The Timing, Duration and Conditions of UHT Metamorphism in Remnants of the Former Eastern Gondwana
Abstract Early Palaeozoic ultrahigh-temperature (UHT) metamorphism in eastern Gondwana was an event that started with Gondwana amalgamation at c. 580 Ma and lasted at least 50 Myr. Sapphirine + quartz, Mg–Al granulites preserve a record of the timing and duration of the event along the metamorphic b...
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| Veröffentlicht in: | Journal of petrology 2021-12, Vol.62 (12), Article 068 |
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| creator | Durgalakshmi, Sajeev, K Williams, Ian S Reddy, D Harinadha Satish-Kumar, M Jöns, Niels Malaviarachchi, Sanjeewa P K Samuel, Vinod O George, P M |
| description | Abstract
Early Palaeozoic ultrahigh-temperature (UHT) metamorphism in eastern Gondwana was an event that started with Gondwana amalgamation at c. 580 Ma and lasted at least 50 Myr. Sapphirine + quartz, Mg–Al granulites preserve a record of the timing and duration of the event along the metamorphic belt. U–Th–Pb dating of zircon and monazite shows that metamorphism peaked almost simultaneously in Antarctica (554.0 ± 4.7 Ma), Sri Lanka (555.5 ± 4.6 Ma), southern India (548.1 ± 8.1 Ma) and Madagascar (550.6 ± 6.0 Ma), and ended in all locations at the same time, 530–520 Ma. Rare earth element (REE) compositions of the metamorphic zircon zones can be matched to the REE zoning in the associated garnet. Phase-diagram modelling indicates that the peak UHT P–T conditions in Antarctica, Sri Lanka, and India were very similar, 1020–1040 °C at 0.8 GPa. Peak conditions in Madagascar were at higher T and similar P: 1090 °C and 0.8 GPa. The East African Orogeny before 600 Ma preconditioned the crust of the eastern Gondwanan terranes by thickening it and harbouring heat-producing elements, heating the crust over c. 60 Myr; such that UHT conditions were reached when East and West Gondwana collided. |
| doi_str_mv | 10.1093/petrology/egab068 |
| format | Article |
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Early Palaeozoic ultrahigh-temperature (UHT) metamorphism in eastern Gondwana was an event that started with Gondwana amalgamation at c. 580 Ma and lasted at least 50 Myr. Sapphirine + quartz, Mg–Al granulites preserve a record of the timing and duration of the event along the metamorphic belt. U–Th–Pb dating of zircon and monazite shows that metamorphism peaked almost simultaneously in Antarctica (554.0 ± 4.7 Ma), Sri Lanka (555.5 ± 4.6 Ma), southern India (548.1 ± 8.1 Ma) and Madagascar (550.6 ± 6.0 Ma), and ended in all locations at the same time, 530–520 Ma. Rare earth element (REE) compositions of the metamorphic zircon zones can be matched to the REE zoning in the associated garnet. Phase-diagram modelling indicates that the peak UHT P–T conditions in Antarctica, Sri Lanka, and India were very similar, 1020–1040 °C at 0.8 GPa. Peak conditions in Madagascar were at higher T and similar P: 1090 °C and 0.8 GPa. The East African Orogeny before 600 Ma preconditioned the crust of the eastern Gondwanan terranes by thickening it and harbouring heat-producing elements, heating the crust over c. 60 Myr; such that UHT conditions were reached when East and West Gondwana collided.