Chapter 7.1 Deception Island

A. Geyer, D. Pedrazzi, J. Almendros, M. Berrocoso, J. López-Martínez, A. Maestro, E. Carmona, A. Álvarez-Valero, A. de Gil
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引用次数: 12

Abstract

Abstract Deception Island (South Shetland Islands) is one of the most active volcanoes in Antarctica, with more than 15 explosive eruptive events registered over the past two centuries. Recent eruptions (1967, 1969 and 1970) and volcanic unrest episodes in 1992, 1999 and 2014–15 demonstrate that the occurrence of future volcanic activity is a valid and pressing concern for scientists, logistic personnel and tourists that are visiting or are working on or near the island. Over the last few decades, intense research activity has been carried out on Deception Island to decipher the origin and evolution of this very complex volcano. To that end, a solid integration of related scientific disciplines, such as tectonics, petrology, geochemistry, geophysics, geomorphology, remote sensing, glaciology, is required. A proper understanding of the island's evolution in the past, and its present state, is essential for improving the efficiency in interpreting monitoring data recorded during volcanic unrest periods and, hence, for future eruption forecasting. In this chapter, we briefly present Deception Island's most relevant tectonic, geomorphological, volcanological and magmatic features, as well as the results obtained from decades of monitoring the island's seismic activity and ground deformation.
第7.1章欺骗岛
欺骗岛(南设得兰群岛)是南极洲最活跃的火山之一,在过去的两个世纪里发生了超过15次爆炸性喷发事件。最近的火山喷发(1967年、1969年和1970年)以及1992年、1999年和2014年至2015年的火山动荡事件表明,未来火山活动的发生是科学家、后勤人员和在岛上或附近访问或工作的游客的一个有效和紧迫的问题。在过去的几十年里,人们在欺骗岛进行了激烈的研究活动,以破译这座非常复杂的火山的起源和演变。为此目的,需要将有关的科学学科,例如构造学、岩石学、地球化学、地球物理、地貌学、遥感、冰川学等牢固地结合起来。正确了解该岛过去的演变及其现状,对于提高解释火山不稳定时期记录的监测数据的效率,从而对未来的喷发预测至关重要。在本章中,我们简要介绍了欺骗岛最相关的构造、地貌、火山和岩浆特征,以及几十年来监测岛上地震活动和地面变形的结果。
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