Difference between revisions of "PYTTA8QZBTE.acc rate dust"
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( InferredVariable (L) )
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| − | [[Category:InferredVariable_(L)]] | + | [[Category:InferredVariable_(L)]]{{#set:| |
| + | FoundInTable (L)=ODP659.Tiedemann.1994.paleo1measurement1| | ||
| + | HasColumnNumber (L)=4| | ||
| + | HasMaxValue (L)=3.012| | ||
| + | HasMeanValue (L)=0.90804435483871| | ||
| + | HasMedianValue (L)=0.79| | ||
| + | HasMinValue (L)=0.162| | ||
| + | HasUnits (L)=g/cm^2/kyr| | ||
| + | HasVariableID (L)=PYTTA8QZBTE| | ||
| + | InferredFrom (L)=PYTBMGCSUBM.dust| | ||
| + | InferredVariableType (L)=Accumulation_rate| | ||
| + | Name (L)=acc rate dust| | ||
| + | Notes (L)=Depth is a result from correlations between holes A, B and C (see Depth, composite). The noncarbonate fraction (100% minus %CaCO3) is considered to be purely eaolian, because the concentrations of biogenic opal (<2%), organic carbon (<0.5%), and volcanic glass are negligible and fluvial sediment supply and turbidites cannot reach this position (Tiedemann et al., 1989)| | ||
| + | TakenAtDepth (L)=PYTMNX90B5M.depth}} | ||
