Griffin, John J; Windom, Herbert; Goldberg, Edward D (1968): Mineralogy of some Australian desert samples (Table 3) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.399426, Supplement to: Griffin, JJ et al. (1968): The distribution of clay minerals in the World Ocean. Deep-Sea Research and Oceanographic Abstracts, 15(4), 433-459, https://doi.org/10.1016/0011-7471(68)90051-X
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Abstract:
The relative amounts of chlorite, montmorillonite, kaolinite and illite in the less than 2 micron size fraction of pelagic sediments are related to the sources and transport paths of solid phases from the continents to the oceans and to injections of volcanic materials to the marine environment. Three modes of entry of solid phases from the lands to the seas are considered: by glaciers, by rivers and by atmospheric winds. The compositions of the clay size fraction are also related to rates of accumulation of the non-biogenous phases.
Coverage:
Median Latitude: -26.163330 * Median Longitude: 131.642917 * South-bound Latitude: -33.166700 * West-bound Longitude: 119.500000 * North-bound Latitude: -23.000000 * East-bound Longitude: 139.050000
Comment:
size fraction <2µm, value <1 means traces
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | LATITUDE | Latitude | Geocode | |||
| 2 | LONGITUDE | Longitude | Geocode | |||
| 3 | Description | Description | Griffin, John J | |||
| 4 | Montmorillonite | Mnt | % | Griffin, John J | X-ray diffraction TEXTUR, clay fraction | |
| 5 | Illite | Ill | % | Griffin, John J | X-ray diffraction TEXTUR, clay fraction | |
| 6 | Kaolinite | Kln | % | Griffin, John J | X-ray diffraction TEXTUR, clay fraction | |
| 7 | Chlorite | Chl | % | Griffin, John J | X-ray diffraction TEXTUR, clay fraction | |
| 8 | Minerals | Minerals | Griffin, John J |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
239 data points