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An ensialic volcanic arc along the northwestern edge of Palaeotethys—Insights from the Mid‐Triassic volcano‐sedimentary succession of Ivanščica Mt. (northwestern Croatia)
This work aims to unveil the origin, geodynamic significance, and diagenetic history of pyroclastites and associated chert documented within the Upper Anisian volcano‐sedimentary succession of the Ivanščica Mt. in Central Europe. An abundance of pyroclastic material points to polyphase volcanic acti...
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Published in: | Geological journal (Chichester, England) England), 2020-06, Vol.55 (6), p.4324-4351 |
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description | This work aims to unveil the origin, geodynamic significance, and diagenetic history of pyroclastites and associated chert documented within the Upper Anisian volcano‐sedimentary succession of the Ivanščica Mt. in Central Europe. An abundance of pyroclastic material points to polyphase volcanic activity and deep‐water sedimentation along the rim of an oceanic realm. Radiolarian‐based dating revealed Illyrian age of chert intercalated with pyroclastites. The latter are largely vitro‐crystalloclastic and were emplaced as airborne tuff. The crystalloclasts of sanidine, plagioclase, altered pyroxene, and amphibole are principal tuff constituents merged in the altered glassy matrix consisted of palagonite, clay minerals, and calcite. Variations in alteration assemblages reflect an extensive in situ eogenesis in an open hydrologic system that gradually evolved toward a restricted fluid percolation environment. Mineralogy, chemistry, and occurrence of andesitic tuff clearly denote an explosive volcanic activity formed at the top of suprasubduction zone. Such scenario presumes a complex genesis outlined in following steps: (a) partial melting and dehydration of down‐going Palaeotethyan slab which gave rise to the subduction‐related magmatism {LILE, Th, and LREE [(La/Lu)cn = 6.51−9.42] enrichment; negative anomalies of Nb‐Ta, P, and Ti [e.g., (Nb/La)n = 0.31−0.44]}; (b) magma contamination via interaction with continental crust during magma uplift along tectonically weakened zones of upper crust [positive Pb spikes, negative εNd (−4.18 to −4.44), and 147Sm/144Nd ≤ 0.113175]. This is in favour of geodynamic evolution that hypothesizes the existence of an active, ensialic, and mature volcanic arc developed along the southern active continental margins of Euramerica (Laurussia) during Late Anisian subduction of Palaeotethyan lithosphere. |
doi_str_mv | 10.1002/gj.3664 |
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(northwestern Croatia)</title><source>Wiley-Blackwell Journals</source><creator>Slovenec, Damir ; Šegvić, Branimir ; Halamić, Josip ; Goričan, Špela ; Zanoni, Giovanni ; Bozkurt, E.</creator><contributor>Bozkurt, E.</contributor><creatorcontrib>Slovenec, Damir ; Šegvić, Branimir ; Halamić, Josip ; Goričan, Špela ; Zanoni, Giovanni ; Bozkurt, E. ; Bozkurt, E.</creatorcontrib><description>This work aims to unveil the origin, geodynamic significance, and diagenetic history of pyroclastites and associated chert documented within the Upper Anisian volcano‐sedimentary succession of the Ivanščica Mt. in Central Europe. An abundance of pyroclastic material points to polyphase volcanic activity and deep‐water sedimentation along the rim of an oceanic realm. Radiolarian‐based dating revealed Illyrian age of chert intercalated with pyroclastites. The latter are largely vitro‐crystalloclastic and were emplaced as airborne tuff. The crystalloclasts of sanidine, plagioclase, altered pyroxene, and amphibole are principal tuff constituents merged in the altered glassy matrix consisted of palagonite, clay minerals, and calcite. Variations in alteration assemblages reflect an extensive in situ eogenesis in an open hydrologic system that gradually evolved toward a restricted fluid percolation environment. Mineralogy, chemistry, and occurrence of andesitic tuff clearly denote an explosive volcanic activity formed at the top of suprasubduction zone. Such scenario presumes a complex genesis outlined in following steps: (a) partial melting and dehydration of down‐going Palaeotethyan slab which gave rise to the subduction‐related magmatism {LILE, Th, and LREE [(La/Lu)cn = 6.51−9.42] enrichment; negative anomalies of Nb‐Ta, P, and Ti [e.g., (Nb/La)n = 0.31−0.44]}; (b) magma contamination via interaction with continental crust during magma uplift along tectonically weakened zones of upper crust [positive Pb spikes, negative εNd (−4.18 to −4.44), and 147Sm/144Nd ≤ 0.113175]. This is in favour of geodynamic evolution that hypothesizes the existence of an active, ensialic, and mature volcanic arc developed along the southern active continental margins of Euramerica (Laurussia) during Late Anisian subduction of Palaeotethyan lithosphere.