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Paul Fourmarier | |
|---|---|
| Born | December 25, 1877 La Hulpe, Province of Brabant, Belgium |
| Died | January 20, 1970 (aged 92) Liège, Liège Province, Belgium |
| Alma mater | University of Liège, Wallonia, Belgium |
| Known for | study of fold structures and cleavage, description the overthrust nappes |
| Awards | Penrose Gold Medal (1952), Wollaston Medal (1957) |
| Scientific career | |
| Fields | Geology, tectonics |
Paul Frédéric Joseph Fourmarier (1877—1970) was a Belgian geologist and specialist in tectonics and stratigraphy,[1] after whom the Fourmarierite mineral is named.[2]
Fourmarier was born in La Hulpe, Province of Brabant, Belgium and studied at the University of Liège, graduating in 1899. He became a professor of geology at the university in 1920.[1]
He won the Wollaston Medal in 1957[3] and the Penrose Gold Medal in 1952.[4]
His specialist area was the study of fold structures and cleavage and he described the overthrust nappes in the Ardennes.[1] Fourmarier was much involved in the geology of his native Belgium, as well as Zaire (then the Belgian Congo) and other African places. He also worked on continental drift.[1]
An award named after him, the Fourmarier Prize, was established.[5] In addition, a secondary uranium-lead mineral, fourmarierite, was named in his memory.[2]