spilite
- 网络细碧岩
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The other rocks , such as silicalite , jaspilite , spilite , tuffaceous sandstone , show high resistivity and low chargeability ( 1 % ~ 3 % ) in nature .
其余硅质岩、碧玉岩、细碧岩、凝灰质砂岩为高阻低极化,视极化率一般在1%~3%。
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The mineral parageneses of the volcanic rocks are generally consistent with that of spilite or keratophyre .
这些火山岩所含的次生矿物群大致符合细碧岩或角斑岩之定义。
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Its ore types include altered spilite and pyrite quartz - sericite altered and quartz vein .
矿石类型为蚀变细碧岩型和石英脉型。
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The pattern distributed of rare elements and REE in spilite is analogous to that of tholeiite in island curve .
细碧岩微量元素及稀土元素分配型式类似岛弧拉斑玄武岩。
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Thin basalt ( spilite ) layers are often interbedded in those deep marine radiolaria-bearing siliceous rocks .
与深海相放射虫硅质岩相伴,则夹有玄武岩(细碧岩)层。
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Suggestion on the classification of spilite keratophyre and their nomenclature
对细碧-石英角斑岩系种属划分和命名的建议
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Spilite-keratophyre sequence is generally divided into spilite , keratophyre and quartz keratophyre .
细碧&角斑岩系一般分为细碧岩、斑岩和石英角斑岩三类。
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It was considered earlier that the spilite and keratophyre were formed by direct crystallization from a mixture of magma and seawater .
过去认为北祁连褶皱带的细碧-角斑质火山岩,在成因上是由于岩浆与海水混染后的结晶产物。
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The spilite is greyish-green , display massive structure and locally pillow structures with palimpsest interweave texture and intergranular texture .
岩石呈灰绿色,块状构造,局部可见枕状构造,可见变余交织和变余粒间结构。
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It mainly consists of spilite , keratophyre and volcanic clastics , intercalated with siliceous rocks , limestone and clastic rocks or lens .
主要由细碧岩、角斑岩及火山碎屑岩组成,其中有硅质岩、灰岩及碎屑岩夹层或凸镜体。