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前言东地中海和土耳其东南部安纳托利亚断层南界的构造轮廓,是由截然不同的两类型式组成的:①土耳其和叙利亚东南部为大陆板块碰撞型地震带;②东地中海东部莱万蒂尼(Leva-ntine)盆地为海洋板块消减地震带。在大陆碰撞区,观测到的三个地震带,地震活动多数沿比特利斯呈带状分布,地震活动与该区存在的逆冲断层的活动有关。莱万蒂尼盆地中心区的非洲与土耳其间的板块界限,已转移到安纳克西曼德尔山脉与弗洛伦斯隆起以南,对安纳托利亚断层南界大部分地震的震源机制解表明
Foreword The tectonic profile of the eastern boundary of the Anatolian Fault in the Eastern Mediterranean and in Turkey is composed of two distinct types: ① the continental slab-collision belt in Turkey and the southeastern Syrian Arab Republic; ② the Levantin in the eastern East Mediterranean The Leva-ntine basin is a seismic zone for the ocean plate. In the collision zone of the mainland, the observed three seismic zones are mostly belt-shaped distribution along Bitlisle, and the seismic activity is related to the activity of the thrust faults existing in the area. The plate boundary between Africa and Turkey in the center of the Levandin Basin has been shifted to the south of the Annaksarmandal Range and the uplift of the Florens up to the focal mechanism underlying most of the Anatolia Fault Solution shows