Donelly, Thomas W; Francheteau, Jean; Flower, Martin F J (2005): Smear slide analysis of Hole 53-418B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230791
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Donnelly, Thomas W; Francheteau, Jean; Bryan, Wilfred B; Robinson, P; Flower, M; Salisbury, Matthew H; et al. (1980): Initial Reports of the Deep Sea Drilling Project, 51/52/53. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, 51/52/53, 718 pp + 1613 pp, https://doi.org/10.2973/dsdp.proc.515253.1980
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 25.034667 * Longitude: -68.057500
Date/Time Start: 1977-04-14T00:00:00 * Date/Time End: 1977-04-14T00:00:00
Minimum DEPTH, sediment/rock: 1.33 m * Maximum DEPTH, sediment/rock: 310.94 m
Event(s):
53-418B * Latitude: 25.034667 * Longitude: -68.057500 * Date/Time: 1977-04-14T00:00:00 * Elevation: -5514.0 m * Penetration: 329.6 m * Recovery: 172.3 m * Campaign: Leg53 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 34 cores; 320.3 m cored; 9.3 m drilled; 53.8 % 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 | Siliceous microfossils | Silic foss | % | Smear slide analysis | other siliceous material | |
14 | Opal, biogenic silica | bSiO2 | % | Smear slide analysis | ||
15 | Radiolarians | Rad | % | Smear slide analysis | ||
16 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
17 | Spiculae | Spiculae | % | Smear slide analysis | ||
18 | Minerals, other | Min other | % | Smear slide analysis | ||
19 | Manganese carbonate, rhodochrosite | Rds | % | Smear slide analysis | ||
20 | Barite | Brt | % | Smear slide analysis | ||
21 | Quartz | Qz | % | Smear slide analysis | ||
22 | Feldspar | Fsp | % | Smear slide analysis | ||
23 | Zeolite | Zeo | % | Smear slide analysis | ||
24 | Mica | Mica | % | Smear slide analysis | ||
25 | Clay minerals | Clay min | % | Smear slide analysis | ||
26 | Glauconite | Glt | % | Smear slide analysis | ||
27 | Opaque minerals | Opaque | % | Smear slide analysis | ||
28 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
29 | Iron | Fe | % | Smear slide analysis | ||
30 | Heavy minerals | HM | % | Smear slide analysis | ||
31 | Rutile | Rt | % | Smear slide analysis | ||
32 | Apatite | Ap | % | Smear slide analysis | ||
33 | Hornblende | Hbl | % | Smear slide analysis | ||
34 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
35 | Organic matter | OM | % | Smear slide analysis | organic debris | |
36 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4076 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 Silic foss [%] | 14 bSiO2 [%] | 15 Rad [%] | 16 Silicoflag [%] | 17 Spiculae [%] | 18 Min other [%] | 19 Rds [%] | 20 Brt [%] | 21 Qz [%] | 22 Fsp [%] | 23 Zeo [%] | 24 Mica [%] | 25 Clay min [%] | 26 Glt [%] | 27 Opaque [%] | 28 Py [%] | 29 Fe [%] | 30 HM [%] | 31 Rt [%] | 32 Ap [%] | 33 Hbl [%] | 34 Volc glass [%] | 35 OM [%] | 36 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.33 | 53-418B-1-11,133 | 0 | 0 | 0 | Lower quaternary | FORAM NANNO OOZE | relative abundance | 0 | 0 | 20 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 50 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1.42 | 53-418B-1-11,142 | 0 | 0 | 0 | Lower quaternary | NANNOFOSSIL OOZE | numerical abundance | 0 | 0 | 40 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 40 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
7.22 | 53-418B-2-1,42 | 0 | 0 | 0 | Lower quaternary | FORAM RICH NANNO OOZE | relative abundance | 0 | 0 | 60 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 5 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
7.51 | 53-418B-2-1,71 | 0 | 0 | 0 | Lower quaternary | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 83 | 0 | 10 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
9.20 | 53-418B-2-2,90 | 0 | 0 | 0 | Lower quaternary | MANGANESE RICH CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 62 | 0 | 0 | 0 | 2 | 30 | 3 | 0 | 0 | 0 | 0 | 0 |
17.04 | 53-418B-3-1,74 | 0 | 0 | 0 | MICRONODULE RICH PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 73 | 0 | 20 | 0 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | |
17.29 | 53-418B-3-1,99 | 0 | 0 | 0 | MICRONODULE BEARING PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 10 | |
20.03 | 53-418B-3-3,73 | 0 | 0 | 0 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 87 | 0 | 5 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
26.78 | 53-418B-4-1,88 | 0 | 0 | 0 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 88 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
