Hinz, Karl; Winterer, Edward L (2005): Smear slide analysis of Hole 79-547A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.231072
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
Wiegand, George E; Vuchev, Vassil T; Steiger, Torsten; Schaftenaar, C H; Rullkötter, Jürgen; Moore, Johnnie N; Jansa, Lubomir F; Jaffrezo, Michel; Channell, James E T; Bradshaw, Martin J; Leckie, R Mark; Baumgartner, Peter O; Hinz, Karl; Winterer, Edward L (1984): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXXIX, 934 pp, https://doi.org/10.2973/dsdp.proc.79.1984
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 33.780700 * Longitude: -9.349700
Date/Time Start: 1981-05-03T00:00:00 * Date/Time End: 1981-05-03T00:00:00
Minimum DEPTH, sediment/rock: 52.20 m * Maximum DEPTH, sediment/rock: 718.52 m
Event(s):
79-547A * Latitude: 33.780700 * Longitude: -9.349700 * Date/Time: 1981-05-03T00:00:00 * Elevation: -3938.0 m * Penetration: 744.5 m * Recovery: 329.2 m * Location: North Atlantic/PLATEAU * Campaign: Leg79 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 72 cores; 665 m cored; 0 m drilled; 49.5 % 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 | Lamellibranchiata | Lamellibranchiata | % | Smear slide analysis | ||
14 | Radiolarians | Rad | % | Smear slide analysis | ||
15 | Diatoms | Diatoms | % | Smear slide analysis | ||
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Quartz | Qz | % | Smear slide analysis | ||
18 | Mica | Mica | % | Smear slide analysis | ||
19 | Clay minerals | Clay min | % | Smear slide analysis | ||
20 | Iron | Fe | % | Smear slide analysis | ||
21 | Heavy minerals | HM | % | Smear slide analysis | ||
22 | Volcanic glass | Volc glass | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2562 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 Lamellibranchiata [%] | 14 Rad [%] | 15 Diatoms [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Mica [%] | 19 Clay min [%] | 20 Fe [%] | 21 HM [%] | 22 Volc glass [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
52.20 | 79-547A-1-11,120 | 15 | 10 | 75 | Pleistocene | SLIGHTLY CLAYEY FORAM NANNO OOZE M QTZ 5,MICA 2,CLAY 10,PYR TR,DOLO 2 | numerical abundance | 0 | 0 | 60 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
56.04 | 79-547A-1-4,54 | 5 | 15 | 80 | Pleistocene | CLAYEY NANNO OOZE M QTZ 2,CLAY 20,PYR 1,DOLO 3 | numerical abundance | 0 | 0 | 70 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
84.40 | 79-547A-2-4,40 | 5 | 10 | 85 | Lower pleistocene | CLAYEY FORAM NANNO OOZE M QTZ 1,MICA 1,CLAY 20,PYR TR,DOLO 1 | numerical abundance | 0 | 0 | 70 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
99.30 | 79-547A-4-1,80 | 0 | 0 | 0 | Pliocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ 1,CLAY 15,DOLO.RHOMB 1 | Dominat lithology; numerical abundance | 0 | 0 | 10 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
112.00 | 79-547A-5-31,100 | 0 | 0 | 0 | Upper miocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ TR,CLAY 15,DOLO 1/N SILT | numerical abundance | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
121.10 | 79-547A-6-3,60 | 0 | 0 | 0 | Upper miocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ TR,FEL TR/N VERY CORRODED,CLAY 10, DOLO | numerical abundance | 0 | 0 | 85 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
128.30 | 79-547A-7-11,130 | 0 | 0 | 0 | Upper miocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ TR,FEL 1/N CORRODED,MICA TR/N MUSCOVITE | numerical abundance | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
