大浪滩梁中矿床是在青藏高原区域性隆升构造动力背景下，逐渐从统一的柴达木盆地中分隔出来而形成的次级盆地。
The Dalangtan Liangzhong deposit is a secondary basin gradually divided from the united Qaidam basin, under the background of Qinghai-Tibet Plateau's regional uplift tectonic motion.
大浪滩梁中矿床是在青藏高原区域性隆升构造动力背景下，逐渐从统一的柴达木盆地中分隔出来而形成的次级盆地。
The Dalangtan Liangzhong deposit is a secondary basin gradually divided from the united Qaidam basin, under the background of Qinghai-Tibet Plateau's regional uplift tectonic motion.
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