By Dieter K. Fütterer, Detlef Damaske, Georg Kleinschmidt, Hubert Miller, Franz Tessensohn
Sixty articles prepared in 8 thematic sections check with newest geological and geophysical result of Antarctic examine. The Precambrian of the East Antarctic defend and its geological background is taken into account in addition to sub-ice topography, geophysics and stratigraphy, sedimentology and geophysics of the encircling Southern Ocean. specific emphasis is given to the relationship of the Antarctic and the encircling continents whilst forming a part of Gondwana.
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Additional resources for Antarctica: Contributions to Global Earth Sciences
The metamorphosed rocks of the layered gneiss in the Mt. , Motoyoshi and Matsueda 1984) and in intrusive rocks for some mafic gneiss (Ishizuka et al. 1998). The precursor of metamorphosed rocks in the layered gneiss accomplished the sedimentation, intrusion and metamorphism between 3 930 and 2 500 Ma. Field observation in the Mt. Riiser-Larsen area clarified the existence of widely extended meta-BIF layers. These frequently showed natural shrinkage at the end of the layers, but they are cut by faults or dyke intrusions occasionally.
Continental drift became “self-evident” by way of the overwhelming evidence for plate tectonic mechanism by which it took place. And now, “Rodinia”? “Antarctica and Rodinia”, a separate session of the Potsdam meeting, is for future historians to evaluate. References Holmes A (1944) Principles of physical geology. Thomas Nelson & Sons, London Schmidt DL, Williams PL, Nelson WH (1978) Geologic map of the Schmidt Hills quadrangle and part of the Gambacorta Peak quadrangle, Pensacola Mountains, Antarctica, scale 1 : 250000.
Ayers et al. (1992) reported a new technique using a lid on the sample container without welding to seal a capsule for hydrothermal experiments. In cases where we adopted the conventional crimping method, the experiments failed due to addition of the H2O component from surroundings. We found glass and bubbles in the run no. MS930917, even if the run temperature was about 150 °C below the solidus. We adopted the Mo/ Pt double capsule method in the later runs to prevent addition or escape of volatile components.
Antarctica: Contributions to Global Earth Sciences by Dieter K. Fütterer, Detlef Damaske, Georg Kleinschmidt, Hubert Miller, Franz Tessensohn