Geomorphology and Neotectonics of Eastern Siberia. On the Centenary of the Birth of A.G. Zolotarev

O. Bazhenova, E. Kononov, V. Plyusnin, A. Tulokhonov
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Abstract

Doctor of Geography, Professor Anatoly Gavrilovich Zolotarev (02.18.1921– 01.15.2011) takes a worthy place in the history of Siberian science and Irkutsk State University. He was a bright and, we can say, unique personality, combining the qualities of a recognized leader, a talented organizer of science and higher university education, a brilliant lecturer and teacher, and, finally, a geologist – a highly qualified investigator. The area of his scientific interests was the geomorphology of Eastern Siberia, the latest tectonics of the Siberian platform and pre-rift transition zones of Eastern Siberia. He examined in detail the stages and features of the formation and structure of the Baikal-Patom step-vaulted uplift, as well as the latest tectonics and geomorphological structure of the Khubsugul region. He developed corrections for calculating the total amplitudes of vertical neotectonic movements – for the initial level, given the fluctuations of the World Ocean and corrections for the lithomorphic level. The result of these studies was the conclusion about the subsidence of some parts of the Siberian platform, and not their uplift, as previously thought. These new data were taken into account when compiling maps of the latest tectonics of the south of Eastern Siberia on a scale of 1: 1,500,000 under the guidance of A.G. Zolotarev. Zolotarev created a powerful Siberian scientific and educational geomorphological school, distinguished by high efficiency both in the field of fundamental and applied geomorphology, and in the training of specialists in geomorphology.
东西伯利亚的地貌与新构造。佐罗塔列夫诞辰一百周年纪念
地理学博士,教授阿纳托利·佐洛塔列夫(1921年2月18日- 2011年1月15日)在西伯利亚科学史和伊尔库茨克国立大学占有重要地位。他是一个聪明的,我们可以说,独特的个性,集公认的领导者,科学和高等大学教育的天才组织者,杰出的讲师和教师,最后,一个地质学家-一个高素质的调查员的品质于一身。他的科学兴趣领域是东西伯利亚的地貌学,西伯利亚地台的最新构造和东西伯利亚的裂谷前过渡带。他详细研究了贝加尔湖-帕托姆阶梯式隆起的形成和结构的阶段和特征,以及库布苏古尔地区最新的构造和地貌结构。他提出了计算垂直新构造运动总振幅的修正方法——考虑到世界海洋的波动,计算初始水平的新构造运动的总振幅;这些研究的结果是关于西伯利亚地台某些部分的下沉,而不是之前认为的凸起的结论。在佐罗塔列夫(A.G. Zolotarev)的指导下,以1:15万比例尺绘制东西伯利亚南部最新构造图时,考虑了这些新数据。佐洛塔列夫创建了一个强大的西伯利亚地貌学科学和教育学校,其特点是在基础地貌学和应用地貌学领域以及地貌学专家的培训方面效率很高。
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