Titlebook: Geological History of the Polar Oceans: Arctic versus Antarctic; Ulrich Bleil,Jörn Thiede Book 1990 Kluwer Academic Publishers 1990 Arctic

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书目名称Geological History of the Polar Oceans: Arctic versus Antarctic影响因子(影响力)




书目名称Geological History of the Polar Oceans: Arctic versus Antarctic影响因子(影响力)学科排名




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书目名称Geological History of the Polar Oceans: Arctic versus Antarctic网络公开度学科排名




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书目名称Geological History of the Polar Oceans: Arctic versus Antarctic年度引用学科排名




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VALID

Zusammenfassung der Ergebnisse,pe off Halley Bay, a deep buried channel is observed, bordered to the north by a steep and high buried scarp. The channel fill deposits are characterized by the presence of large olistolith-like structures.

linguistics

bleach

Elektromagnetische Schwingungen,late glacial acccumulation rate only by a factor of about three as compared to the present value. The explanation of this discrepancy could be that, either .Be is not as reliable an indicator of glacial/interglacial accumulation rate changes in Greenland as it seems to be in Antarctica, or the deepe

leniency

https://doi.org/10.1007/978-3-642-91334-1l of these events by orbitally driven insolation minima. Together with factors not recognized or poorly understood they resulted in the development of the first Arctic Ocean ice-cover..Interpretations of the Arctic Ocean condition during the late Cenozoic include the idea of a continual warm ocean u

geometrician

geometrician

Erythropoietin

The Opening of the Arctic Oceane Chukotka margin at 175 Ma, and progressed southward along what is now the southern edge of the Brooks Range to the Stable Yukon Block margin at 165 Ma, and may have eventually included the Fransican of western North America. Opening in the Central and Viking Grabens occurred concurrently in the No

asthma

A Fine-Scale Seismic Stratigraphy of the Eastern Margin of the Weddell Seape off Halley Bay, a deep buried channel is observed, bordered to the north by a steep and high buried scarp. The channel fill deposits are characterized by the presence of large olistolith-like structures.

Indecisive