Schirrmeister, Lutz; Siegert, Christine (2017): Heavy mineral composition at site Byk_98_MB-6.3 [dataset]. Alfred Wegener Institute - Research Unit Potsdam, PANGAEA, https://doi.org/10.1594/PANGAEA.879584
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Siegert, Christine; Schirrmeister, Lutz; Babiy, O (2002): The Sedimentological, Mineralogical and Geochemical Composition of Late Pleitocene Deposits from the Ice Complex on the Bykovsky Peninsula, Northern Siberia. Polarforschung, 70, 3-11, https://doi.org/10.2312/polarforschung.70.3
Project(s):
Permafrost Research (Periglacial Dynamics) @ AWI (AWI_PerDyn)
Coverage:
Latitude: 71.807466 * Longitude: 129.351535
Date/Time Start: 1998-08-18T00:00:00 * Date/Time End: 1998-08-20T00:00:00
Event(s):
Byk_98_MB-6.3 * Latitude: 71.807466 * Longitude: 129.351535 * Date/Time Start: 1998-08-18T00:00:00 * Date/Time End: 1998-08-20T00:00:00 * Location: Lena Delta, Siberia, Russia * Campaign: RU-Land_1998_Lena (Lena-Delta1998) * Basis: AWI Arctic Land Expedition * Method/Device: Multiple investigations (MULT)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
54 data points
Data
1 Sample ID | 2 Height [m a.s.l.] | 3 Sediment | 4 HM [%] | 5 HM magn frac [%] | 6 Ilm [%] | 7 Leucox [%] | 8 Ep-Zo [%] | 9 Cpx [%] | 10 Opx [%] | 11 Pyrox gr [%] | 12 Amp [%] | 13 Grt [%] | 14 Zrn [%] | 15 Ap [%] | 16 Tur [%] | 17 Spn [%] | 18 Rt [%] | 19 Ant [%] | 20 Disthene [%] | 21 St [%] | 22 And [%] | 23 Cld [%] | 24 Chl [%] | 25 Mica weath [%] | 26 Bt [%] | 27 Grains [#] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
MB-6.3.-1 | 1.500 | silt | 3.2 | 0.7 | 4.8 | 3.2 | 11.5 | 26.5 | 2.9 | 29.4 | 41.8 | 2.6 | 0.0 | 2.3 | 0.9 | 2.9 | 0.0 | 0.0 | 0.0 | <0.1 | 0.0 | 0.3 | 0.3 | 0.0 | 0.0 | 347 |
MB-6.3.-3 | 1.000 | silt | 1.0 | <0.1 | 10.5 | 7.8 | 8.9 | 50.3 | 0.0 | 50.3 | 11.3 | 4.2 | 0.5 | 3.9 | 0.3 | 1.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 1.3 | 0.0 | 0.0 | 382 |