 | 0 | 0 | 0 | 20 | 0 | 0 | 0 |
201.03 | 80-549-2-21,103 | 10 | 45 | 45 | Middle eocene | NANNO CHALK M CARB 5 | numerical abundance | 80 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
201.07 | 80-549-2-21,107 | 10 | 45 | 45 | Middle eocene | NANNO CHALK M MICA TR,VOLC.GLAS TR,CARB 10 | relative abundance | 70 | 5 | 2 | 0 | 0 | 5 | 0 | 2 | 0 |
202.80 | 80-549-2-31,130 | 20 | 40 | 40 | Middle eocene | M VOLC.GLAS 20 | numerical abundance | 70 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
208.89 | 80-549-3-1,89 | 10 | 45 | 45 | Middle eocene | NANNO CHALK M CARB 10 | numerical abundance | 70 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
223.60 | 80-549-4-5,10 | 10 | 45 | 45 | Middle eocene | NANNO CHALK P FORAMS 5,NANNOS 70,DISC TR,DIAT TR,RADS TR, SP.SPIC 5 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
224.10 | 80-549-4-5,60 | 10 | 45 | 45 | Middle eocene | NANNO CHALK M CARB 5 | relative abundance | 70 | 5 | 2 | 0 | 0 | 10 | 0 | 0 | 0 |
240.28 | 80-549-6-3,78 | 15 | 25 | 60 | Middle eocene | SILICEOUS FORAM NANNOFOSSIL CHALK M QTZ 4,FEL 2,MICA 2,HVY.MINS 2,CLAY 1 | numerical abundance | 35 | 10 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
243.41 | 80-549-6-5,91 | 10 | 20 | 70 | Middle eocene | NANNO CHALK M TOT.DET 5,CLAY 5,PYR TR,CARB 5 | relative abundance | 70 | 10 | 0 | 2 | 0 | 10 | 0 | 0 | 0 |
246.16 | 80-549-7-1,16 | 2 | 3 | 95 | Middle eocene | NANNO OOZE M CLAY 15 | numerical abundance | 80 | 1 | 2 | 0 | 0 | 2 | 0 | 0 | 0 |
246.36 | 80-549-7-1,36 | 10 | 15 | 75 | Middle eocene | NANNOFOSSIL OOZE M HVY.MINS 2,CLAY 20,CARB 5 | numerical abundance | 60 | 5 | 5 | 0 | 0 | 5 | 0 | 0 | 0 |
252.53 | 80-549-7-5,53 | 5 | 10 | 85 | Middle eocene | NANNOFOSSIL OOZE M CLAY 20,CARB 3 | numerical abundance | 65 | 2 | 3 | 0 | 0 | 7 | 0 | 0 | 0 |
265.10 | 80-549-9-1,10 | 10 | 20 | 70 | Middle eocene | NANNOFOSSIL CHALK M QTZ 10,CLAY 15,VOLC.GLAS P,CARB 20 | numerical abundance | 50 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
274.54 | 80-549-10-1,4 | 0 | 0 | 95 | Lower eocene | MARLY NANNOFOSSIL CHALK M QTZ TR,CLAY 20,PYR TR,CARB 40 | relative abundance | 30 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
274.94 | 80-549-10-1,44 | 5 | 5 | 90 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,MICA TR,CLAY 10,PYR TR,CARB 20 | relative abundance | 40 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
275.17 | 80-549-10-1,67 | 0 | 0 | 0 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 10,PYR TR,CARB 10 | relative abundance | 55 | 10 | 2 | 0 | 0 | 5 | 0 | 0 | 0 |
276.30 | 80-549-10-2,30 | 0 | 0 | 0 | Lower eocene | NANNOFOSSIL CHALK M QTZ TR,CLAY 20,PYR TR,CARB 20 | numerical abundance | 50 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
276.90 | 80-549-10-2,90 | 5 | 0 | 95 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 20,CARB 10 | numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
277.59 | 80-549-10-3,9 | 10 | 0 | 90 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 10,CARB 20 | numerical abundance | 50 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
278.09 | 80-549-10-3,59 | 0 | 0 | 100 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 10,CARB 20 | relative abundance | 60 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
278.28 | 80-549-10-3,78 | 0 | 0 | 100 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,FEL TR,CLAY 10,CARB 10 | numerical abundance | 70 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
278.60 | 80-549-10-31,110 | 10 | 0 | 90 | Lower eocene | NANNOFOSSIL CHALK M QTZ 10,CLAY 10,CARB 20 | numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