128.62 | 79-547A-7-2,12 | 0 | 0 | 0 | Upper miocene | SLIGHTLY CLAYEY NANNO OOZE M FEL TR/N CORRODED,CLAY 25,GLAUC TR | numerical abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
138.20 | 79-547A-8-2,20 | 0 | 0 | 0 | Upper miocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ TR,FEL 1/N SILT CORRODED,CLAY 15,DOLO 1 | numerical abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
141.20 | 79-547A-8-4,20 | 0 | 0 | 0 | Miocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ TR,FEL TR/N CORRODED,CLAY 15,DOLO 1/N S | relative abundance | 0 | 0 | 85 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
142.90 | 79-547A-8-5,40 | 0 | 0 | 0 | Miocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ TR,CLAY 15,GLAUC 1/N SILT VERY FINE,DOL | numerical abundance | 0 | 0 | 83 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
148.30 | 79-547A-9-2,80 | 0 | 0 | 0 | Middle miocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ TR,FEL TR,CLAY 15,GLAUC TR,DOLO 1/N SIL | numerical abundance | 0 | 0 | 80 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
151.20 | 79-547A-9-4,70 | 0 | 0 | 0 | Middle miocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ 1/N SILT,FEL TR/N SILT,CLAY 10,GLAUC 10 | numerical abundance | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
157.80 | 79-547A-10-2,80 | 1 | 1 | 98 | Middle miocene | NANNO OOZE M QTZ TR,CLAY 5,PYR TR,DOLO TR | numerical abundance | 0 | 0 | 94 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
166.90 | 79-547A-11-2,40 | 0 | 1 | 90 | Middle miocene | NANNO OOZE M QTZ TR,CLAY 3,PYR TR,DOLO.RHOMB 1 | relative abundance | 0 | 0 | 95 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
166.90 | 79-547A-11-2,40 | 0 | 10 | 99 | Middle miocene | NANNO OOZE M QTZ TR,MICA TR,CLAY 5,PYR TR,DOLO TR | relative abundance | 0 | 0 | 95 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
169.18 | 79-547A-11-31,118 | 15 | 15 | 70 | Middle miocene | GLAUCONITIC FORAM NANNO OOZE M QTZ 2,CLAY 10,GLAUC 4,PYR 1,DOLO.RHOMB 1 | Minor lithology; numerical abundance | 0 | 0 | 60 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
186.00 | 79-547A-13-2,50 | 5 | 10 | 85 | Middle miocene | SLIGHTLY CLAYEY NANNO OOZE M CLAY 10,PYR 1,DOLO 1 | numerical abundance | 0 | 0 | 85 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
196.80 | 79-547A-14-3,30 | 0 | 10 | 90 | Middle miocene | NANNO OOZE M QTZ TR,HVY.MINS TR/N PYROXENE,CLAY 7,GLAUC TR, PYR TR,DOLO. | numerical abundance | 0 | 0 | 85 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
198.55 | 79-547A-14-4,55 | 2 | 3 | 95 | Lower miocene | SLIGHTLY CLAYEY NANNO OOZE M QTZ 1,CLAY 15,GLAUC TR,PYR 1,DOLO 1 | relative abundance | 0 | 0 | 80 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
203.90 | 79-547A-15-1,90 | 1 | 5 | 94 | Lower tertiary | SLIGHTLY CLAYEY NANNO OOZE M QTZ TR,MICA TR,CLAY 20,PYR 1,DOLO 2 | relative abundance | 0 | 0 | 75 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
205.34 | 79-547A-15-CC,5 | 0 | 2 | 98 | Lower tertiary | CLAYEY NANNO OOZE M QTZ TR,CLAY 30 | relative abundance | 0 | 5 | 65 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
213.20 | 79-547A-16-1,70 | 0 | 5 | 95 | Lower tertiary | SLIGHTLY CLAYEY NANNO OOZE M QTZ TR,MICA TR,CLAY 10,PYR 2,DOLO 2 | relative abundance | 0 | 0 | 85 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
