1) potassic trachyte porphyry
钾质粗面斑岩
1.
The ore featured by veinlets and disseminations is hosted both inside the fault zone in the upper Jurassic Ehuling ignimbrite and the potassic trachyte porphyry.
生米坑铅锌矿床位于北武夷中生代火山岩带的黄岗山火山盆地内,已知铅锌矿体呈脉状产于侏罗系上统鹅湖岭组流纹质熔结凝灰岩的断裂内,或呈细脉——浸染状分布于钾质粗面斑岩内,发育钾长石化、绿泥石化、硅化等蚀变。
2) potassic trachybasalt
钾质粗面玄武岩
3) trachyte porphyry
粗面斑岩
1.
The Oulituozi and the Huangshatuo trachyte porphyry intrusions, that are separated less than 10 km apart, occur in the middle segment of the Eastern depression of the Liaohe basin and intrude in the Eocene carbonaceous and argillic hydrocarbon source beds of the third member of the Shahejie formation.
地球化学分析表明,两岩体均为粗面斑岩,成分非常一致,很可能在深部相连或来源于同一岩浆房。
4) 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。
5) K-bentonite
钾质斑脱岩
1.
K-bentonites and black shales from the Wufeng-Longmaxi formations(Early Paleozoic, South China) and Xiamaling formation (Early Neoproterozoic, North China)—implications for tectonic processes during two important transitions;
华南五峰组—龙马溪组与华北下马岭组的钾质斑脱岩及黑色岩系——两个地史转折期板块构造运动的沉积响应
2.
An overview of Ordovician and Silurian K-bentonites
奥陶纪和志留纪钾质斑脱岩研究评述
3.
Advances in research on K-bentonite have been systematically reviewed in this paper.
从矿物学、地球化学两个方面对钾质斑脱岩的研究进展进行综合评述。
6) kalium rich trachyte
富钾粗面岩
补充资料：玄武
| 玄武 见四方之神。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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