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赤铁矿矿石形态
Hematite ore morphology
单晶常呈板状，主要由板面（平行双面）与菱面体等所组成的聚形。集合体形态多样：显晶质的有片状、鳞片状或块状；隐晶质的又鲕状、肾状、粉末状和土状等。赤铁矿根据形态等特征，又有以下的一些名称：具金属光泽的片状集合体者，称镜铁矿；具金属光泽的细鳞片状集合体者，称云母赤铁矿；呈鲕状或肾状的称鲕状或肾状赤铁矿；粉末状的赤铁矿称铁赭石。
Crystal often presents a plate shape, mainly by the surface (parallel sided) and rhombohedral consisting of poly shape. A collection of morphological diversity: explicit crystalline flake, flake or block; cryptocrystalline and oolitic, reniform, powder and earthy etc.. According to the morphological characteristics of hematite, and some of the names of the following: the metallic luster of lamellar aggregates, called Specularite; metallic luster of fine scale like aggregates, called mica hematite; is called the oolitic or kidney shaped oolitic hematite or kidney shaped; powdered hematite called iron ochre.
赤铁矿的形态特征与其形成条件的关系是：一般由热液作用形成的赤铁矿可呈板状、片状或菱面体的晶体形态；云母赤铁矿是沉积变质作用的产物；鲕状和肾状赤铁矿是沉积作用的产物。
The relationship between morphological features of hematite and forming condition is: generally formed by the hydrothermal process of hematite crystalline morphology of plate, sheet or rhombohedral; mica hematite is a product of sedimentary metamorphism; oolitic and kidney shaped hematite is a product of sedimentation.
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