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- W2393531612 abstract "Antarctica can be divided into 2 big structural units, ie East antarctica shield and West Antarctica Mesozoic Cenozoic fold belt. And the Transantarctica Mts between them is a transitional zone composed of basement and covering strata. The former is a bi structure of Proterozoic and Early Palaeozoic. And the latter consists of Devonian Permian. In Mid Jurassic, Gondwana began separation. In Late Cretaceous, Antarctica moved southwards and to the present position in Early Miocene. The mineral resources are mainly Precambrian stripped iron formation in East Antarctica, U, Th mineralization connected with Ordovician granite, Fe, Ti, Cr, Ni, Cu, Pt group elements mineralization connected with Jurassic basic complex and Permian alluvial coal beds in Transantarctica Mts, Cu polymetallic mineralization connected with Mesozoic Cenozoic magmatism in West Antarctica. There are oil gas potential areas in East Antarctica shelf, Weddell Sea, Ross Sea and Antarctica Peninsula. And Bitumen and gas have been discovered by a drill hole in Ross Sea." @default.
- W2393531612 created "2016-06-24" @default.
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- W2393531612 date "2000-01-01" @default.
- W2393531612 modified "2023-09-26" @default.
- W2393531612 title "A SUMMARY OF GEOLOGY AND MINERAL RESOURCES OF ANTARCTICA" @default.
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