...表小区域红外线反射研究(Cruikshank, 1969)即出现数条吸收带,其位置与实验室中橄榄石(Olivine)和正 辉石 ( Orthopyroxene )所含之二价铁的光谱位置相当。此种比较研究,当可有助于月球表面岩石组成的识别。
基于24个网页-相关网页
The Yangyuan pyroxenite xenoliths all are websterites in which clinopyroxene is more abundant than orthopyroxene.
阳原辉石岩包体均为二辉岩,且多数样品中单斜辉石的含量大于斜方辉石。
参考来源 - 华北克拉通西部岩石圈地幔的性质:河北阳原新生代玄武岩中幔源包体提供的信息·2,447,543篇论文数据,部分数据来源于NoteExpress
N a member of the pyroxene group of minerals having an orthorhombic crystal structure, such as enstatite and hypersthene 斜方辉石类
The major rock forming minerals include olivine, orthopyroxene, clinopyroxene, plagioclase and amphibole.
其主要造岩矿物为橄榄石、斜方辉石、单斜辉石、斜长石和角闪石。
According to the study of olivine and peridotite anisotropy and the mineral compositions in the peridotite, the orthopyroxene can reduce the overall effect of the anisotropy.
橄榄石、橄榄岩地震波各向异性与橄榄岩中矿物含量的研究,定量的说明了斜方辉石的效果是降低总体的各向异性。
应用推荐