半自形粒状结构

矿石为自形-半自形粒状结构、浸染状构造。

The ores show idiomorphic or hypidiomorphic granular structure and disseminated texture .

金红石呈半自形粒状结构，多分布于透闪石矿物之间。

Rutile exists as subhedral granular texture , and is mainly distributed between tremolite .

矿石结构主要为压碎结构、半自形-自形粒状结构、填隙结构，矿石构造主要为脉状构造、细网脉状构造、浸染状构造。

The main ore textures are cataclastic texture , hypidiomorphic-euhedral granular texture and interstitial texture . Ore structures are mainly vein structures , fine stockwork structures and disseminated structures .

矿石多具自形、半自形、他形粒状结构，以脉状、浸染状构造为主。

The automorphic , hypidiomorphic and xenomorphic granular textures are the main ore textures and vein and disseminated structures are the main ore structure .