220.05 | 79-547A-16-CC,5 | 0 | 5 | 95 | Lower tertiary | SLIGHTLY CLAYEY NANNO OOZE M QTZ 1,MICA TR,CLAY 10,GLAUC TR,PYR 1,DOLO 1 | relative abundance | 0 | 0 | 85 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
222.79 | 79-547A-17-1,79 | 0 | 5 | 95 | Lower tertiary | SLIGHTLY CLAYEY NANNO CHALK M QTZ 1,MICA TR,CLAY 10,PYR 1,DOLO 1 | relative abundance | 0 | 0 | 85 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
225.80 | 79-547A-17-3,80 | 0 | 20 | 80 | Lower tertiary | NANNOFOSSIL MUDSTONE M QTZ 5,HVY.MINS TR,CLAY 55,PYR TR,DOLO.RHOMB 5 | relative abundance | 0 | 0 | 35 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
225.84 | 79-547A-17-3,84 | 1 | 3 | 96 | Lower tertiary | CLAYEY NANNO CHALK M QTZ 1,CLAY 30,PYR 2,DOLO 1 | numerical abundance | 0 | 0 | 65 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
225.85 | 79-547A-17-3,85 | 2 | 18 | 80 | Lower tertiary | DOLOOMITIC NANNO CLAYSTONE M QTZ 4,CLAY 65,PYR TR,DOLO 10 | relative abundance | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
225.87 | 79-547A-17-3,87 | 40 | 30 | 30 | Lower tertiary | CALCAREOUS GLAUCONITIC SAND M QTZ 5,CLAY 30,GLAUC 40,PYR 2,DOLO 1 | numerical abundance | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
226.04 | 79-547A-17-31,104 | 10 | 20 | 70 | Lower tertiary | FORAMINIFERAL CLAYSTONE M QTZ 10,FEL 2,CLAY 60,PYR 4,DOLO 1 | numerical abundance | 0 | 0 | 10 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
226.10 | 79-547A-17-31,110 | 0 | 0 | 0 | Lower tertiary | NANNO CLAYSTONE M QTZ 1,MICA 1,CLAY 65,PYR 1,DOLO 3 | numerical abundance | 0 | 0 | 25 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
226.38 | 79-547A-17-31,138 | 10 | 15 | 75 | Lower tertiary | NANNO CLAYSTONE M QTZ 1,CLAY 60,PYR TR,DOLO 5 | numerical abundance | 0 | 0 | 25 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
226.45 | 79-547A-17-31,145 | 0 | 20 | 80 | Lower tertiary | NANNO CLAYSTONE M QTZ 1,MICA TR,CLAY 45,GLAUC TR,DOLO.RHOMB 7 | numerical abundance | 0 | 0 | 45 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
226.60 | 79-547A-17-4,10 | 4 | 6 | 90 | Lower tertiary | CLAYEY NANNO CHALK M QTZ 3,MICA 2,CLAY 40,PYR 2,DOLO 2 | numerical abundance | 0 | 0 | 50 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
226.90 | 79-547A-17-4,40 | 1 | 9 | 90 | Lower tertiary | CLAYEY NANNO CHALK M QTZ TR,CLAY 20,PYR 2,DOLO 4 | numerical abundance | 0 | 0 | 70 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
227.13 | 79-547A-17-4,63 | 5 | 10 | 85 | Lower tertiary | NANNO CLAYSTONE M QTZ 4,CLAY 55,PYR 1,DOLO 2 | relative abundance | 0 | 0 | 35 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
227.18 | 79-547A-17-4,68 | 0 | 5 | 95 | Lower tertiary | CLAYEY NANNO CHALK M QTZ TR,CLAY 40,PYR 1,DOLO 1 | numerical abundance | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
227.38 | 79-547A-17-4,88 | 1 | 4 | 95 | Lower tertiary | NANNO CLAYSTONE M QTZ 1,CLAY 85,PYR 2,DOLO 1 | relative abundance | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
227.44 | 79-547A-17-4,94 | 0 | 0 | 0 | Lower tertiary | NANNO CLAYSTONE M QTZ 2,CLAY 60,GLAUC TR,PYR 6,DOLO 2 | numerical abundance | 0 | 0 | 25 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
227.73 | 79-547A-17-41,123 | 0 | 0 | 0 | Lower tertiary | CLAYEY NANNO CHALK M QTZ 1,CLAY 40,DOLO 1,PYR TR | numerical abundance | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
227.87 | 79-547A-17-41,137 | 10 | 15 | 75 | Lower tertiary | FORAM NANNO CLAYSTONE M QTZ 1,CLAY 50,PYR 1,DOLO 3 | relative abundance | 0 | 0 | 30 | 15 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
