Distribution of radioactive isotopes in rock and ore of Arkhangelskaya pipe from the Arkhangelsk diamond province
The contents of radioactive elements and the uranium isotopic composition of kimberlite in the Arkhangelskaya pipe at the M.V. Lomonosov deposit and of nearby country rocks have been studied. A surplus of 234 U isotope has been established in rocks from the near-pipe space. The high γ = 234 U/ 238 U...
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Veröffentlicht in: | Geology of ore deposits 2017-09, Vol.59 (5), p.391-406 |
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creator | Kiselev, G. P. Yakovlev, E. Yu Druzhinin, S. V. Galkin, A. S. |
description | The contents of radioactive elements and the uranium isotopic composition of kimberlite in the Arkhangelskaya pipe at the M.V. Lomonosov deposit and of nearby country rocks have been studied. A surplus of
234
U isotope has been established in rocks from the near-pipe space. The high γ =
234
U/
238
U ratio is controlled by the geological structure of the near-pipe space. A nonequilibrium uranium halo reaches two pipe diameters in size and can be regarded as a local ore guide for kimberlite discovery. The rocks in the nearpipe space are also characterized by elevated or anomalous U, Th, and K contents with respect to the background. |
doi_str_mv | 10.1134/S1075701517050014 |
format | Article |
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234
U isotope has been established in rocks from the near-pipe space. The high γ =
234
U/
238
U ratio is controlled by the geological structure of the near-pipe space. A nonequilibrium uranium halo reaches two pipe diameters in size and can be regarded as a local ore guide for kimberlite discovery. The rocks in the nearpipe space are also characterized by elevated or anomalous U, Th, and K contents with respect to the background.</description><identifier>ISSN: 1075-7015</identifier><identifier>EISSN: 1555-6476</identifier><identifier>DOI: 10.1134/S1075701517050014</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Composition ; Diamonds ; Earth and Environmental Science ; Earth Sciences ; Geological structures ; Isotopes ; Mineral Resources ; Pipes ; Radioisotopes ; Rock ; Rocks ; Uranium</subject><ispartof>Geology of ore deposits, 2017-09, Vol.59 (5), p.391-406</ispartof><rights>Pleiades Publishing, Ltd. 2017</rights><rights>Copyright Springer Science & Business Media 2017</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-18f663f0bd7efa58d744dbe9412a1ca64eda3b3acbe99d87f44b396949402c163</citedby><cites>FETCH-LOGICAL-a339t-18f663f0bd7efa58d744dbe9412a1ca64eda3b3acbe99d87f44b396949402c163</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1075701517050014$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1075701517050014$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>315,781,785,27929,27930,41493,42562,51324</link.rule.ids></links><search><creatorcontrib>Kiselev, G. P.</creatorcontrib><creatorcontrib>Yakovlev, E. Yu</creatorcontrib><creatorcontrib>Druzhinin, S. V.</creatorcontrib><creatorcontrib>Galkin, A. S.</creatorcontrib><title>Distribution of radioactive isotopes in rock and ore of Arkhangelskaya pipe from the Arkhangelsk diamond province</title><title>Geology of ore deposits</title><addtitle>Geol. Ore Deposits</addtitle><description>The contents of radioactive elements and the uranium isotopic composition of kimberlite in the Arkhangelskaya pipe at the M.V. Lomonosov deposit and of nearby country rocks have been studied. A surplus of
234
U isotope has been established in rocks from the near-pipe space. The high γ =
234
U/
238
