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虽然由沉积盆地活化作用形成的金属矿床最终取决于沉积场所的物理和化学条件,然而矿化的格式、规模及时间的选择要受总体上与地壳环境演化有关的构造和岩浆事件的影响。在地热梯度高、火成活动广泛的太古宙期间,沉积作用对矿化没有起什么作用。元古宙初克拉通地块发育,紧接着沉积盆地中形成的矿床种类和规模增加,从此以后克拉通盖层的形成为金属沉积提供了重要场所。这些金属从各种源区进入盆地,一些是来自基底的风化剥蚀,另一些是被产生于地幔或下部地壳的岩浆和挥发份携带到地表的,说明矿化时间的选择与由全球构造特征所确定的主要岩浆和构造事件有关。
Although the metal deposits formed by the activation of sedimentary basins ultimately depend on the physical and chemical conditions at the depositional site, the choice of mineralization format, size and timing is subject to structural and magmatic events that are generally associated with the evolution of the crustal environment. Sedimentation does not play a role in mineralization during the Archean, which has a high geothermal gradient and extensive fire activities. Early Proterozoic cratonic massif developed, followed by sedimentary basins formed in the type and size of deposits increased, since the formation of cratonic caprock provides an important place for metal deposition. These metals enter the basin from a variety of source areas, some from weathering and denudation from the substrate and others carried to the surface by magma and volatiles originating in the mantle or lower crust, indicating that the choice of mineralization time corresponds to the choice of mineralization time by the Global Structural Feature Institute Determined by the main magma and tectonic events.