26.96 | 53-418B-4-11,106 | 0 | 0 | 0 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 78 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
31.16 | 53-418B-4-4,76 | 0 | 0 | 0 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 86 | 0 | 5 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
36.00 | 53-418B-5-1,60 | 0 | 0 | 0 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 87 | 0 | 5 | 0 | 1 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | |
37.79 | 53-418B-5-2,89 | 0 | 0 | 0 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 82 | 0 | 5 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | |
40.61 | 53-418B-5-4,71 | 0 | 0 | 0 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 85 | 0 | 5 | 0 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
48.68 | 53-418B-6-3,78 | 0 | 0 | 0 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 87 | 0 | 3 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
51.31 | 53-418B-6-5,41 | 0 | 0 | 0 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 85 | 0 | 5 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
52.77 | 53-418B-6-6,37 | 0 | 0 | 0 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 94 | 0 | 3 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
52.82 | 53-418B-6-6,42 | 0 | 0 | 0 | RHODOCHROSITE BEARING ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 20 | 0 | 70 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
61.09 | 53-418B-7-5,69 | 0 | 0 | 0 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 80 | 0 | 10 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
64.54 | 53-418B-8-1,64 | 0 | 0 | 0 | ZEOLITE BEARING CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 10 | 0 | 74 | 0 | 5 | 0 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
64.74 | 53-418B-8-1,84 | 0 | 0 | 0 | ZEOL BEARING CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 75 | 0 | 10 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
64.99 | 53-418B-8-11,109 | 0 | 0 | 0 | MICRONOD ZONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 80 | |
65.93 | 53-418B-8-2,53 | 0 | 0 | 0 | MICRONOD ZONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 60 | |
68.54 | 53-418B-8-4,14 | 0 | 0 | 0 | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 30 | 0 | 50 | 0 | 5 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | |
78.76 | 53-418B-9-4,96 | 0 | 0 | 0 | ZEOL BEARING CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 10 | 0 | 80 | 0 | 2 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
81.33 | 53-418B-9-6,53 | 0 | 0 | 0 | MICRONOD AND ZEOL BEARING CLAY | relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 | 75 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 5 | |
83.19 | 53-418B-10-1,49 | 0 | 0 | 0 | Lower tertiary | ZEOL RICH CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 15 | 0 | 70 | 0 | 5 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
86.06 | 53-418B-10-3,36 | 0 | 0 | 0 | Lower tertiary | ZEOL RICH CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 | 58 | 0 | 25 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 |
87.41 | 53-418B-10-4,21 | 0 | 0 | 0 | Lower tertiary | ZEOLITIC CLAY | relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 25 | 0 | 64 | 0 | 3 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 |
87.61 | 53-418B-10-4,41 | 0 | 0 | 0 | Lower tertiary | ZEOL CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 30 | 0 | 60 | 0 | 3 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
92.23 | 53-418B-11-1,13 | 0 | 0 | 0 | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 69 | 0 | 2 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | |
94.72 | 53-418B-11-21,112 | 0 | 0 | 0 | ASH BED | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | |
95.97 | 53-418B-11-3,87 | 0 | 0 | 0 | ZEOLITIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 70 | 0 | 3 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
100.02 | 53-418B-11-6,42 | 0 | 0 | 0 | ZEOL RICH CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 83 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
101.94 | 53-418B-12-1,44 | 0 | 0 | 0 | ASH BED | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | |
102.21 | 53-418B-12-1,71 | 0 | 0 | 0 | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 74 | 0 | 3 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
104.83 | 53-418B-12-3,33 | 0 | 0 | 0 | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 58 | 0 | 5 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
