K-rich titanate from the Jharia ultrapotassic rock, Gondwana coal fields, eastern India, and its petrological significance
We report a rare accessory groundmass mineral of K-rich titanate, having a composition close to that of potassium triskaidecatitanate (K 2 Ti 13 O 27 ), from an underground drill-core sample of ultrapotassic rock from southwestern part of the Jharia coal field in the Damodar valley, at the northern...
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| Veröffentlicht in: | Journal of the Geological Society of India 2013-06, Vol.81 (6), p.733-736 |
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| creator | Chalapathi Rao, N. V. Sinha, Anup K. Kumar, Suresh Srivastava, Rajesh K. |
| description | We report a rare accessory groundmass mineral of K-rich titanate, having a composition close to that of potassium triskaidecatitanate (K
2
Ti
13
O
27
), from an underground drill-core sample of ultrapotassic rock from southwestern part of the Jharia coal field in the Damodar valley, at the northern margin of the Singhbhum craton, Eastern India. Potassium triskaidecatitanate is regarded as a typomorphic mineral of orangeites (Group II kimberlites) of Kaapvaal craton, southern Africa, and its occurrence in the Jharia ultrapotassic rock is significant since ultrapotassic suite of rocks elsewhere from the Damodar valley have been recently suggested to be peralkaline lamproites based on mineral-genetic classification. The important role played by a unique geodynamic setting (involving a thinned metasomatised lithospheric mantle and inheritance of an Archaean subduction component) at the northern margin of the Singhbhum craton in deciding the petrological diversity of the early Cretaceous ultrapotassic intrusives from the Damodar valley is highlighted in this study. |
| doi_str_mv | 10.1007/s12594-013-0097-4 |
| format | Article |
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2
Ti
13
O
27
), from an underground drill-core sample of ultrapotassic rock from southwestern part of the Jharia coal field in the Damodar valley, at the northern margin of the Singhbhum craton, Eastern India. Potassium triskaidecatitanate is regarded as a typomorphic mineral of orangeites (Group II kimberlites) of Kaapvaal craton, southern Africa, and its occurrence in the Jharia ultrapotassic rock is significant since ultrapotassic suite of rocks elsewhere from the Damodar valley have been recently suggested to be peralkaline lamproites based on mineral-genetic classification. The important role played by a unique geodynamic setting (involving a thinned metasomatised lithospheric mantle and inheritance of an Archaean subduction component) at the northern margin of the Singhbhum craton in deciding the petrological diversity of the early Cretaceous ultrapotassic intrusives from the Damodar valley is highlighted in this study.</description><identifier>ISSN: 0016-7622</identifier><identifier>EISSN: 0974-6889</identifier><identifier>DOI: 10.1007/s12594-013-0097-4</identifier><language>eng</language><publisher>India: Springer-Verlag</publisher><subject>Coal ; Cratons ; Cretaceous ; Earth and Environmental Science ; Earth Sciences ; Geology ; Hydrogeology ; India ; Minerals ; Petrology ; Potassium ; Research Article ; Rock ; Rocks ; Titanates ; Valleys</subject><ispartof>Journal of the Geological Society of India, 2013-06, Vol.81 (6), p.733-736</ispartof><rights>Geological Society of India 2013</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a372t-84ec34f4aae433dbef4ada7b3b259099cb4b017e85f95cfb5704dfd4fc87f4f03</citedby><cites>FETCH-LOGICAL-a372t-84ec34f4aae433dbef4ada7b3b259099cb4b017e85f95cfb5704dfd4fc87f4f03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12594-013-0097-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12594-013-0097-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Chalapathi Rao, N. V.</creatorcontrib><creatorcontrib>Sinha, Anup K.</creatorcontrib><creatorcontrib>Kumar, Suresh</creatorcontrib><creatorcontrib>Srivastava, Rajesh K.</creatorcontrib><title>K-rich titanate from the Jharia ultrapotassic rock, Gondwana coal fields, eastern India, and its petrological significance</title><title>Journal of the Geological Society of India</title><addtitle>J Geol Soc India</addtitle><description>We report a rare accessory groundmass mineral of K-rich titanate, having a composition close to that of potassium triskaidecatitanate (K
