The xenoliths are characterized by protogranular and equigranular textures. They consist of olivine, clinopyroxene, orthopyroxene, and brown spinel. Two xenoliths contain garnet beside spinel. The xenolith include wherlite and pyroxenite which are characterized by abundant black and green spinel and garnet. They are characterized by igneous texture and by the presence of abundant spinel and or garnet exsolution blebs as well as broad exsolution lamellae of orthopyroxene in clinopyroxene.
Few xenoliths consist of lherzolite and pyroxenite viens.
Mafic two pyroxene granulite, gabbronorite and plagioclase gabbro are abundant. Xenoliths from other part of the Arabian Plate. Xenolith data from the Arabian Plate are few and are still poorly documented. The xenolith suit of Syria includes spinel and garnet peridotite, pyroxenite as well as lower crustal granulites. Magnetic study on lower crustal and upper mantle xenoliths from northeast Jordan.