对西南极菲尔德斯半岛早第三纪火山岩岩石学、地球化学特征及岩浆作用过程的具体分析表明，其岩浆演化过程是岩浆系统与周围环境（介质）进行能量和物质交换的热能耗散过程，具有动态平衡和阶段性的特点。岩浆结晶的多级复合结构和高位岩浆房中的分带构造，是岩浆作用非平衡过程的自组织现象。这种自组织现象也称作耗散结构 The analysis of the petrological, geochemical characteristics and magmatism of Early Tertiary volcanic rocks in the Fields Peninsula, Western Antarctica shows that the magmatic evolution process is the thermal energy dissipation process of energy exchange between the magma system and the surrounding environment (medium) With dynamic balance and stage characteristics. The multistage composite structure of the magma and the zonation structure of the high-lying magma chamber are self-organized phenomena of the non-equilibrium magmatic process. This phenomenon of self-organization is also called dissipative structure