Analysis of the ore-controlling structure of the Shihu gold deposit, Hebei Province and deep-seated ore-prospecting prediction
Under the guidance of the theory of mantle-branch structure-associated metallogenesis and on the basis of the geological characteristics, analysis of the ore-forming and ore-controlling structures, the geochemical characteristics of metallogenesis, the source of ore-forming materials, changes in the...
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| Veröffentlicht in: | Acta geochimica 2009-12, Vol.28 (4), p.386-396 |
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| creator | Niu, Shuyin Wang, Baode Sun, Aiqun Chen, Chao Wang, Zili Ma, Baojun Wang, Wenxue Jiang, Xiaoping Zhao, Yongli Gao, Yincang Liu, Huabin Qiu, Jianping |
| description | Under the guidance of the theory of mantle-branch structure-associated metallogenesis and on the basis of the geological characteristics, analysis of the ore-forming and ore-controlling structures, the geochemical characteristics of metallogenesis, the source of ore-forming materials, changes in the physical and chemical conditions of metallogenesis, changes in the vertical width of ore veins, and changes in gold grade of the Shihu gold deposit, the mechanism of its metallogenesis was discussed and the rules of vertical variation of ore veins were summarized in this study. It is pointed out that the orebodies under exploitation at present time should be in the middle and upper portions of gold veins in the Shihu gold mining district. Particularly on the basis of the characteristics of mantle-branch structure-associated metallogenesis, it is indicated that metallogenesis is controlled mainly by such ore-forming conditions as temperature and pressure. Deep-seated ore-forming fluids are characterized mainly by injection and precipitation. So the vein bodies in the adjacent metallogenic structures are of obvious comparability, and there would be great prospects for ore search both at depth and in the periphery of the Shihu gold deposit. Therefore, ore prospecting should be strengthened both at depth and in the peripheries. |
| doi_str_mv | 10.1007/s11631-009-0386-1 |
| format | Article |
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It is pointed out that the orebodies under exploitation at present time should be in the middle and upper portions of gold veins in the Shihu gold mining district. Particularly on the basis of the characteristics of mantle-branch structure-associated metallogenesis, it is indicated that metallogenesis is controlled mainly by such ore-forming conditions as temperature and pressure. Deep-seated ore-forming fluids are characterized mainly by injection and precipitation. So the vein bodies in the adjacent metallogenic structures are of obvious comparability, and there would be great prospects for ore search both at depth and in the periphery of the Shihu gold deposit. Therefore, ore prospecting should be strengthened both at depth and in the peripheries.</description><identifier>ISSN: 1000-9426</identifier><identifier>ISSN: 2096-0956</identifier><identifier>EISSN: 1993-0364</identifier><identifier>EISSN: 2365-7499</identifier><identifier>DOI: 10.1007/s11631-009-0386-1</identifier><language>eng</language><publisher>Heidelberg: SP Science Press</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Geology ; Gold ; Metallography ; Veins (geology)</subject><ispartof>Acta geochimica, 2009-12, Vol.28 (4), p.386-396</ispartof><rights>Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg 2009</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a2878-d8f2952f4ec6c6cb0eca60c6f132ee14e7717ea671a52bad9f06b56931dfe3653</citedby><cites>FETCH-LOGICAL-a2878-d8f2952f4ec6c6cb0eca60c6f132ee14e7717ea671a52bad9f06b56931dfe3653</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/zgdqhx-e/zgdqhx-e.jpg</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Niu, Shuyin</creatorcontrib><creatorcontrib>Wang, Baode</creatorcontrib><creatorcontrib>Sun, Aiqun</creatorcontrib><creatorcontrib>Chen, Chao</creatorcontrib><creatorcontrib>Wang, Zili</creatorcontrib><creatorcontrib>Ma, Baojun</creatorcontrib><creatorcontrib>Wang, Wenxue</creatorcontrib><creatorcontrib>Jiang, Xiaoping</creatorcontrib><creatorcontrib>Zhao, Yongli</creatorcontrib><creatorcontrib>Gao, Yincang</creatorcontrib><creatorcontrib>Liu, Huabin</creatorcontrib><creatorcontrib>Qiu, Jianping</creatorcontrib><title>Analysis of the ore-controlling structure of the Shihu gold deposit, Hebei Province and deep-seated ore-prospecting prediction</title><title>Acta geochimica</title><addtitle>Chin. J. Geochem</addtitle><description>Under the guidance of the theory of mantle-branch structure-associated metallogenesis and on the basis of the geological characteristics, analysis of the ore-forming and ore-controlling structures, the geochemical characteristics of metallogenesis, the source of ore-forming materials, changes in the physical and chemical conditions of metallogenesis, changes in the vertical width of