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云南区域地质面貌比较复杂,既不完全体现所谓地台的稳定性,也不是象地槽区那样的活动类型,而是在不同地质阶段,既表现有相对稳定及相对活动复杂的地质体。地质结构是以块断型式为主,各块体问虽有一定的内在联系,但在发展的各个阶段中却各自有着不同的发展历史。如象“山字型”东翼的滇东区,则以海相碳酸盐岩为主,自下古生代～中生代三叠系基本上沦为海域;而西翼的楚雄盆地则为陆源区,其中的次级块体也有不同的发展史及构造格局,往往只一大断裂或一古构造带相隔,沉积条件及构造
The geology of Yunnan region is rather complicated. It neither completely reflects the stability of the so-called platform nor the type of activities like the geosyncline area, but shows the geological bodies of relatively stable and relatively complex activities in different geological stages. Geological structure is based on the block pattern, although the block asked a certain intrinsic relationship, but in all stages of development but each has a different history of development. For example, the eastern Yunnan region of the “Shanzi type” is dominated by marine carbonates and has basically become a sea area since the Paleozoic to Mesozoic Triassic, while the Chuxiong basin in the west wing is a land source area Of the secondary blocks also have different development history and tectonic structure, often only a large fault or an ancient tectonic belt apart, deposition conditions and structure