279.52 | 80-549-10-4,52 | 5 | 5 | 90 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,FEL TR,CLAY 10,CARB 10 | numerical abundance | 60 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
281.36 | 80-549-10-5,86 | 5 | 0 | 95 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 20,CARB 30 | numerical abundance | 40 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
282.98 | 80-549-10-6,98 | 0 | 0 | 100 | Lower eocene | MARLY NANNOFOSSIL CHALK M QTZ 5,FEL 5,CLAY 20,CARB 20 | numerical abundance | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
284.93 | 80-549-11-1,93 | 0 | 0 | 100 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 10,CARB 25 | numerical abundance | 45 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 |
286.10 | 80-549-11-2,60 | 0 | 0 | 0 | Lower eocene | SAMPLE FROM PYRITE BAND M QTZ 5,PYR 70 | numerical abundance | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
287.44 | 80-549-11-3,44 | 0 | 0 | 0 | Lower eocene | NANNOFOSSIL CHALK M QTZ 10,FEL 5,CLAY 10,VOLC.GLAS TR,CARB 10 | relative abundance | 50 | 5 | 2 | 0 | 0 | 10 | 0 | 0 | 0 |
290.69 | 80-549-11-5,69 | 0 | 0 | 0 | Lower eocene | M QTZ 5,CLAY 10,PYR 5,CARB 20 | numerical abundance | 50 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
292.62 | 80-549-11-61,112 | 0 | 0 | 0 | Lower eocene | NANNOFOSSIL CHALK M QTZ 10,CLAY 5,CARB 10 | numerical abundance | 45 | 10 | 10 | 0 | 0 | 10 | 0 | 0 | 0 |
292.90 | 80-549-11-61,140 | 0 | 0 | 0 | Lower eocene | M QTZ 5,CLAY 10,CARB 20 | numerical abundance | 40 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 |
294.56 | 80-549-12-11,106 | 0 | 0 | 0 | Lower eocene | M QTZ 5,FEL 5,CLAY 10,PYR 5,CARB 10 | relative abundance | 40 | 0 | 2 | 0 | 0 | 15 | 0 | 0 | 0 |
297.27 | 80-549-12-3,77 | 0 | 0 | 0 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 10,CARB 10 | relative abundance | 60 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 0 |
298.68 | 80-549-12-4,68 | 0 | 0 | 0 | Lower eocene | NANNOFOSSIL CHALK M QTZ 10,CLAY 10,CARB 10 | numerical abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
299.44 | 80-549-12-41,144 | 0 | 0 | 100 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 5,PYR TR,CARB 10 | relative abundance | 60 | 2 | 2 | 0 | 0 | 15 | 0 | 0 | 0 |
303.66 | 80-549-13-1,66 | 0 | 0 | 100 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,FEL TR,CLAY 20,CARB 10 | numerical abundance | 40 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 |
306.85 | 80-549-13-3,85 | 0 | 0 | 0 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 10,CARB 10 | numerical abundance | 60 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
308.08 | 80-549-13-4,58 | 0 | 0 | 0 | Lower eocene | MARLY NANNOFOSSIL CHALK M QTZ 10,CLAY 20,CARB 10 | numerical abundance | 45 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 |
309.22 | 80-549-13-5,22 | 0 | 0 | 0 | Lower eocene | NANNOFOSSIL CHALK M QTZ 5,CLAY 15,CARB 10 | relative abundance | 60 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
313.20 | 80-549-14-1,70 | 0 | 10 | 90 | Lower eocene | MARLY NANNOFOSSIL CHALK M QTZ 15,FEL 5,CLAY 15,CARB 5 | relative abundance | 50 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
316.44 | 80-549-14-3,94 | 0 | 0 | 0 | Lower eocene | M QTZ 15,FEL TR,CLAY 15,CARB 10 | numerical abundance | 50 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
318.91 | 80-549-14-5,41 | 0 | 0 | 100 | Lower eocene | M QTZ 10,CLAY 25,CARB 10 | numerical abundance | 40 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
