对岩墙延伸机制的分析在某种程度上依赖于对与岩墙的侵入作用伴生的小构造的详细填图。在以色列的Ramon地区发现了许多极好的这类构造露头,为分析岩墙的延伸过程提供了新的依据。在Ramon地区大约出露有200个玄武质和粗面质成分的岩墙和岩席,它们在早白垩纪时侵入到三叠系和侏罗系的地层中。岩墙群由位于南部未出露的中心侵入体向外延伸达30km,形成一个放射状 The analysis of the extension mechanism of the dyke depends to some extent on the detailed mapping of the small structures that accompany the intrusion of the dyke. In the Ramon area of ​​Israel many excellent tectonic outcrops have been discovered that provide a new basis for the analysis of the extension of dikes. Approximately 200 basaltic and epicontinental dikes and mats were revealed in the area of ​​Ramon, which intruded into Triassic and Jurassic formations during the Early Cretaceous. The dyke swarm extends outward by up to 30 km from the undisturbed central intrusion in the south to form a radial