The origin of magnetic remanence components of westphalian C to Stephanian C sediments, West Bohemia : a record of waning Variscan tectonism | Charles Explorer

The origin of magnetic remanence components of westphalian C to Stephanian C sediments, West Bohemia : a record of waning Variscan tectonism

Publication at First Faculty of Medicine, Faculty of Mathematics and Physics |

1997

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