105.20 | 53-418B-12-3,70 | 0 | 0 | 0 | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 73 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
111.18 | 53-418B-13-1,28 | 0 | 0 | 0 | ZEOL BEARING CLAY | relative abundance | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 5 | 0 | 78 | 0 | 5 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
111.56 | 53-418B-13-1,66 | 0 | 0 | 0 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | 0 | 89 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
111.81 | 53-418B-13-1,91 | 0 | 0 | 0 | ZEOL BEARING CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 88 | 0 | 5 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | |
112.03 | 53-418B-13-11,113 | 0 | 0 | 0 | ZEOL BEARING CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 83 | 0 | 2 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | |
131.90 | 53-418B-15-2,80 | 0 | 0 | 0 | ZEOL BEARING CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 86 | 0 | 2 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | |
139.13 | 53-418B-16-1,3 | 0 | 0 | 0 | ZEOL AND RAD BEARING CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 7 | 0 | 70 | 0 | 5 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
139.31 | 53-418B-16-1,21 | 0 | 10 | 90 | ZEOL RICH CLAY | relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 85 | 0 | 10 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | |
149.20 | 53-418B-17-1,60 | 0 | 0 | 0 | ZEOL RICH CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 12 | 0 | 70 | 0 | 15 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
150.20 | 53-418B-17-2,10 | 0 | 0 | 0 | ZEOL RICH CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 12 | 0 | 85 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
158.96 | 53-418B-18-1,76 | 0 | 0 | 0 | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 40 | 0 | 55 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
159.08 | 53-418B-18-1,88 | 0 | 0 | 0 | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 50 | 0 | 45 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
167.85 | 53-418B-19-1,15 | 0 | 0 | 0 | Middle eocene | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 50 | 0 | 45 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
167.89 | 53-418B-19-1,19 | 0 | 0 | 0 | Middle eocene | ZEOLITIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 45 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
168.84 | 53-418B-19-11,114 | 0 | 0 | 0 | Middle eocene | SI RICH ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 5 | 0 | 0 | 0 | 2 | 0 | 45 | 0 | 45 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
169.26 | 53-418B-19-2,6 | 0 | 0 | 0 | Middle eocene | FORAM AND RAD BEARING ZEOL-NANNO CHALK | numerical abundance | 0 | 0 | 40 | 5 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
169.30 | 53-418B-19-2,10 | 0 | 0 | 0 | Middle eocene | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 50 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
179.47 | 53-418B-20-2,77 | 0 | 0 | 0 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 90 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
181.40 | 53-418B-20-31,120 | 0 | 0 | 0 | PELAGIC CLAY | numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
183.94 | 53-418B-20-5,73 | 0 | 0 | 0 | ZEOL RICH CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 15 | 0 | 70 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
195.10 | 53-418B-21-6,90 | 0 | 0 | 0 | ZEOL BEARING CLAY | relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 75 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
195.42 | 53-418B-21-61,122 | 0 | 0 | 0 | ZEOLITIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 20 | 0 | 65 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
197.21 | 53-418B-22-1,91 | 0 | 0 | 0 | ZEOL SEDIMENT | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
197.36 | 53-418B-22-11,106 | 0 | 0 | 0 | ZEOL SEDIMENT | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
197.68 | 53-418B-22-11,138 | 0 | 0 | 0 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 50 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | ||
205.96 | 53-418B-23-1,16 | 0 | 0 | 0 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 50 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | ||
206.14 | 53-418B-23-1,34 | 0 | 0 | 0 | ZEOLITIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 25 | 0 | 55 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
225.08 | 53-418B-25-1,18 | 0 | 0 | 0 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 90 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