232.30 | 79-547A-18-1,80 | 5 | 20 | 75 | Lower tertiary | NANNO MUDSTONE M QTZ 10,FEL TR,MICA TR,HVY.MINS TR,CLAY 45, VOLC.GLAS TR | numerical abundance | 0 | 0 | 35 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
241.03 | 79-547A-19-1,3 | 0 | 0 | 0 | Lower tertiary | NANNO BEARING CLAYSTONE M QTZ 2,CLAY 85,DOLO 3/N EUHEDRAL SILT | numerical abundance | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
241.50 | 79-547A-19-1,50 | 0 | 0 | 0 | Lower tertiary | CALCAREOUS CLAYSTONE M QTZ 5/N VERY FINE SILT,FEL TR,CLAY 60,DOLO 3/N SI | numerical abundance | 0 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
242.10 | 79-547A-19-11,110 | 0 | 0 | 0 | Lower tertiary | NANNOFOSSIL CLAYSTONE M QTZ 1,FEL 3/N CORRODED,CLAY 57,GLAUC 1/N VERY FI | numerical abundance | 0 | 0 | 35 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
242.53 | 79-547A-19-2,3 | 0 | 0 | 0 | Lower tertiary | CLAYEY NANNOFOSSIL OOZE/CHALK M QTZ 1,CLAY 33,DOLO 2 | numerical abundance | 0 | 0 | 60 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
242.90 | 79-547A-19-2,40 | 0 | 0 | 0 | Lower tertiary | CLAYEY NANNOFOSSIL CHALK M QTZ 1,CLAY 20,DOLO 3/N SILT,CARB 10 | relative abundance | 0 | 0 | 65 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
243.16 | 79-547A-19-CC,3 | 0 | 0 | 0 | Lower tertiary | CLAYEY NANNO CHALK M QTZ TR,CLAY 25,DOLO 3/N SILT EUHEDRAL, CARB 20/N SI | numerical abundance | 0 | 0 | 50 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
243.23 | 79-547A-19-CC,10 | 0 | 0 | 0 | Lower tertiary | CLAYEY FORAM NANNO CHALK M QTZ TR,CLAY 15,CARB 30/N MICROSPAR | numerical abundance | 0 | 0 | 40 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
251.85 | 79-547A-20-11,135 | 0 | 0 | 0 | Lower tertiary | NANNO OOZE M QTZ 5/N VERY FINE SAND,CLAY 20,GLAUC 4/N VERY FINE SAND,DOL | numerical abundance | 0 | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
252.60 | 79-547A-20-2,60 | 0 | 0 | 0 | Lower tertiary | PARTIALLY RECRYST CLAYEY NANNO OOZE M QTZ 3,CLAY 25,DOLO 5/N SILT VERY F | numerical abundance | 0 | 0 | 55 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
253.90 | 79-547A-20-3,40 | 0 | 0 | 0 | Lower tertiary | CLAYEY NANNO CHALK M QTZ 1,CLAY 40,DOLO 1/N SILT VERY FINE SAND, CARB 5/ | numerical abundance | 0 | 0 | 49 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
257.33 | 79-547A-20-5,83 | 0 | 0 | 0 | Lower tertiary | SLIGHTLY CLAYEY NANNO OOZE CHALK M QTZ 1,FEL P/N CORRODED,HVY.MINS TR,CL | numerical abundance | 0 | 0 | 67 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
260.40 | 79-547A-21-1,40 | 0 | 0 | 0 | Lower tertiary | CLAYEY NANNO CHALK M CLAY 40,DOLO 2 | Dominat lithology; numerical abundance | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
261.08 | 79-547A-21-11,108 | 0 | 0 | 0 | Lower tertiary | NANNO BEARINNG CLAYSTONE M CLAY 88,CARB 2/N MICROSPAR | numerical abundance | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
262.00 | 79-547A-21-2,50 | 0 | 0 | 0 | Lower tertiary | NANNO CHALK M DOLO.RHOMB 2 | Minor lithology; relative abundance | 0 | 0 | 98 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
262.60 | 79-547A-21-21,110 | 0 | 0 | 0 | Lower tertiary | CLAYEY NANNO CHALK M QTZ 7/N FINE SAND,MICA TR/N CHLORITE,CLAY 35, PYR 2 | Dominat lithology; relative abundance | 0 | 0 | 51 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
