在上世纪末,地质学家已经认识到阿尔卑斯主要由向北和向西移动并且相互叠置的逆冲岩系组成的(Bertrand,1984等)。从那个时期起,阿尔卑斯已成为逆冲断裂带的经典例子。从构造来看,阿尔卑斯是欧亚大陆与亚得里亚-非洲大陆碰撞的结果,在它们之间的彭奈恩洋俯冲在亚得里亚-非洲大陆之下(B(?)gel和Roeder,1978)。 At the end of the last century, geologists have recognized that the Alps are composed mainly of thrust strata that move north and west and are superimposed on each other (Bertrand, 1984, etc.). Since then, the Alps has become a classic example of a thrust belt. Structurally, the Alps were the result of the collision between the Eurasian continent and the Adriatic-African continent beneath the Adriatic-African continent (B (?) Gel and Roeder , 1978).