Petrology and geochemistry of Bhanjada Bet phonolites, Kutch, Gujarat in Western Deccan Province: Possibility of a mantle-derived primary phonolite magma
Bhanjada Bet igneous rock lies to the east of Pachham Island and west of Khadir Island, well within the Great Rann of Kutch, Gujarat, western India. It is a small isolated hillock made up largely of phonolite with patches of trachyte and traversed by a mafic dyke. The phonolite is composed dominantl...
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description | Bhanjada Bet igneous rock lies to the east of Pachham Island and west of Khadir Island, well within the Great Rann of Kutch, Gujarat, western India. It is a small isolated hillock made up largely of phonolite with patches of trachyte and traversed by a mafic dyke. The phonolite is composed dominantly of sanidine, nepheline, aegirine, Ti-amphibole and glass. Sanidine occurs as phenocryst and nepheline as microphenocryst. Groundmass is composed of smaller alkali feldspar, aegirine, Ti-amphibole and glass. The lath-shaped feldspar in the groundmass defines excellent flow texture. Major element chemical composition indicates occurrence of two groups of phonolite-low silica (around 53%) and high silica (around 58%). The phonolite has higher abundance of MgO (2.21–3.5%) over FeO (2.43–2.6%) and very high Mg# (65–69
)
suggesting its primitive nature. Trace element abundances suggest an overall enrichment in LILE and selected HFSE, highly fractionated LREE pattern. High Mg# of the Bhanjada bet phonolite along with low values of Zr and Hf compared to phonolites of basanite phonolite suite where phonolite is an evolved member, is noted. The lower Zr and Hf values hint towards a less evolved primary phonolitic magma rather than phonolite as late differentiates of basanitic–phonolite suite. Experimental studies indicate low degree partial melting of a metasomatised lherzolite mantle at a pressure around 1–1.5 GPa can produce primary phonolite magma. Mantle xenoliths, found in alkali basalt of Kutch basin, show evidence of carbonatite metasomatism of lithospheric mantle. Bhanjada Bet phonolites are associated with layered mafic complex of Nir Wandh and other magmatic rocks of Pachham Island. Ages of Nir Wandh magmatic rocks and magmatic rocks of Pachham Island coincide with ages of early Deccan magmatism. Age of phonolite is not yet known. From field association and petro-mineralogy, we propose that Bhanjada Bet phonolite represents alkali magmatism of early Deccan age in Western Deccan Province. |
doi_str_mv | 10.1007/s12040-022-01955-5 |
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)
suggesting its primitive nature. Trace element abundances suggest an overall enrichment in LILE and selected HFSE, highly fractionated LREE pattern. High Mg# of the Bhanjada bet phonolite along with low values of Zr and Hf compared to phonolites of basanite phonolite suite where phonolite is an evolved member, is noted. The lower Zr and Hf values hint towards a less evolved primary phonolitic magma rather than phonolite as late differentiates of basanitic–phonolite suite. Experimental studies indicate low degree partial melting of a metasomatised lherzolite mantle at a pressure around 1–1.5 GPa can produce primary phonolite magma. Mantle xenoliths, found in alkali basalt of Kutch basin, show evidence of carbonatite metasomatism of lithospheric mantle. Bhanjada Bet phonolites are associated with layered mafic complex of Nir Wandh and other magmatic rocks of Pachham Island. Ages of Nir Wandh magmatic rocks and magmatic rocks of Pachham Island coincide with ages of early Deccan magmatism. Age of phonolite is not yet known. From field association and petro-mineralogy, we propose that Bhanjada Bet phonolite represents alkali magmatism of early Deccan age in Western Deccan Province.