1) Hypo-rhyolite porphyry
次流纹斑岩
2) rhyolite porphyry
流纹斑岩
1.
The ore deposit was surrounded by fractures of NE and NW directions,and generically relat-ed to rhyolite porphyry,The early alterations are mainly of K-feldsparization and biotitiza-tion,and the laters are mainly of silication,sericitization and propylitization.
成矿主要与流纹斑岩有关。
3) liparitic mortar lava
流纹质碎斑熔岩
1.
A special kind of liparitic mortar lava with the texture of both lava and ignimbrite is developed in Simuke area,Northern Daxinganling.
在大兴安岭北段斯木科地区发育一种具有独特结构特征的火山岩石类型———流纹质碎斑熔岩,其具有熔岩和熔结凝灰岩的双重结构。
4) rhyolite?dacite porphyry
流纹英安斑岩
1.
Identification of rhyolite?dacite porphyry and its relation to uranium mineralization at Xiangshan uranium ore-field;
相山铀矿田流纹英安斑岩的厘定及与铀矿化的关系
5) perthitophyre
纹长斑岩
6) perthitophyre
条纹长斑岩
补充资料:流纹岩
流纹岩 rhyolite 一种酸性喷出岩。成分与花岗岩相当。灰白色或浅粉红色。常见有流纹构造和斑状玻璃质、球粒、霏细、显微文象等结构。斑晶常为石英、碱性长石,有时有少量斜长石;基质一般为致密的隐晶质或玻璃质。产状多为岩丘。脱玻化明显的流纹岩称为流纹斑岩。流纹岩在中国东南沿海各省有广泛分布,北方辽宁、内蒙古、河北、山西、山东、吉林、黑龙江也都有分布。与之有关的矿产有高岭石、蒙脱石、叶蜡石、明矾石和黄铁矿等。
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