在本文中我们着重评述了由与新第三纪晚期东Betic剪切带有关的扭断裂作用产生的、并有很好的文献记载的Trans-Alboran剪切带的沉积盆地类型。描述了这种扭动“走廊”的一般特征,其中包括继承性构造的作用。强调了各种盆地类型,正如同时存在挤压与伸展机制下形成的盆地那样。在东Betic剪切带,拉分盆地看来不是最普遍的盆地类型。相反,平行于主走滑断层展布的挤压“槽状向斜”(与走滑断层走向或运动方向无关)是更有代表性的构造。这类构造以强烈 In this paper, we highlight the types of sedimentary basins in the Trans-Alboran shear zone that have been well documented by the torsional cleavage associated with the East Betic shear zone of the late Neogene. Describes the general characteristics of this twisted “corridor”, including the role of inherited constructs. Various types of basins are emphasized, just as there are basins formed under both extrusion and extension mechanisms. In the East Betic shear zone, the pull-apart basin does not appear to be the most prevalent basin type. In contrast, the extrusion “trough slant” parallel to the strike of the main strike slip (independent of strike or slip direction) is the more representative one. This type of construction is intense