</description><identifier>ISSN: 0973-774X</identifier><identifier>ISSN: 0253-4126</identifier><identifier>EISSN: 0973-774X</identifier><identifier>DOI: 10.1007/s12040-022-01955-5</identifier><language>eng</language><publisher>New Delhi: Springer India</publisher><subject>Abundance ; Alkali basalts ; Amphiboles ; Basalt ; Chemical composition ; Deccan Traps and other Flood Basalt Provinces – Recent Research Trends ; Earth and Environmental Science ; Earth Sciences ; Fault lines ; Feldspars ; Geochemistry ; Geology ; Glass ; Igneous rocks ; Lava ; Magma ; Magnesium ; Mineralogy ; Nepheline ; Petrogenesis ; Petrology ; Plate tectonics ; Rock intrusions ; Silica ; Silicon dioxide ; Space Exploration and Astronautics ; Space Sciences (including Extraterrestrial Physics ; Trace elements ; Trachyte ; Zirconium</subject><ispartof>Journal of Earth System Science, 2022-09, Vol.131 (4), p.213, Article 213</ispartof><rights>Indian Academy of Sciences 2022</rights><rights>Indian Academy of Sciences 2022.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c200t-a77189f31aa7915278a9810e72e8ff8e3ccc5ace674ed94ebe867b19d6c543f53</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/s12040-022-01955-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12040-022-01955-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Mukherjee, Debarun</creatorcontrib><creatorcontrib>Ray, Arijit</creatorcontrib><creatorcontrib>Paul, Dalim K</creatorcontrib><creatorcontrib>Chakraborty, Kuhu</creatorcontrib><creatorcontrib>Thakkar, Mahesh</creatorcontrib><creatorcontrib>Chouhan, Gaurav</creatorcontrib><title>Petrology and geochemistry of Bhanjada Bet phonolites, Kutch, Gujarat in Western Deccan Province: Possibility of a mantle-derived primary phonolite magma</title><title>Journal of Earth System Science</title><addtitle>J Earth Syst Sci</addtitle><description>Bhanjada Bet igneous rock lies to the east of Pachham Island and west of Khadir Island, well within the Great Rann of Kutch, Gujarat, western India. It is a small isolated hillock made up largely of phonolite with patches of trachyte and traversed by a mafic dyke. The phonolite is composed dominantly of sanidine, nepheline, aegirine, Ti-amphibole and glass. Sanidine occurs as phenocryst and nepheline as microphenocryst. Groundmass is composed of smaller alkali feldspar, aegirine, Ti-amphibole and glass. The lath-shaped feldspar in the groundmass defines excellent flow texture. Major element chemical composition indicates occurrence of two groups of phonolite-low silica (around 53%) and high silica (around 58%). The phonolite has higher abundance of MgO (2.21–3.5%) over FeO (2.43–2.6%) and very high Mg# (65–69
)
suggesting its primitive nature. Trace element abundances suggest an overall enrichment in LILE and selected HFSE, highly fractionated LREE pattern. High Mg# of the Bhanjada bet phonolite along with low values of Zr and Hf compared to phonolites of basanite phonolite suite where phonolite is an evolved member, is noted. The lower Zr and Hf values hint towards a less evolved primary phonolitic magma rather than phonolite as late differentiates of basanitic–phonolite suite. Experimental studies indicate low degree partial melting of a metasomatised lherzolite mantle at a pressure around 1–1.5 GPa can produce primary phonolite magma. Mantle xenoliths, found in alkali basalt of Kutch basin, show evidence of carbonatite metasomatism of lithospheric mantle. Bhanjada Bet phonolites are associated with layered mafic complex of Nir Wandh and other magmatic rocks of Pachham Island. Ages of Nir Wandh magmatic rocks and magmatic rocks of Pachham Island coincide with ages of early Deccan magmatism. Age of phonolite is not yet known. From field association and petro-mineralogy, we propose that Bhanjada Bet phonolite represents alkali magmatism of early Deccan age in Western Deccan Province.