225.86 | 53-418B-25-1,96 | 0 | 0 | 0 | ZEOLITIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 50 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
235.32 | 53-418B-26-1,92 | 0 | 0 | 0 | Cenomanian | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 5 | 0 | 10 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
235.69 | 53-418B-26-11,129 | 0 | 0 | 0 | Cenomanian | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 45 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
244.14 | 53-418B-27-1,14 | 0 | 0 | 0 | Cenomanian | NANNO BEARING SILICEOUS CLAYSTONE | numerical abundance | 0 | 0 | 5 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
244.35 | 53-418B-27-1,35 | 0 | 0 | 0 | Cenomanian | FORAM RICH NANNO CHALK | relative abundance | 0 | 0 | 50 | 30 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
244.85 | 53-418B-27-1,85 | 0 | 0 | 0 | Cenomanian | FORAM RICH NANNO CHALK | relative abundance | 0 | 0 | 75 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
256.17 | 53-418B-28-21,127 | 5 | 15 | 80 | Upper albian | RAD BEARING NANNO CHALK | relative abundance | 0 | 2 | 0 | 5 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
256.45 | 53-418B-28-3,5 | 0 | 0 | 0 | Upper albian | RAD BEARING NANNO CHALK | relative abundance | 0 | 5 | 70 | 2 | 0 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
256.61 | 53-418B-28-3,21 | 0 | 0 | 0 | Upper albian | BLACK CLAYSTONE | relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 10 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
256.75 | 53-418B-28-3,35 | 0 | 0 | 0 | Upper albian | MARLY CHALK | numerical abundance | 0 | 3 | 40 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 52 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
256.81 | 53-418B-28-3,41 | 0 | 0 | 0 | Upper albian | CLAYSTONE | relative abundance | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
263.23 | 53-418B-29-1,33 | 0 | 20 | 80 | Lower cretaceous | NANNO CHALK | relative abundance | 0 | 2 | 50 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 15 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
264.12 | 53-418B-29-11,122 | 0 | 5 | 95 | Lower cretaceous | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
264.20 | 53-418B-29-11,130 | 0 | 0 | 0 | Lower cretaceous | SILICA RICH CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
272.91 | 53-418B-30-1,51 | 0 | 0 | 0 | Lower cretaceous | RAD RICH CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.56 | 53-418B-30-11,116 | 0 | 10 | 90 | Lower cretaceous | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.59 | 53-418B-30-11,119 | 0 | 0 | 0 | Lower cretaceous | BLACK CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 78 | 0 | 10 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.65 | 53-418B-30-11,125 | 0 | 0 | 0 | Lower cretaceous | BLACK CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 20 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.69 | 53-418B-30-11,129 | 0 | 0 | 0 | Lower cretaceous | RAD BEARING CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.82 | 53-418B-30-11,142 | 20 | 40 | 40 | Lower cretaceous | RADIOLARITE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.96 | 53-418B-30-2,6 | 0 | 10 | 90 | Lower cretaceous | RAD BEARING CLAYSTONE | relative abundance | 2 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 83 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
274.19 | 53-418B-30-2,29 | 0 | 0 | 0 | Lower cretaceous | RADIOLARITE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
275.24 | 53-418B-30-21,134 | 0 | 0 | 0 | Lower cretaceous | CLAYSTONE WITH AUTHIGENIC XTALS OF? | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
282.08 | 53-418B-31-1,18 | 0 | 15 | 85 | Lower cretaceous | NANNO OOZE | relative abundance | 30 | 0 | 30 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
282.78 | 53-418B-31-1,88 | 0 | 30 | 70 | Lower cretaceous | OPAL RICH CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
282.94 | 53-418B-31-11,104 | 0 | 20 | 80 | Lower cretaceous | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
284.14 | 53-418B-31-2,74 | 10 | 40 | 50 | Lower cretaceous | BLACK RAD CLAY | numerical abundance | 0 | 0 | 13 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 7 | 8 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
284.36 | 53-418B-31-2,96 | 0 | 10 | 90 | Lower cretaceous | BLACK CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 70 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
