柞山地区为一泥盆纪热水沉积盆地，其遥感环形构造是矿化集中区的基本格局。
Zhashan area is a slurry sedimentary basin, it's remote annular structure is main pattern of mineral region.
构造格局与沉积特征、生产实践均表明，该地层格架较为合理。
Structure patterns, sedimentary features and production reveal that the formation framework is reasonable.
地裂运动形成的构造格局对沉积、成岩有一定的控制作用，进而在一定程度上控制了该区油气的分布。
The structural framework, formed by Emei Taphrogenesis, controlled the sedimentation and diagenesis, thus more or less controlled the distribution of hydrocarbon in the area.
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