ore veins, and changes in gold grade of the Shihu gold deposit, the mechanism of its metallogenesis was discussed and the rules of vertical variation of ore veins were summarized in this study. It is pointed out that the orebodies under exploitation at present time should be in the middle and upper portions of gold veins in the Shihu gold mining district. Particularly on the basis of the characteristics of mantle-branch structure-associated metallogenesis, it is indicated that metallogenesis is controlled mainly by such ore-forming conditions as temperature and pressure. Deep-seated ore-forming fluids are characterized mainly by injection and precipitation. So the vein bodies in the adjacent metallogenic structures are of obvious comparability, and there would be great prospects for ore search both at depth and in the periphery of the Shihu gold deposit. Therefore, ore prospecting should be strengthened both at depth and in the peripheries.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Gold</subject><subject>Metallography</subject><subject>Veins (geology)</subject><issn>1000-9426</issn><issn>2096-0956</issn><issn>1993-0364</issn><issn>2365-7499</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kU1r3DAQhk1poJuPH9Cb6K0QJSPJK1nHZWmaQCCFJmehtUdeB1fySnY-eshvjzZOyanooBHzvC-aeYviK4MzBqDOE2NSMAqgKYhKUvapWDCtRX7J8nOuAYDqkssvxWFK9wBcCKUWxcvK2_45dYkER8YtkhCR1sGPMfR951uSxjjV4xTxH_B7220n0oa-IQ0OIXXjKbnEDXbkVwwPna-RWL_v4UAT2hGbN88hhjRgPe49h4hNl8vgj4sDZ_uEJ-_3UXF38eN2fUmvb35erVfX1PJKVbSpHNdL7kqsZT4bwNpKqKVjgiOyEpViCq1UzC75xjbagdwspRascSjkUhwV32ffR-ud9a25D1PMkyfzt2122yeDPK8OSoAqs99mNn95N2EaP2AOpdIctMoQm6E6z5UiOjPE7o-Nz4aB2Sdi5kRMtjX7RAzLGj5rUmZ9i_HD-P-iV4cmj9o</recordid><startdate>20091201</startdate><enddate>20091201</enddate><creator>Niu, Shuyin</creator><creator>Wang, Baode</creator><creator>Sun, Aiqun</creator><creator>Chen, Chao</creator><creator>Wang, Zili</creator><creator>Ma, Baojun</creator><creator>Wang, Wenxue</creator><creator>Jiang, Xiaoping</creator><creator>Zhao, Yongli</creator><creator>Gao, Yincang</creator><creator>Liu, Huabin</creator><creator>Qiu, Jianping</creator><general>SP Science Press</general><general>Springer Nature B.V</general><general>College of Resources, Shijiazhuang University of Economics, Shijiazhuang 050031, China%Shijiazhuang Integrated Geological Party, Shijiazhuang 050081, China%Shihu Gold Mine, Shijiazhuang 050506, China</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20091201</creationdate><title>Analysis of the ore-controlling structure of the Shihu gold deposit, Hebei Province and deep-seated ore-prospecting prediction</title><author>Niu, Shuyin ; 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J. Geochem</stitle><date>2009-12-01</date><risdate>2009</risdate><volume>28</volume><issue>4</issue><spage>386</spage><epage>396</epage><pages>386-396</pages><issn>1000-9426</issn><issn>2096-0956</issn><eissn>1993-0364</eissn><eissn>2365-7499</eissn><abstract>Under the guidance of the theory of mantle-branch structure-associated metallogenesis and on the basis of the geological characteristics, analysis of the ore-forming and ore-controlling structures, the geochemical characteristics of metallogenesis, the source of ore-forming materials, changes in the physical and chemical conditions of metallogenesis, changes in the vertical width of ore veins, and changes in gold grade of the Shihu gold deposit, the mechanism of its metallogenesis was discussed and the rules of vertical variation of ore veins were summarized in this study. It is pointed out that the orebodies under exploitation at present time should be in the middle and upper portions of gold veins in the Shihu gold mining district. Particularly on the basis of the characteristics of mantle-branch structure-associated metallogenesis, it is indicated that metallogenesis is controlled mainly by such ore-forming conditions as temperature and pressure. Deep-seated ore-forming fluids are characterized mainly by injection and precipitation. So the vein bodies in the adjacent metallogenic structures are of obvious comparability, and there would be great prospects for ore search both at depth and in the periphery of the Shihu gold deposit. Therefore, ore prospecting should be strengthened both at depth and in the peripheries.</abstract><cop>Heidelberg</cop><pub>SP Science Press</pub><doi>10.1007/s11631-009-0386-1</doi><tpages>11</tpages></addata></record> |
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| ispartof | Acta geochimica, 2009-12, Vol.28 (4), p.386-396 |
| issn | 1000-9426 2096-0956 1993-0364 2365-7499 |
| language | eng |
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| source | SpringerLink Journals; Alma/SFX Local Collection |
| subjects | Earth and Environmental Science Earth Sciences Geochemistry Geology Gold Metallography Veins (geology) |
| title | Analysis of the ore-controlling structure of the Shihu gold deposit, Hebei Province and deep-seated ore-prospecting prediction |
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