Titlebook: Antarctica; Contributions to Glo Dieter Karl Fütterer,Detlef Damaske,Franz Tessenso Book 20061st edition Springer-Verlag Berlin Heidelberg

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Einleitung und Problemstellung,raphic rise of the lake bottom dividing the lake into two sub-basins. Our inversion results suggest that water thickness in Lake Concordia does not exceed 200 m for all possible density contrasts between ice/water and surrounding rock; the sediment layer cannot be resolved.

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Exploring the Unknown: History of the First German South Polar Expedition 1901–1903tland, and France took part in the international meteorological and magnetic co-operation. Unfortunately the “Gauss” was beset by ice close to the Antarctic Circle 85 km off the ice-covered coast of Kaiser Wilhelm II. Land, where a winter station was established on sea ice. After 50 weeks of captivi

LARK

Characteristics of Metamorphosed Banded Iron Formation and Its Relation to the Magnetic Anomaly in tyses. The results indicated that almost pure magnetite with pseudosingle-domain (PSD) and multi-domain structure is the dominant composition of meta-BIF as well as quartz. The PSD magnetite grains were along the quartz crystal boundaries and formed a network structure. The electric conductivity of t

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Sapphirine — Orthopyroxene — Garnet Granulite from Schirmacher Hills, Central Dronning Maud Landzoic granulite-facies event elsewhere in central Dronning Maud Land. Metamorphic temperatures estimated to exceed 900°C imply that the tectonothermal regime in the Schirmacher Hills was distinct and could be critical in determining relationships between central Dronning Maud Land and metamorphic bel

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Late Pan-African Fluid Infiltration in the Mühlig-Hofmann- and Filchnerfjella of Central Dronning Maked colour change is caused by transformation of feldspars, spread of dusty micas, opaques and fluid inclusions in addition to replacement of coarse to finer grains. The process is locally penetrative indicating that fluid infiltration can affect large rock volumes. The frequent distribution of alte

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