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http://dbpedia.org/ontology/abstract Ганс Штілле (нім. Hans Stille; 8 жовтня 1876, Ганновер — 26 грудня 1966, Ганновер) — німецький геолог. , Га́нс (Ха́нс) Вильгельм Шти́лле (нем. Hans Wilhelm Stille; 1876—1966) — немецкий геолог, тектонист. Профессор, вице-президент Немецкой Академии наук Леопольдина, основатель Геотектонического института в Берлине. , Hans (Johannes) Wilhelm Stille (* 8. OktobHans (Johannes) Wilhelm Stille (* 8. Oktober 1876 in Hannover; † 26. Dezember 1966 ebenda) zählt zu den bedeutendsten Geologen des 20. Jahrhunderts. Er war Professor der Geologie an mehreren Universitäten. 1946 gründete er in Ost-Berlin das Geotektonische Institut, aus dem später das geophysikalische Zentralinstitut ZIPE hervorging. Stilles Forschungen – insbesondere zur Gebirgsbildung – trugen wesentlich dazu bei, dass sich die Geologie zum Mobilismus weiterentwickelte. Als Vertreter der Kontraktionstheorie der Erde war er ein Gegner von Alfred Wegeners Hypothese der Kontinentalverschiebung und trug zur verzögerten Akzeptanz der Plattentektonik in Deutschland bei.nz der Plattentektonik in Deutschland bei. , Hans Wilhelm Stille (8 October 1876 – 26 DHans 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. Stille adhered to the contracting Earth hypothesis and together with Leopold Kober he worked on the geosyncline theory to explain orogeny. 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. This competing view rejected Earth contraction and argued for continental drift. As Stille opposed continental drift he came to be labelled a "fixist". 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. 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. 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 (English: craton). The Geotectonic Research journal was founded in 1937 by Hans Stille and . The enormous influence that Stille's concepts had on tectonics is obvious from many of the tectonic terms still in use today, despite the fact that almost everything he postulated was later shown to be completely erroneous. — Celâl Şengör, 1982completely erroneous. — Celâl Şengör, 1982 , ハンス・ヴィルヘルム・シュティレ (Hans Wilhelm Stille, 1876年8月8日 - 1966年12月26日) は主に顕生代のテクトニクスと構造事象の対照調査についての業績で影響力のあるドイツの地質学者。 , Wilhelm Hans Stille (Hannover, 8 oktober 1Wilhelm Hans Stille (Hannover, 8 oktober 1876 - Hannover, 26 december 1966) was een invloedrijk Duits structureel geoloog. Stille is vooral bekend om zijn onderscheid van tektonische fasen in de ontwikkeling van een continent. Het mineraal is naar hem vernoemd.tinent. Het mineraal is naar hem vernoemd. , Hans Stille, född 8 oktober 1876 i HannoveHans Stille, född 8 oktober 1876 i Hannover, död där 26 december 1966, var en tysk geolog. Stille blev 1912 professor vid universitetet i Leipzig och chef för Sachsens geologiska undersökning, från 1913 professor i geologi och paleontologi i Göttingen. Hans mest betydande arbeten faller inom tektonikens område. Särskilt framhöll han sammanhanget emellan geosynklinaler, d.v.s. områden med mäktiga sedimentära avsättningar, som är stadda i sekulär sänkning, och bergskedjezoner: den veckning, som ger upphov till bergskedjor, är bunden vid zoner för stark sedimentation och är att betrakta som en revolution, ett avbrott i områdets lugna sedimentära evolution. Han utgav bland annat det sammanfattande verket Grundfragen der vergleichenden Tektonik (1924).fragen der vergleichenden Tektonik (1924). , Hans Wilhelm Stille (né le 8 octobre 1876 à Hanovre et mort le 26 décembre 1966 dans la même ville) est un géologue allemand travaillant principalement sur la tectonique et le classement des événements tectoniques au cours du Phanérozoïque. , 汉斯·施蒂勒(Hans Wilhelm Stille,1876年10月8日-1967年12月26日),德国地质学家。1899年毕业于格丁根大学地质学专业,其毕业论文是关于条顿堡森林山体构造的研究。后曾任教于莱比锡大学、格丁根大学、柏林大学,并曾任所长。他对克拉通形成的研究有重要的贡献。 , Hans Wilhelm Stille (Hannover, 8 de outubrHans Wilhelm Stille (Hannover, 8 de outubro de 1876 – Hannover, 26 de dezembro de 1966) foi um geólogo alemão. É considerado um dos mais significativos geólogos do século XX. Foi professor de geologia da Universidade de Göttingen, Universidade de Hannover e a partir de 1932 da Universidade Humboldt de Berlim. Em 1946 fundou em Berlim Oriental o , do qual originou-se mais tarde o (ZIPE)., do qual originou-se mais tarde o (ZIPE).
