2) 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。
3) Cryptoexplosive breccia
隐爆角砾岩
1.
Discovery of cryptoexplosive breccia type Cu (-Au) orebodies in Tonglushan skarn-type Cu-Fe deposit of Hubei Province and ore-searching vista;
湖北铜绿山矽卡岩型铜铁矿床中隐爆角砾岩型金(铜)矿体的发现及其找矿前景
2.
The recently discovered Chenjiazhangzi gold deposit in southern Chifeng, Inner Mongolia belongs to the cryptoexplosive breccia type related to Mesozoic magmatism - a new type in this area.
赤峰市南部地区位于北东向中生代大兴安岭岩浆火山岩带与华北地台北缘东西向构造的交汇部位,中生代岩浆火山岩带侵入并覆盖了前寒武纪结晶基底,形成了一套广泛分布的火山、次火山岩系,成矿地质条件优越,陈家杖子金矿床是近年来在该区发现的与中生代岩浆火山岩带有关的隐爆角砾岩(潜火山岩)型新类型矿床,通过对其地质、地球物理、地球化学特征的分析,初步认为陈家杖子金矿床应为一斑岩型金(铜)成矿系统的组成部分,目前查明的金矿体仅为矿床的顶部,其深部应赋存有规模更大的金、铜多金属矿体。
3.
570 cryptoexplosive breccia type U (Ag, Mo) deposit in north Fujian and No.
为进一步阐明长英质隐爆角砾岩的成因及其气热溶浸成矿流体和成矿物质的来源 ,文章对闽北 5 70及赣南 6 72 2隐爆角砾岩型铀矿床的矿石矿物、蚀变围岩、基底岩石的氧、氢、硫、碳、铅同位素地球化学特征进行了综合研究 ,并得出以下结论 :①在主成矿期和矿后期有大气降水成分的外来水混合加入成矿流体 ;②蚀变流纹岩和蚀变花岗岩的水_岩氧原子质量比值 (分别为 0 。
4) 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。
5) cryptoexplosion breccia
隐爆角砾岩
1.
Different cryptoexplosion breccia is the host rock of the gold deposit.
隐爆角砾岩型金矿是国内外一种具有重要经济价值的矿床类型。
2.
The gold-bearing hydrothermal cryptoexplosion breccias can be divided into three types ofmagmatic water,precipituted water,and mixed water.
含金热液隐爆角砾岩可划分为岩浆热液隐爆角砾岩、岩浆一天水混合热液隐爆角砾岩和天水热液隐爆角砾岩。
6) hydrothermal breccia
隐爆角砾岩
1.
Zhuojiazhuang gold deposit is a type of hydrothermal breccia pipe deposit , the main ores can be divided into four types: breccia ore cemented with ore liquid, cemented with ore-bearing hydrothermal, cemented with Syenite-porphry magma, and tuffaceous materials.
卓家庄金矿为隐爆角砾岩型金矿床 ,主要矿石类型可分为 4种 :矿浆胶结隐爆角砾岩矿石、热液胶结隐爆角砾岩矿石、熔浆胶结隐爆角砾岩矿石、凝灰质胶结隐爆角砾岩矿石。
2.
Zhuojiazhuang gold deposit is a hydrothermal breccia pipe gold deposit and characterized by high gold tenor (average gold tenor is large to 100 ×10 -6 ) and by gold mineralization in whole pipe.
平邑卓家庄金矿是隐爆角砾岩型金矿床 ,以高金品位 (平均在 10 0× 10 -6以上 )、全筒式矿化为特点。
补充资料：角砾岩
| 角砾岩 breccia 沉积碎屑岩的一种。由大于2毫米的棱角状的砾石胶结而成。组成角砾岩的碎屑物质，一般因原地堆积或搬运距离很短，因此磨圆度极低，分选很差，形状各异，棱角分明 。按形成原因可分为岩溶角砾岩、火山角砾岩、山麓堆积角砾岩、冰川角砾岩、断层角砾岩（亦称构造角砾岩）、成岩角砾岩以及陨石撞击角砾岩等。研究角砾岩可帮助恢复古地理环境，推断构造变动，有些矿产与角砾岩有关。 |
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