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Erwin Suess | Akateeminen Kirjakauppa

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Coastal Upwelling Its Sediment Record - Part A: Responses of the Sedimentary Regime to Present Coastal Upwelling
Tekijä: Erwin Suess; Jörn Thiede
Kustantaja: Springer-Verlag New York Inc. (2012)
Saatavuus: Noin 17-20 arkipäivää
EUR   97,90
Coastal Upwelling Its Sediment Record - Part B: Sedimentary Records of Ancient Coastal Upwelling
Tekijä: Jörn Thiede; Erwin Suess
Kustantaja: Springer Science+Business Media (1983)
Saatavuus: Ei tiedossa
EUR   118,60
Coastal Upwelling, Its Sediment Record: Responses of the Sedimentary Regime to Present Coastal Upwelling Part A
Tekijä: Erwin Suess
Kustantaja: Plenum Publishing Corporation (1983)
Saatavuus: Ei tiedossa
EUR   125,70
Coastal Upwelling Its Sediment Record - Part B: Sedimentary Records of Ancient Coastal Upwelling
Tekijä: Jörn Thiede; Erwin Suess
Kustantaja: Springer-Verlag New York Inc. (2012)
Saatavuus: Noin 17-20 arkipäivää
EUR   49,60
    
Coastal Upwelling Its Sediment Record - Part A: Responses of the Sedimentary Regime to Present Coastal Upwelling
97,90 €
Springer-Verlag New York Inc.
Sivumäärä: 604 sivua
Asu: Pehmeäkantinen kirja
Painos: Softcover reprint of
Julkaisuvuosi: 2012, 22.12.2012 (lisätietoa)
Kieli: Englanti
NATO Advanced Research Institutes are designed to explore unre­ solved problems. By focusing complementary expertise from various disciplines onto one unifying theme, they approach old problems in new ways. In line with this goal of the NATO Science Committee, and with substantial support from the u.s. Office of Naval Research and the Seabed Assessment Program of the U. S. National Science Founda­ tion, such a Research Institute on the theme of Coastal Upwelling and Its Sediment Record was held september 1-4, 1981, in Vilamoura, Portugal. The theme implies a modification of uniformitarian thinking in earth science. Expectations were directed not so much towards find­ ing the key to the past as towards exploring the limits of interpret­ ing the past based on present upwelling oceanography. Coastal up­ welling and its imprint on sediments are particularly well-suited for such a scientific inquiry. The oceanic processes and conditions characteristic of upwelling are well understood and are a well­ packaged representation of ocean science that are familiar to geolo­ gists, just as the magnitude of bioproduction and sedimentation in upwelling regimes --among other biological and geological processes-­ have made oceanographers realize that the bottom has a feedback role for their models.

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Coastal Upwelling Its Sediment Record - Part A: Responses of the Sedimentary Regime to Present Coastal Upwellingzoom
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9781461566533
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