regional data also show that a large-scale regional uplift of mountains in the northern edge of the qinghai-tibetan plateau occurred during oligocene-miocene period.
区域资料分析表明,青藏高原北缘在渐新世至中新世期间发生了大规模的、区域性的抬升。
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.
there is a regional uplift on the premountain belt in the south margin of the qingxi depression and local structures on this uplift is favorable for petroleum accumulation;