The Christiana-Santorini-Kolumbo Volcanic Field

被引:22
|
作者
Nomikou, Paraskevi [1 ]
Huebscher, Christian [2 ]
Carey, Steven [3 ]
机构
[1] Univ Athens, Dept Geol & Geoenvironm, Athens 15784, Greece
[2] Univ Hamburg, Inst Geophys, Ctr Earth Syst Res & Sustainabil, Bundesstr 55, D-20146 Hamburg, Germany
[3] Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA
关键词
swath mapping; seismic profiles; tectonic faults; submarine volcanoes; hydrothermal vents; geohazards; SUBMARINE VOLCANO; AEGEAN SEA; ERUPTION; AMORGOS; EVOLUTION; TSUNAMI; MORPHOLOGY; GREECE;
D O I
10.2138/gselements.15.3.171
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Christiana-Santorini-Kolumbo volcanic field in the South Aegean Sea (Greece) is one of the most important in Europe, having produced more than 100 explosive eruptions in the last 400,000 years. Its volcanic centers include the extinct Christiana Volcano and associated seamounts, Santorini caldera with its intracaldera Kameni Volcano, Kolumbo Volcano, and 24 other submarine cones of the Kolumbo chain. Earthquakes, volcanic eruptions, submarine mass wasting, neotectonics and gas releases from these centers pose significant geohazards to human populations and infrastructures of the Eastern Mediterranean region. Defining the geological processes and structures that contribute to these geohazards will provide an important framework to guide future monitoring and research activities aimed at hazard mitigation.
引用
收藏
页码:171 / 176
页数:6
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