263.50 | 79-547A-21-3,50 | 0 | 15 | 85 | Lower tertiary | NANNO CLAYSTONE M QTZ 2/N SILT,FEL TR,CLAY 65,PYR 1,CARB 10/N SILT SIZE | Dominat lithology; relative abundance | 0 | 2 | 20 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
270.40 | 79-547A-22-1,90 | 0 | 20 | 80 | Upper eocene | CLAYEY NANNO CHALK M TOT.DET 2,CLAY 30,CARB 5/N SILT SPAR,DOLO.RHOMB 1 | Dominat lithology; relative abundance | 0 | 0 | 60 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
282.27 | 79-547A-23-3,27 | 0 | 20 | 80 | Lower tertiary | VERY CLAYEY NANNO CHALK M QTZ 2,CLAY 40,DOLO.RHOMB TR,CARB 10/N MICROSPA | Dominat lithology; numerical abundance | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
283.95 | 79-547A-23-4,45 | 0 | 30 | 70 | Lower tertiary | CLAYEY NANNO CHALK M QTZ 2/N SILT,CLAY 30,DOLO.RHOMB TR,CARB 7/N MICROSP | Dominat lithology; numerical abundance | 0 | 0 | 50 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
298.90 | 79-547A-25-1,90 | 0 | 30 | 70 | Upper paleocene | CLAYEY NANNO CHALK M QTZ 2,CLAY 30,CARB 10/N MICROSPAR,DOLO.RHOMB TR | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
298.92 | 79-547A-25-1,92 | 0 | 0 | 0 | Upper paleocene | CLAYEY NANNO CHALK M QTZ 2,CLAY 40,PYR TR,DOLO.RHOMB TR,CARB 12/N MICROS | Dominat lithology; relative abundance | 0 | 0 | 45 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
307.75 | 79-547A-26-1,25 | 0 | 0 | 0 | Upper paleocene | NANNO CLAYSTONE M CLAY 55,PYR 1,DOLO.RHOMB 1 | Dominat lithology; relative abundance | 0 | 0 | 42 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
317.70 | 79-547A-27-1,70 | 0 | 5 | 95 | Paleocene | SLIGHTLY CLAYEY NANNO CHALK M QTZ 2,CLAY 25,VOLC.GLAS TR/N GLASS FRAGS, | relative abundance | 0 | 0 | 60 | 3 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
327.33 | 79-547A-28-1,83 | 0 | 25 | 75 | Paleocene | NANNO CLAYSTONE M QTZ 1,CLAY 50,PYR 1,CARB 7/N MICROSPAR, DOLO.RHOMB TR | Dominat lithology; numerical abundance | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
336.68 | 79-547A-29-1,68 | 0 | 30 | 70 | Paleocene | NANNO CLAYSTONE M QTZ 1,CLAY 55,PYR 1,CARB 10/N MICROSPAR, DOLO.RHOMB TR | Dominat lithology; numerical abundance | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
346.30 | 79-547A-30-1,80 | 0 | 30 | 70 | Lower paleocene | SILICEOUS NANNO CLAYSTONE M QTZ 5,MICA TR,HVY.MINS TR,CLAY 50,VOLC.GLAS | relative abundance | 0 | 1 | 35 | 0 | 0 | 4 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
350.10 | 79-547A-30-4,10 | 0 | 20 | 80 | Lower paleocene | SILICEOUS NANNO CLAYSTONE M QTZ 15,MICA 3,HVY.MINS 1,CLAY 50,VOLC.GLAS T | relative abundance | 0 | 0 | 20 | 0 | 0 | 7 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
350.97 | 79-547A-30-CC,0 | 0 | 25 | 75 | Lower paleocene | SILICEOUS NANNO CLAYSTONE M QTZ 10,HVY.MINS 3,CLAY 50,VOLC.GLAS 5,CARB T | numerical abundance | 0 | 0 | 25 | 0 | 0 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
355.30 | 79-547A-31-1,30 | 0 | 20 | 80 | Lower paleocene | SILICEOUS NANNO MUDSTONE | relative abundance | 0 | 1 | 25 | 0 | 0 | 4 | 4 | 1 | 10 | 2 | 50 | 0 | 2 | 5 |
355.52 | 79-547A-31-1,52 | 0 | 0 | 0 | Lower paleocene | SILICEOUS MUDSTONE | numerical abundance | 2 | 1 | 15 | 0 | 0 | 20 | 0 | 5 | 10 | 0 | 35 | 0 | 2 | 10 |
364.95 | 79-547A-32-1,45 | 0 | 0 | 0 | Lower paleocene | NANNO BEARING CLAYSTONE M QTZ 2,FEL 2/N CORRODED,CLAY 82,DOLO 2/N SILT | relative abundance | 0 | 0 | 12 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
