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Fault zones in shales are brecciaed and clayey, while those in limestones are of blocky structure.
断层带的页岩主要是由亚黏土和角砾岩组成，而石灰岩主要呈块状结构。
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In this deposit, ore bodies exist in the stratoid form and are c ontrolled by thrust faults. The host rocks are limestone in Bolila Formation of Late Triassic Jiezha Group and in Gadikao Formation of Early-Middle Permian Kaix i nling Group, with strong dolomitization and weak silicification. Minerals are ra ther simple and consist of sphalerite, galena, pyrite, calcite, dolomite and barite. The important ore textures are colloforms such as framboid and crust and xenom orphic grains, and the ore structures are in disseminated, brecciated, veinlike and lumpy forms.
东莫扎抓铅锌矿床矿体呈似层状展布，产状严格受到矿区逆冲断层的控制，赋矿围岩为上三叠统结扎群波里拉组灰岩和下-中二叠统开心岭群尕迪考组灰岩，发育强白云石化和弱硅化，矿物组合简单，主要为闪锌矿+方铅矿+黄铁矿+白云石+方解石+重晶石，矿石结构以皮壳状、草莓状等胶状结构和他形粒状结构为主，矿石构造为浸染状、角砾状、团块状和脉状。
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antithetic fault：反倾断层
"对偶块状断层,反向块状断层","antithetic block fault" | "反倾断层","antithetic fault" | "反信风,反贸易风","antitrade wind"
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block faulting：块状断层作用
块状 massive | 块状断层作用 block faulting | 块状泥炭 amorphous peat