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厄尔布鲁斯山位于土耳其板块俯冲至西徐亚板块之下而形成的大高加索弧形构造带的弧顶部位,本身为晚更新世和全新世两个火山口组成的复式火山锥。厄尔布鲁斯山隆升过程和机制可划分为4 个阶段:中生代板块俯冲形成大高加索相对隆起区;新生代早期板块碰撞使大高加索成为强烈隆起区;新生代晚期发育了厄尔布鲁斯复式火山锥,并使之成为欧洲最高峰;许多迹象表明,厄尔布鲁斯火山现代并未熄灭,厄尔布鲁斯山以10 m m /a 的速度继续隆升。
The Elbrus Mountain is located on the top of the arc of the Greater Caucasus arc tectonic belt formed by the subduction of the Turkish plate beneath the Xisuanya plateau. It is itself a volcanic cone of two volcanoes late Pleistocene and Holocene. The uplift process and mechanism of Elbrus Hill can be divided into four stages: the Mesozoic plate subduction formed the Great Caucasus relative uplift zone; the Early Paleozoic plate collision caused the Great Caucasus to become a strong uplift zone; and the late El Cenozoic developed the Elbrus complex volcanic cone And made it Europe’s highest peak; there are many signs that the Elbrus volcano has not ceased to be modern and that Elbrus Hill continues its uplift at a rate of 10 mm / a.