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本文由区域地质背景及成矿系列两大部份组成。按台槽——多旋回和板块构造的观点,扼要论述了云南及其周围的区域地质背景;从区域大地构造、板内运动及其发展、裂谷成矿、岛弧成矿、陆壳形变与重熔型壳源酸碱性岩演化、浅层活化成矿等方面来论述云南矿产成矿系列及其控制因素。按矿源亲缘岩系和成矿定位环境两大要素,将云南矿产划分为亲缘于碱性超基性岩浆的、蛇绿岩套的、铁质(超)基性杂岩的、富钠质及拉斑质基性火山岩的、幔壳混合源岛弧——造山带闪长质岩浆的、壳源重熔花岗质岩浆的、混合岩化和区域变质的、浅成活化的、沉积的、风化的十个成矿系列。
This article is composed of two parts of regional geological background and metallogenic series. According to the theory of platform trough-multi-cycles and plate tectonics, the regional geological background of Yunnan and its surroundings is briefly discussed. From the regional tectonics, intra-plate movement and its development, rifting and mineralization, island arc mineralization and continental crustal deformation And the remelting of crustal source acid-base alkaline rock evolution, shallow activation and mineralization and other aspects to discuss mineral deposits in Yunnan and its control factors. Based on the two major elements of source rock series and metallogenic positioning environment, the mineral resources of Yunnan are classified into basic magma, ophiolite suite, iron (ultra) basic complex, sodium rich and Porphyry basic volcanic rocks, mantle-shell mixed source island arc-orogenic dioritic magma, crustal remelted granitic magma, migmatitic and regional metamorphic, shallowly activated, sedimentary, Weathered ten metallogenic series.