Anonymous (2005): Smear slide analysis of Hole 2-12C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230448
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
von der Borch, Christopher C; Nigrini, Catherine A; Goll, Robert M; Gartner, Stefan; Cita, Maria Bianca; Edgar, Terence; Peterson, Melvin N A (1969): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, II, 999 pp, https://doi.org/10.2973/dsdp.proc.2.1970
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 19.695000 * Longitude: -26.000000
Date/Time Start: 1968-11-16T00:00:00 * Date/Time End: 1968-11-16T00:00:00
Minimum DEPTH, sediment/rock: 1.50 m * Maximum DEPTH, sediment/rock: 107.20 m
Event(s):
2-12C * Latitude: 19.695000 * Longitude: -26.000000 * Date/Time: 1968-11-16T00:00:00 * Elevation: -4557.0 m * Penetration: 114.9 m * Recovery: 29.7 m * Location: North Atlantic/BASIN * Campaign: Leg2 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 100.6 m cored; 9.1 m drilled; 29.5 % 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 | Quartz | Qz | % | Smear slide analysis | ||
14 | Feldspar | Fsp | % | Smear slide analysis | ||
15 | Zeolite | Zeo | % | Smear slide analysis | ||
16 | Clay minerals | Clay min | % | Smear slide analysis | ||
17 | Opaque minerals | Opaque | % | Smear slide analysis | ||
18 | Zircon | Zrn | % | Smear slide analysis | ||
19 | Tourmaline | Tur | % | Smear slide analysis | ||
20 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
21 | Pumice | Pumice | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1380 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 Qz [%] | 14 Fsp [%] | 15 Zeo [%] | 16 Clay min [%] | 17 Opaque [%] | 18 Zrn [%] | 19 Tur [%] | 20 Volc glass [%] | 21 Pumice [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.50 | 2-12C-1-11,150 | 0 | 80 | 20 | Pleistocene | FORAMINIFERAL COCCOLITH CHALK OOZE WITH ?QTZ FELDSPAR MINOR ZEOLITE | Dominat lithology; numerical abundance | 0 | 0 | 15 | 65 | 15 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
3.00 | 2-12C-1-21,150 | 5 | 70 | 25 | Pleistocene | FORAMINIFERAL COCCOLITH CHALK OOZE WITH ?ZEOLITES AND DETRITAL OOZE | Dominat lithology; relative abundance | 0 | 0 | 22 | 55 | 13 | 0 | 5 | 0 | 0 | 0 | 1 | 0 | 0 |
4.50 | 2-12C-1-31,150 | 5 | 70 | 25 | Pleistocene | FORAMINIFERAL COCCOLITH CHALK OOZE WITH ?QTZ AND ?ZEOLITE | Dominat lithology; relative abundance | 0 | 1 | 25 | 70 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.00 | 2-12C-1-41,150 | 0 | 70 | 30 | Pleistocene | FORAMINIFERAL-COCCOLITH CHALK OOZE WITH SILTY DETRITUS | Dominat lithology; numerical abundance | 0 | 1 | 25 | 49 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
15.80 | 2-12C-2-11,150 | 0 | 60 | 40 | Pleistocene | FORAMINIFERAL NANNOFOSSIL CHALK OOZE | Dominat lithology; relative abundance | 10 | 0 | 42 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
17.30 | 2-12C-2-21,150 | 0 | 70 | 30 | Pleistocene | FORAMINIFERAL NANNOFOSSIL CHALK OOZE | Dominat lithology; relative abundance | 10 | 0 | 32 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
