东北太平洋堪察加半岛中部堪察加坳陷地貌学

IF 1.9 4区 地球科学 Q2 GEOGRAPHY
E. Zelenin, A. Gurinov, S. Garipova, A. Zakharov
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引用次数: 0

摘要

堪察加半岛位于欧亚大陆东部活动边缘,毗邻千岛-堪察加俯冲带。在这项研究中,我们提供了勘察加半岛中部凹陷的地形图——勘察加半岛最大的沉积盆地,也是北太平洋所有岛弧中的沉积盆地。该凹陷沿着勘察加半岛在纬度~ 44 - 46°N延伸400多公里,宽达100公里。勘察加中部洼地的地形图以1:50万的比例设计,包含约3000个地图对象。火山和构造地貌已从出版的资料中收集,并按地图比例尺进行了归纳。利用遥感数据和野外地貌调查绘制了冰川和河流地貌图。已概述了解释不明确的领域。该图是该地区发表的最详细的地貌图,对进一步的地貌和古地理研究具有指导意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geomorphology of the Central Kamchatka Depression, the Kamchatka Peninsula, NE Pacific
The Kamchatka Peninsula lies on the eastern active margin of Eurasia, adjacent to the Kuril-Kamchatka subduction zone. In this study, we provide a geomorphological map of the Central Kamchatka Depression – the largest sedimentary basin in Kamchatka and also in all the island arcs of the North Paci fi c. The depression extends along Kamchatka at latitudes ∼ 44 – 46° N for more than 400 km and is up to 100 km wide. The geomorphological map of the Central Kamchatka Depression is designed at a scale of 1:500,000 and contains ∼ 3000 mapped objects. Volcanic and tectonic landforms have been collected from published sources and generalised to the map scale. Glacial and fl uvial landforms have been mapped using remote sensing data and fi eld geomorphological surveys. Areas of ambiguous interpretation have been outlined. This map is the most detailed geomorphological map published for this region that may guide further geomorphological and paleogeographical investigations.
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来源期刊
Journal of Maps
Journal of Maps 地学-自然地理
CiteScore
4.30
自引率
9.10%
发文量
83
审稿时长
6-12 weeks
期刊介绍: The Journal of Maps is a peer-reviewed, inter-disciplinary, online journal that aims to provide a forum for researchers to publish maps and spatial diagrams.
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