</description><identifier>ISSN: 0022-3530</identifier><identifier>EISSN: 1460-2415</identifier><identifier>DOI: 10.1093/petrology/egab068</identifier><language>eng</language><publisher>OXFORD: Oxford University Press</publisher><subject>Geochemistry & Geophysics ; Physical Sciences ; Science & Technology</subject><ispartof>Journal of petrology, 2021-12, Vol.62 (12), Article 068</ispartof><rights>The Author(s) 2021. Published by Oxford University Press. All rights reserved. For permissions, please e-mail: journals.permissions@oup.com 2021</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>true</woscitedreferencessubscribed><woscitedreferencescount>10</woscitedreferencescount><woscitedreferencesoriginalsourcerecordid>wos000745055500011</woscitedreferencesoriginalsourcerecordid><citedby>FETCH-LOGICAL-a371t-315920f2269dd4c5dbb42bccdcfe5c612dda9727fa01568874b16c22b73ce0c93</citedby><cites>FETCH-LOGICAL-a371t-315920f2269dd4c5dbb42bccdcfe5c612dda9727fa01568874b16c22b73ce0c93</cites><orcidid>0000-0002-9567-2752 ; 0000-0002-6890-3439</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,781,785,1585,27929,27930,39263</link.rule.ids></links><search><creatorcontrib>Durgalakshmi, </creatorcontrib><creatorcontrib>Sajeev, K</creatorcontrib><creatorcontrib>Williams, Ian S</creatorcontrib><creatorcontrib>Reddy, D Harinadha</creatorcontrib><creatorcontrib>Satish-Kumar, M</creatorcontrib><creatorcontrib>Jöns, Niels</creatorcontrib><creatorcontrib>Malaviarachchi, Sanjeewa P K</creatorcontrib><creatorcontrib>Samuel, Vinod O</creatorcontrib><creatorcontrib>George, P M</creatorcontrib><title>The Timing, Duration and Conditions of UHT Metamorphism in Remnants of the Former Eastern Gondwana</title><title>Journal of petrology</title><addtitle>J PETROL</addtitle><description>Abstract
Early Palaeozoic ultrahigh-temperature (UHT) metamorphism in eastern Gondwana was an event that started with Gondwana amalgamation at c. 580 Ma and lasted at least 50 Myr. Sapphirine + quartz, Mg–Al granulites preserve a record of the timing and duration of the event along the metamorphic belt. U–Th–Pb dating of zircon and monazite shows that metamorphism peaked almost simultaneously in Antarctica (554.0 ± 4.7 Ma), Sri Lanka (555.5 ± 4.6 Ma), southern India (548.1 ± 8.1 Ma) and Madagascar (550.6 ± 6.0 Ma), and ended in all locations at the same time, 530–520 Ma. Rare earth element (REE) compositions of the metamorphic zircon zones can be matched to the REE zoning in the associated garnet. Phase-diagram modelling indicates that the peak UHT P–T conditions in Antarctica, Sri Lanka, and India were very similar, 1020–1040 °C at 0.8 GPa. Peak conditions in Madagascar were at higher T and similar P: 1090 °C and 0.8 GPa. The East African Orogeny before 600 Ma preconditioned the crust of the eastern Gondwanan terranes by thickening it and harbouring heat-producing elements, heating the crust over c. 60 Myr; such that UHT conditions were reached when East and West Gondwana collided.</description><subject>Geochemistry & Geophysics</subject><subject>Physical Sciences</subject><subject>Science & Technology</subject><issn>0022-3530</issn><issn>1460-2415</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>HGBXW</sourceid><recordid>eNqNkMlqwzAURUVpoWnaD-hO-8bNk2x5WBY3QyGlUJy1kWQ5UYmlICmE_H2dgayzetM9l8dF6JXAO4EiHm9VcHZjV4exWnEBaX6HBiRJIaIJYfdoAEBpFLMYHtGT938ApN_DAIlqrXClO21WI_y5czxoazA3DS6tafRx8ti2eDmv8LcKvLNuu9a-w9rgX9UZbsLpHnqbqXWdcnjCfVDO4FlvsOeGP6OHlm-8ernUIVpOJ1U5jxY_s6_yYxHxOCMhigkrKLSUpkXTJJI1QiRUSNnIVjGZEto0vMho1nIgLM3zLBEklZSKLJYKZBEPETn7Sme9d6qtt0533B1qAvUxpPoaUn0JqWfyM7NXwrZeamWkunIAkCUMGGN9R0ipwyme0u5M6NG329FePTqr7W57w1__DsuPng</recordid><startdate>20211201</startdate><enddate>20211201</enddate><creator>Durgalakshmi, </creator><creator>Sajeev, K</creator><creator>Williams, Ian S</creator><creator>Reddy, D Harinadha</creator><creator>Satish-Kumar, M</creator><creator>Jöns, Niels</creator><creator>Malaviarachchi, Sanjeewa P K</creator><creator>Samuel, Vinod O</creator><creator>George, P M</creator><general>Oxford University Press</general><general>Oxford Univ Press</general><scope>BLEPL</scope><scope>DTL</scope><scope>HGBXW</scope><scope>AAYXX</scope><scope>CITATION</scope><orcidid>https://orcid.org/0000-0002-9567-2752</orcidid><orcidid>https://orcid.org/0000-0002-6890-3439</orcidid></search><sort><creationdate>20211201</creationdate><title>The