Rift basins in mountain belts shed light on the palaeogeography and tectonic development of adjacent sutured ocean basins, as for the Antalya Complex in the S Neotethys region. Based on literature review, supplemented by multidisciplinary new data, the Antalya Complex in this area represents an Upper Permian-Triassic rift basin and subsequent Jurassic-Cretaceous passive margin that encompasses a marginal shallow-water carbonate platform, slope facies and deeper water axial pelagic sediments and basaltic volcanics. The rift basin was bordered to the north by the Tauride Carbonate Platform, and to the south by the metamorphic Alanya Massif farther south. The S Neotethys was located further south, adjacent to N Africa.

中文翻译：

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东地中海地区南新特提斯北部大陆边缘深水裂谷（古泽尔苏走廊）的下古生代-古近纪地质发育：来自安塔利亚杂岩和邻近的牛里德碳酸盐台地的证据

山地带中的裂谷盆地揭示了邻近缝合洋盆的古地理和构造发育，就像南新特提斯地区的安塔利亚杂岩一样。根据文献综述，并辅以多学科新数据，该地区的安塔利亚杂岩代表了上二叠统-三叠统裂谷盆地和随后的侏罗纪-白垩纪被动边缘，包括边缘浅水碳酸盐台地、斜坡相和更深的水轴中上层沉积物和玄武岩火山岩。该裂谷盆地的北部与塔夫里德碳酸盐台地接壤，南部与更南边的变质阿拉尼亚地块接壤。南新特提斯群岛位于更南端，毗邻北非。