Donelly, Thomas W; Bryan, Wilfred B; Flower, Martin F J (2005): Smear slide analysis of Hole 52-418A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230790
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 (1980): Initial Reports of the Deep Sea Drilling Project. 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: 25.035000 * Longitude: -68.057300
Date/Time Start: 1977-02-10T00:00:00 * Date/Time End: 1977-02-10T00:00:00
Minimum DEPTH, sediment/rock: 111.50 m * Maximum DEPTH, sediment/rock: 329.60 m
Event(s):
52-418A * Latitude: 25.035000 * Longitude: -68.057300 * Date/Time: 1977-02-10T00:00:00 * Elevation: -5511.0 m * Penetration: 570.5 m * Recovery: 205.5 m * Location: North Atlantic/CONT RISE * Campaign: Leg52 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 48 cores; 374 m cored; 0 m drilled; 54.9 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Sand | Sand | % | Smear slide analysis | ||
4 | Silt | Silt | % | Smear slide analysis | ||
5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
6 | Stratigraphy | Stratigraphy | Smear slide analysis | |||
7 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
8 | Comment | Comment | Smear slide analysis | |||
9 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Nannofossils | Nannos | % | Smear slide analysis | ||
11 | Foraminifera | Foram | % | Smear slide analysis | ||
12 | Siliceous microfossils | Silic foss | % | Smear slide analysis | other siliceous material | |
13 | Chert | Chert | % | Smear slide analysis | fragments | |
14 | Radiolarians | Rad | % | Smear slide analysis | ||
15 | Diatoms | Diatoms | % | Smear slide analysis | ||
16 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
17 | Spiculae | Spiculae | % | Smear slide analysis | ||
18 | Collophane | Collophane | % | Smear slide analysis | ||
19 | Barite | Brt | % | Smear slide analysis | ||
20 | Quartz | Qz | % | Smear slide analysis | ||
21 | Feldspar | Fsp | % | Smear slide analysis | ||
22 | Zeolite | Zeo | % | Smear slide analysis | ||
23 | Mica | Mica | % | Smear slide analysis | ||
24 | Biotite | Bt | % | 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 | Zircon | Zrn | % | Smear slide analysis | ||
32 | Hornblende | Hbl | % | Smear slide analysis | ||
33 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
34 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4195 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 Chert [%] | 14 Rad [%] | 15 Diatoms [%] | 16 Silicoflag [%] | 17 Spiculae [%] | 18 Collophane [%] | 19 Brt [%] | 20 Qz [%] | 21 Fsp [%] | 22 Zeo [%] | 23 Mica [%] | 24 Bt [%] | 25 Clay min [%] | 26 Glt [%] | 27 Opaque [%] | 28 Py [%] | 29 Fe [%] | 30 HM [%] | 31 Zrn [%] | 32 Hbl [%] | 33 Volc glass [%] | 34 Minerals [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
111.50 | 52-418A-1-1,50 | 0 | 10 | 90 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 90 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
111.68 | 52-418A-1-1,68 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 5 | 0 | 0 | 84 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | |
111.80 | 52-418A-1-1,80 | 0 | 10 | 90 | PEL. CLAY (ZEOL RICH) | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 83 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
112.52 | 52-418A-1-2,2 | 0 | 90 | 10 | VITRIC-CRYSTAL ASH-DEVITRIFIED CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 98 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 0 | |
113.00 | 52-418A-1-2,50 | 0 | 10 | 90 | ZEOLITE RICH PELAGIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 2 | 0 | 68 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | |
113.11 | 52-418A-1-2,61 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 90 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
113.43 | 52-418A-1-2,93 | 0 | 10 | 90 | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 89 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 5 | |
114.75 | 52-418A-1-3,75 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 95 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
115.49 | 52-418A-1-CC,10 | 0 | 10 | 90 | BLUE PELAGIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 5 | 2 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
115.50 | 52-418A-1-CC,11 | 0 | 15 | 85 | NOT NAMED | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 93 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
121.21 | 52-418A-2-1,71 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 93 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | |
121.95 | 52-418A-2-11,145 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
