The sedimentary fillings of Qianjiang Formation are mainly controlled by structural evolution and ancient climate conditions.
潜江组沉积充填主要受到盆地的构造演化和古气候条件控制.
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Mineralization occurred in the stages of the structural evolution, resulting in the corresponding deposit types.
盆地构造演化的各阶段都伴随著特定的成矿作用, 形成了相应的矿床类型.
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