2024-03-29T09:28:35Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:902016-11-25T15:12:08ZDOIDBDOIDB.SDDBfalse3DOIDB.SDDB
10.1594/GFZ.SDDB.1131
Yuretich, Richard
Melles, Martin
Sarata, Brenn
Grobe, Hannes
Clay mineralogy and sedimentology of coring Site BDP-1-B (BDP93-2)
Deutsches GeoForschungsZentrum GFZ
2008
Baikal Drilling Project
Mission Specific Platform
δ13C, organic carbon
Amphibole/standard ratio
Calcium carbonate
Chlorite
Chlorite/standard ratio
Element analyser CHN
Feldspar/standard ratio
Illite
Illite/standard ratio
Kaolinite
Kaolinite/standard ratio
Nitrogen
Quartz/standard ratio
Sand
Silt
Size fraction < 0,002mm, clay
Smectite
Smectite/standard ratio
total organic carbon
X-ray diffraction
2008-01-03
eng
Dataset
10.1594/PANGAEA.56129
10013/epic.14025.d001
8244 DataPoints
text/tab-separated-values
Lake Baikal, in south-central Siberia, has been the focus of an international effort (the Baikal Drilling Project; BDP) to obtain continuous long cores (upwards of 100 m) from this unique rift-valley lake and to interpret the paleoclimatic history from various proxy data. As part of this effort, the clay minerals were examined by two research teams. A consistent clay-mineral assemblage, containing illite, interstratified illite-smectite, chlorite, and kaolinite as the major minerals, characterizes much of the modern sediments. The relative abundance of these minerals changes with depth in both short piston cores from various parts of the lake and in 100-m-long cores taken from the distal toe of the Selenga Delta (BDP-93).
52.518 103 56 106.153