通过对湖南沃溪矿床的宏观至微观尺度上的矿石组构学研究，揭示出矿床系同生热水沉积成因。
Ore fabric studies of the Woxi W_Sb_Au deposit on macro_ to micro_ scales have revealed that the deposit is of syngenetic hydrothermal sedimentary origin.
层序地层学为沉积盆地分析的一个重要手段和方法。层序地层学在沉积盆地分析中的参数包括宏观参数和微观参数。
As an important method, the parameter of sequence stratigraphy applied to the sedimentary basin includes macroscopic one and microcosmic one.
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