Displacement and distortion in orogenic systems

山地带代表了地球上最具活力和最复杂的构造体系。除了重塑地壳和改变地幔动力学之外，山脉带还可以对生物圈、水圈和大气层产生深远的影响。这些带不是静态的实体，而是动态的系统，对板块构造的大规模变化和更局部的因素（如集中的剧烈侵蚀）做出反应。山带的动态性质可以导致一系列复杂的时空上不同的变形、变质和热事件的保存。了解这些有时看起来完全不同的地质历史如何在一个单一的带内联系起来，对于阐明控制其演化的过程至关重要。最近提出的假设如何大的山区带演变可以通过调查动态的空间和时间之间的关系，位移和变形的造山带，并通过确定收敛是如何适应整个不断变化的山区带进行测试。

Mountain belts represent the most dynamic and complex tectonic systems on earth. In addition to remoulding the earth's crust and altering mantle dynamics, mountain belts can also have a profound effect on the biosphere, hydrosphere, and atmosphere. These belts are not static entities, but rather are dynamic systems that react to both large- scale changes in plate tectonics and more local factors such as focused vigorous erosion. The dynamic nature of mountain belts can result in the preservation of a complex series of spatially and temporally distinct deformational, metamorphic, and thermal episodes. Understanding how these sometimes seemingly disparate geologic histories relate within a single belt is critical to elucidating the processes that govern its evolution. Recent hypotheses proposed for how large mountain belts evolve can be tested by investigating the dynamic spatial and temporal relationships between displacement and distortion within orogens and by ascertaining how convergence is accommodated throughout evolving mountain belts.