</description><identifier>ISSN: 0072-1050</identifier><identifier>EISSN: 1099-1034</identifier><identifier>DOI: 10.1002/gj.3664</identifier><language>eng</language><publisher>Liverpool: Wiley Subscription Services, Inc</publisher><subject>active continental margin ; Anomalies ; Calcite ; Chert ; Clay ; Clay minerals ; Contamination ; Continental crust ; Continental margins ; Croatia ; Dehydration ; Diagenesis ; Ecological succession ; ensialic volcanic arc ; Evolution ; Hydrology ; Ivanščica Mt ; Lava ; Lithosphere ; Magma ; Middle Triassic volcano‐sedimentary succession ; Mineralogy ; Minerals ; Niobium ; Palaeotethys ; Palagonite ; palagonitization ; Percolation ; Plagioclase ; Sedimentation ; Subduction ; Tantalum ; Triassic ; Tuff ; Uplift ; Volcanic activity ; Volcanoes</subject><ispartof>Geological journal (Chichester, England), 2020-06, Vol.55 (6), p.4324-4351</ispartof><rights>2019 John Wiley & Sons, Ltd.</rights><rights>2020 John Wiley & Sons, Ltd.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2894-2c2ab8aefca7907001824542b9fb4d2b4f437f735f73a926ddd630a5adb5146a3</citedby><cites>FETCH-LOGICAL-c2894-2c2ab8aefca7907001824542b9fb4d2b4f437f735f73a926ddd630a5adb5146a3</cites><orcidid>0000-0002-4303-7781 ; 0000-0002-6485-7930 ; 0000-0002-3769-7249</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fgj.3664$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fgj.3664$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>315,786,790,27957,27958,50923,51032</link.rule.ids></links><search><contributor>Bozkurt, E.</contributor><creatorcontrib>Slovenec, Damir</creatorcontrib><creatorcontrib>Šegvić, Branimir</creatorcontrib><creatorcontrib>Halamić, Josip</creatorcontrib><creatorcontrib>Goričan, Špela</creatorcontrib><creatorcontrib>Zanoni, Giovanni</creatorcontrib><creatorcontrib>Bozkurt, E.</creatorcontrib><title>An ensialic volcanic arc along the northwestern edge of Palaeotethys—Insights from the Mid‐Triassic volcano‐sedimentary succession of Ivanščica Mt. (northwestern Croatia)</title><title>Geological journal (Chichester, England)</title><description>This work aims to unveil the origin, geodynamic significance, and diagenetic history of pyroclastites and associated chert documented within the Upper Anisian volcano‐sedimentary succession of the Ivanščica Mt. in Central Europe. An abundance of pyroclastic material points to polyphase volcanic activity and deep‐water sedimentation along the rim of an oceanic realm. Radiolarian‐based dating revealed Illyrian age of chert intercalated with pyroclastites. The latter are largely vitro‐crystalloclastic and were emplaced as airborne tuff. The crystalloclasts of sanidine, plagioclase, altered pyroxene, and amphibole are principal tuff constituents merged in the altered glassy matrix consisted of palagonite, clay minerals, and calcite. Variations in alteration assemblages reflect an extensive in situ eogenesis in an open hydrologic system that gradually evolved toward a restricted fluid percolation environment. Mineralogy, chemistry, and occurrence of andesitic tuff clearly denote an explosive volcanic activity formed at the top of suprasubduction zone. Such scenario presumes a complex genesis outlined in following steps: (a) partial melting and dehydration of down‐going Palaeotethyan slab which gave rise to the subduction‐related magmatism {LILE, Th, and LREE [(La/Lu)cn = 6.51−9.42] enrichment; negative anomalies of Nb‐Ta, P, and Ti [e.g., (Nb/La)n = 0.31−0.44]}; (b) magma contamination via interaction with continental crust during magma uplift along tectonically weakened zones of upper crust [positive Pb spikes, negative εNd (−4.18 to −4.44), and 147Sm/144Nd ≤ 0.113175]. This is in favour of geodynamic evolution that hypothesizes the existence of an active, ensialic, and mature volcanic arc developed along the southern active continental margins of Euramerica (Laurussia) during Late Anisian subduction of Palaeotethyan lithosphere.</description><subject>active continental margin</subject><subject>Anomalies</subject><subject>Calcite</subject><subject>Chert</subject><subject>Clay</subject><subject>Clay minerals</subject><subject>Contamination</subject><subject>Continental crust</subject><subject>Continental margins</subject><subject>Croatia</subject><subject>Dehydration</subject><subject>Diagenesis</subject><subject>Ecological succession</subject><subject>ensialic volcanic arc</subject><subject>Evolution</subject><subject>Hydrology</subject><subject>Ivanščica Mt</subject><subject>Lava</subject><subject>Lithosphere</subject><subject>Magma</subject><subject>Middle Triassic volcano‐sedimentary