Английская Википедия:Hans Stille

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Hans Wilhelm Stille (8 October 1876 – 26 December 1966) was an influential German geologist working primarily on tectonics and the collation of tectonic events during the Phanerozoic.[1] Stille adhered to the contracting Earth hypothesis and together with Leopold Kober he worked on the geosyncline theory to explain orogeny.[2] Stille's ideas emerged in the aftermath of Eduard Suess' book Das Antlitz der Erde (1883–1909). Stille's and Kober's school of thought was one of two that emerged in the post-Suess era the other being headed by Alfred Wegener and Émile Argand.[2] This competing view rejected Earth contraction and argued for continental drift.[3] As Stille opposed continental drift he came to be labelled a "fixist".[4]

Part of Stille's work dealt with massifs and sedimentary basins in Central Europe; differing from Suess' interpretations for the same area showing that between the Bohemian and Rhine massifs Mesozoic rocks were folded.[3]

A central tenet in Stille's geology was that geosynclines became depressions without any faulting with any fault found being the product of later processes like the final collapse of the geosyncline.[5]

In 1933 Stille would shorten Leopold Kober's concept of kratogen, that was used to describe those portions of the continental crust that were old and stable, into kraton (Шаблон:Lang-en).[6] The Geotectonic Research journal was founded in 1937 by Hans Stille and Franz Lotze.

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Awards and honours

The Hans-Stille-Medaille of German Geological Society, awarded annually, is named after him. Also named for him is the mineral stilleite (ZnSe) and the wrinkle ridge Dorsa Stille on the Moon.

References

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Bibliography

External links

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