A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts, South Tibet
The Himalayan leucogranite occurs as two extensive（〉1000 km） E-W trending belts on the Tibetan Plateau with the unique features. The leucogranite comprised biotite granite, two-mica/muscovite granite, tourmaline granite and garnet granite, which have been identified in previous studies, as well as a...
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| Veröffentlicht in: | Science China. Earth sciences 2017-09, Vol.60 (9), p.1655-1663 |
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| creator | Wang, RuCheng Wu, FuYuan Xie, Lei Liu, XiaoChi Wang, JiaMin Yang, Lei Lai, Wen Liu, Chen |
| description | The Himalayan leucogranite occurs as two extensive（〉1000 km） E-W trending belts on the Tibetan Plateau with the unique features. The leucogranite comprised biotite granite, two-mica/muscovite granite, tourmaline granite and garnet granite, which have been identified in previous studies, as well as albite granite and granitic pegmatite that were identified in this investigation. Fifteen leucogranite plutons were studied and 12 were found to contain rare-metal bearing minerals such as beryl（the representative of Be mineralization）, columbite-group minerals, tapiolite, pyrochlore-microlite, fergusonite, Nb-Ta rutile（the representative of Nb-Ta mineralization）, and cassiterite（the representative of Sn mineralization） mainly based on the field trip,microscope observation and microprobe analysis. The preliminary result shows that the Himalayan leucogranite is commonly related to the rare-metal mineralization and warrants future investigation. Further exploration and intensive research work is important in determining the rare-metal resource potential of this area. |
| doi_str_mv | 10.1007/s11430-017-9075-8 |
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The leucogranite comprised biotite granite, two-mica/muscovite granite, tourmaline granite and garnet granite, which have been identified in previous studies, as well as albite granite and granitic pegmatite that were identified in this investigation. Fifteen leucogranite plutons were studied and 12 were found to contain rare-metal bearing minerals such as beryl（the representative of Be mineralization）, columbite-group minerals, tapiolite, pyrochlore-microlite, fergusonite, Nb-Ta rutile（the representative of Nb-Ta mineralization）, and cassiterite（the representative of Sn mineralization） mainly based on the field trip,microscope observation and microprobe analysis. The preliminary result shows that the Himalayan leucogranite is commonly related to the rare-metal mineralization and warrants future investigation. Further exploration and intensive research work is important in determining the rare-metal resource potential of this area.</description><identifier>ISSN: 1674-7313</identifier><identifier>EISSN: 1869-1897</identifier><identifier>DOI: 10.1007/s11430-017-9075-8</identifier><language>eng</language><publisher>Beijing: Science China Press</publisher><subject>Beryllium aluminum silicates ; Biotite ; Cassiterite ; Earth and Environmental Science ; Earth Sciences ; Exploration ; Garnet ; Granite ; Identification ; Igneous rocks ; Metals ; Mica ; Mineral exploration ; Mineralization ; Minerals ; Muscovite ; Niobium ; Pegmatite ; Plateaus ; Plutons ; Research Paper ; Rutile ; Tantalum ; Tourmaline ; 喜马拉雅 ; 淡色花岗岩 ; 电子探针分析 ; 花岗岩带 ; 西藏南部 ; 金属矿化 ; 钠长石花岗岩 ; 黑云母花岗岩</subject><ispartof>Science China. Earth sciences, 2017-09, Vol.60 (9), p.1655-1663</ispartof><rights>Science China Press and Springer-Verlag GmbH Germany 2017</rights><rights>Science China Earth Sciences is a copyright of Springer, 2017.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c343t-d4da6ea95923bf0e1b6b7435c765c290d191fead019876293a6582a51ef31a0c3</citedby><cites>FETCH-LOGICAL-c343t-d4da6ea95923bf0e1b6b7435c765c290d191fead019876293a6582a51ef31a0c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/60111X/60111X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11430-017-9075-8$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11430-017-9075-8$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Wang, RuCheng</creatorcontrib><creatorcontrib>Wu, FuYuan</creatorcontrib><creatorcontrib>Xie, Lei</creatorcontrib><creatorcontrib>Liu, XiaoChi</creatorcontrib><creatorcontrib>Wang, JiaMin</creatorcontrib><creatorcontrib>Yang, Lei</creatorcontrib><creatorcontrib>Lai, Wen</creatorcontrib><creatorcontrib>Liu, Chen</creatorcontrib><title>A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts, South Tibet</title><title>Science China. Earth sciences</title><addtitle>Sci. China Earth Sci</addtitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><description>The Himalayan leucogranite occurs as two extensive（〉1000 km） E-W trending belts on the Tibetan Plateau with the unique features. The leucogranite comprised biotite granite, two-mica/muscovite granite, tourmaline granite and garnet granite, which have been identified in previous studies, as well as albite granite and granitic pegmatite that were identified in this investigation. Fifteen leucogranite plutons were studied and 12 were found to contain rare-metal bearing minerals such as beryl（the representative of Be mineralization）, columbite-group minerals, tapiolite, pyrochlore-microlite, fergusonite, Nb-Ta rutile（the representative of Nb-Ta mineralization）, and cassiterite（the representative of Sn mineralization） mainly based on the field trip,microscope observation and microprobe analysis. The preliminary result shows that the Himalayan leucogranite is commonly related to the rare-metal mineralization and warrants future investigation. Further exploration and intensive research work is important in determining the rare-metal resource potential of this area.