CAJ | 학술논문

通过对无水芒硝矿床的构造、厚度及分布特征等描述．认为顺河次凹矿层构造稳定；无水芒硝沉积厚度变化大，主要分布在次凹南部，北部缺失；主要矿层为Ⅷ层，具有分布范围广、厚度大、品位好的特点。通过对次凹内无水芒硝岩分布及岩矿特征的精细描述．指出了顺河次凹无水芒硝矿床的分布规律。对该区盐类矿床的勘探、开发具有十分重要的意义。
통과대무수망초광상적구조、후도급분포특정등묘술．인위순하차요광층구조은정；무수망초침적후도변화대，주요분포재차요남부，북부결실；주요광층위Ⅷ층，구유분포범위엄、후도대、품위호적특점。통과대차요내무수망초암분포급암광특정적정세묘술．지출료순하차요무수망초광상적분포규률。대해구염류광상적감탐、개발구유십분중요적의의。
Through description of the thenardite ore formation structure, thickness and distribution, this article indicates that the Shunhe sub-depression structure is steady and with big changes in sedimentation thickness. It is mainly distributed in south part while absent in north part. The main ore formation is VIII with wide and thick distribution and fine quality. The accurate descriptions of thenardite distribution and feature in sub-depression are of great significance for the exploration and development of salt ore in this area.