284.57 | 53-418B-31-21,117 | 0 | 15 | 85 | Lower cretaceous | RAD BEARING PELAGIC CLAY | relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 80 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
284.58 | 53-418B-31-21,118 | 40 | 40 | 20 | Lower cretaceous | RADIOLARITE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
291.63 | 53-418B-32-1,23 | 0 | 0 | 0 | Lower cretaceous | NANNOCHALK | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
292.01 | 53-418B-32-1,61 | 0 | 0 | 0 | Lower cretaceous | NANNO CHALK | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
292.07 | 53-418B-32-1,67 | 0 | 0 | 0 | Lower cretaceous | NANNO CHALK | Dominat lithology; numerical abundance | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
292.49 | 53-418B-32-11,109 | 0 | 0 | 0 | Lower cretaceous | (FORAM) RAD-NANNO CHALK | Minor lithology; numerical abundance | 0 | 0 | 75 | 5 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
292.58 | 53-418B-32-11,118 | 0 | 0 | 0 | Lower cretaceous | (REDDISH) NANNO CHALK | Dominat lithology; numerical abundance | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
292.60 | 53-418B-32-11,120 | 0 | 15 | 80 | Lower cretaceous | RED NANNO CLAY | Minor lithology; numerical abundance | 0 | 0 | 28 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
301.28 | 53-418B-33-1,28 | 0 | 15 | 80 | Lower cretaceous | RED-BRN CLAY | Minor lithology; numerical abundance | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 8 |
301.29 | 53-418B-33-1,29 | 10 | 40 | 50 | Lower cretaceous | NANNO CLAY (MARL) | Minor lithology; numerical abundance | 0 | 0 | 30 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.30 | 53-418B-33-1,30 | 30 | 15 | 30 | Lower cretaceous | RAD CLAY | Minor lithology; numerical abundance | 2 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 8 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
301.32 | 53-418B-33-1,32 | 5 | 25 | 70 | Lower cretaceous | RAD SILICEOUS CLAYSTONE | numerical abundance | 5 | 0 | 1 | 0 | 25 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.51 | 53-418B-33-1,51.5 | 0 | 0 | 0 | Lower cretaceous | NANNO CLAY | Minor lithology; relative abundance | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 2 | 75 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
301.57 | 53-418B-33-1,57 | 0 | 0 | 0 | Lower cretaceous | BLACK NANNO CHALK TO MARL | Minor lithology; numerical abundance | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.60 | 53-418B-33-1,60 | 0 | 0 | 0 | Lower cretaceous | BLACK NANNO MARL | Minor lithology; numerical abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.72 | 53-418B-33-1,72 | 0 | 0 | 0 | Lower cretaceous | NANNO CHALK | numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.96 | 53-418B-33-1,96 | 0 | 0 | 0 | Lower cretaceous | RAD NANNO CHALK | Minor lithology; numerical abundance | 0 | 0 | 60 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
302.18 | 53-418B-33-11,118 | 0 | 0 | 0 | Lower cretaceous | NANNO CHALK | Minor lithology; relative abundance | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.52 | 53-418B-34-1,2 | 0 | 5 | 95 | Lower cretaceous | NANNO MARL (CHALK) AND CLAY | numerical abundance | 0 | 0 | 60 | 0 | 0 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.61 | 53-418B-34-1,11 | 0 | 50 | 50 | Lower cretaceous | COARSE IN BLACK CLAY | Minor lithology; relative abundance | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 15 | 30 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.63 | 53-418B-34-1,13 | 60 | 30 | 10 | Lower cretaceous | SILIC RAD SAND | Minor lithology; relative abundance | 2 | 0 | 2 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.66 | 53-418B-34-1,16 | 0 | 40 | 60 | Lower cretaceous | ORG NANNO CLAY MARL | Minor lithology; numerical abundance | 0 | 0 | 60 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.71 | 53-418B-34-1,21 | 10 | 50 | 40 | Lower cretaceous | ORG CLAY | Dominat lithology; numerical abundance | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 5 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.76 | 53-418B-34-1,26 | 0 | 20 | 80 | Lower cretaceous | NANNO MARL | Minor lithology; numerical abundance | 15 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 10 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
310.94 | 53-418B-34-1,44 | 0 | 50 | 50 | Lower cretaceous | SILICEOUS (RAD) CLAY | Minor lithology; numerical abundance | 0 | 0 | 2 | 0 | 0 | 30 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 15 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |