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Index to Marine and Lacustrine Geological Samples (IMLGS)

Repository: Lamont-Doherty Earth Observatory
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Ship: Vema
Cruise: VM33 (V3309)
Sample: 084
Device: core, piston
Latitude: -3.167
Longitude: 125.2
Water Depth(m): 5348
Date: 19760805
IGSN: DSR000VB4
Core length (cm): 1005
Diameter (cm): 6
Storage: room temperature, dry
1 :    0 to 105 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
2 :    105 to 113 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
3 :    113 to 400 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Components: siliceous
4 :    400 to 551 cm in core
Primary composition: terrigenous
Primary texture: sand
Secondary composition: terrigenous
Secondary texture: sandy mud or ooze
5 :    551 to 560 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
6 :    560 to 583 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
7 :    583 to 605 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
8 :    605 to 618 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
9 :    618 to 655 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Components: pyrite or marcasite
10 :    655 to 706 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
11 :    706 to 712 cm in core
Primary composition: terrigenous
Primary texture: sand
12 :    712 to 938 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Components: siliceous
13 :    938 to 952 cm in core
Primary composition: terrigenous
Primary texture: sand
Components: calcareous, foraminifera
14 :    952 to 1001 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
15 :    1001 to 1005 cm in core
Primary composition: siliceous, diatoms
Primary texture: mud or ooze
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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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