</description><subject>Abundance</subject><subject>Alkali basalts</subject><subject>Amphiboles</subject><subject>Basalt</subject><subject>Chemical composition</subject><subject>Deccan Traps and other Flood Basalt Provinces – Recent Research Trends</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fault lines</subject><subject>Feldspars</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Glass</subject><subject>Igneous rocks</subject><subject>Lava</subject><subject>Magma</subject><subject>Magnesium</subject><subject>Mineralogy</subject><subject>Nepheline</subject><subject>Petrogenesis</subject><subject>Petrology</subject><subject>Plate tectonics</subject><subject>Rock intrusions</subject><subject>Silica</subject><subject>Silicon dioxide</subject><subject>Space Exploration and Astronautics</subject><subject>Space Sciences (including Extraterrestrial Physics</subject><subject>Trace elements</subject><subject>Trachyte</subject><subject>Zirconium</subject><issn>0973-774X</issn><issn>0253-4126</issn><issn>0973-774X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kc1OwzAQhCMEEqXwApwscSVgO3Ecc-MfRCV6AMHN2jqbNlVrF9ut1EfhbTEUASdOu4eZb3c0WXbI6AmjVJ4GxmlJc8p5TpkSIhdbWY8qWeRSlq_bf_bdbC-EKaVFVUvVy96HGL2bufGagG3IGJ2Z4LwL0a-Ja8nFBOwUGiAXGMli4qybdRHDMXlYRjM5JrfLKXiIpLPkBUNEb8kVGgOWDL1bddbgGRm6ELpRl4xfSCBzsHGGeYO-W2FDFr6bQzr3g0-C8Rz2s50WZgEPvmc_e765frq8ywePt_eX54PccEpjDlKyWrUFA5CKCS5rUDWjKDnWbVtjYYwRYLCSJTaqxBHWlRwx1VRGlEUrin52tOEuvHtbphB66pbeppOaK06rigohk4pvVManOB5b_f22ZlR_VqA3FehUgf6qQH-ii40pJLEdo_9F_-P6AMFkjFk</recordid><startdate>20220930</startdate><enddate>20220930</enddate><creator>Mukherjee, Debarun</creator><creator>Ray, Arijit</creator><creator>Paul, Dalim K</creator><creator>Chakraborty, Kuhu</creator><creator>Thakkar, Mahesh</creator><creator>Chouhan, Gaurav</creator><general>Springer India</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>PHGZM</scope><scope>PHGZT</scope><scope>PKEHL</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20220930</creationdate><title>Petrology and geochemistry of Bhanjada Bet phonolites, Kutch, Gujarat in Western Deccan Province: Possibility of a mantle-derived primary phonolite magma</title><author>Mukherjee, Debarun ; Ray, Arijit ; Paul, Dalim K ; Chakraborty, Kuhu ; Thakkar, Mahesh ; Chouhan, Gaurav</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c200t-a77189f31aa7915278a9810e72e8ff8e3ccc5ace674ed94ebe867b19d6c543f53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Abundance</topic><topic>Alkali basalts</topic><topic>Amphiboles</topic><topic>Basalt</topic><topic>Chemical composition</topic><topic>Deccan Traps and other Flood Basalt Provinces – Recent Research Trends</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Fault lines</topic><topic>Feldspars</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Glass</topic><topic>Igneous rocks</topic><topic>Lava</topic><topic>Magma</topic><topic>Magnesium</topic><topic>Mineralogy</topic><topic>Nepheline</topic><topic>Petrogenesis</topic><topic>Petrology</topic><topic>Plate tectonics</topic><topic>Rock intrusions</topic><topic>Silica</topic><topic>Silicon dioxide</topic><topic>Space Exploration and Astronautics</topic><topic>Space Sciences (including Extraterrestrial Physics</topic><topic>Trace elements</topic><topic>Trachyte</topic><topic>Zirconium</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mukherjee, Debarun</creatorcontrib><creatorcontrib>Ray, Arijit</creatorcontrib><creatorcontrib>Paul, Dalim K</creatorcontrib><creatorcontrib>Chakraborty, Kuhu</creatorcontrib><creatorcontrib>Thakkar, Mahesh</creatorcontrib><creatorcontrib>Chouhan, Gaurav</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 Central (New)</collection><collection>ProQuest One Academic (New)</collection><collection>ProQuest One Academic Middle East (New)</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><jtitle>Journal of Earth System Science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mukherjee, Debarun</au><au>Ray, Arijit</au><au>Paul, Dalim K</au><au>Chakraborty, Kuhu</au><au>Thakkar, Mahesh</au><au>Chouhan, Gaurav</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Petrology and geochemistry of Bhanjada Bet phonolites, Kutch, Gujarat in Western Deccan Province: Possibility of a mantle-derived primary phonolite magma</atitle><jtitle>Journal of Earth System Science</jtitle><stitle>J Earth Syst Sci</stitle><date>2022-09-30</date><risdate>2022</risdate><volume>131</volume><issue>4</issue><spage>213</spage><pages>213-</pages><artnum>213</artnum><issn>0973-774X</issn><issn>0253-4126</issn><eissn>0973-774X</eissn><abstract>Bhanjada Bet igneous rock lies to the east of Pachham Island and west of Khadir Island, well within the Great Rann of Kutch, Gujarat, western India. It is a small isolated hillock made up largely of phonolite with patches of trachyte and traversed by a mafic dyke. The phonolite is composed dominantly of sanidine, nepheline, aegirine, Ti-amphibole and glass. Sanidine occurs as phenocryst and nepheline as microphenocryst. Groundmass is composed of smaller alkali feldspar, aegirine, Ti-amphibole and glass. The lath-shaped feldspar in the groundmass defines excellent flow texture. Major element chemical composition indicates occurrence of two groups of phonolite-low silica (around 53%) and high silica (around 58%). The phonolite has higher abundance of MgO (2.21–3.5%) over FeO (2.43–2.6%) and very high Mg# (65–69
)
suggesting its primitive nature. Trace element abundances suggest an overall enrichment in LILE and selected HFSE, highly fractionated LREE pattern. High Mg# of the Bhanjada bet phonolite along with low values of Zr and Hf compared to phonolites of basanite phonolite suite where phonolite is an evolved member, is noted. The lower Zr and Hf values hint towards a less evolved primary phonolitic magma rather than phonolite as late differentiates of basanitic–phonolite suite. Experimental studies indicate low degree partial melting of a metasomatised lherzolite mantle at a pressure around 1–1.5 GPa can produce primary phonolite magma. Mantle xenoliths, found in alkali basalt of Kutch basin, show evidence of carbonatite metasomatism of lithospheric mantle. Bhanjada Bet phonolites are associated with layered mafic complex of Nir Wandh and other magmatic rocks of Pachham Island. Ages of Nir Wandh magmatic rocks and magmatic rocks of Pachham Island coincide with ages of early Deccan magmatism. Age of phonolite is not yet known. From field association and petro-mineralogy, we propose that Bhanjada Bet phonolite represents alkali magmatism of early Deccan age in Western Deccan Province.</abstract><cop>New Delhi</cop><pub>Springer India</pub><doi>10.1007/s12040-022-01955-5</doi></addata></record> |
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subjects | Abundance Alkali basalts Amphiboles Basalt Chemical composition Deccan Traps and other Flood Basalt Provinces – Recent Research Trends Earth and Environmental Science Earth Sciences Fault lines Feldspars Geochemistry Geology Glass Igneous rocks Lava Magma Magnesium Mineralogy Nepheline Petrogenesis Petrology Plate tectonics Rock intrusions Silica Silicon dioxide Space Exploration and Astronautics Space Sciences (including Extraterrestrial Physics Trace elements Trachyte Zirconium |
title | Petrology and geochemistry of Bhanjada Bet phonolites, Kutch, Gujarat in Western Deccan Province: Possibility of a mantle-derived primary phonolite magma |
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