Hydrothermalism in the Mediterranean Sea
Hydrothermalism in the Mediterranean Sea
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DOI：
10.1016/s0079-6611(99)00032-4
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发表时间：
1999-01-01
影响因子：
4.1
通讯作者：
Varnavas, SP
中科院分区：
文献类型：
--
作者：
Dando, PR;Stüben, D;Varnavas, SP
地中海的热液作用是非洲板块和欧洲板块碰撞的结果，非洲板块的海洋部分俯冲到欧洲之下。火山弧及其弧后拉张区的高热流形成了热液对流系统。大多数已知的热液地点都在沿海浅沃茨，
Hydrothermalism in the Mediterranean Sea results from the collision of the African and European plates, with the subduction of the oceanic part of the African plate below Europe. High heat Rows in the resulting volcanic arcs and back-are extensional areas have set-up hydrothermal convection systems. Most of the known hydrothermal sites are in shallow coastal waters,