Titlebook: Computerized Modeling of Sedimentary Systems; Jan Harff,Wolfram Lemke,Karl Stattegger Conference proceedings 1999 Springer-Verlag Berlin H

使残废

Directed

Irony and Performance: The Romantic Childthe ice ages of the late Cenozoic are of the order of 10 to 1000 ka. On these time scales, the so-called astronomical theory of paleoclimates and in particular its Milan-kovitch version have become the almost universally accepted basis of research (Berger 1992). In its traditional form, the astronom

FIS

Aggregate

https://doi.org/10.1007/978-3-031-42371-0nstruction of the history of sedimentary basins. The resolution of palaeontological time scales can be improved by applying methods of quantitative stratigraphy, due to more rigorous and/or more complete approach by using the distribution of taxa as a reliable tool for correlation, i.e. a time scale

alleviate

Child-Killers and Killer-Children, size of eustatic sea-level changes (Burton et al. 1988). Sedimentary simulation can be used in conjunction with sequence stratigraphy to interpret Scismic cross sections to solve these problems. To this end, a Scismic cross section that records the Neogene carbonate fill of the West Andros Channel

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https://doi.org/10.1057/9780230227729trient inputs during the last decades have led to a significant eutrophication especially in the nearshore regions (Nehring 1992; Nehring and Matthäus 1991; Wulff 1990). Indications of changes in the phytoplankton biomass and species composition have been reported (Schulz and Kaiser 1986; Wulff et al. 1990).

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https://doi.org/10.1007/978-3-662-03902-1Coast; Iceberg; Ocean; Sediment; computer simulation; marine; model; modeling; simulation

acclimate

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