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在Montmarault花岗岩体东部分支上进行了磁性组构研究.磁性面理(与围岩中的磁性面理一致)和磁性线理的代表性倾向在岩体东部(二长花岗岩)向SE,在岩体西部(花岗闪长岩)向NWW,暗示着存在一个轴向SW倾的背形构造,该SW方向与某些点上的磁性线理相一致.
Magnetic fabric studies have been performed on the eastern part of the Montmarault granite body.The representative trends in magnetic (consistent with the magnetic in the surrounding rock) and magnetic linearises are toward the SE in the eastern part of the rock (SE) The body west (granodiorite) toward NWW suggests the existence of an axial SW-tilted back-shaped structure that is consistent with the magnetic principles at some points.