云南龙陵县团坡铷矿的富集规律 : = THE CONCENTRATION RULE OF TUANPO RB DEPOSIT IN LONGLING,YUNNAN
云南龙陵县团坡铷矿为典型的风化壳淋积矿床,矿体呈面状赋存于加里东晚期松坡岩体细粒含云二长花岗岩相之风化壳中,其Rb_2O组分在风化壳的全风化层中最为富集含量较高,现已探明的Rb_2O资源储量已达到大型。因该地区温暖潮湿的气候,促使花岗岩体风化壳发育,充沛的降雨有利于Rb_2O的淋溶下渗富集成矿床。.
Tuanpo Rb deposit in Longling,Yunnan is a typical leaching deposit in weathering crust.The deposit is in an areal weathering crust of Late Caledonian fine grained mica-bearing adamellite,Rb_2O_3 is most rich in the complete weathering bed of weathering crust,explored reserves have reached the large scale.Because the weather in this area is warm and moist,the weathering crust of graite body is developed.And the abundant rain is advantageous to the formation of deposit by the leaching and concentration..
| Medienart: |
E-Artikel |
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| Erscheinungsjahr: |
2019-12-15 2019 |
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| Erschienen: |
2019-12-15 |
| Enthalten in: |
Zur Gesamtaufnahme - year:2019 |
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| Enthalten in: |
Yun nan di zhi - (2019), 04 vom: 15. Dez., Seite 454-460 Original Letters: Enthalten in 云南地质 (DE-600)2998732-5 (DE-600)2998732-5 云南省昆明市 |
| Reihe: |
China Academic Journals (CAJ), A, 理工A(数学物理力学天地生) = Mathematics/ Physics/ Mechanics/ Astronomy |
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| Sprache: |
Chinesisch |
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| Weiterer Titel: |
THE CONCENTRATION RULE OF TUANPO RB DEPOSIT IN LONGLING,YUNNAN |
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| Beteiligte Personen: |
侯良刚 [VerfasserIn] |
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| Links: |
oversea.cnki.net [lizenzpflichtig] |
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| Anmerkungen: |
Author info:HOU Liang-gang;YUAN Ling;YUAN Ke-qi;Chuxiong Exploration Institute,Yunnan Bureau of Nonferrous Geology |
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| 245 | 1 | 0 | |a 云南龙陵县团坡铷矿的富集规律 |b = THE CONCENTRATION RULE OF TUANPO RB DEPOSIT IN LONGLING,YUNNAN |
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| 520 | |a 云南龙陵县团坡铷矿为典型的风化壳淋积矿床,矿体呈面状赋存于加里东晚期松坡岩体细粒含云二长花岗岩相之风化壳中,其Rb_2O组分在风化壳的全风化层中最为富集含量较高,现已探明的Rb_2O资源储量已达到大型。因该地区温暖潮湿的气候,促使花岗岩体风化壳发育,充沛的降雨有利于Rb_2O的淋溶下渗富集成矿床。 | ||
| 520 | |a Tuanpo Rb deposit in Longling,Yunnan is a typical leaching deposit in weathering crust.The deposit is in an areal weathering crust of Late Caledonian fine grained mica-bearing adamellite,Rb_2O_3 is most rich in the complete weathering bed of weathering crust,explored reserves have reached the large scale.Because the weather in this area is warm and moist,the weathering crust of graite body is developed.And the abundant rain is advantageous to the formation of deposit by the leaching and concentration. | ||
| 610 | 2 | 4 | |a 云南省有色地质局楚雄勘查院 |
| 650 | 4 | |a 矿床学 | |
| 650 | 4 | |a 天文学、地球科学 | |
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| 650 | 4 | |a 加里东期花岗岩 | |
| 650 | 4 | |a 风化壳 | |
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| 650 | 4 | |a 云南陵县团坡 | |
| 650 | 4 | |a Caledonian Granite | |
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