Timing, Duration and Conditions of UHT Metamorphism in Remnants of the Former Eastern Gondwana</title><author>Durgalakshmi, ; Sajeev, K ; Williams, Ian S ; Reddy, D Harinadha ; Satish-Kumar, M ; Jöns, Niels ; Malaviarachchi, Sanjeewa P K ; Samuel, Vinod O ; George, P M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a371t-315920f2269dd4c5dbb42bccdcfe5c612dda9727fa01568874b16c22b73ce0c93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Geochemistry & Geophysics</topic><topic>Physical Sciences</topic><topic>Science & Technology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Durgalakshmi, </creatorcontrib><creatorcontrib>Sajeev, K</creatorcontrib><creatorcontrib>Williams, Ian S</creatorcontrib><creatorcontrib>Reddy, D Harinadha</creatorcontrib><creatorcontrib>Satish-Kumar, M</creatorcontrib><creatorcontrib>Jöns, Niels</creatorcontrib><creatorcontrib>Malaviarachchi, Sanjeewa P K</creatorcontrib><creatorcontrib>Samuel, Vinod O</creatorcontrib><creatorcontrib>George, P M</creatorcontrib><collection>Web of Science Core Collection</collection><collection>Science Citation Index Expanded</collection><collection>Web of Science - Science Citation Index Expanded - 2021</collection><collection>CrossRef</collection><jtitle>Journal of petrology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Durgalakshmi, </au><au>Sajeev, K</au><au>Williams, Ian S</au><au>Reddy, D Harinadha</au><au>Satish-Kumar, M</au><au>Jöns, Niels</au><au>Malaviarachchi, Sanjeewa P K</au><au>Samuel, Vinod O</au><au>George, P M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Timing, Duration and Conditions of UHT Metamorphism in Remnants of the Former Eastern Gondwana</atitle><jtitle>Journal of petrology</jtitle><stitle>J PETROL</stitle><date>2021-12-01</date><risdate>2021</risdate><volume>62</volume><issue>12</issue><artnum>068</artnum><issn>0022-3530</issn><eissn>1460-2415</eissn><abstract>Abstract
Early Palaeozoic ultrahigh-temperature (UHT) metamorphism in eastern Gondwana was an event that started with Gondwana amalgamation at c. 580 Ma and lasted at least 50 Myr. Sapphirine + quartz, Mg–Al granulites preserve a record of the timing and duration of the event along the metamorphic belt. U–Th–Pb dating of zircon and monazite shows that metamorphism peaked almost simultaneously in Antarctica (554.0 ± 4.7 Ma), Sri Lanka (555.5 ± 4.6 Ma), southern India (548.1 ± 8.1 Ma) and Madagascar (550.6 ± 6.0 Ma), and ended in all locations at the same time, 530–520 Ma. Rare earth element (REE) compositions of the metamorphic zircon zones can be matched to the REE zoning in the associated garnet. Phase-diagram modelling indicates that the peak UHT P–T conditions in Antarctica, Sri Lanka, and India were very similar, 1020–1040 °C at 0.8 GPa. Peak conditions in Madagascar were at higher T and similar P: 1090 °C and 0.8 GPa. The East African Orogeny before 600 Ma preconditioned the crust of the eastern Gondwanan terranes by thickening it and harbouring heat-producing elements, heating the crust over c. 60 Myr; such that UHT conditions were reached when East and West Gondwana collided.</abstract><cop>OXFORD</cop><pub>Oxford University Press</pub><doi>10.1093/petrology/egab068</doi><tpages>38</tpages><orcidid>https://orcid.org/0000-0002-9567-2752</orcidid><orcidid>https://orcid.org/0000-0002-6890-3439</orcidid></addata></record> |
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| subjects | Geochemistry & Geophysics Physical Sciences Science & Technology |
| title | The Timing, Duration and Conditions of UHT Metamorphism in Remnants of the Former Eastern Gondwana |
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