366.90 | 79-547A-32-2,90 | 0 | 0 | 0 | Lower paleocene | CLAYEY FORAM NANNO CHALK M TOT.DET 3,CLAY 30,DOLO 3/N SILT | numerical abundance | 0 | 0 | 57 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
369.73 | 79-547A-32-4,73 | 0 | 0 | 0 | Lower paleocene | CLAYEY FORAM NANNO CHALK M QTZ 2,FEL 1,CLAY 35,DOLO 1,CARB 24/N MICROSPA | relative abundance | 0 | 0 | 30 | 7 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
374.61 | 79-547A-33-1,61 | 0 | 0 | 0 | Lower paleocene | CLAYEY NANNO CHALK M QTZ 5/N ANGULAR SILT,CLAY 30,PYR TR,DOLO P | Dominat lithology; relative abundance | 0 | 0 | 55 | 5 | 0 | 2 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
375.24 | 79-547A-33-11,124 | 0 | 0 | 0 | Lower paleocene | SLIGHTLY NANNO CHALK M CLAY 10,DOLO 2 | Dominat lithology; numerical abundance | 0 | 0 | 85 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
378.18 | 79-547A-33-31,118 | 0 | 0 | 0 | Lower paleocene | CLAYEY NANNO OOZE M QTZ 1,CLAY 40 | Dominat lithology; numerical abundance | 0 | 0 | 57 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
378.27 | 79-547A-33-31,127 | 0 | 0 | 0 | Lower paleocene | NANNO CLAYSTONE M QTZ TR,CLAY 55 | Minor lithology; numerical abundance | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
378.33 | 79-547A-33-31,133 | 0 | 0 | 0 | Lower paleocene | CLAYEY NANNO CHALK M QTZ 1,CLAY 40,PYR TR,DOLO 2 | Minor lithology; numerical abundance | 0 | 0 | 55 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
385.50 | 79-547A-34-2,50 | 0 | 0 | 0 | Lower paleocene | CLAYEY NANNO CHALK M QTZ 2/N SILT,CLAY 35,DOLO 2 | Dominat lithology; numerical abundance | 0 | 0 | 58 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
387.19 | 79-547A-34-3,69 | 0 | 0 | 0 | Lower paleocene | NANNO CLAYSTONE M QTZ 2/N SAND SIZE SUBANGULAR,CLAY 55,PYR TR, DOLO 2 | Minor lithology; relative abundance | 0 | 0 | 43 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
393.34 | 79-547A-35-1,34 | 0 | 0 | 0 | Lower paleocene | CLAYEY NANNO CHALK M QTZ 7/N SILT ANGULAR TO SUBROUNDED,CLAY 40, HVY.MIN | Minor lithology; relative abundance | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
405.86 | 79-547A-37-3,36 | 0 | 0 | 0 | Lower paleocene | NANNO CLAYSTONE M QTZ 1/N SILT,CLAY 65,DOLO 3 | Minor lithology; numerical abundance | 0 | 0 | 40 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
405.90 | 79-547A-37-3,40 | 0 | 0 | 0 | Lower paleocene | CLAYSTONE M CLAY 95,DOLO TR | Minor lithology; numerical abundance | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
412.84 | 79-547A-38-1,84 | 2 | 7 | 90 | Lower paleocene | NANNO BEARING CLAYSTONE M QTZ 2,FEL TR,MICA TR,CLAY 70,PYR 2,DOLO 1 | Minor lithology; relative abundance | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
413.33 | 79-547A-38-11,133 | 0 | 0 | 0 | Lower paleocene | NANNO CLAYSTONE M QTZ 2,CLAY 50,PYR TR,DOLO.RHOMB 2 | Dominat lithology; relative abundance | 0 | 0 | 45 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
421.75 | 79-547A-39-1,25 | 0 | 20 | 80 | Cenomanian | NANNO MUDSTONE M QTZ 5,FEL TR,CLAY 65,DOLO.RHOMB 2,CARB 2/N MICROSPAR | Dominat lithology; relative abundance | 0 | 0 | 20 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
422.40 | 79-547A-39-1,90 | 0 | 45 | 55 | Cenomanian | CALCAREOUS MUDSTONE M QTZ 10,MICA TR,CLAY 40,PYR 1,DOLO 2,CARB 30 | Dominat lithology; numerical abundance | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
432.16 | 79-547A-40-1,66 | 0 | 10 | 90 | Cenomanian | NANNO CLAYSTONE M QTZ 2,MICA 1,CLAY 50,PYR 1,DOLO 2 | Dominat lithology; numerical abundance | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
