1) explosive pipe
爆破角砾岩筒
1.
studies show that the so called “tourmalinization explosion breccia" within some explosive pipes,in which there are copper and gold metallization,in the Eastern Xizang porphyry copper ore belt is characterized by primary volcanic subvolcanic texture and structure.
世界不少斑岩矿床内都发育有隐爆爆破角砾岩筒，其胶结物是电英岩；这些电英质胶结物一直被视为单一电英岩化产物。
2) explosion breccia
爆破角砾岩
1.
Characteristics of explosion breccia type gold deposit in Hulalin, Inner Mongolia;
内蒙古虎拉林爆破角砾岩型金矿床特征
2.
According to the gold metallogenic character in north western Qiyugou area,it is believed that the gold deposit types in the research area mainly belong to either altered fracture zone type,or explosion breccia type characterized by repeated mineralization in different times and epoches with a multiple source,and is potential for further exploration.
根据祁雨沟北西部金矿成矿地质特征,认为研究区内金矿床类型主要为蚀变破碎带型和爆破角砾岩筒型,在成因上具有多时代、多期次、成矿物质多来源特点,具有较好的找矿前景。
3) cryptoexplosive breccia pipe
隐爆角砾岩筒
1.
Qibaoshan goldcuprid deposit in Wulian county occurrs in cryptoexplosive breccia pipe, and has a close relation with subvolcano.
五莲七宝山金铜矿床赋存于隐爆角砾岩筒中 ,与次火山岩关系密切。
4) explosive breccia pipe
爆发角砾岩筒
1.
6702 explosive breccia pipe, which occurred in intercrossing section between NE arc fault and NW fault, is located at southern margin of damaged volcanic vent formed in Northeastern part of baisa-shengong volcanic active belt.
在揭露6702铀矿点的过程中，发现该矿点是处在一个典型的爆发角砾岩筒内，就着手进行研究，了解到岩筒具有一系列的隐蔽爆发特征。
5) breccia pipe
角砾岩筒
1.
Based on the research of ore-controlling laws in Hulalin gold deposit in Inner Mongolia,the authors consider that dominate disseminated mineralization was absolutely controlled by a breccia pipe.
通过对虎拉林金矿构造控矿规律研究,认为矿区占绝对优势的浸染状矿化主要受角砾岩筒构造控制,矿化不均匀,矿体形态不规则;通过分析该角砾岩筒内角砾岩的特点,结合一般浅成、半浅成角砾岩筒的垂向分带规律,推测该角砾岩筒已剥蚀到了中下部。
2.
The Yantang CuMo deposit is located in a breccia pipe of northeast Wuzhishan uplift,Hainan Island.
琼海烟塘梅岭铜钼矿床位于海南五指山隆起东北侧的一个"角砾岩筒"中,该"角砾岩筒"的形成受南北向、东西向构造-岩浆岩带控制,与燕山期花岗闪长岩、花岗闪长斑岩关系密切。
3.
There are many types of fluidogeneous tectonites inside and outside the breccia pipe with distinct space time texture.
山东七宝山角砾岩筒内外流体构造 （岩） 类型多样， 具自身特有的时空结构。
6) crypto-explosive breccia pipe-type deposits
隐爆角砾岩筒型矿床
1.
The paper describes the basic features of ore-forming fluid evolution tread curves of the crypto-explosive breccia pipe-type deposits.
阐述了隐爆角砾岩筒型矿床及其成矿过程中的隐爆流体演化趋势曲线的一般特征,在此基础上,讨论了凹山铁矿床、祁雨沟金矿床、七宝山铜金矿床等典型矿床的矿体产出特征与隐爆流体演化趋势曲线之间存在的耦合关系,结合隐爆角砾岩筒型矿床成矿流体演化的一般特征和特殊情况,对轻微剥蚀岩筒、中等剥蚀岩筒和深度剥蚀岩筒的成矿性进行了分析。
补充资料：角砾岩透镜体
分子式：
CAS号：
性质：简单撞击坑视坑底下伏一层较厚由回落角砾岩块、熔岩组成的透镜状沉积层，如Meteor、Brent、Lonar Lake、West Hawk Lake等简单撞击坑。通常上伏晚期湖相沉积物，下伏冲击压力15～20GPa的原生坑底单矿物碎屑角砾岩。整个撞击坑显示出地球物理场异常。这一沉积构造特征，可通过地球物理方法寻找被掩藏的撞击坑。
CAS号：
性质：简单撞击坑视坑底下伏一层较厚由回落角砾岩块、熔岩组成的透镜状沉积层，如Meteor、Brent、Lonar Lake、West Hawk Lake等简单撞击坑。通常上伏晚期湖相沉积物，下伏冲击压力15～20GPa的原生坑底单矿物碎屑角砾岩。整个撞击坑显示出地球物理场异常。这一沉积构造特征，可通过地球物理方法寻找被掩藏的撞击坑。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条