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青藏高原北部可可西里鲸鱼湖、雄鹰台、双泉子火山岩中含有辉石岩包体,其主要矿物为单斜辉石和斜方辉石.辉石的化学成分与国内外慢源包体——橄榄岩和辉石岩中的类似,与麻粒岩中的明显不同;辉石温压计计算结果表明,辉石形成的温度为1101～1400℃(平均为1250℃),压力为3～6 GPa(平均为4.6 GPa),推测岩浆的来源深度大于150 km.
In the northern part of the Qinghai-Tibet Plateau, there are pyroxenite inclusions in the Hoh Xil Lake, Xiong Yingtai and Shuangquanzi volcanic rocks in Hoh Xil, and the main minerals are clinopyroxene and orthopyroxene. The chemical composition of pyroxene is similar to that of the slow- The pyroxene thermometer shows that the pyroxene formation temperature is 1101-1400 ℃ (average 1250 ℃) and the pressure is 3-6 GPa (4.6 GPa on average), suggesting that the origin of magma is greater than 150 km.