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PANGAEA.
Data Publisher for Earth & Environmental Science

Ehrmann, Werner (1998): Clay mineralogy on sediment core CIROS-2. PANGAEA, https://doi.org/10.1594/PANGAEA.105253, In supplement to: Ehrmann, W (1998): Implications of late Eocene to early Miocene clay mineral assemblages in McMurdo Sound (Ross Sea, Antarctica) on paleoclimate and ice dynamics. Palaeogeography, Palaeoclimatology, Palaeoecology, 139(3-4), 213-231, https://doi.org/10.1016/S0031-0182(97)00138-7

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Coverage:
Latitude: -77.683333 * Longitude: 163.533333
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 165.64 m
Event(s):
CIROS-2 * Latitude: -77.683333 * Longitude: 163.533333 * Elevation: -211.0 m * Location: McMurdo Sound * Campaign: CIROS * Basis: Sampling/drilling ice * Method/Device: Drilling/drill rig (DRILL)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepthmGeocode
2SmectiteSme%Ehrmann, WernerX-ray diffraction TEXTUR, clay fraction
3IlliteIll%Ehrmann, WernerX-ray diffraction TEXTUR, clay fraction
4ChloriteChl%Ehrmann, WernerX-ray diffraction TEXTUR, clay fraction
5KaoliniteKln%Ehrmann, WernerX-ray diffraction TEXTUR, clay fraction
6Smectite/standard ratioSmec/stdEhrmann, WernerX-ray diffraction TEXTUR, clay fraction
7Illite/standard ratioIll/stdEhrmann, WernerX-ray diffraction TEXTUR, clay fraction
8Chlorite/standard ratioChl/stdEhrmann, WernerX-ray diffraction TEXTUR, clay fraction
9Kaolinite/standard ratioKln/stdEhrmann, WernerX-ray diffraction TEXTUR, clay fraction
10Smectite, integral widthSmec IWd2ThetaEhrmann, WernerX-ray diffraction TEXTUR, clay fraction
11Smectite (Half height width)Sme HHWd2ThetaEhrmann, WernerX-ray diffraction TEXTUR, clay fraction
12Illite, integral widthIll IWd2ThetaEhrmann, WernerX-ray diffraction TEXTUR, clay fraction
13Illite half height width, glycolizedIll HHW glycd2ThetaEhrmann, WernerX-ray diffraction TEXTUR, clay fraction
14Illite 5Å/10Å Esquevin-indexIll EIEhrmann, WernerX-ray diffraction TEXTUR, clay fraction
Size:
637 data points

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