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1)  diabaseprophyrite
辉绿玢岩脉
1.
There are two types of diabaseprophyrite dikes in the third member of the Cretaceous Yingcheng Formation at the Shanghewan area in the southeastern uplift of the Songliao Basin.
在松辽盆地东南隆起上河湾地区出露的白垩系营城组第三岩性段火山岩中有两种产状的辉绿玢岩脉侵入:其一,沿着NE30°~35°走向的追踪张节理侵入,岩脉边界呈锯齿状,岩脉宽度1~5 m,倾角75°~88°;其二,岩脉沿NE40°~45°走向的一组剪切节理侵入,岩脉边界光滑平直,围岩接触面上发育倾角平缓的线理或擦痕,运动方向总体呈现左行,脉体倾角75°~88°,岩脉宽度2~10 m。
2)  diabase porphyrite dikes
辉绿玢岩
1.
During the Late Cretaceous the Taipingyan diabase porphyrite dikes with NNE strike emplaced into the eastern part of the Guidong composite granitoids in northern Guangdong Province.
晚白垩世太平奄组辉绿玢岩位于粤北贵东复式岩体东部,呈NNE向展布。
3)  diabasite
辉绿玢岩类
4)  diabase dike
辉绿岩脉
1.
Selecting the representative test area,the technology of high-pressure cement-chemical compound grouting is adopted to carry out experimental research on grouting reinforcement treatment of diabase dikes for determining grouting technique,and the effect and mechanism of reinforcement,etc.
选择代表性试验区,采用高压水泥–化学复合灌浆技术,对辉绿岩脉的灌浆加固处理开展灌浆工艺、加固效果和机制等试验研究。
5)  pyroxene porphyrite
辉石玢岩
1.
Based on petrochemical and geochemical studies,the paper comes to the conclusion that the pyroxene porphyrite bodies are an alkalic basalt series,which have generated from the different evolutionary stages of a primary magma,i.
对岚皋地区辉石玢岩岩石化学和地球化学研究表明,本区辉石玢岩为碱性玄武岩系列;不同期次活动的辉石玢岩为同源岩浆在不同阶段上演化的产物;演化趋势属跨越B型,本区辉石纷岩形成于板内稳定区,是早古生代南秦岭被动大陆边缘裂谷的岩浆活动时的产物,该裂谷扩张速度与东非埃塞俄比亚相近。
6)  olivine-pyroxene prphyrite
橄辉玢岩
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1.明亮貌。
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