318.98 | 80-549-14-5,48 | 0 | 0 | 100 | Lower eocene | M QTZ 10,FEL TR,CLAY 30,CARB 5 | numerical abundance | 40 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
321.01 | 80-549-14-61,101 | 0 | 0 | 0 | Lower eocene | M QTZ 5,CLAY 25,PYR 5,CARB 10 | relative abundance | 50 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
322.06 | 80-549-15-1,6 | 0 | 0 | 0 | Lower eocene | PYRITE BAND W/IN NANNO CHALK M HVY.MINS 90/N PYRITE | numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
325.63 | 80-549-15-3,63 | 0 | 0 | 0 | Lower eocene | NANNO CHALK M QTZ 10/N SHARDS,CLAY 10 | relative abundance | 60 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
326.46 | 80-549-15-31,146 | 0 | 0 | 0 | Lower eocene | NANNO CHALK M MICA 5,CARB 20 | relative abundance | 65 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
327.65 | 80-549-15-41,115 | 0 | 0 | 0 | Lower eocene | NANNO CHALK M QTZ 5,MICA 10,VOLC.GLAS 5,CARB 20 | numerical abundance | 60 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
330.89 | 80-549-15-61,139 | 0 | 0 | 0 | Lower eocene | NANNO CHALK M QTZ 5,FEL 5,MICA TR,CLAY 5,CARB 20 | relative abundance | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
331.33 | 80-549-15-7,33 | 0 | 0 | 0 | Lower eocene | NANNO CHALK M QTZ 15/N SHARDS AND CHIPS,MICA 10,CARB 20 | relative abundance | 50 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
332.14 | 80-549-16-1,64 | 10 | 20 | 70 | Upper paleocene | VERY MARLY NANNOFOSSIL CHALK M QTZ 10,CLAY 30,CHLOR 5,CARB 10 | numerical abundance | 40 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
338.87 | 80-549-16-51,137 | 5 | 15 | 80 | Upper paleocene | CALCAREOUS CLAYSTONE M QTZ 5,FEL 2,MICA 2,HVY.MINS 1,CLAY 40, CHLOR 5,VO | relative abundance | 30 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
339.92 | 80-549-16-6,92 | 10 | 30 | 60 | Upper paleocene | CALCAREOUS SILTSTONE M QTZ 10,CLAY 20,CHLOR 10,VOLC.GLAS 5,CARB 20 | relative abundance | 30 | 5 | 0 | 1 | 0 | 1 | 0 | 0 | 0 |
340.27 | 80-549-16-61,127 | 10 | 20 | 70 | Upper paleocene | MARLY NANNOFOSSIL CHALK M QTZ 4,FEL 2,MICA 2,HVY.MINS 2,CLAY 20, CHLOR 5 | relative abundance | 40 | 10 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
351.51 | 80-549-18-11,101 | 5 | 15 | 80 | Upper paleocene | SILICEOUS NANNOFOSSIL CHALK M QTZ P,CLAY 20,CHLOR 5,GLAUC P,CARB 10 | relative abundance | 50 | 0 | 1 | 0 | 10 | 0 | 0 | 0 | 0 |
352.66 | 80-549-18-2,66 | 50 | 40 | 10 | Upper paleocene | SANDY ASH M QTZ 25,CHLOR 10,VOLC.GLAS 60,PYR P/N ON THE VOLC GLAS,CARB P | relative abundance | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
353.84 | 80-549-18-3,34 | 10 | 30 | 60 | Upper paleocene | DIATOM NANNOFOSSIL CHALK M QTZ P,CLAY 20,CHLOR P,GLAUC P,CARB 10 | numerical abundance | 30 | 0 | 5 | 20 | 0 | 10 | 0 | 0 | 0 |
360.47 | 80-549-19-1,47 | 5 | 30 | 65 | Upper paleocene | SILICEOUS NANNOFOSSIL CHALK M CLAY 20,VOLC.GLAS 5 | numerical abundance | 60 | 0 | 3 | 3 | 0 | 10 | 0 | 0 | 0 |
363.75 | 80-549-19-3,75 | 5 | 5 | 90 | Upper paleocene | NANNO CHALK M CLAY 10,CARB 10 | numerical abundance | 77 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
365.22 | 80-549-19-4,72 | 3 | 10 | 87 | Upper paleocene | NANNOFOSSIL CHALK M CLAY 5,CARB 5 | relative abundance | 90 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
371.56 | 80-549-20-2,56 | 5 | 25 | 70 | Upper paleocene | M QTZ 5,CLAY 20,CHLOR 5,CARB 10 | numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
376.23 | 80-549-20-5,73 | 5 | 25 | 70 | Upper paleocene | M QTZ 20,FEL 5,CLAY 15,CHLOR P,CARB 20 | relative abundance | 40 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
