苦橄质玄武岩
苦橄质玄武岩-
本文对在峨眉山玄武岩省中新发现的苦橄质岩石及其共生玄武岩的地球化学特征进行了研究，结果表明，除苦橄质岩石外，与其共生的玄武质岩石均属高Ti玄武岩。
The geochemical characteristics of the picritic rocks that we discovered recently and their associated basalts show that except the picrites , all the associated basaltic rocks belong to the high-Ti type .
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苦橄岩、苦橄质玄武岩和玄武岩组成的熔岩层厚100～200m。
The lava layer composed of picrite , picritic basalt and basalts is 100 to 200 m thick .