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西藏伦坡拉盆地发育了一套第三纪内陆湖相碎屑岩系.由于其中具有较丰富的油气显示,历来受到人们的重视.
A set of Tertiary lacustrine clastic rocks developed in Tibet’s Penrapula Basin has always been valued by people because of its abundant oil and gas displays.