Contrasting platinum-group mineral assemblages from chromitites of the Nizhny Tagil and Guli massifs (Russia): Implications for composition, sources and age
The Nizhny Tagil and Guli clinopyroxenite-dunite massifs, located in the Middle Urals and Maimecha-Kotui Province, respectively, are associated with world-class platinum-group elements (PGE) placer deposits. Both massifs contain small bodies of schlieren to massive chromitite associated with dunite....
Gespeichert in:
| Veröffentlicht in: | Doklady earth sciences 2011-11, Vol.441 (1), p.1514-1518 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1518 |
|---|---|
| container_issue | 1 |
| container_start_page | 1514 |
| container_title | Doklady earth sciences |
| container_volume | 441 |
| creator | Malitch, K. N. Efimov, A. A. Badanina, I. Yu |
| description | The Nizhny Tagil and Guli clinopyroxenite-dunite massifs, located in the Middle Urals and Maimecha-Kotui Province, respectively, are associated with world-class platinum-group elements (PGE) placer deposits. Both massifs contain small bodies of schlieren to massive chromitite associated with dunite. The predominance of Pt-Fe alloys at Nizhny Tagil is consistnt with the whole-rock “M”-shaped mantle-normalized PGE pattern of the chromitite. In contrast, the preponderance of laurite and Os-Ir alloys at Guli is consistent with a negatively sloped PGE pattern, the latter being characteristic of ophiolite-type podiform chromitites. The ‘unradiogenic’
187
Os/
188
Os values obtained for both platinum-group minerals (PGM) and chromitite are indicative of a common near-to-chondritic source for the PGE and implies that the osmium isotope budget of chromitite is largely controlled by laurite and Os-rich alloy. Average model
187
Os/
188
Os ages calculated for the Nizhny Tagil and Guli massifs correspond to the late Riphean (e.g., 862 ± 48 Ma and 616 ± 8 Ma, respectively). The compositional and isotope-geochemical results provide new constraints on the temporal evolution of ultramafic rocks of the Uralian Platinum Belt and northern segment of the Siberian Platform. |
| doi_str_mv | 10.1134/S1028334X11110067 |
| format | Article |
| fullrecord | <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_1671559308</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A360119718</galeid><sourcerecordid>A360119718</sourcerecordid><originalsourceid>FETCH-LOGICAL-a443t-251fb57f06038fea80e1398325bade07822193c661fe37f75c313f638a686d143</originalsourceid><addsrcrecordid>eNqFUl1rFTEQXUTBWv0BvgWfKrg1s_lc38pF20JR0Aq-Lbm5yd6UTbImuw_1t_hjO5crCIqYQGaYOefMDJmmeQn0HIDxt1-Adpox_g3wUCrVo-YEBINWM8Efo4_p9pB_2jyr9Y5SzrnoT5qfm5yWYuoS0kjmyaBdYzuWvM4khuSKmYip1cXtZEZXiS85ErvHNyxhwUD2ZNk78jH82Kd7cmvGgIS0I5frFEhEavCVnH1e0TGv35HrOE_BYpmcUCwXYnOccw2HwBtS81osih4EsNzz5ok3U3UvftnT5uuH97ebq_bm0-X15uKmNZyzpe0E-K1QnkrKtHdGUwes16wTW7NzVOmug55ZKcE7prwSlgHzkmkjtdwBZ6fN2VF3Lvn76uoyxFCtmyaTXF7rAFKBED2j-v9Q2lEtJFcKoa_-gN7heAkHGXroeC-Uogg6P4JGM7khJJ_xNyzenYvB5uR8wPgFkxSgV3BoAI4EW3KtxflhLiGaco-lh8MqDH-tAnK6I6ciNo2u_O7k36QHci-2JA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>912495770</pqid></control><display><type>article</type><title>Contrasting platinum-group mineral assemblages from chromitites of the Nizhny Tagil and Guli massifs (Russia): Implications for composition, sources and age</title><source>SpringerLink Journals - AutoHoldings</source><creator>Malitch, K. N. ; Efimov, A. A. ; Badanina, I. Yu</creator><creatorcontrib>Malitch, K. N. ; Efimov, A. A. ; Badanina, I. Yu</creatorcontrib><description>The Nizhny Tagil and Guli clinopyroxenite-dunite massifs, located in the Middle Urals and Maimecha-Kotui Province, respectively, are associated with world-class platinum-group elements (PGE) placer deposits. Both massifs contain small bodies of schlieren to massive chromitite associated with dunite. The predominance of Pt-Fe alloys at Nizhny Tagil is consistnt with the whole-rock “M”-shaped mantle-normalized PGE pattern of the chromitite. In contrast, the preponderance of laurite and Os-Ir alloys at Guli is consistent with a negatively sloped PGE pattern, the latter being characteristic of ophiolite-type podiform chromitites. The ‘unradiogenic’
187
Os/
188
Os values obtained for both platinum-group minerals (PGM) and chromitite are indicative of a common near-to-chondritic source for the PGE and implies that the osmium isotope budget of chromitite is largely controlled by laurite and Os-rich alloy. Average model
