Robert Jameson's transition from Neptunism to Plutonism as reflected in his lectures at Edinburgh University, 1820–33

IF 0.5 4区 地球科学 Q4 GEOLOGY
P. Stone
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引用次数: 2

Abstract

Robert Jameson is generally remembered for championing Neptunist geology (originated by Abraham Werner) during its early nineteenth-century competition with the rival Plutonist theory (initiated by James Hutton). Hutton's ideas prevailed and Jameson's intellectual transition to Plutonism is documented in the surviving notes taken by students who attended his lectures at Edinburgh University: one early record is from 1809, a second record is from c. 1820 and four sets of notes are from the early 1830s. Of the latter four, two have not been previously considered from a geological perspective and prove to be the most revelatory of Jameson's conversion; notes compiled by the Royal Navy surgeon Robert McCormick are particularly comprehensive. Although Jameson attempted to maintain the essentials of Werner's theory for its well-ordered stratigraphy, he progressively adopted a Plutonist approach to more contentious issues such as the origin of granite, veining and mountain building. Jameson used Edinburgh's Salisbury Crags sill for field demonstrations and the students’ notes illustrate his changing views in terms of the origins of this classic geological feature. Of the students whose lecture notes survive, it is only McCormick for whom Jameson appears to have been a lasting geological influence.
罗伯特·詹姆逊从海王星论到冥王星论的转变反映在他1820 - 1833年在爱丁堡大学的演讲中
罗伯特·詹姆森因在19世纪初与竞争对手钚理论(由詹姆斯·赫顿提出)的竞争中支持海王星地质学(由亚伯拉罕·维纳提出)而广为人知。赫顿的思想占了上风,詹姆逊向普鲁顿主义的思想转变记录在爱丁堡大学参加他的讲座的学生们留下的幸存笔记中:一份早期记录来自1809年,第二份记录来自约1820年,四套笔记来自1830年代初。在后四种中,有两种以前没有从地质学的角度考虑过,被证明是詹姆逊转变的最具启示性的;皇家海军外科医生罗伯特·麦考密克编写的笔记尤其全面。尽管詹姆逊试图保持维尔纳理论的精髓,使其形成有序的地层学,但他逐渐采用了普鲁顿主义的方法来解决更具争议的问题,如花岗岩的起源、矿脉和造山。詹姆森用爱丁堡的索尔兹伯里岩床进行实地演示,学生们的笔记说明了他对这一经典地质特征起源的不断变化的看法。在那些讲义幸存下来的学生中,只有麦考密克受到了詹姆森的持久地质影响。
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来源期刊
Scottish Journal of Geology
Scottish Journal of Geology 地学-地质学
CiteScore
1.70
自引率
0.00%
发文量
10
审稿时长
>12 weeks
期刊介绍: Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh. Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology. The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors. The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.
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