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1)  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
2)  hydrothermal explosion breccia
热液气爆角砾岩
3)  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。
4)  Hydrothermal crypto-explosive breccia
热液隐爆角砾岩
5)  hydrothermal breccia
热水角砾岩
6)  breccio-conglomerate
角砾砾岩
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。
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