187
Os/
188
Os ages calculated for the Nizhny Tagil and Guli massifs correspond to the late Riphean (e.g., 862 ± 48 Ma and 616 ± 8 Ma, respectively). The compositional and isotope-geochemical results provide new constraints on the temporal evolution of ultramafic rocks of the Uralian Platinum Belt and northern segment of the Siberian Platform.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X11110067</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Age ; Alloys ; Budgeting ; Deposition ; Earth and Environmental Science ; Earth Sciences ; Geology ; Massifs ; Mathematical models ; Mineralogy ; Minerals ; Mines and mineral resources ; Ophiolites ; Osmium ; Platinum ; Platinum base alloys ; Rocks</subject><ispartof>Doklady earth sciences, 2011-11, Vol.441 (1), p.1514-1518</ispartof><rights>Pleiades Publishing, Ltd. 2011</rights><rights>COPYRIGHT 2011 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a443t-251fb57f06038fea80e1398325bade07822193c661fe37f75c313f638a686d143</citedby><cites>FETCH-LOGICAL-a443t-251fb57f06038fea80e1398325bade07822193c661fe37f75c313f638a686d143</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/S1028334X11110067$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1028334X11110067$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Malitch, K. N.</creatorcontrib><creatorcontrib>Efimov, A. A.</creatorcontrib><creatorcontrib>Badanina, I. Yu</creatorcontrib><title>Contrasting platinum-group mineral assemblages from chromitites of the Nizhny Tagil and Guli massifs (Russia): Implications for composition, sources and age</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><description>The Nizhny Tagil and Guli clinopyroxenite-dunite massifs, located in the Middle Urals and Maimecha-Kotui Province, respectively, are associated with world-class platinum-group elements (PGE) placer deposits. Both massifs contain small bodies of schlieren to massive chromitite associated with dunite. The predominance of Pt-Fe alloys at Nizhny Tagil is consistnt with the whole-rock “M”-shaped mantle-normalized PGE pattern of the chromitite. In contrast, the preponderance of laurite and Os-Ir alloys at Guli is consistent with a negatively sloped PGE pattern, the latter being characteristic of ophiolite-type podiform chromitites. The ‘unradiogenic’
187
Os/
188
Os values obtained for both platinum-group minerals (PGM) and chromitite are indicative of a common near-to-chondritic source for the PGE and implies that the osmium isotope budget of chromitite is largely controlled by laurite and Os-rich alloy. Average model
187
Os/
188
Os ages calculated for the Nizhny Tagil and Guli massifs correspond to the late Riphean (e.g., 862 ± 48 Ma and 616 ± 8 Ma, respectively). The compositional and isotope-geochemical results provide new constraints on the temporal evolution of ultramafic rocks of the Uralian Platinum Belt and northern segment of the Siberian Platform.</description><subject>Age</subject><subject>Alloys</subject><subject>Budgeting</subject><subject>Deposition</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geology</subject><subject>Massifs</subject><subject>Mathematical models</subject><subject>Mineralogy</subject><subject>Minerals</subject><subject>Mines and mineral resources</subject><subject>Ophiolites</subject><subject>Osmium</subject><subject>Platinum</subject><subject>Platinum base alloys</subject><subject>Rocks</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqFUl1rFTEQXUTBWv0BvgWfKrg1s_lc38pF20JR0Aq-Lbm5yd6UTbImuw_1t_hjO5crCIqYQGaYOefMDJmmeQn0HIDxt1-Adpox_g3wUCrVo-YEBINWM8Efo4_p9pB_2jyr9Y5SzrnoT5qfm5yWYuoS0kjmyaBdYzuWvM4khuSKmYip1cXtZEZXiS85ErvHNyxhwUD2ZNk78jH82Kd7cmvGgIS0I5frFEhEavCVnH1e0TGv35HrOE_BYpmcUCwXYnOccw2HwBtS81osih4EsNzz5ok3U3UvftnT5uuH97ebq_bm0-X15uKmNZyzpe0E-K1QnkrKtHdGUwes16wTW7NzVOmug55ZKcE7prwSlgHzkmkjtdwBZ6fN2VF3Lvn76uoyxFCtmyaTXF7rAFKBED2j-v9Q2lEtJFcKoa_-gN7heAkHGXroeC-Uogg6P4JGM7khJJ_xNyzenYvB5uR8wPgFkxSgV3BoAI4EW3KtxflhLiGaco-lh8MqDH-tAnK6I6ciNo2u_O7k36QHci-2JA</recordid><startdate>20111101</startdate><enddate>20111101</enddate><creator>Malitch, K. N.</creator><creator>Efimov, A. A.