1) potassic lamprophyre
钾质煌斑岩
1.
They are potassic lamprophyre, not lamproites as the previous researchers believed.
塔里木板块西南缘克里阳山区的钾质煌斑岩呈脉状产于前寒武纪埃连卡特群变质沉积岩中,其主要岩石类型有:金云母透辉石煌斑岩、假白榴石透辉石煌斑岩和含球粒透辉石煌斑岩。
2) shoshonictic lamprophyres
钾玄质煌斑岩
3) lamproite
钾镁煌斑岩
1.
Up to now, the known diamond bearing rocks, pro alkaline and ultra mafic, include kimberlite, lamproite, eclogite, ophiolite suite, alkaline ultrabasic complex, alkaline ultrabasic lamprophyre, peridotite series (including harzburgite and dunite).
目前所知产金刚石的岩石类型包括金伯利岩、钾镁煌斑岩、榴辉岩、蛇绿岩套、碱性超基性杂岩、碱性超基性煌斑岩和橄榄岩类 (方辉橄榄岩、纯橄榄岩等 )等偏碱性超镁铁质岩石 ,而有经济价值的金刚石原生矿床仅见于金伯利岩和钾镁煌斑岩中 ,除此之外的其他岩石类型中仅见有少量微粒金刚石 。
2.
It is the first time that lamproites are found in south margin of the Tarim Platform.
首次在塔里木地台南缘皮山县境内找到钾镁煌斑岩，它们呈脉状产出，围岩为白云母石英片岩。
4) olive potash magnesia lamprophyre
橄榄钾镁煌斑岩
5) lamproite
钾镁煌斑岩类
6) kimberlitic lamprophyre
金伯利质煌斑岩
1.
PPAEGSS Research on kimberlitic lamprophyre pipe at Lujing in Anyuan area,Jiangxi Province——A new type of mantle-derived alkaline ultrabasic rock;
江西安远路迳金伯利质煌斑岩筒研究——一种新型的幔源碱性超基性岩
2.
In this paper,hydrogen and oxygen isotopic composition of pyroxenes from mantle-derived megacryst and xenolith of the kimberlitic lamprophyre pipe in Lujing,Anyuan,Jiangxi Province has been obtained by ion microprobe and mass spectrometer respectively.
利用离子探针和质谱技术分别分析测试了江西安远路迳金伯利质煌斑岩筒辉石巨晶和包体中辉石的氢氧同位素组成。
补充资料：煌熠
1.辉耀。
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