122.57 | 52-418A-2-CC,0 | 0 | 0 | 0 | NO NAME | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 94 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | |
130.75 | 52-418A-3-1,75 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
131.21 | 52-418A-3-11,121 | 0 | 5 | 95 | PEL. CLAY | Minor lithology; relative abundance | 1 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 88 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
132.19 | 52-418A-3-2,69 | 0 | 10 | 90 | PEL. CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | |
132.83 | 52-418A-3-21,133 | 0 | 10 | 90 | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 94 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | ||
133.75 | 52-418A-3-3,75 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | |
134.40 | 52-418A-3-31,140 | 0 | 10 | 90 | PEL. CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
136.10 | 52-418A-3-5,10 | 0 | 10 | 90 | PEL. CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 96 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
136.75 | 52-418A-3-5,75 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
137.61 | 52-418A-3-6,11 | 0 | 10 | 90 | BLUE (PEL. CLAY?) | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 2 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
138.25 | 52-418A-3-6,75 | 0 | 0 | 95 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
138.26 | 52-418A-3-6,75 | 0 | 10 | 90 | BROWN PELAGIC CLAY | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
139.53 | 52-418A-3-CC,0 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 94 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | |
140.25 | 52-418A-4-1,75 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 93 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | |
145.90 | 52-418A-4-5,40 | 0 | 0 | 95 | PEL. CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
146.10 | 52-418A-4-5,60 | 0 | 10 | 90 | PEL. CLAY | Minor lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 91 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
146.34 | 52-418A-4-CC,0 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | |
151.55 | 52-418A-5-21,105 | 0 | 0 | 100 | PELAGIC CLAY | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 95 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
151.95 | 52-418A-5-21,145 | 0 | 0 | 100 | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 98 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
153.78 | 52-418A-5-4,28 | 0 | 0 | 100 | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
154.47 | 52-418A-5-4,97 | 0 | 0 | 100 | (CLAY?) | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
156.00 | 52-418A-5-51,100 | 0 | 0 | 100 | ZEOLITE CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 36 | 0 | 0 | 58 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | |
156.35 | 52-418A-5-51,135 | 0 | 0 | 100 | (CLAY?) | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
156.74 | 52-418A-5-CC,0 | 0 | 0 | 100 | ZEOLITIC BROWN CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 93 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
156.74 | 52-418A-5-CC,0 | 0 | 0 | 100 | ZEOLITIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
159.00 | 52-418A-6-1,50 | 0 | 0 | 100 | Middle eocene | V.SPARSELY RAD. PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 96 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
159.50 | 52-418A-6-11,100 | 0 | 2 | 98 | Middle eocene | RADIOLARIAN-RICH CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
159.96 | 52-418A-6-11,146 | 0 | 30 | 70 | Middle eocene | PELAGIC CLAY OR RADIOLARIAN OOZE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
160.62 | 52-418A-6-2,62 | 0 | 7 | 93 | Middle eocene | RAD. RICH CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
161.06 | 52-418A-6-21,106 | 0 | 15 | 85 | Middle eocene | RAD.-RICH CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 83 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
162.18 | 52-418A-6-3,68 | 10 | 10 | 80 | Middle eocene | RADIOLARIAN RICH CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
162.79 | 52-418A-6-31,129 | 0 | 0 | 100 | Middle eocene | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
163.45 | 52-418A-6-4,45 | 0 | 10 | 90 | Middle eocene | PEL.CLAY CONT. FINE PIECES OF RAD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
164.71 | 52-418A-6-5,21 | 1 | 1 | 98 | Middle eocene | PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
164.98 | 52-418A-6-CC,0 | 1 | 0 | 99 | Middle eocene | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
