Table 2. The element content of manganese crust
| Cobertura |
LATITUDE: 19.500000 * LONGITUDE: 114.300000 * MINIMUM ELEVATION: -2470.0 m * MAXIMUM ELEVATION: -2470.0 m |
|---|---|
| Data(s) |
17/09/1990
|
| Resumo |
The terrains in the South China Sea were apart of the Southeast China continent, and their rift-departing process dominated the formation and evolution of the South China Sea. The survey results of topography and paleoenvironment of the northern South China Sea during SO-49 cruise demonstrate that the terrains rift-departed from the South China continent before early Eocene. |
| Formato |
text/tab-separated-values, 380 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.849672 doi:10.1594/PANGAEA.849672 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Quanxing, Li; Shengdi, Wu (1990): The age of the South China Sea terrains rift - departing from South China continent. In: Jin Xiang- long, Hermann Rudolf Kudrass and Guy Pautot (eds), Marine Geology and Geophysics of the South China Sea. China Ocean Press, Hangzhou, China, 101-107, hdl:10013/epic.46006.d011 |
| Palavras-Chave | #Aluminium oxide; Arsenic; Barium; Beryllium; Bismuth; Boron; Cadmium; Calcium oxide; Chlorine; Chromium; Cobalt; Copper; Dredge; DRG; Gallium; Indium; Iron oxide, Fe2O3; Layer number; Lead; Loss on ignition; Magnesium oxide; Manganese dioxide; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus oxide; Potassium oxide; Rubidium oxide; SCSea; Silicon dioxide; Silver; Sodium oxide; South China Sea; Strontium; Strontium oxide; Sulfite; Sum; Tin; Titanium oxide; Tungsten; Vanadium; Water content of wet mass; Zinc |
| Tipo |
Dataset |