440.60 | 79-547A-41-1,10 | 0 | 20 | 80 | Cenomanian | CLAYEY NANNO (OOZE) CHALK M QTZ 1,CLAY 40,DOLO.RHOMB 2,CARB 1/N MICROSPA | Minor lithology; relative abundance | 0 | 0 | 55 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
441.55 | 79-547A-41-11,105 | 0 | 10 | 90 | Cenomanian | CLAYSTONE M MICA TR,CLAY 90,DOLO 5 | Dominat lithology; numerical abundance | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
442.50 | 79-547A-41-2,50 | 0 | 0 | 0 | Cenomanian | SLIGHTLY DOLOMITIC CLAYSTONE M QTZ 2,MICA TR,CLAY 80,PYR 3,DOLO 10 | Dominat lithology; numerical abundance | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
451.14 | 79-547A-42-11,114 | 0 | 20 | 80 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ 5/N SILT,CLAY 70,PYR 1,DOLO.RHOMB 2,GYP 1 | Dominat lithology; numerical abundance | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
469.72 | 79-547A-44-1,72 | 0 | 0 | 0 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ 1,CLAY 78,PYR 1,BARI TR,DOLO P | Dominat lithology; numerical abundance | 0 | 0 | 20 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
480.40 | 79-547A-45-2,40 | 0 | 0 | 0 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ TR,CLAY 82,DOLO TR | relative abundance | 0 | 0 | 12 | 4 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
498.00 | 79-547A-47-1,50 | 0 | 0 | 0 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ TR,CLAY 62,DOLO 1,CARB 2/N MICROSPAR | relative abundance | 0 | 0 | 30 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
517.90 | 79-547A-49-11,140 | 0 | 0 | 0 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ 1/N SILT SIZE,CLAY 75,PYR 2,ZEOL TR, BARI | Dominat lithology; numerical abundance | 0 | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
526.95 | 79-547A-50-1,95 | 0 | 10 | 90 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ 2,CLAY 75,PYR 2,BARI TR,DOLO.RHOMB TR | Minor lithology; relative abundance | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
540.17 | 79-547A-51-4,17 | 0 | 10 | 90 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ 2,CLAY 75,VOLC.GLAS TR,PYR 1,DOLO.RHOMB TR | Dominat lithology; relative abundance | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
556.20 | 79-547A-53-2,20 | 0 | 10 | 90 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ 2,CLAY 80,VOLC.GLAS TR,GLAUC TR,PYR TR, CA | numerical abundance | 0 | 0 | 8 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
557.40 | 79-547A-53-21,140 | 0 | 10 | 90 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ 2,MICA TR,CLAY 85,GLAUC TR,PYR TR,CARB 3 | relative abundance | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
577.60 | 79-547A-55-31,110 | 0 | 20 | 80 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ 5,MICA TR,HVY.MINS TR,CLAY 80,VOCL.GLAS TR | relative abundance | 0 | 2 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
597.20 | 79-547A-57-4,20 | 0 | 0 | 0 | Cenomanian | NANNO BEARING CLAYSTONE M QTZ TR,MICRONOD 2,BARI 1/N CRYSTALS,DOLO.RHOMB | Minor lithology; relative abundance | 0 | 0 | 15 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
600.20 | 79-547A-57-6,20 | 0 | 0 | 0 | Cenomanian | NANNO BEARING CLAYSTONE M CLAY 75,PYR 1,DOLO 1 | Minor lithology; relative abundance | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 |
651.69 | 79-547A-63-2,69 | 0 | 20 | 80 | Upper albian | NANNO BEARING CLAYSTONE M QTZ 6/N SILT,CLAY 70,GLAUC TR,PYR 2, DOLO.RHOM | Minor lithology; numerical abundance | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
