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history THE BASALT CONTROVERSY IV (PART 18)

机译:历史玄武岩之争IV(PART 18)

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Even while Werner was at the height of his influence as the leader of the Neptunists (see Part 16), a few German geologists had attempted, without success, to challenge his ideas on the origin of basalt. One of the first was Rudolf Erich Raspe (1771), who re ognized that columnar basalt along the lower Rhine River was volcanic (Sigurdsson, 1999, p. 142-143). He is better known as the author of 'Baron Munchausen's Narrative his Marvellous Travels.' Another serious critic was one of Werner's first students, J.K.W. Voigt, who disputed his interpretation of the Scheibenberg basalt (Sigurdsson, 1999, p. 117; see Part 16). As time went by and many locations were found in France, Italy, and Britain, where volcanic and granitic rocks could be observed cutting sediments and each other, Werner's ideas on basalt became more suspect. Even worse, some of his most famous students became advocates rather than critics of Vulcanism as they travelled the globe and began to realize that the field evidence didn't support what they had been taught. These included: Leopold von Buch, probably Werner's most illustrious protege (Sigurdsson 1999, p. 123); Jean Baptiste Barthelemy de Lessups, who observed active volcanoes in Kamchatka in 1790; Alexander von Humboldt, who witnessed the eruption of Cotopaxi in Ecuador in 1803 and wrote classic descriptions of the natural history of South America; and William Maclure, who published the first geological map of the United States in 1809. By the time of Werner's death in 1817, his theories about the 'universal formation' and the sedimentary origin of basalt were badly tarnished and rejected by everyone except Robert Jameson.
机译:即使在沃纳(Werner)作为海王星的领袖的影响力达到顶峰的时候(参见第16部分),一些德国地质学家仍未成功地挑战他关于玄武岩起源的观点。最早的人之一是鲁道夫·埃里希·拉斯佩(Rudolf Erich Raspe,1771年),他认识到莱茵河下游的柱状玄武岩是火山岩(Sigurdsson,1999,第142-143页)。他以《蒙克豪森男爵的奇妙旅行记》的作者而著称。另一位严肃的评论家是维尔纳(Werner)的第一批学生之一J.K.W. Voigt对他对Scheibenberg玄武岩的解释提出异议(Sigurdsson,1999年,第117页;请参阅第16部分)。随着时间的流逝,在法国,意大利和英国发现了许多地点,在那里可以观察到火山岩和花岗石相互切割并沉积,因此,沃纳关于玄武岩的想法变得更加可疑。更糟糕的是,他最着名的一些学生在环球旅行时变成了Vulcanism的拥护者,而不是批评家。他们开始意识到实地证据不支持他们所学的内容。其中包括:利奥波德·冯·布赫(Leopold von Buch),可能是维尔纳最杰出的蛋白质(Sigurdsson 1999,p。123);让·巴蒂斯特·巴泰勒米·德·莱瑟普斯(Jean Baptiste Barthelemy de Lessups),他于1790年在堪察加观察到活火山。亚历山大·冯·洪堡(Alexander von Humboldt),他于1803年在厄瓜多尔目睹了科托帕希的爆发,并撰写了有关南美自然历史的经典描述。威廉·麦克卢尔(William Maclure)于1809年出版了美国的第一张地质图。在维尔纳(Werner)于1817年去世时,他关于玄武岩的“普遍形成”和沉积成因的理论遭到了严重的污损和拒绝,除了罗伯特·詹姆森之外。

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