John, Cédric M; Adatte, Thierry; Mutti, Maria (2006): (Table 2) Mineralogical events in the middle Miocene section of ODP Site 194-1194 from Marion Plateau, northeast of Australia [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.693979, In supplement to: John, CM et al. (2006): Regional trends in clay mineral fluxes to the Queensland margin and ties to middle Miocene global cooling. Palaeogeography, Palaeoclimatology, Palaeoecology, 233(3-4), 204-224, https://doi.org/10.1016/j.palaeo.2005.09.010
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -20.242550 * Longitude: 151.983110
Date/Time Start: 2001-01-22T00:00:00 * Date/Time End: 2001-01-22T00:00:00
Minimum DEPTH, sediment/rock: 163.40 m * Maximum DEPTH, sediment/rock: 200.00 m
Event(s):
194-1194 * Latitude: -20.242550 * Longitude: 151.983110 * Date/Time: 2001-01-22T00:00:00 * Elevation: -373.9 m * Penetration: 597 m * Recovery: 215.4 m * Location: Coral Sea * Campaign: Leg194 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 53 cores; 487 m cored; 0 m drilled; 44.2% recovery
Comment:
Relative content in clay: AD, MP, K1, Sm1. Mineral ratios based on peak height: KS2
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Ageprofile Datum Description | Ageprof dat des | John, Cédric M | |||
| 3 | Age model | Age model | ka | John, Cédric M | ||
| 4 | Comment | Comment | John, Cédric M |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
11 data points
Data
| 1 Depth sed [m] | 2 Ageprof dat des | 3 Age model [ka] | 4 Comment |
|---|---|---|---|
| 163.40 | Minima in Phyllosilicate content (MP) | 14000 | |
| 186.40 | Drop in ankerite content (AD) | 14600 | |
| 190.00 | Decrease in relative abundance of smectite (Sm1) | 14600 | |
| 196.80 | Increase in the kaolinite to smectite ratio (KS2) | 14300 | age questionable |
| 200.00 | Increase in relative abundance of kaolinite (K1) | 15100 |