</description><subject>Beryllium aluminum silicates</subject><subject>Biotite</subject><subject>Cassiterite</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Exploration</subject><subject>Garnet</subject><subject>Granite</subject><subject>Identification</subject><subject>Igneous rocks</subject><subject>Metals</subject><subject>Mica</subject><subject>Mineral exploration</subject><subject>Mineralization</subject><subject>Minerals</subject><subject>Muscovite</subject><subject>Niobium</subject><subject>Pegmatite</subject><subject>Plateaus</subject><subject>Plutons</subject><subject>Research Paper</subject><subject>Rutile</subject><subject>Tantalum</subject><subject>Tourmaline</subject><subject>喜马拉雅</subject><subject>淡色花岗岩</subject><subject>电子探针分析</subject><subject>花岗岩带</subject><subject>西藏南部</subject><subject>金属矿化</subject><subject>钠长石花岗岩</subject><subject>黑云母花岗岩</subject><issn>1674-7313</issn><issn>1869-1897</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kTFPwzAQhSMEEgj6A9gsWDH44sSOx6oCilSJgTJbl-TSpkqT1naG8utxVYSY8HKW7r17uu-S5BbEIwihnzxAJgUXoLkROufFWXIFhTIcCqPP41_pjGsJ8jKZeL8R8cnYSfVVglO2c9S127ZHd2A-jPWBDQ1z6IhvKWDHYoscdu0XhnboWduzsCY2b7fY4QF71tFYDSuHfRuIldQF_8A-hjGs2bItKdwkFw12niY_9Tr5fHlezuZ88f76NpsueCUzGXid1agITW5SWTaCoFSlzmReaZVXqRE1GGgIawGm0Co1ElVepJgDNRJQVPI6uT_N3blhP5IPdjOMro-RFozMdaoijaiCk6pyg_eOGrtzcRN3sCDsEaY9wbQRpj3CtEX0pCePj9p-Re7P5H9Mdz9B66Ff7aPvN0nFU6S5NoX8BjTUgpc</recordid><startdate>20170901</startdate><enddate>20170901</enddate><creator>Wang, RuCheng</creator><creator>Wu, FuYuan</creator><creator>Xie, Lei</creator><creator>Liu, XiaoChi</creator><creator>Wang, JiaMin</creator><creator>Yang, Lei</creator><creator>Lai, Wen</creator><creator>Liu, Chen</creator><general>Science China Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>20170901</creationdate><title>A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts, South Tibet</title><author>Wang, RuCheng ; 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Earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, RuCheng</au><au>Wu, FuYuan</au><au>Xie, Lei</au><au>Liu, XiaoChi</au><au>Wang, JiaMin</au><au>Yang, Lei</au><au>Lai, Wen</au><au>Liu, Chen</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts, South Tibet</atitle><jtitle>Science China. Earth sciences</jtitle><stitle>Sci. China Earth Sci</stitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><date>2017-09-01</date><risdate>2017</risdate><volume>60</volume><issue>9</issue><spage>1655</spage><epage>1663</epage><pages>1655-1663</pages><issn>1674-7313</issn><eissn>1869-1897</eissn><abstract>The Himalayan leucogranite occurs as two extensive（〉1000 km） E-W trending belts on the Tibetan Plateau with the unique features. The leucogranite comprised biotite granite, two-mica/muscovite granite, tourmaline granite and garnet granite, which have been identified in previous studies, as well as albite granite and granitic pegmatite that were identified in this investigation. Fifteen leucogranite plutons were studied and 12 were found to contain rare-metal bearing minerals such as beryl（the representative of Be mineralization）, columbite-group minerals, tapiolite, pyrochlore-microlite, fergusonite, Nb-Ta rutile（the representative of Nb-Ta mineralization）, and cassiterite（the representative of Sn mineralization） mainly based on the field trip,microscope observation and microprobe analysis. The preliminary result shows that the Himalayan leucogranite is commonly related to the rare-metal mineralization and warrants future investigation. Further exploration and intensive research work is important in determining the rare-metal resource potential of this area.</abstract><cop>Beijing</cop><pub>Science China Press</pub><doi>10.1007/s11430-017-9075-8</doi><tpages>9</tpages></addata></record> |
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| subjects | Beryllium aluminum silicates Biotite Cassiterite Earth and Environmental Science Earth Sciences Exploration Garnet Granite Identification Igneous rocks Metals Mica Mineral exploration Mineralization Minerals Muscovite Niobium Pegmatite Plateaus Plutons Research Paper Rutile Tantalum Tourmaline 喜马拉雅 淡色花岗岩 电子探针分析 花岗岩带 西藏南部 金属矿化 钠长石花岗岩 黑云母花岗岩 |
| title | A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts, South Tibet |
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