The Geology of Antarctica
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چکیده
منابع مشابه
Dredging up Mawson: Implications for the Geology of Coastal East Antarctica
PP51E–1359. Steed, R.H.N. & Drewry, D.J. 1982: Radio echo-sounding investigations of Wilkes Land, Antarctica. In Craddock, C. (ed.): Proceedings of the 3rd International Symposium on Antarctic Geology and Geophysics. University of Wisconsin
متن کاملCorrelation of China loess and Antarctica ice records
Strong asymmetry of hemispheric climates during MIS-13 inferred from correlating China loess and Antarctica ice records Z. T. Guo, A. Berger, Q. Z. Yin, and L. Qin Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing, 100029, China Institut d’Astronomie et de Géophysique G. Lemaı̂tre, Université Catholique de...
متن کاملPlankton diversity and aquatic ecology of a freshwater lake (L3) at Bharti Island, Larsemann Hills, east Antarctica
The Larsemann Hills range is an ice-free oasis on the Ingrid Christensen Coast of Princess Elizabeth Land, East Antarctica, which includes Bharti Island, Fisher Island, McLeod Island, Broknes Peninsula, Stornes Peninsula, and several other islands, promontories, and nunataks. The Larsemann Hills is an ice-free area of approximately 50 km2, located halfway between the Vestfold Hills a...
متن کاملGeology of the Byrd Glacier Discontinuity (Ross Orogen): New survey data from the Britannia Range, Antarctica
Field activities in the Britannia Range (Transantarctic Mountains, Antarctica) highlighted new geological features around the so-called Byrd Glacier discontinuity. Recent field surveys revealed the occurrence of significant amounts of mediumto high-grade metamorphic rocks, intruded by abundant coarse-grained porphyritic granitoids. Most of the granitoids are deformed, with foliation parallel to...
متن کاملThe seismic structure of Precambrian and early Palaeozoic terranes in the Lambert Glacier region, East Antarctica
The Lambert Glacier region of East Antarctica encompasses the proposed boundary between three of the ancient continents that formed East Gondwana: Indo-Antarctica, the central East Antarctic Craton and a proposed extension of the Pinjarra Orogen of Australia. The only area of extensive rock exposure in central East Antarctica, it uniquely allows the seismic structure to be linked to surface geo...
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