符山石是典型的接触交代变质形成的矿物,常见于酸性火成岩与碳酸盐岩(石灰岩与白云岩)及其他含钙沉积岩的接触带,与所谓的硅卡岩矿物—石榴子石、透辉石、硅灰石等共生。近来,由于对矿床矿物学的研究结果,已知,不仅在硅卡岩、正长岩、霞石正长岩和微粒正长岩(Orthoclasite)中有发现,而且在碱性伟晶岩中亦有 Fu Shan is a typical contact metasomatism mineralization, common in acidic igneous and carbonate rocks (limestone and dolomite) and other calcium-bearing sedimentary rock contact zone, and the so-called slay minerals - garnet, Stone, wollastonite and other symbiosis. Recently, as a result of the mineralogy of the deposit, it has been known that it has been found not only in siclane, syenite, nepheline syenite, and Orthoclasite, but also in basic pegmatites Have