2
Ti
13
O
27
), from an underground drill-core sample of ultrapotassic rock from southwestern part of the Jharia coal field in the Damodar valley, at the northern margin of the Singhbhum craton, Eastern India. Potassium triskaidecatitanate is regarded as a typomorphic mineral of orangeites (Group II kimberlites) of Kaapvaal craton, southern Africa, and its occurrence in the Jharia ultrapotassic rock is significant since ultrapotassic suite of rocks elsewhere from the Damodar valley have been recently suggested to be peralkaline lamproites based on mineral-genetic classification. The important role played by a unique geodynamic setting (involving a thinned metasomatised lithospheric mantle and inheritance of an Archaean subduction component) at the northern margin of the Singhbhum craton in deciding the petrological diversity of the early Cretaceous ultrapotassic intrusives from the Damodar valley is highlighted in this study.</description><subject>Coal</subject><subject>Cratons</subject><subject>Cretaceous</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geology</subject><subject>Hydrogeology</subject><subject>India</subject><subject>Minerals</subject><subject>Petrology</subject><subject>Potassium</subject><subject>Research Article</subject><subject>Rock</subject><subject>Rocks</subject><subject>Titanates</subject><subject>Valleys</subject><issn>0016-7622</issn><issn>0974-6889</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</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>eNp1kTFvFDEQhVcIJEKSH0BniYbiDPZ6du0tUURCIBINqa1Z7_jOYc8-bJ9Q-PU4OgqERDWv-N7TG72uey3FOymEfl9kP0zAhVRciElzeNadtQt8NGZ63rSQI9dj37_sXpXyIMQIwqiz7tcXnoPbsRoqRqzEfE57VnfEPu8wB2THtWY8pIqlBMdyct837CbF5WfDmUu4Mh9oXcqGEZZKObLbuATcMIwLC7WwA9Wc1rQNrrElbGPwTUZHF90Lj2uhyz_3vLu__vjt6hO_-3pze_XhjqPSfeUGyCnwgEig1DJTkwvqWc3tYzFNboZZSE1m8NPg_DxoAYtfwDujPXihzru3p9xDTj-OVKrdh-JoXTFSOhYrAYwGAzA09M0_6EM65tjaWdnKiL5Xo2mUPFEup1IyeXvIYY_50Uphn9awpzVsW8M-rWGhefqTpzQ2bin_lfxf02-q5Y5a</recordid><startdate>20130601</startdate><enddate>20130601</enddate><creator>Chalapathi Rao, N. 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2
Ti
13
O
27
), from an underground drill-core sample of ultrapotassic rock from southwestern part of the Jharia coal field in the Damodar valley, at the northern margin of the Singhbhum craton, Eastern India. Potassium triskaidecatitanate is regarded as a typomorphic mineral of orangeites (Group II kimberlites) of Kaapvaal craton, southern Africa, and its occurrence in the Jharia ultrapotassic rock is significant since ultrapotassic suite of rocks elsewhere from the Damodar valley have been recently suggested to be peralkaline lamproites based on mineral-genetic classification. The important role played by a unique geodynamic setting (involving a thinned metasomatised lithospheric mantle and inheritance of an Archaean subduction component) at the northern margin of the Singhbhum craton in deciding the petrological diversity of the early Cretaceous ultrapotassic intrusives from the Damodar valley is highlighted in this study.</abstract><cop>India</cop><pub>Springer-Verlag</pub><doi>10.1007/s12594-013-0097-4</doi><tpages>4</tpages></addata></record> |
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| subjects | Coal Cratons Cretaceous Earth and Environmental Science Earth Sciences Geology Hydrogeology India Minerals Petrology Potassium Research Article Rock Rocks Titanates Valleys |
| title | K-rich titanate from the Jharia ultrapotassic rock, Gondwana coal fields, eastern India, and its petrological significance |
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