Herbert Henry Thomas. 1876-1935

Alfred Harker
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引用次数: 2

Abstract

Herbert Henry Thomas, born March 13, 1876, was the son of Mr. Frederick Thomas of Exeter and Harrow. He received his early education at Exeter School, and in 1894 entered at Sidney Sussex College, Cambridge, where he was first Exhibitioner and afterwards Scholar. At Cambridge he laid the foundation of not a few life-long friendships. His natural bent towards Geology soon became apparent, and he was an active member of the Sedgwick Club, in which he continued to take an interest in later years. He took the Natural Sciences Tripos in 1897-8, being placed in the first class in both parts, and he was awarded the Harkness Scholarship "for proficiency in Geology, including Palaeontology.” After graduating he acted for three years as assistant to Professor W. J. Sollas at Oxford, where he joined Balliol College, and took the Oxford degrees of B.A. and B.Sc. During this time, too, he carried out his first important original research, a study of the Trias of Devon and Somerset on somewhat new lines. The results were embodied in a paper presented to the Geological Society in 1902 on “The Mineralogical Constitution of the Fine Material of the Bunter Pebble-Bed in the West of England.” Divergent views had been held concerning the source of the pebbles in this formation, and Thomas accordingly turned his attention to the materials of their matrix. His method, since widely practised, was to trace the various mineral constituents of the sand to their probable parent-rocks, and so to throw light on the distribution of land-areas and the direction of currents in Triassic times. In a later paper (1909) he extended the investigation to the whole of the New Red Sandstone of the West. His interest in the mineralogy of detrital deposits was shown also in his essay which gained the Sedgwick Prize (1904), the prescribed subject being “The Petrology of some group of British Sedimentary Rocks.”
赫伯特·亨利·托马斯(1876-1935
赫伯特·亨利·托马斯生于1876年3月13日,是埃克塞特和哈罗的弗雷德里克·托马斯先生的儿子。他接受了他的早期教育在埃克塞特学校,并于1894年进入悉尼苏塞克斯学院,剑桥,在那里他是第一个参展商和后来的学者。在剑桥,他为不少终生的友谊奠定了基础。他对地质学的天生爱好很快就显露出来,他是塞奇威克俱乐部的积极成员,在后来的几年里,他一直对这个俱乐部很感兴趣。1897- 1898年,他以两科第一的成绩获得了自然科学奖,并因“精通地质学,包括古生物学”而获得哈克尼斯奖学金。毕业后,他在牛津大学担任w·j·索拉斯教授的助理三年,在那里他加入了贝利奥尔学院,并获得了牛津大学的学士学位和学士学位。在此期间,他也进行了他的第一个重要的原创研究,对德文郡和萨默塞特郡的Trias进行了一些新的研究。研究结果在1902年提交给地质学会的一篇题为《英格兰西部邦特卵石床精细材料的矿物学构成》的论文中得到了体现。关于这种地层中鹅卵石的来源,人们持有不同的观点,于是托马斯把注意力转向了它们的基质材料。他的方法被广泛应用,即追踪沙子的各种矿物成分,找到它们可能的母体岩石,从而阐明三叠纪时期陆地面积的分布和洋流的方向。在后来的一篇论文(1909年)中,他将调查扩展到整个西部的新红砂岩。他对碎屑沉积物矿物学的兴趣也表现在他获得塞奇威克奖(1904年)的论文中,规定的主题是“英国沉积岩组的岩石学”。
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