Evolution of volcanism and magmatism during initial arc stage: constraints on the tectonic setting of the Oman Ophiolite

التفاصيل البيبلوغرافية
العنوان: Evolution of volcanism and magmatism during initial arc stage: constraints on the tectonic setting of the Oman Ophiolite
المؤلفون: Yuki Kusano, Sumio Miyashita, Maika Hayashi, Susumu Umino, Yoshiko Adachi
المصدر: Geological Society, London, Special Publications. 392:177-193
بيانات النشر: Geological Society of London, 2014.
سنة النشر: 2014
مصطلحات موضوعية: Arc (geometry), Tectonics, Stage (stratigraphy), Magmatism, Geochemistry, Geology, Ocean Engineering, Volcanism, Petrology, Ophiolite, Water Science and Technology
الوصف: Based on detailed stratigraphy, petrology and geochemistry, the initial arc magmatism of the Oman Ophiolite consisting of tholeiitic lavas followed by boninite flows and tephras is studied in the Wadi Bidi area, northern Oman Mountains. An 1110-m-thick V2 sequence is divided into the lower 970 m (LV2) and upper 140 m (UV2) thick subsequences by a 1.0-m-thick sedimentary layer. Pahoehoe flows dominate in the lower part of the LV2, while the upper part consists mainly of sheet flows with sparse interbedded pelagic sediments and a cylindrical plug. In addition to the presence of a feeder conduit, the flow-dominant lithofacies with a few thin sedimentary interbeds in the LV2 indicates that the study area was the centre of a volcano grown in a short period. The UV2 is composed of boninite sheet flows overlain by a 2.0-m-thick pyroclastic fall deposit. A small amount of boninite lavas at the end of the V2 sequence overlain by thick pelagic sediments suggests that the subduction-related arc volcanism was short lived and terminated long before the ophiolite obduction. Supplementary material: Locations, mode of occurrence, phenocryst assemblages and bulk-rock major and trace element compositions of lavas in the Wadi Bidi area are available at http://www.geolsoc.org.uk/SUP18684 .
تدمد: 2041-4927
0305-8719
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_________::1536eca4b39619ace513336647ded3d9
https://doi.org/10.1144/sp392.9
حقوق: CLOSED
رقم الأكسشن: edsair.doi...........1536eca4b39619ace513336647ded3d9
قاعدة البيانات: OpenAIRE