Structural and Geological Elements of Teide Volcanic Complex : Rift Zones and Gravitational Collapses
Structural and Geological Elements of Teide Volcanic Complex : Rift Zones and Gravitational Collapses
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泰德火山群的结构和地质要素：裂谷带和重力塌陷
DOI：
10.1007/978-3-642-25893-0_4
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发表时间：
2013
期刊：
影响因子：
--
通讯作者：
V. Troll
中科院分区：
文献类型：
--
作者：
J. Carracedo;V. Troll
最初在夏威夷群岛发现的火山裂谷带和相关的巨型山体滑坡在加那利群岛得到了广泛的研究，并在那里确定了几个更重要的结构和遗传要素。加那利群岛西部有近3，000公里长的水道（galerías），为进入岛屿建筑物的深层结构提供了独特的可能性。最近的工作表明，控制岛屿建造的裂谷带可能从岛屿发展的最初阶段就开始形成主要的地貌特征（形状和地形），并集中爆发活动，使其成为确定海洋岛屿上火山灾害分布的关键因素。
Initially recognised in the Hawaiian Islands, volcanic rift zones and associated giant landslides have been extensively studied in the Canaries, where several of their more significant structural and genetic elements have been established. Almost 3,000 km of water tunnels (galerías) that exist in the western Canaries provide a unique possibility to access the deep structure of the island edifices. Recent work shows that rift zones to control the construction of the islands, possibly from the initial stages of island development, form the main relief features (shape and topography), and concentrate eruptive activity, making them crucial elements in defining the distribution of volcanic hazards on ocean islands.