U ratio is controlled by the geological structure of the near-pipe space. A nonequilibrium uranium halo reaches two pipe diameters in size and can be regarded as a local ore guide for kimberlite discovery. The rocks in the nearpipe space are also characterized by elevated or anomalous U, Th, and K contents with respect to the background.</description><subject>Composition</subject><subject>Diamonds</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geological structures</subject><subject>Isotopes</subject><subject>Mineral Resources</subject><subject>Pipes</subject><subject>Radioisotopes</subject><subject>Rock</subject><subject>Rocks</subject><subject>Uranium</subject><issn>1075-7015</issn><issn>1555-6476</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp1UEtLAzEQDqJgrf4AbwHPq5lNstkcS31CwYN6XrKbxKaPzTZJC_33ptRDQTzNMN-L-RC6BXIPQNnDBxDBBQEOgnBCgJ2hEXDOi4qJ6jzvGS4O-CW6inFBCOMlgRHaPLqYgmu3yfkee4uD0s6rLrmdwS765AcTsetx8N0Sq15jH8yBNwnLueq_zSou1V7hwQ0G2-DXOM3NKYi1U2ufdUPwO9d35hpdWLWK5uZ3jtHX89Pn9LWYvb-8TSezQlEqUwG1rSpqSauFsYrXWjCmWyMZlAo6VTGjFW2p6vJN6lpYxloqK8kkI2UHFR2ju6NvDt5sTUzNwm9DnyMbkLwWNchaZBYcWV3wMQZjmyG4tQr7BkhzaLb502zWlEdNzNz8ZThx_lf0A3wEfAk</recordid><startdate>20170901</startdate><enddate>20170901</enddate><creator>Kiselev, G. P.</creator><creator>Yakovlev, E. Yu</creator><creator>Druzhinin, S. V.</creator><creator>Galkin, A. S.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20170901</creationdate><title>Distribution of radioactive isotopes in rock and ore of Arkhangelskaya pipe from the Arkhangelsk diamond province</title><author>Kiselev, G. P. ; Yakovlev, E. Yu ; Druzhinin, S. V. ; Galkin, A. S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-18f663f0bd7efa58d744dbe9412a1ca64eda3b3acbe99d87f44b396949402c163</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Composition</topic><topic>Diamonds</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geological structures</topic><topic>Isotopes</topic><topic>Mineral Resources</topic><topic>Pipes</topic><topic>Radioisotopes</topic><topic>Rock</topic><topic>Rocks</topic><topic>Uranium</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kiselev, G. P.</creatorcontrib><creatorcontrib>Yakovlev, E. Yu</creatorcontrib><creatorcontrib>Druzhinin, S. V.</creatorcontrib><creatorcontrib>Galkin, A. S.</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geology of ore deposits</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kiselev, G. P.</au><au>Yakovlev, E. Yu</au><au>Druzhinin, S. V.</au><au>Galkin, A. S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Distribution of radioactive isotopes in rock and ore of Arkhangelskaya pipe from the Arkhangelsk diamond province</atitle><jtitle>Geology of ore deposits</jtitle><stitle>Geol. Ore Deposits</stitle><date>2017-09-01</date><risdate>2017</risdate><volume>59</volume><issue>5</issue><spage>391</spage><epage>406</epage><pages>391-406</pages><issn>1075-7015</issn><eissn>1555-6476</eissn><abstract>The contents of radioactive elements and the uranium isotopic composition of kimberlite in the Arkhangelskaya pipe at the M.V. Lomonosov deposit and of nearby country rocks have been studied. A surplus of
234
U isotope has been established in rocks from the near-pipe space. The high γ =
234
U/
238
U ratio is controlled by the geological structure of the near-pipe space. A nonequilibrium uranium halo reaches two pipe diameters in size and can be regarded as a local ore guide for kimberlite discovery. The rocks in the nearpipe space are also characterized by elevated or anomalous U, Th, and K contents with respect to the background.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1075701517050014</doi><tpages>16</tpages></addata></record> |
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subjects | Composition Diamonds Earth and Environmental Science Earth Sciences Geological structures Isotopes Mineral Resources Pipes Radioisotopes Rock Rocks Uranium |
title | Distribution of radioactive isotopes in rock and ore of Arkhangelskaya pipe from the Arkhangelsk diamond province |
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