西班牙东南科迪勒拉Betic的内带,由几个重叠的大型逆冲岩席组成,但其各自具有不同的p-T-t演化史。根据野外和实验研究,现已确定了Mulhacen杂岩体和Almanzora单元的p-T-t轨迹和变形图解(图1,略)。在Mulhacen杂岩体的q-T-t轨迹的最初部分,可以鉴别出三个有不同意义的阶段,它们与地壳俯冲有关。第一阶段发生沉积岩的俯冲并迅速向地壳深部迁移。p-T条件表明大约俯冲到37km深度。但未观察到变形构造,这就证明了该构造作用 The inner zone of the Cordillera Betic in southeastern Spain consists of several superimposed large thrust beds, each with a different p-T-t evolution history. Based on field and experimental studies, p-T-t traces and deformation diagrams of the Mulhacen complex and Almanzora unit have been identified (Fig. 1, omitted). In the initial part of the q-T-t orbit of the Mulhacen complex, three distinct phases can be identified that are related to crustal subduction. Sedimentary rocks subducted in the first stage and migrated rapidly to the deep crust. The p-T condition indicates a subduction to a depth of 37 km. However, no deformation was observed, demonstrating the tectonic effect