</creator><creator>Badanina, I. Yu</creator><general>SP MAIK Nauka/Interperiodica</general><general>Springer</general><general>Springer Nature B.V</general><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>ATCPS</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>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20111101</creationdate><title>Contrasting platinum-group mineral assemblages from chromitites of the Nizhny Tagil and Guli massifs (Russia): Implications for composition, sources and age</title><author>Malitch, K. N. ; Efimov, A. A. ; Badanina, I. Yu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a443t-251fb57f06038fea80e1398325bade07822193c661fe37f75c313f638a686d143</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Age</topic><topic>Alloys</topic><topic>Budgeting</topic><topic>Deposition</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geology</topic><topic>Massifs</topic><topic>Mathematical models</topic><topic>Mineralogy</topic><topic>Minerals</topic><topic>Mines and mineral resources</topic><topic>Ophiolites</topic><topic>Osmium</topic><topic>Platinum</topic><topic>Platinum base alloys</topic><topic>Rocks</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Malitch, K. N.</creatorcontrib><creatorcontrib>Efimov, A. A.</creatorcontrib><creatorcontrib>Badanina, I. Yu</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Doklady earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Malitch, K. N.</au><au>Efimov, A. A.</au><au>Badanina, I. Yu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Contrasting platinum-group mineral assemblages from chromitites of the Nizhny Tagil and Guli massifs (Russia): Implications for composition, sources and age</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2011-11-01</date><risdate>2011</risdate><volume>441</volume><issue>1</issue><spage>1514</spage><epage>1518</epage><pages>1514-1518</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>The Nizhny Tagil and Guli clinopyroxenite-dunite massifs, located in the Middle Urals and Maimecha-Kotui Province, respectively, are associated with world-class platinum-group elements (PGE) placer deposits. Both massifs contain small bodies of schlieren to massive chromitite associated with dunite. The predominance of Pt-Fe alloys at Nizhny Tagil is consistnt with the whole-rock “M”-shaped mantle-normalized PGE pattern of the chromitite. In contrast, the preponderance of laurite and Os-Ir alloys at Guli is consistent with a negatively sloped PGE pattern, the latter being characteristic of ophiolite-type podiform chromitites. The ‘unradiogenic’
187
Os/
188
Os values obtained for both platinum-group minerals (PGM) and chromitite are indicative of a common near-to-chondritic source for the PGE and implies that the osmium isotope budget of chromitite is largely controlled by laurite and Os-rich alloy. Average model
187
Os/
188
Os ages calculated for the Nizhny Tagil and Guli massifs correspond to the late Riphean (e.g., 862 ± 48 Ma and 616 ± 8 Ma, respectively). The compositional and isotope-geochemical results provide new constraints on the temporal evolution of ultramafic rocks of the Uralian Platinum Belt and northern segment of the Siberian Platform.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S1028334X11110067</doi><tpages>5</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1028-334X |
| ispartof | Doklady earth sciences, 2011-11, Vol.441 (1), p.1514-1518 |
| issn | 1028-334X 1531-8354 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1671559308 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Age Alloys Budgeting Deposition Earth and Environmental Science Earth Sciences Geology Massifs Mathematical models Mineralogy Minerals Mines and mineral resources Ophiolites Osmium Platinum Platinum base alloys Rocks |
| title | Contrasting platinum-group mineral assemblages from chromitites of the Nizhny Tagil and Guli massifs (Russia): Implications for composition, sources and age |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-12T22%3A29%3A13IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Contrasting%20platinum-group%20mineral%20assemblages%20from%20chromitites%20of%20the%20Nizhny%20Tagil%20and%20Guli%20massifs%20(Russia):%20Implications%20for%20composition,%20sources%20and%20age&rft.jtitle=Doklady%20earth%20sciences&rft.au=Malitch,%20K.%20N.&rft.date=2011-11-01&rft.volume=441&rft.issue=1&rft.spage=1514&rft.epage=1518&rft.pages=1514-1518&rft.issn=1028-334X&rft.eissn=1531-8354&rft_id=info:doi/10.1134/S1028334X11110067&rft_dat=%3Cgale_proqu%3EA360119718%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=912495770&rft_id=info:pmid/&rft_galeid=A360119718&rfr_iscdi=true |