阿尔卑斯期是“阿尔卑斯构造阶段”的通称。
非洲板块与欧洲板块的相对运动方向和由阿尔卑斯期变质岩。
No direct relationship has been demonstrated between the direction of relative plate motion and linear …
在“板块物理学”科学期刊的最新一期期刊（NO.474，S.236-249 ）中，科学家们证实当今的阿尔卑斯山的升高是因为这些剧烈的气候变迁。
In the latest volume of the science magazine "Tectonophysics" ( No. 474, S.236-249) the scientists prove that today's uplifting of the Alps is driven by these strong climatic variations.
这一时期，非洲还是一个岛屿，与中东和欧洲还未连接上。它北上顶起阿尔卑斯山脉的征程仍在继续。
At this time Africa was an island, not yet joined to the Middle East and Europe, but its own journey north was to trigger the formation of the Alps.
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