据角砾灰岩的岩石学特征及其与围岩地层的组合关系,该角砾岩主要属岩屑流和浊流沉积的深水碳酸盐岩。
According to their petrological characteristics and relations with surrounding rocks, we can regard them as deep water carbonate rocks of the debris flow and turbidity current sediments.
碳酸盐岩岩屑流具有以下特征:(1)角砾岩为块状,具有清楚的边界。
Its features are: 1. The carbonate breccias are massive and have clear boundary with a plane or wavy bottom.
主要容矿岩石为浅变质细碎屑岩,钠长碳酸盐角砾岩及碳硅泥质岩;
The ore-bearing rock are mainly fine elastic rocks, breccia of albite-carbonate and carbonaceous- siliceous argillaceous rock.
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