甘布尔泽夫山脉是南极洲冰盖下隐藏的一座山脉，位于南极洲东部的冰穹A附近，海拔高度为3500米。1958年，苏联地震专家小组首次发现甘布尔泽夫山脉。2009年，澳大利亚、英国、加拿大、中国、德国、日本和美国7个国家的科学家组成的国际研究小组在冰穹A的营地上进驻，派出两架飞机，使用雷达和航空测磁、重力传感器等对该山脉进行探测。探测结果表明，该山脉的形状和大小与欧洲阿尔卑斯山脉相似，冰川下有河流和湖泊。

The Gamburtsev Mountain Range (also known as the Gamburtsev Subglacial Mountains) is a subglacial mountain range located in East Antarctica, just underneath the lofty Dome A, near the Southern Pole of Inaccessibility. The range was discovered by the 3rd Soviet Antarctic Expedition in 1958 and is named for Soviet geophysicist Grigoriy A. Gamburtsev. It is approximately 1,200 kilometres (750 mi) long, and the mountains are believed to be about 2,700 metres (8,900 ft) high, although they are completely covered by over 600 metres (2,000 ft) of ice and snow. The Gamburtsev Mountain Range is currently believed to be about the same size as the European Alps, and, as of 2008, it is unknown how the mountains were formed, though the current speculated age of the range is over 34 million years and possibly 500 million years. Current models suggest that the East Antarctic ice sheet was formed from the glaciers that began sliding down the Gamburtsev range at the end of the Eocene. Vostok Subglacial Highlands form an east extension of Gamburtsev Subglacial Mountains.