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rdfs:comment Hans Wilhelm Stille (né le 8 octobre 1876 à Hanovre et mort le 26 décembre 1966 dans la même ville) est un géologue allemand travaillant principalement sur la tectonique et le classement des événements tectoniques au cours du Phanérozoïque. , Hans (Johannes) Wilhelm Stille (* 8. OktobHans (Johannes) Wilhelm Stille (* 8. Oktober 1876 in Hannover; † 26. Dezember 1966 ebenda) zählt zu den bedeutendsten Geologen des 20. Jahrhunderts. Er war Professor der Geologie an mehreren Universitäten. 1946 gründete er in Ost-Berlin das Geotektonische Institut, aus dem später das geophysikalische Zentralinstitut ZIPE hervorging.ikalische Zentralinstitut ZIPE hervorging. , Ганс Штілле (нім. Hans Stille; 8 жовтня 1876, Ганновер — 26 грудня 1966, Ганновер) — німецький геолог. , Wilhelm Hans Stille (Hannover, 8 oktober 1Wilhelm Hans Stille (Hannover, 8 oktober 1876 - Hannover, 26 december 1966) was een invloedrijk Duits structureel geoloog. Stille is vooral bekend om zijn onderscheid van tektonische fasen in de ontwikkeling van een continent. Het mineraal is naar hem vernoemd.tinent. Het mineraal is naar hem vernoemd. , Га́нс (Ха́нс) Вильгельм Шти́лле (нем. Hans Wilhelm Stille; 1876—1966) — немецкий геолог, тектонист. Профессор, вице-президент Немецкой Академии наук Леопольдина, основатель Геотектонического института в Берлине. , Hans Wilhelm Stille (8 October 1876 – 26 DHans 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. Stille adhered to the contracting Earth hypothesis and together with Leopold Kober he worked on the geosyncline theory to explain orogeny. 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. This competing view rejected Earth contraction and argued for continental drift. As Stille opposed continental drift he came to be labelled a "fixist".l drift he came to be labelled a "fixist". , Hans Stille, född 8 oktober 1876 i HannoveHans Stille, född 8 oktober 1876 i Hannover, död där 26 december 1966, var en tysk geolog. Stille blev 1912 professor vid universitetet i Leipzig och chef för Sachsens geologiska undersökning, från 1913 professor i geologi och paleontologi i Göttingen. Hans mest betydande arbeten faller inom tektonikens område. Särskilt framhöll han sammanhanget emellan geosynklinaler, d.v.s. områden med mäktiga sedimentära avsättningar, som är stadda i sekulär sänkning, och bergskedjezoner: den veckning, som ger upphov till bergskedjor, är bunden vid zoner för stark sedimentation och är att betrakta som en revolution, ett avbrott i områdets lugna sedimentära evolution. Han utgav bland annat det sammanfattande verket Grundfragen der vergleichenden Tektonik (1924).fragen der vergleichenden Tektonik (1924). , Hans Wilhelm Stille (Hannover, 8 de outubrHans Wilhelm Stille (Hannover, 8 de outubro de 1876 – Hannover, 26 de dezembro de 1966) foi um geólogo alemão. É considerado um dos mais significativos geólogos do século XX. Foi professor de geologia da Universidade de Göttingen, Universidade de Hannover e a partir de 1932 da Universidade Humboldt de Berlim. Em 1946 fundou em Berlim Oriental o , do qual originou-se mais tarde o (ZIPE)., do qual originou-se mais tarde o (ZIPE). , ハンス・ヴィルヘルム・シュティレ (Hans Wilhelm Stille, 1876年8月8日 - 1966年12月26日) は主に顕生代のテクトニクスと構造事象の対照調査についての業績で影響力のあるドイツの地質学者。 , 汉斯·施蒂勒(Hans Wilhelm Stille,1876年10月8日-1967年12月26日),德国地质学家。1899年毕业于格丁根大学地质学专业,其毕业论文是关于条顿堡森林山体构造的研究。后曾任教于莱比锡大学、格丁根大学、柏林大学,并曾任所长。他对克拉通形成的研究有重要的贡献。
rdfs:label Hans Stille , ハンス・シュティレ , Штилле, Ганс Вильгельм , Ганс Штілле , 汉斯·施蒂勒
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