18.80 | 2-12C-2-31,150 | 0 | 70 | 30 | Pleistocene | FORAMINIFERAL COCCOLITH OOZE WITH ZZEOLITES AND/OR FELDSPAR | Dominat lithology; numerical abundance | 0 | 1 | 25 | 55 | 0 | 15 | 10 | 5 | 0 | 0 | 0 | 0 | 0 |
18.80 | 2-12C-2-31,150 | 0 | 70 | 30 | Pleistocene | FORAMINIFERAL NANNOFOSSIL FELDSPATHIC? CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 25 | 58 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
33.06 | 2-12C-4-1,46 | 0 | 60 | 40 | Pliocene | FORAMINIFERAL NANNOFOSSIL CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 30 | 60 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 |
33.20 | 2-12C-4-1,60 | 0 | 60 | 40 | Pliocene | FORAMINIFERAL NANNOFOSSIL CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 30 | 60 | 0 | 0 | 1 | 10 | 0 | 0 | 0 | 0 | 0 |
33.36 | 2-12C-4-1,76 | 0 | 70 | 30 | Pliocene | FORAM NANNOFOSSIL CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 25 | 65 | 0 | 3 | 2 | 5 | 0 | 0 | 0 | 0 | 0 |
33.50 | 2-12C-4-1,90 | 0 | 70 | 30 | Pliocene | FORAM NANNOFOSSIL OOZE SLIGHTLY SOLOMITIC | Dominat lithology; numerical abundance | 0 | 0 | 25 | 54 | 0 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
33.65 | 2-12C-4-11,105 | 0 | 50 | 50 | Pliocene | FORAM NANNOFOSSIL MARL OOZE WITH ?FELDSPAR | Dominat lithology; numerical abundance | 0 | 0 | 45 | 45 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
34.14 | 2-12C-4-2,4 | 0 | 60 | 40 | Pliocene | FELDSPATHIC? FORAM COCCOLITH MARL OOZE | Dominat lithology; numerical abundance | 0 | 1 | 30 | 20 | 0 | 20 | 10 | 10 | 0 | 0 | 0 | 0 | 10 |
34.43 | 2-12C-4-2,33 | 0 | 60 | 40 | Pliocene | FELDSPATHIC? FORAM COCCOLITH MARL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 30 | 20 | 0 | 20 | 10 | 10 | 0 | 0 | 0 | 0 | 10 |
34.59 | 2-12C-4-2,49 | 0 | 60 | 40 | Pliocene | FELDSPATHIC FORAM COCCOLITH MARL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 30 | 20 | 0 | 20 | 10 | 10 | 0 | 0 | 0 | 0 | 10 |
35.45 | 2-12C-4-21,135 | 0 | 60 | 40 | Pliocene | FELDSPATHIC FORAM COCCOLITH MARL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 30 | 20 | 0 | 20 | 10 | 10 | 0 | 0 | 0 | 0 | 10 |
35.73 | 2-12C-4-3,13 | 0 | 100 | 0 | Pliocene | NANNOFOSSIL CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 85 | 10 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
35.95 | 2-12C-4-3,35 | 0 | 75 | 25 | Pliocene | VOLCANIC SILTY MUD | Dominat lithology; relative abundance | 0 | 0 | 3 | 0 | 0 | 1 | 70 | 25 | 0 | 0 | 0 | 5 | 0 |
35.98 | 2-12C-4-3,38 | 0 | 5 | 95 | Pliocene | PHILLIPCITIC SILTY MUD | Dominat lithology; relative abundance | 0 | 0 | 2 | 1 | 0 | 0 | 60 | 35 | 0 | 0 | 0 | 5 | 0 |
36.25 | 2-12C-4-3,65 | 5 | 75 | 20 | Pliocene | NANNOFOSSIL CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 75 | 5 | 1 | 1 | 10 | 10 | 0 | 0 | 0 | 0 | 0 |
36.32 | 2-12C-4-3,72 | 20 | 60 | 20 | Pliocene | NANNOFOSSIL CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 42 | 20 | 1 | 0 | 20 | 20 | 0 | 0 | 0 | 0 | 0 |
36.36 | 2-12C-4-3,76 | 0 | 30 | 70 | Pliocene | ZEOLITIC SILTY MUD | Dominat lithology; relative abundance | 0 | 0 | 2 | 1 | 0 | 0 | 45 | 45 | 0 | 0 | 0 | 10 | 0 |
36.38 | 2-12C-4-3,78 | 0 | 30 | 70 | Pliocene | ZEOLITIC SILTY MUD | Dominat lithology; relative abundance | 0 | 0 | 6 | 1 | 0 | 0 | 45 | 50 | 0 | 0 | 0 | 0 | 0 |
36.51 | 2-12C-4-3,91 | 0 | 75 | 25 | Pliocene | ZEOLITIC SILTY MUD | Dominat lithology; relative abundance | 0 | 0 | 3 | 1 | 0 | 0 | 25 | 25 | 0 | 0 | 0 | 50 | 0 |
36.80 | 2-12C-4-31,120 | 0 | 50 | 50 | Pliocene | ALTERED VOLCANIC ASH ZEOLITIC SILTY MUD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 50 | 0 | 0 | 0 | 35 | 0 |
43.09 | 2-12C-5-11,129 | 0 | 40 | 60 | Tertiary | ZEOLITIC NANNOFOSSIL FORAM CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 25 | 20 | 0 | 0 | 20 | 5 | 0 | 1 | 0 | 0 | 0 |
43.15 | 2-12C-5-11,135 | 0 | 80 | 20 | Tertiary | FELDSPATHIC COCCOLITH MARL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 15 | 5 | 0 | 70 | 5 | 5 | 0 | 0 | 0 | 0 | 0 |
43.29 | 2-12C-5-11,149 | 0 | 90 | 10 | Tertiary | FELDSPATHIC SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 10 | 80 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
43.60 | 2-12C-5-2,30 | 0 | 90 | 10 | Tertiary | ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 20 | 70 | 10 | 0 | 0 | 0 | 0 | 0 |
43.74 | 2-12C-5-2,44 | 0 | 0 | 0 | Tertiary | VOLCANIC ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
43.90 | 2-12C-5-2,60 | 0 | 95 | 5 | Tertiary | ZEOLITIC SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 4 | 90 | 5 | 0 | 1 | 0 | 0 | 0 |
44.03 | 2-12C-5-2,73 | 0 | 95 | 5 | Tertiary | ZEOLITIC SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 4 | 90 | 5 | 0 | 1 | 0 | 0 | 0 |
44.70 | 2-12C-5-21,140 | 0 | 95 | 5 | Tertiary | ZEOLITIC SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 4 | 90 | 5 | 0 | 1 | 0 | 0 | 0 |
45.48 | 2-12C-5-3,68 | 0 | 80 | 20 | Tertiary | ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 79 | 20 | 0 | 1 | 0 | 0 | 0 |
45.56 | 2-12C-5-3,76 | 0 | 90 | 10 | Tertiary | ZEOLITIC-FELDSPATHIC SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 9 | 80 | 10 | 0 | 1 | 0 | 0 | 0 |
51.90 | 2-12C-6-11,100 | 0 | 80 | 20 | Tertiary | ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 20 | 0 | 0 | 0 | 0 | 0 |
52.13 | 2-12C-6-11,123 | 0 | 80 | 20 | Tertiary | ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 20 | 0 | 0 | 0 | 0 | 0 |
52.23 | 2-12C-6-11,133 | 0 | 60 | 40 | Tertiary | FELDSPATHIC ZEOLITE CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 20 | 60 | 20 | 0 | 0 | 0 | 0 | 0 |
52.33 | 2-12C-6-11,143 | 0 | 50 | 50 | Tertiary | FELDSPAR-ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 40 | 55 | 5 | 0 | 0 | 0 | 0 | 0 |
52.61 | 2-12C-6-2,21 | 0 | 70 | 30 | Tertiary | ZEOLITE (FELDSPATHIC?) CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 20 | 50 | 30 | 0 | 0 | 0 | 0 | 0 |
52.69 | 2-12C-6-2,29 | 0 | 70 | 30 | Tertiary | ZEOLITE CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 65 | 15 | 0 | 0 | 0 | 20 | 0 |
52.74 | 2-12C-6-2,34 | 0 | 80 | 20 | Tertiary | ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 20 | 0 | 0 | 0 | 0 | 0 |
53.66 | 2-12C-6-21,126 | 0 | 0 | 0 | Tertiary | MANGANIFEROUS ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
60.30 | 2-12C-7-1,20 | 0 | 80 | 20 | Tertiary | ZEOLITE CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 20 | 0 | 0 | 0 | 0 | 0 |
60.40 | 2-12C-7-1,30 | 0 | 70 | 30 | Tertiary | ZEOLITE CLAYEY SILT | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 1 | 70 | 30 | 0 | 1 | 0 | 0 | 0 |
69.92 | 2-12C-8-1,72 | 0 | 80 | 20 | Tertiary | ZEOLITE CLAYEY SILT | Dominat lithology; relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 80 | 20 | 1 | 0 | 0 | 0 | 0 |
79.46 | 2-12C-9-11,106 | 0 | 70 | 30 | Tertiary | ZEOLITIC SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 1 | 0 |
79.55 | 2-12C-9-11,115 | 0 | 70 | 30 | Tertiary | ZEOLITIC SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 1 | 0 |
79.70 | 2-12C-9-11,130 | 0 | 70 | 30 | Tertiary | ZEOLITIC SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 1 | 0 |
79.85 | 2-12C-9-11,145 | 0 | 70 | 30 | Tertiary | ZEOLITIC SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 1 | 0 |
79.95 | 2-12C-9-2,5 | 0 | 80 | 20 | Tertiary | CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 |
80.18 | 2-12C-9-2,28 | 0 | 50 | 50 | Tertiary | CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 |
80.60 | 2-12C-9-2,70 | 0 | 70 | 30 | Tertiary | CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 |
81.13 | 2-12C-9-21,123 | 0 | 90 | 10 | Tertiary | CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 |
81.37 | 2-12C-9-21,147 | 0 | 80 | 20 | Tertiary | CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 |
87.50 | 2-12C-10-1,0 | 0 | 30 | 70 | Tertiary | ZEOLITIC SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 45 | 0 | 0 | 0 | 5 | 0 |
88.47 | 2-12C-10-1,97 | 0 | 25 | 75 | Tertiary | VOLCANIC ZEOLITIC MUD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 50 | 0 | 0 | 0 | 5 | 0 |
88.54 | 2-12C-10-11,104 | 0 | 25 | 75 | Tertiary | VOLCANIC ZEOLITIC SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 50 | 0 | 0 | 0 | 0 | 0 |
97.16 | 2-12C-11-1,56 | 0 | 80 | 20 | Tertiary | ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 20 | 0 | 0 | 0 | 0 | 0 |
97.50 | 2-12C-11-1,90 | 0 | 60 | 40 | Tertiary | ALTERED PYROCLASTIC GLASS AND ZEOLITE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 50 | 40 | 0 | 0 | 0 | 0 | 0 |
97.64 | 2-12C-11-11,104 | 0 | 70 | 30 | Tertiary | ZEOLITE CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 15 | 55 | 30 | 0 | 0 | 0 | 0 | 0 |
97.97 | 2-12C-11-11,137 | 0 | 0 | 0 | Tertiary | QTZ-FELDSPATHIC SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
98.00 | 2-12C-11-11,140 | 0 | 80 | 20 | Tertiary | ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
106.60 | 2-12C-12-1,80 | 0 | 60 | 40 | Tertiary | CLAYEY ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 5 | 55 | 40 | 0 | 0 | 0 | 0 | 0 |
106.70 | 2-12C-12-1,90 | 0 | 60 | 40 | Tertiary | CLAYEY ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 5 | 55 | 40 | 0 | 0 | 0 | 0 | 0 |
106.94 | 2-12C-12-11,114 | 0 | 100 | 0 | Tertiary | FELDSPAR SILT | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 1 | 1 | 0 | 0 |
107.10 | 2-12C-12-11,130 | 0 | 70 | 30 | Tertiary | ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 30 | 0 | 0 | 0 | 0 | 0 |
107.20 | 2-12C-12-11,140 | 0 | 60 | 40 | Tertiary | CLAYEY ZEOLITE SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 5 | 55 | 40 | 0 | 0 | 0 | 0 | 0 |