377.82 | 80-549-20-6,82 | 2 | 5 | 93 | Upper paleocene | CALCAREOUS NANNO CHALK M QTZ 1,MICA 2,CLAY 5,CARB 10 | numerical abundance | 78 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
382.98 | 80-549-21-3,98 | 5 | 15 | 80 | Upper maestrichtian | NANNOFOSSIL OOZE M QTZ 5,CLAY 10,CHLOR P,VOLC.GLAS P,OP P/N REDDISH OP D | numerical abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
383.83 | 80-549-21-4,33 | 20 | 20 | 60 | Upper maestrichtian | FORAM NANNOFOSSIL CHALK M QTZ P,CARB 20 | numerical abundance | 60 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
398.73 | 80-549-23-1,73 | 0 | 0 | 100 | Upper campanian | M CARB 30 | numerical abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
398.79 | 80-549-23-1,79 | 5 | 0 | 95 | Upper campanian | M CARB 20 | numerical abundance | 75 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
401.59 | 80-549-23-3,59 | 0 | 0 | 100 | Upper campanian | M CARB 30 | numerical abundance | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
403.53 | 80-549-23-41,103 | 0 | 0 | 100 | Upper campanian | M CARB 10 | numerical abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
405.30 | 80-549-23-51,130 | 0 | 0 | 100 | Upper campanian | M CARB 20 | numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
408.02 | 80-549-24-1,52 | 0 | 0 | 100 | Santonian | M CARB 20 | numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
409.70 | 80-549-24-2,70 | 0 | 0 | 100 | Santonian | M CARB 20 | numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
410.15 | 80-549-24-21,115 | 0 | 0 | 100 | Santonian | M CARB 30 | numerical abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
417.67 | 80-549-25-1,67 | 0 | 0 | 100 | Lower senonian | M CARB 20 | relative abundance | 80 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
427.00 | 80-549-26-1,50 | 0 | 0 | 100 | Lower senonian | M CARB 20 | numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
436.11 | 80-549-27-1,11 | 0 | 0 | 0 | Cenomanian | M PYR 10,CARB 20 | numerical abundance | 50 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
436.11 | 80-549-27-1,11 | 0 | 0 | 100 | Cenomanian | M QTZ 5,FEL TR,CLAY 20,PYR TR,CARB 10 | numerical abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
436.56 | 80-549-27-1,56 | 0 | 0 | 0 | Cenomanian | R APPEAR TO BE AN ALTERED VOLCANIC ASH? | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
436.64 | 80-549-27-1,64 | 0 | 0 | 0 | Cenomanian | M PYR 10,CARB 30 | numerical abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
445.60 | 80-549-28-1,10 | 10 | 10 | 80 | Cenomanian | M QTZ 20,FEL 5,CLAY 30,PYR 10,CARB 5 | numerical abundance | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
446.03 | 80-549-28-1,53 | 0 | 10 | 90 | Cenomanian | M QTZ 10,FEL 5,CLAY 20,CARB 10 | numerical abundance | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
447.40 | 80-549-28-2,40 | 0 | 0 | 0 | Cenomanian | M QTZ 5,CLAY 5,CARB 60 | numerical abundance | 20 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
523.89 | 80-549-37-11,139 | 5 | 15 | 80 | Middle albian | NANNOFOSSIL OOZE M QTZ 2,MICA 3,CLAY 15,CARB 10 | numerical abundance | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
540.65 | 80-549-39-1,15 | 0 | 0 | 0 | Middle albian | M QTZ 20,CARB 20,DOLO TR | numerical abundance | 25 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 |
550.14 | 80-549-40-1,14 | 0 | 0 | 0 | Middle albian | M QTZ 15,CARB 40 | numerical abundance | 20 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
550.20 | 80-549-40-1,20 | 0 | 0 | 0 | Middle albian | M QTZ 20,CARB 60 | numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 |
570.50 | 80-549-42-2,0 | 10 | 30 | 60 | Middle albian | M QTZ 20,CLAY 50,CARB 10 | numerical abundance | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
572.47 | 80-549-42-3,47 | 10 | 20 | 70 | Middle albian | M QTZ 50,FEL 15,PYR TR,CARB 20 | numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
572.60 | 80-549-42-3,60 | 0 | 0 | 0 | Middle albian | M QTZ 20,FEL 5,CLAY 10,CARB 30 | numerical abundance | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
572.71 | 80-549-42-3,71 | 10 | 30 | 60 | Middle albian | M QTZ 40,FEL 5,CLAY 10,CARB 20 | numerical abundance | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
673.92 | 80-549-53-1,42 | 10 | 40 | 50 | Upper barremian | VERY MARLY CHALK M QTZ 30,CLAY 25,CHLOR 5,CARB 30 | numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
674.92 | 80-549-53-11,142 | 10 | 40 | 50 | Upper barremian | MARLY CHALK M QTZ 10,CLAY 20,CHLOR 5,GLAUC P,CARB 50 | relative abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 |
676.38 | 80-549-53-21,138 | 15 | 35 | 50 | Upper barremian | CALCAREOUS MUDSTONE M QTZ 20,CLAY 20,CHLOR 5,DOLO.RHOMB 10/N CALCITE, CA | numerical abundance | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
694.47 | 80-549-55-2,97 | 10 | 45 | 45 | Upper barremian | M QTZ 5,FEL 5,CLAY 10,VOLC.GLAS 5,CARB 30 | numerical abundance | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
698.70 | 80-549-55-5,70 | 10 | 45 | 45 | Upper barremian | M QTZ 10,MICA 10,CLAY 10,VOLC.GLAS 10,CARB 30 | numerical abundance | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
703.20 | 80-549-56-2,70 | 20 | 50 | 30 | Lower barremian | M QTZ 15,FEL 5,PYR 25,CARB 50 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
706.46 | 80-549-56-4,96 | 0 | 0 | 0 | Lower barremian | M QTZ 35,FEL TR,PYR 20,CARB 30 | relative abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
711.70 | 80-549-57-2,20 | 20 | 40 | 40 | Lower barremian | M QTZ 15,MICA 10,CLAY 10,PYR 5,CARB 30,DOLO TR | relative abundance | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
713.70 | 80-549-57-3,70 | 5 | 50 | 45 | Lower barremian | M QTZ 10,CLAY 20,CHERT TR,PYR 5,CHLOR 20,CARB 20 | relative abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
719.83 | 80-549-58-1,83 | 25 | 35 | 40 | Lower barremian | M QTZ 40,FEL 5,HVY.MINS 3,CHLOR 5,CARB 40 | relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
728.85 | 80-549-59-1,85 | 30 | 30 | 40 | Lower barremian | M QTZ 50,FEL 3,CLAY 10,CHLOR 5,GLAUC P,CARB 30 | relative abundance | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
737.77 | 80-549-60-1,77 | 0 | 0 | 0 | Lower barremian | M QTZ 15,GLAUC 10,PYR TR,CARB 40 | numerical abundance | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
743.28 | 80-549-60-5,28 | 30 | 35 | 35 | Lower barremian | CALCAREOUS CHALK M QTZ 10,HVY.MINS 5,CLAY 10,GLAUC 10,PYR 5, CARB 50 | numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
778.10 | 80-549-66-CC,0 | 40 | 40 | 20 | Lower barremian | M QTZ 40,FEL 5,HVY.MINS 5,ROCK.FRAGS 10,GLAUC 5, CARB 30 | relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
813.12 | 80-549-74-2,62 | 20 | 50 | 30 | Lower barremian | SILTSTONE M QTZ 80,CLAY TR,PYR TR,CARB 10 | relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
816.90 | 80-549-75-1,90 | 10 | 70 | 20 | Lower barremian | M QTZ 65,CLAY TR,CARB 30 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
819.63 | 80-549-75-3,63 | 10 | 40 | 50 | Lower barremian | M QTZ 50,CLAY TR,PYR TR,CARB 40 | relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
820.23 | 80-549-75-CC,0 | 0 | 40 | 60 | Lower barremian | M QTZ 65,CLAY 25,CARB TR | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
825.52 | 80-549-76-1,52 | 0 | 0 | 0 | Lower barremian | M QTZ 60,HVY.MINS TR,CARB 30 | relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
827.15 | 80-549-76-2,65 | 0 | 0 | 0 | Lower barremian | M QTZ 50,CARB 45 | relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
828.00 | 80-549-76-3,0 | 0 | 0 | 0 | Lower barremian | M QTZ 10,HEMA 5,GYP TR,DOLO 40/N CEMENT,GLAUC TR, CARB 40/N SOME FORAMS | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
828.36 | 80-549-76-3,36 | 10 | 20 | 70 | Lower barremian | M QTZ 30,FEL TR,CLAY 10,CARB 50 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
844.17 | 80-549-78-11,117 | 30 | 65 | 5 | Lower barremian | M TOT.DET 75,QTZ 60,FEL 5,MICA 5,HVY.MINS 5, CLAY 5,PYR TR,CARB 25 | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
861.27 | 80-549-80-1,27 | 50 | 30 | 20 | Lower barremian | SILTY FINE SANDSTONE - CALCAREOUS M QTZ 50,FEL P,HVY.MINS P,CLAY 20,OP.M | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
862.40 | 80-549-80-11,140 | 50 | 30 | 20 | Lower barremian | DOLOMITIC SILTY FINE SANDSTONE M QTZ 40,FEL 5,HVY.MINS 5/N REDS GREENS,C | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
863.57 | 80-549-80-21,107 | 60 | 30 | 10 | Lower barremian | M QTZ 65,FEL 5,MICA P,HVY.MINS P,CLAY 10, CHLOR 10,OP 5/N REDDISH,CARB | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
876.16 | 80-549-82-2,16 | 10 | 10 | 80 | Lower barremian | M QTZ 20,CLAY 75 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
876.80 | 80-549-82-2,80 | 20 | 30 | 50 | Lower barremian | M QTZ 60,FEL TR,HVY.MINS TR,CLAY 35 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
897.12 | 80-549-86-1,12 | 10 | 40 | 50 | Lower barremian | SILTY CLAYSTONE M QTZ 70,FEL 5,MICA P,HVY.MINS P,CLAY 15, CHLOR 10 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
897.75 | 80-549-86-1,75 | 40 | 30 | 30 | Lower barremian | SILTY SANDSTONE M QTZ 60,FEL 5,MICA P,HVY.MINS P,CLAY 20, CHLOR 10,CARB | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
899.94 | 80-549-86-21,144 | 70 | 20 | 10 | Lower barremian | SILTY CARBONACEOUS SANDSTONE M QTZ 60,FEL 5,MICA P,HVY.MINS P,CLAY 10, C | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
907.53 | 80-549-87-2,3 | 20 | 50 | 30 | Lower barremian | SILTSTONE M QTZ 60,FEL P,MICA P,HVY.MINS 10,CLAY 10, CARB 20/N SOME CALC | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
911.84 | 80-549-88-11,134 | 30 | 60 | 10 | Lower barremian | M QTZ 90,CARB TR | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
912.45 | 80-549-88-2,45 | 20 | 60 | 20 | Lower barremian | M QTZ 85,CLAY 5,GLAUC 5 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
912.70 | 80-549-88-2,70 | 5 | 5 | 90 | Lower barremian | M QTZ 30,CLAY 65,CARB TR | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
921.10 | 80-549-89-2,10 | 20 | 60 | 20 | M QTZ 70,CLAY 20,PYR TR,CARB TR | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
930.65 | 80-549-90-2,65 | 15 | 45 | 40 | M QTZ 35,HVY.MINS 15,CLAY 30,COALIFIED.WOOD 15, CARB 5 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
939.58 | 80-549-91-2,58 | 0 | 0 | 0 | FROM OLIVE STAINED FINE SANDST R STAIN IS PLANT CELLULAR MATERIAL LEAVES | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
939.70 | 80-549-91-2,70 | 85 | 10 | 5 | M QTZ 85,FEL 10,HVY.MINS P,CLAY 5 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
940.08 | 80-549-91-CC,14 | 20 | 40 | 40 | SILTY CLAY M QTZ 60,HVY.MINS 5,CLAY 30 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |