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| 陕西商县蔷薇辉石玉石矿床地质、工艺性质及成因 | |
| 引用本文： | 李靠社. 陕西商县蔷薇辉石玉石矿床地质、工艺性质及成因[J]. 陕西地质, 1992, 0(2) |
| 作者姓名： | 李靠社 |
| 作者单位： | 陕西省地质矿产局十三地质队 |
| 摘 要： | 陕西商县蔷薇辉石(粉翠)矿床是陕西省首次发现并评价的玉石矿床。蔷薇辉石产于宽坪群四岔口组中段下部二云石英片岩所夹的含锰石英白云石大理岩、含锰石英岩等含锰岩中。矿体既成层分布又相对集中。粉翠玉料质优且加工工艺性能良好。蔷薇辉石矿床的形成主要经历了沉积期和区域变质期两大阶段。成因类型属变质岩型低温变质相蔷薇辉石矿床。 |
| 关 键 词： | 蔷薇辉石 矿床地质 工艺性能 矿床成因 |
THE GEOLOGICAL CHARACTERISTICS AND THE GENESIS OF THE RHODONITE DEPOSIT IN SHAANXI PROVINCE |
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| Li Kaoshe. THE GEOLOGICAL CHARACTERISTICS AND THE GENESIS OF THE RHODONITE DEPOSIT IN SHAANXI PROVINCE[J]. Geology of Shaanxi, 1992, 0(2) | |
| Authors: | Li Kaoshe |
| Affiliation: | The Geological Team No.13 of the Shaanxi Bureau of Geology and Mineral Resources |
| Abstract: | A rhodonite deposit has been discovered and evaluated for the first time in Shaanxi Province.The rhodonite occurs in manganiferous rocks, manganiferous quartz-dolomite marble and quartzite,which are intacalated in the lower part of the middle member in the Sichagou Formation of the lower Proterozoic Kuanping Group.Though the orebodies are distributed in bedding,they are relatively conglomerated.The rhodonite deposit was for- med mainly through two stages,sedimentation and regional metamorphism, and its genetic type belongs to epithermal metamorphic facies. |
| Keywords: | rhodonite geology of ore deposit technological behaviour genesis of ore deposit |
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