矿石组构 meaning in English
ore fabric
Examples
- There are intensive structural and magmatic hydrothermal movement with obvious zonal surface shape alterations , which are demonstrated by silicified function , sericitization , potassium , epidotization , hornstone , etc . the ore structural fabric mainly behaves in form of filling action with minerals such as pyrite , chalcopyrite , salenite , blende and electrum , which typomorphic feature shows a hypothermal pattern of metallogeny
呈面型蚀变，分带特征明显。矿区内矿体规模巨大，矿石组构主要为以充填交代作用为主，矿石矿物主要为黄铁矿、黄铜矿、闪锌矿、方铅矿和银金矿。而且矿物的标型特征显示了低温成矿的特点。 - Taking it for example that zhujiabaobao section of panzhihua vanadic titano - magnetite deposit , the paper detailedly analysed its change regularity in ore texture and structure , mineral composition and content , ore chemical composition , mineral chemical composition , rare element " s change feature of rock and ore , exploding temperature of mineral inclusion . on the basis of above , the feature of rhythmic texture of ore body in panzhihua vanadic titano - magnetite deposit was researched
本文以攀枝花钒钛磁铁矿朱家包包矿段为例，详细分析了该矿段中矿石组构、矿物成分及含量、矿石化学成分、矿物化学成分、岩石及矿石稀土元素变化特征、矿物包裹体爆裂温度等的变化规律，进而研究了攀枝花钒钛磁铁矿矿体中的韵律结构特征。 - Through researching the rhythmic change regularity of ore texture and structure , mineral composition and content , rare element " s change feature and the exploding temperature of mineral inclusion , combining the theory of magmatic ore - forming , the forming process of panzhihua vanadic titano - magnetite deposit could be divided into four periods : rock - forming period , main ore - forming period , hydrothermal period and surficial processing period
通过对矿石组构、矿物成分及含量、稀土元素变化特征、矿物包裹体爆裂温度的韵律式变化规律的研究，结合岩浆成矿理论，将攀枝花钒钛磁铁矿矿床的形成过程划分为四个期：成岩期、主成矿期、热液期、表生期。 - On the basis of the study on ore deposit geology , the paper discussed thedistribution of temperature field of ore body through mineral inclusion thermometry . combining with mineralizing elements distribution condition and the zoning feature of orefabrics , flowing direction of ore - forming fluid was also inferred in the paper
在研究矿床地质的基础上,使用矿物包裹体测温方法,研究矿体温度场的分布,配合矿化元素的分布状态和矿石组构分带特征,推断成矿流体的喷口位置和运移方向。