164.98 | 52-418A-6-CC,0 | 1 | 0 | 99 | Middle eocene | PELAGIC MUD | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
168.82 | 52-418A-7-1,82 | 0 | 2 | 98 | Middle eocene | ZEOLITIC-RICH (?) CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 91 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
169.94 | 52-418A-7-2,44 | 0 | 2 | 98 | Middle eocene | (ZEOLITIC) PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 4 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
170.41 | 52-418A-7-2,91 | 1 | 1 | 98 | Middle eocene | ZEOLITIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 90 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
172.61 | 52-418A-7-4,11 | 0 | 0 | 100 | Middle eocene | ZEOLITIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
173.27 | 52-418A-7-4,77 | 0 | 1 | 99 | Middle eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 90 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
174.53 | 52-418A-7-5,53 | 0 | 0 | 100 | Middle eocene | ZEOLITE CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
174.89 | 52-418A-7-5,89 | 0 | 0 | 100 | Middle eocene | ZEOLITIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 80 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
176.00 | 52-418A-7-6,50 | 0 | 3 | 97 | Middle eocene | ZEOLITIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
176.38 | 52-418A-7-CC,0 | 0 | 0 | 100 | Middle eocene | RAD.-RICH PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 90 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
176.38 | 52-418A-7-CC,0 | 0 | 0 | 100 | Middle eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
197.65 | 52-418A-8-11,115 | 0 | 10 | 90 | PEL. CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 5 | 0 | 0 | 72 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | |
197.78 | 52-418A-8-11,128 | 0 | 5 | 95 | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | ||
198.00 | 52-418A-8-11,150 | 0 | 0 | 90 | CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 93 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
198.10 | 52-418A-8-CC,0 | 0 | 1 | 99 | (ZEOLITIC) PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 100 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | |
198.10 | 52-418A-8-CC,0 | 0 | 1 | 99 | PELAGIC CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 0 | 97 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | |
234.56 | 52-418A-9-CC,6 | 0 | 10 | 90 | (?) ORG. RICH CLAY | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 78 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
234.58 | 52-418A-9-CC,8 | 0 | 5 | 95 | GREEN(?) CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 95 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
234.60 | 52-418A-9-CC,0 | 0 | 0 | 0 | BROWN SILIC CLAY/CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 45 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
234.60 | 52-418A-9-CC,0 | 0 | 0 | 0 | SILIC. CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
234.60 | 52-418A-9-CC,0 | 0 | 10 | 90 | SILIC. CLAYSTONE TO CHERT | Minor lithology; relative abundance | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
234.64 | 52-418A-9-CC,14 | 0 | 0 | 0 | GREY(?) CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 92 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
272.58 | 52-418A-10-1,8 | 0 | 5 | 95 | Cretaceous | GREEN CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
272.84 | 52-418A-10-1,34 | 0 | 20 | 80 | Cretaceous | CLAY (OLIVE GREY) W/NANNOS | Dominat lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 85 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.03 | 52-418A-10-1,53 | 0 | 5 | 95 | Cretaceous | BROWN NANNO CLAY | numerical abundance | 0 | 40 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 38 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 |
273.37 | 52-418A-10-1,87 | 0 | 50 | 50 | Cretaceous | BLACK TO BROWN CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.40 | 52-418A-10-1,90 | 0 | 50 | 50 | Cretaceous | BROWNISH (0.5 CM) LAYER CLAY | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 56 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.48 | 52-418A-10-1,98 | 0 | 60 | 40 | Cretaceous | BROWN CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 65 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
274.12 | 52-418A-10-2,12 | 0 | 1 | 99 | Cretaceous | GREEN CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
274.27 | 52-418A-10-2,27 | 0 | 5 | 95 | Cretaceous | YELLOW GREEN (CLAY?) | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 90 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
274.48 | 52-418A-10-CC,5 | 1 | 4 | 95 | Cretaceous | CLAY (GREEN) | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
274.53 | 52-418A-10-CC,0 | 50 | 40 | 10 | Cretaceous | RADIOLARITE CLAYEY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
274.63 | 52-418A-10-CC,20 | 0 | 10 | 50 | Cretaceous | BROWN CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
274.63 | 52-418A-10-CC,20 | 0 | 10 | 90 | Cretaceous | CLAY (BLACK) | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 87 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
274.63 | 52-418A-10-CC,20 | 0 | 50 | 90 | Cretaceous | CLAY (GREY),SILIC? | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
282.10 | 52-418A-11-CC,0 | 0 | 0 | 0 | DARK SILIC. CLAY? (SILIC RADS) | numerical abundance | 0 | 0 | 0 | 25 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
282.10 | 52-418A-11-CC,0 | 0 | 5 | 95 | GREEN CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
282.20 | 52-418A-11-CC,20 | 0 | 50 | 50 | NANNO CLAY (GREEN) | numerical abundance | 0 | 50 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
291.62 | 52-418A-12-1,10 | 0 | 0 | 0 | Lower cretaceous | CHERT CLAYEY | Dominat lithology; numerical abundance | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
291.88 | 52-418A-12-1,35 | 0 | 1 | 99 | Lower cretaceous | CLAYEY N.O. | Dominat lithology; relative abundance | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
292.10 | 52-418A-12-1,60 | 0 | 20 | 80 | Lower cretaceous | DARK GREEN CLAY | Dominat lithology; relative abundance | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 8 | 0 | 70 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
292.28 | 52-418A-12-1,78 | 0 | 10 | 90 | Lower cretaceous | OLIVE GREEN NANNO RICH CLAY | Dominat lithology; relative abundance | 0 | 26 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
292.49 | 52-418A-12-1,99 | 0 | 10 | 90 | Lower cretaceous | NANNO-RICH CLAY TO NANNO OOZE | Dominat lithology; numerical abundance | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
292.99 | 52-418A-12-11,149 | 0 | 0 | 100 | Lower cretaceous | TAN CLAY (N. OOZE) | Minor lithology; relative abundance | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
293.21 | 52-418A-12-2,21 | 0 | 0 | 100 | Lower cretaceous | LT. RAD RICH CLAY-N.O. | Dominat lithology; numerical abundance | 0 | 40 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
293.30 | 52-418A-12-2,30 | 0 | 0 | 95 | Lower cretaceous | DK. BROWN CLAY N.O. | Dominat lithology; numerical abundance | 2 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
293.30 | 52-418A-12-2,30 | 0 | 0 | 99 | Lower cretaceous | LT. BROWN CLAY N.O. | Dominat lithology; numerical abundance | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
293.41 | 52-418A-12-CC,6 | 0 | 0 | 100 | Lower cretaceous | PINK CLAY N.O. | Minor lithology; relative abundance | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
293.44 | 52-418A-12-CC,9 | 0 | 0 | 99 | Lower cretaceous | CLAY N.O. | Dominat lithology; numerical abundance | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
293.45 | 52-418A-12-CC,10 | 0 | 0 | 100 | Lower cretaceous | N. OOZE | Dominat lithology; numerical abundance | 0 | 60 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
293.48 | 52-418A-12-CC,13 | 0 | 0 | 0 | Lower cretaceous | BROWN FE CLAY N.O. | Minor lithology; relative abundance | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
293.51 | 52-418A-12-CC,16 | 0 | 0 | 100 | Lower cretaceous | DK. GREEN CLAYEY N.O. | Minor lithology; numerical abundance | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.30 | 52-418A-13-1,30 | 0 | 0 | 100 | Lower cretaceous | NANNO OOZE TO NANNO-RICH CLAY | Minor lithology; numerical abundance | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.44 | 52-418A-13-1,44 | 0 | 5 | 95 | Lower cretaceous | NANNO RICH CLAY | Minor lithology; relative abundance | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
301.60 | 52-418A-13-1,60 | 0 | 10 | 90 | Lower cretaceous | NANNO OOZE | Minor lithology; relative abundance | 2 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.77 | 52-418A-13-1,77 | 0 | 0 | 0 | Lower cretaceous | NANNO RICH CLAY TO NANNO OOZE | Dominat lithology; relative abundance | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.81 | 52-418A-13-1,81 | 0 | 25 | 75 | Lower cretaceous | YELLOW CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.84 | 52-418A-13-1,84 | 0 | 15 | 85 | Lower cretaceous | GREEN MUD | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 95 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
301.93 | 52-418A-13-1,93 | 0 | 10 | 90 | Lower cretaceous | NANNO-RICH CLAY | Minor lithology; relative abundance | 2 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
303.49 | 52-418A-13-2,99 | 0 | 0 | 0 | Lower cretaceous | LIGHT GREY CLAY | Minor lithology; relative abundance | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
303.50 | 52-418A-13-21,100 | 0 | 20 | 80 | Lower cretaceous | DARK CLAY | Minor lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 2 | 2 | 0 | 75 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
303.58 | 52-418A-13-21,108 | 0 | 0 | 100 | Lower cretaceous | GREEN CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 95 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
303.94 | 52-418A-13-CC,9 | 1 | 14 | 85 | Lower cretaceous | BROWN CLAY | Minor lithology; numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
303.95 | 52-418A-13-CC,0 | 30 | 20 | 50 | Lower cretaceous | BRIGHT GREEN RAD RICH CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 76 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
303.98 | 52-418A-13-CC,13 | 0 | 0 | 0 | Lower cretaceous | CLAYEY N.O. | Minor lithology; numerical abundance | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 68 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
304.00 | 52-418A-13-CC,15 | 0 | 10 | 90 | Lower cretaceous | GREY CLAY NANNO OOZE | Minor lithology; numerical abundance | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 30 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.60 | 52-418A-14-CC,0 | 0 | 0 | 0 | Lower cretaceous | N. OOZE OR NANNO-RICH CLAY | Dominat lithology; numerical abundance | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 20 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.60 | 52-418A-14-CC,0 | 0 | 0 | 100 | Lower cretaceous | NANNO OOZE,SOFT OOZE | Minor lithology; relative abundance | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.64 | 52-418A-14-CC,14 | 0 | 0 | 0 | Lower cretaceous | LT. GREEN CLAY RICH N.O. | Minor lithology; numerical abundance | 0 | 68 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
320.05 | 52-418A-15-1,5 | 0 | 0 | 0 | Lower aptian | BASALT CONTACT-NANNO CLAY | Dominat lithology; numerical abundance | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 10 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
320.15 | 52-418A-15-1,15 | 0 | 20 | 75 | Lower aptian | BASALT CONTACT-CLAY NANNO CHALK | Dominat lithology; numerical abundance | 1 | 40 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 1 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
320.15 | 52-418A-15-1,15 | 0 | 25 | 80 | Lower aptian | BASALT CONTACT-CLAYEY NANNO CHALK | Minor lithology; relative abundance | 0 | 47 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 3 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
320.19 | 52-418A-15-1,19 | 0 | 30 | 70 | Lower aptian | BASALT CONTACT-NANNO CLAY | Dominat lithology; relative abundance | 0 | 28 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 1 | 28 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
321.66 | 52-418A-15-2,16 | 0 | 10 | 90 | INTERBED,CLAYEY CHALK | Dominat lithology; numerical abundance | 0 | 68 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | |
322.47 | 52-418A-15-2,97 | 2 | 10 | 88 | INTERBED,CLAYEY CHALK | Dominat lithology; relative abundance | 5 | 64 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
323.90 | 52-418A-15-3,90 | 0 | 10 | 90 | INTERBED CLAY NANNO CHALK | Dominat lithology; relative abundance | 0 | 63 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | |
324.94 | 52-418A-15-4,44 | 0 | 0 | 0 | MARL CLAYEY | Dominat lithology; numerical abundance | 25 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
324.95 | 52-418A-15-4,45 | 20 | 50 | 30 | SILTY CLAYSTONE-ALTERED | Dominat lithology; numerical abundance | 20 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
325.03 | 52-418A-15-4,53 | 5 | 10 | 85 | INTERBED-GLAUCONITE? CO3 CLAY | Dominat lithology; relative abundance | 35 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
329.55 | 52-418A-16-1,5 | 50 | 30 | 20 | INTERBED | Dominat lithology; relative abundance | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 40 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | |
329.60 | 52-418A-16-1,10 | 0 | 0 | 0 | INTERBED | Dominat lithology; numerical abundance | 15 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 75 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
329.60 | 52-418A-16-1,10 | 5 | 20 | 75 | INTERBED | Dominat lithology; relative abundance | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |