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pro vyhledávání: '"multiple paleostre"'
The dense fault network that separates the tectonic units of northern Victoria Land to the E from the East Antarctic Craton to the W represents a regionally sized, NNW-SSE trending deformation zone that is also known as the Rennick Graben Fault syste
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::72e1a0b6f6eb48d78dd8f0d160fa9109
https://hdl.handle.net/11590/427033
https://hdl.handle.net/11590/427033
