1) hydrothermal explosion breccia
热液气爆角砾岩
2) Hydrothermal crypto-explosive breccia
热液隐爆角砾岩
3) hydro thermal breccia
热液角砾岩
1.
The ore-hosting sequence has been formed into hydro thermal breccia due to the thermal alteration and structural brecciation.
新疆伊宁县金山金矿床是一正在进行勘探的大型金矿,属于浅成低温热液型金矿,金山金矿床产于早石炭纪大哈拉军山组火山岩下部,容矿岩层受热液蚀变和构造角砾岩化作用形成了热液角砾岩。
4) hydrothermally eruptive
热液喷发角砾岩
1.
The Yiarmand gold deposit occurs in hydrothermally eruptive breccia of the 2nd Member of Lower Carboniferous Dahalajunshan Formation and its underlying arsenopyritized and pyritized tuffaceous clastic rocks,and the ore forming process can be divided into hydrothermally eruptive and sedimentary stage and metasomatic stage.
伊尔曼德金矿床赋存于下石炭统大哈拉军山组第二岩性段硅化热液喷发角砾岩及其下伏上泥盆统吐呼拉苏组毒砂黄铁矿化凝灰质碎屑岩中，成矿作用可分为热液喷发沉积期和热液交代蚀变成矿期。
5) 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 。
6) 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。
补充资料：角气
1.斗气。
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