succession</subject><subject>Mineralogy</subject><subject>Minerals</subject><subject>Niobium</subject><subject>Palaeotethys</subject><subject>Palagonite</subject><subject>palagonitization</subject><subject>Percolation</subject><subject>Plagioclase</subject><subject>Sedimentation</subject><subject>Subduction</subject><subject>Tantalum</subject><subject>Triassic</subject><subject>Tuff</subject><subject>Uplift</subject><subject>Volcanic activity</subject><subject>Volcanoes</subject><issn>0072-1050</issn><issn>1099-1034</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1kc1KAzEQx4MoWD_wFQIeVKQ1yWa_jlK0VhQ96HmZzWa3KdtEk1TpzRcQPPgCvoLPoC_SJzG1InjwMGSY_PL_z2QQ2qGkRwlhR824FyUJX0EdSvK8S0nEV1GHkJSFPCbraMO5MSGUEk476P1YY6mdglYJ_GBaATokYEO0RjfYjyTWxvrRo3Re2gBXjcSmxtfQgjRe-tHMzZ9eh0GjGXmHa2sm368uVTV_ermxCpz71Tah5GSlJlJ7sDPspkLIcG_0QnP4APrz7eNZCcCXvof3_zj3rQGv4GALrdXQOrn9c26i29OTm_5Z9-JqMOwfX3QFy3LeZYJBmYGsBaQ5ScPEGeMxZ2Vel7xiJa95lNZpFIeAnCVVVSURgRiqMqY8gWgT7S5176y5n4YmirGZWh0sC8ZJFmVx-OdA7S0pYY1zVtbFnVWTMFtBSbFYSNGMi8VCAnm4JB9VK2f_YcXg_Jv-AkpvkuA</recordid><startdate>202006</startdate><enddate>202006</enddate><creator>Slovenec, Damir</creator><creator>Šegvić, Branimir</creator><creator>Halamić, Josip</creator><creator>Goričan, Špela</creator><creator>Zanoni, Giovanni</creator><creator>Bozkurt, E.</creator><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-4303-7781</orcidid><orcidid>https://orcid.org/0000-0002-6485-7930</orcidid><orcidid>https://orcid.org/0000-0002-3769-7249</orcidid></search><sort><creationdate>202006</creationdate><title>An ensialic volcanic arc along the northwestern edge of Palaeotethys—Insights from the Mid‐Triassic volcano‐sedimentary succession of Ivanščica Mt. 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(northwestern Croatia)</atitle><jtitle>Geological journal (Chichester, England)</jtitle><date>2020-06</date><risdate>2020</risdate><volume>55</volume><issue>6</issue><spage>4324</spage><epage>4351</epage><pages>4324-4351</pages><issn>0072-1050</issn><eissn>1099-1034</eissn><abstract>This work aims to unveil the origin, geodynamic significance, and diagenetic history of pyroclastites and associated chert documented within the Upper Anisian volcano‐sedimentary succession of the Ivanščica Mt. in Central Europe. An abundance of pyroclastic material points to polyphase volcanic activity and deep‐water sedimentation along the rim of an oceanic realm. Radiolarian‐based dating revealed Illyrian age of chert intercalated with pyroclastites. The latter are largely vitro‐crystalloclastic and were emplaced as airborne tuff. The crystalloclasts of sanidine, plagioclase, altered pyroxene, and amphibole are principal tuff constituents merged in the altered glassy matrix consisted of palagonite, clay minerals, and calcite. Variations in alteration assemblages reflect an extensive in situ eogenesis in an open hydrologic system that gradually evolved toward a restricted fluid percolation environment. Mineralogy, chemistry, and occurrence of andesitic tuff clearly denote an explosive volcanic activity formed at the top of suprasubduction zone. Such scenario presumes a complex genesis outlined in following steps: (a) partial melting and dehydration of down‐going Palaeotethyan slab which gave rise to the subduction‐related magmatism {LILE, Th, and LREE [(La/Lu)cn = 6.51−9.42] enrichment; negative anomalies of Nb‐Ta, P, and Ti [e.g., (Nb/La)n = 0.31−0.44]}; (b) magma contamination via interaction with continental crust during magma uplift along tectonically weakened zones of upper crust [positive Pb spikes, negative εNd (−4.18 to −4.44), and 147Sm/144Nd ≤ 0.113175]. This is in favour of geodynamic evolution that hypothesizes the existence of an active, ensialic, and mature volcanic arc developed along the southern active continental margins of Euramerica (Laurussia) during Late Anisian subduction of Palaeotethyan lithosphere.</abstract><cop>Liverpool</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1002/gj.3664</doi><tpages>28</tpages><orcidid>https://orcid.org/0000-0002-4303-7781</orcidid><orcidid>https://orcid.org/0000-0002-6485-7930</orcidid><orcidid>https://orcid.org/0000-0002-3769-7249</orcidid></addata></record> |
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subjects | active continental margin Anomalies Calcite Chert Clay Clay minerals Contamination Continental crust Continental margins Croatia Dehydration Diagenesis Ecological succession ensialic volcanic arc Evolution Hydrology Ivanščica Mt Lava Lithosphere Magma Middle Triassic volcano‐sedimentary succession Mineralogy Minerals Niobium Palaeotethys Palagonite palagonitization Percolation Plagioclase Sedimentation Subduction Tantalum Triassic Tuff Uplift Volcanic activity Volcanoes |
title | An ensialic volcanic arc along the northwestern edge of Palaeotethys—Insights from the Mid‐Triassic volcano‐sedimentary succession of Ivanščica Mt. (northwestern Croatia) |
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