653.80 | 79-547A-63-31,130 | 0 | 30 | 70 | Upper albian | NANNO BEARING MUDSTONE M QTZ 5/N VERY ANGULAR TO SUBRND,FEL TR,MICA TR, | Dominat lithology; relative abundance | 0 | 0 | 5 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
668.80 | 79-547A-65-1,30 | 8 | 12 | 75 | Upper albian | NANNO BEARING MUDSTONE M QTZ 5/N ~1/2 IN SAND SIZE,CLAAY 70,CLAY 10/N CL | numerical abundance | 0 | 0 | 9 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
679.05 | 79-547A-66-11,105 | 5 | 20 | 75 | Upper albian | NANNO BEARING MUDSTONE M QTZ 2,CLAY 70,FEC.PEL 15/N CLASTS,PYR 2, DOLO 3 | Dominat lithology; relative abundance | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
680.87 | 79-547A-66-21,137 | 0 | 15 | 85 | Upper albian | NANNO BEARING MUDSTONE M QTZ 6,CLAY 80,PYR 1,DOLO.RHOMB 3 | Minor lithology; relative abundance | 0 | 0 | 7 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
681.06 | 79-547A-66-3,6 | 5 | 20 | 75 | Upper albian | DOLOMITIC MUDSTONE M QTZ 2,MICA 1,CLAY 75,PYR TR,DOLO 18 | Dominat lithology; relative abundance | 0 | 0 | 5 | 4 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
681.07 | 79-547A-66-3,7 | 5 | 15 | 80 | Upper albian | MUDSTONE M QTZ 2,MICA 2,CLAY 80,FEC.PEL 5/N CLASTS,PYR 1, DOLO 5 | Dominat lithology; numerical abundance | 0 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
698.06 | 79-547A-68-11,106 | 2 | 3 | 95 | Upper albian | NANNO BEARING CLAYSTONE M QTZ 1,MICA 1,CLAY 90,PYR TR,DOLO 2 | numerical abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
698.23 | 79-547A-68-11,123 | 5 | 30 | 65 | Upper albian | DOLOMITIC MUDSTONE M QTZ 5,FEL 2,MICA 2,CLAY 60,DOLO 25 | relative abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
700.15 | 79-547A-68-3,15 | 0 | 0 | 0 | Upper albian | NANNOFOSSIL BEARING CLAYSTONE M QTZ 2,MICA 1,CLAY 80,PYR TR,DOLO 4 | Minor lithology; numerical abundance | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
700.32 | 79-547A-68-3,32 | 2 | 13 | 85 | Upper albian | SLT DOLOMITIC NANNO BEARING CLAYSTONE M QTZ 1,MICA 1,CLAY 80,PYR 2,DOLO | Minor lithology; relative abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
700.94 | 79-547A-68-3,94 | 5 | 15 | 80 | Upper albian | FORAM BEARING CLAYSTONE M QTZ 3,MICA 2,CLAY 80,PYR TR,DOLO 5 | Dominat lithology; numerical abundance | 0 | 0 | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
701.87 | 79-547A-68-4,37 | 0 | 0 | 0 | Upper albian | DOLOSTONE M QTZ TR,DOLO 99 | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
703.10 | 79-547A-68-CC,13 | 3 | 7 | 90 | Upper albian | NANNO RICH CLAYSTONE M QTZ 3,MICA 1,CLAY 60,PYR TR,DOLO 2 | Minor lithology; numerical abundance | 0 | 0 | 30 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
706.80 | 79-547A-69-1,30 | 0 | 0 | 0 | Upper albian | NANNO BEARING CLAYSTONE M QTZ 2/N SILT,CLAY 60,CARB 15/N MICROSPAR | Dominat lithology; numerical abundance | 0 | 0 | 20 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
709.25 | 79-547A-69-21,125 | 0 | 0 | 0 | Upper albian | HIGHLY CALCAREOUS CLAYSTONE M QTZ 3,CLAY 51,BARI 1/N CRYSTALS,PYR TR,CAR | Dominat lithology; numerical abundance | 0 | 3 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
718.52 | 79-547A-70-21,102 | 0 | 0 | 0 | Upper albian | CALCAREOUS CLAYSTONE M CLAY 60,CARB 30 | Minor lithology; relative abundance | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |