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Index to Marine and Lacustrine Geological Samples (IMLGS)

Repository: International Ocean Discovery Program
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Ship: Glomar Challenger
Cruise: 28
Hole: 264A
Device: drill
Latitude: -34.968
Longitude: 112.045
Water Depth(m): 2876
Date: 19721223
IGSN: ODP005707
Core length (cm): 15660
Diameter (cm): 7
Storage: refrigerated
1 :    264A 1   850 to 1000
Primary composition: calcareous, nannofossils
Geologic Age: Pleistocene
2 :    264A 1   1008 to 1150
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pleistocene
Comments: AVG.DEN=1.65
3 :    264A 1   1150 to 1300
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pleistocene
4 :    264A 1   1300 to 1450
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pleistocene
5 :    264A 1   1450 to 1600
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pleistocene
Comments: AVG.DEN=1.67
6 :    264A 1   1600 to 1750
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pleistocene
7 :    264A 1   1760 to 1760
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pleistocene
8 :    264A 2   1917 to 1950
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pliocene
9 :    264A 2   1950 to 2100
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pliocene
Comments: AVG.DEN=1.70
10 :    264A 2   2100 to 2250
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pliocene
11 :    264A 2   2250 to 2400
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pliocene
12 :    264A 2   2400 to 2550
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pliocene
Comments: AVG.DEN=1.75
13 :    264A 2   2550 to 2700
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pliocene
14 :    264A 2   2710 to 2710
Primary composition: calcareous, nannofossils
Components: calcareous, foraminifera
Geologic Age: Pliocene
15 :    264A 3   13976 to 14001
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
16 :    264A 3   14001 to 14100
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
17 :    264A 3   14100 to 14250
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
Comments: AVG.DEN=1.80
18 :    264A 3   14250 to 14400
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
19 :    264A 3   14400 to 14550
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
20 :    264A 3   14550 to 14696
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
Comments: AVG.DEN=1.82
21 :    264A 3   14700 to 14850
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
Comments: AVG.DEN=1.84
22 :    264A 3   14860 to 14860
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
23 :    264A 4   14933 to 15050
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
24 :    264A 4   15053 to 15197
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
Comments: AVG.DEN=1.76
25 :    264A 4   15200 to 15350
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
26 :    264A 4   15350 to 15500
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
27 :    264A 4   15500 to 15518
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
Comments: AVG.DEN=1.76
28 :    264A 4   15518 to 15650
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
Comments: AVG.DEN=1.82
29 :    264A 4   15660 to 15660
Primary composition: calcareous, nannofossils
Geologic Age: Eocene
_



When you refer to individual samples/data in the IMLGS, please cite each source repository whose data you use.

More Information and how to cite the IMLGS: doi:10.7289/V5H41PB8.


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