橄榄玄武岩的英文

• dorgalite
• olivine basalt

• "橄榄"英文翻译    Chinese olive; the fruit of ...
• "玄武岩"英文翻译    basalt
• "碱性橄榄玄武岩" 英文翻译 :    alkali olivine basalt
• "碱性橄榄玄武岩岩浆" 英文翻译 :    alkali olivine basalt magma
• "橄榄石玄武岩" 英文翻译 :    olivine basalt
• "长橄榄斑玄武岩" 英文翻译 :    dunsapie basalt
• "碱性橄榄石玄武岩" 英文翻译 :    alkali olivine basalt; alkaline olivine basalt
• "碱性橄榄岩玄武岩" 英文翻译 :    alkaliolivine basalt
• "橄榄硅质玄武岩" 英文翻译 :    olivine tholeiite
• "橄榄拉斑玄武岩" 英文翻译 :    olivine tholeiite
• "橄榄矽质玄武岩" 英文翻译 :    olivine tholeiite
• "橄榄中长玄武岩" 英文翻译 :    hawaiite
• "橄榄玄粗岩" 英文翻译 :    shoshonite
• "玄武岩" 英文翻译 :    basalt
• "玄武岩玄武岩玄武岩底" 英文翻译 :    basalt
• "安粗玄武岩" 英文翻译 :    latibasalt
• "安山玄武岩" 英文翻译 :    andesite basalt; andesite-basalt; andesitic basalt
• "暗色玄武岩" 英文翻译 :    melabasalt
• "暗霞玄武岩" 英文翻译 :    tannbuschite
• "白榴玄武岩" 英文翻译 :    cecilite(cecelite); leucite basalt; leucitoid basalt
• "斑点玄武岩" 英文翻译 :    flecked basalt; freckled basalt
• "斑苏玄武岩" 英文翻译 :    peleeite
• "斑玄武岩" 英文翻译 :    inninmorite
• "板状玄武岩" 英文翻译 :    laminated basalt
• "倍苏玄武岩" 英文翻译 :    sudburite

• Siziwangqi of inner mongolia is located on the north margin of north china craton , the junction of north china craton and siberia . granulite xenoliths are found there in cretaceous basalt . these xenoliths are mainly plagioclase - pyroxenite
  内蒙古四子王旗地区地处华北板块北缘，与西伯利亚板块的接合部，其早白垩世橄榄玄武岩中发现大量下地壳麻粒岩捕虏体，并可见辉石长石捕虏晶。
• 4 . three type of basalt is recognized in changle region : a , sapphire - embodied alkli - olivine - basalt of niushan group ( most distributed in fangshan ) , enriched with a large number of mantle - orignated xenoliths with different extent of weathering ; b , alkli - olivine - basalt of niushan group with little sapphire embodied , but contan a few mantle - orignated xenoliths usually samller than that of fangshan , most of the mantle - orignated xenoliths weathered seriously only lefting with some vacant caves , this kind of rock mostly lies in cangshan , taohuashan . and qiaoguan volcanic vent , contain amount of ilmenite ; c , olivine - basalt of yaoshan group , contain neither xenoliths nor sapphire
  4 、在昌乐地区区分出三类主要的玄武岩： a ，牛山组含矿的碱性橄榄玄武岩，位于方山，含大量的大小不一的风化蚀变程度不同的地幔岩包体； b ，牛山组几乎不含矿的碱性橄榄玄武岩，含少量地幔岩包体，且包体一般比方山小，多数已经遭严重风化而只留下空洞，含有相当数量的钛铁矿，主要位于北岩南部的苍山，桃花山及乔官火山口。