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Kastner, Miriam; Asaro, Frank; Michel, Helen V; Alvarez, Walter; Alvarez, Luis W (1984): (Table 2) Mineralogy of silicates in the noncalcareous fraction od the Cretaceous-Tertiary boundary at Stevns Klint [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.772194, In supplement to: Kastner, M et al. (1984): The precursor of the Cretaceous-Tertiary boundary clays at Stevns Klint, Denmark, and DSDP Hole 465A. Science, 226(4671), 137-143, https://doi.org/10.1126/science.226.4671.137

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Coverage:
Latitude: 55.190000 * Longitude: 12.280000
Minimum POINT DISTANCE from start: 0.0025 m * Maximum POINT DISTANCE from start: 0.4750 m
Event(s):
Stevns-Klint * Latitude: 55.190000 * Longitude: 12.280000 * Method/Device: Sampling by hand (HAND)
Comment:
Mineral abundances: XXX = abundant, XX = present, X = some, tr = trace, - = absent. In bed VI (10 to 15 cm), carbonate-apatite is a raher abundant phase; its abundance increases at 20 to 25 cm and 30 to 35 cm and decreases again at 40 to 45 cn. The abundance of smectite decreases and of quartz increases in this bed from sample (10 to 15 cm) to Wmple (40 to 45 cm). A few samples in beds V and VI contain traces of mixed-layer smectite-illite, not shown in the table.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Layer descriptionLayerKastner, Miriambed numbers are according to Christensen et al. (1973).
POINT DISTANCE from startDistmGeocode
DistanceDistancemKastner, Miriamminimum
DistanceDistancemKastner, Miriammaximum
QuartzQzKastner, Miriam# = quartz was not detected in the clay size fraction, some quartz was observed in the >20 µm size fraction
FeldsparFspKastner, Miriam
SmectiteSmeKastner, Miriam
IlliteIllKastner, Miriam
Size:
105 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Layer
(bed numbers are according to ...)

Dist [m]

Distance [m]
(minimum)

Distance [m]
(maximum)

Qz
(# = quartz was not detected i...)

Fsp

Sme

Ill
VI0.12500.1000.150XX-XX-
VI0.02500.0000.050XXXXXXX
V0.04500.0300.060tr-XXX-
V0.01500.0000.030XXXXX-
IV0.04500.0400.050X-XXXtr
IV0.03500.0300.040XtrXXtr
IV0.02500.0200.030XX-XXXtr
IV0.01500.0100.020X-XXX-
IV0.00750.0050.010X-XXXtr
IV0.00250.0000.005tr #-XXX-
III0.00500.0000.010tr #-XXX-
II0.00750.0050.010XXXXXXX
II0.00250.0000.005XXXtrXXtr
I0.47500.4500.500XXXXXXX
I0.37500.3500.400XXXXXXXtr