{"id":2796,"date":"2025-12-03T10:48:17","date_gmt":"2025-12-03T09:48:17","guid":{"rendered":"https:\/\/alpshop.rgf.bg.ac.rs\/?page_id=2796"},"modified":"2026-04-01T19:27:25","modified_gmt":"2026-04-01T17:27:25","slug":"ft2-triassic-jurassic-basins-of-the-dinarides","status":"publish","type":"page","link":"https:\/\/alpshop.rgf.bg.ac.rs\/?page_id=2796","title":{"rendered":"FT2 \u2013 Triassic\u2013Jurassic basins of the Dinarides"},"content":{"rendered":"\n<div class=\"wp-block-uagb-container uagb-block-ae0bc409 alignfull uagb-is-root-container\"><div class=\"uagb-container-inner-blocks-wrap\">\n<div class=\"wp-block-uagb-advanced-heading uagb-block-8a1eebc0\"><h1 class=\"uagb-heading-text\">Field Trips<\/h1><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-uagb-container uagb-block-a57fc956 alignfull uagb-is-root-container\"><div class=\"uagb-container-inner-blocks-wrap\">\n<div class=\"wp-block-uagb-container uagb-block-82663714 alignfull uagb-is-root-container\"><div class=\"uagb-container-inner-blocks-wrap\">\n<div class=\"wp-block-uagb-container uagb-block-f54a091d alignfull uagb-is-root-container\"><div class=\"uagb-container-inner-blocks-wrap\">\n<div class=\"wp-block-uagb-container uagb-block-f8ec2bd3 alignfull uagb-is-root-container\"><div class=\"uagb-container-inner-blocks-wrap\">\n<div class=\"wp-block-uagb-advanced-heading uagb-block-e874992d\"><h4 class=\"uagb-heading-text\">Post-Meeting Field Trip FT2: TRIASSIC-JURASSIC INTRAPLATFORM BASINS IN THE DINARIDES &#8211; MYTH OR REALITY? THE NEO-TETHYS GEODYNAMIC HISTORY ALONG A CROSS-SECTION THROUGH THE INNER TO OUTER DINARIDES<\/h4><\/div>\n\n\n\n<div class=\"wp-block-uagb-image aligncenter uagb-block-2d710799 wp-block-uagb-image--layout-default wp-block-uagb-image--effect-static wp-block-uagb-image--align-center\"><figure class=\"wp-block-uagb-image__figure\"><img decoding=\"async\" srcset=\"https:\/\/alpshop.rgf.bg.ac.rs\/wp-content\/uploads\/2025\/12\/FT2-FT-2-Komarani-1024x525.jpg ,https:\/\/alpshop.rgf.bg.ac.rs\/wp-content\/uploads\/2025\/12\/FT2-FT-2-Komarani.jpg 780w, https:\/\/alpshop.rgf.bg.ac.rs\/wp-content\/uploads\/2025\/12\/FT2-FT-2-Komarani.jpg 360w\" sizes=\"auto, (max-width: 480px) 150px\" src=\"https:\/\/alpshop.rgf.bg.ac.rs\/wp-content\/uploads\/2025\/12\/FT2-FT-2-Komarani-1024x525.jpg\" alt=\"\" class=\"uag-image-3039\" width=\"1024\" height=\"525\" title=\"FT2 - FT 2 - Komarani\" loading=\"lazy\" role=\"img\"\/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-uagb-advanced-heading uagb-block-9bfac5c5\"><h2 class=\"uagb-heading-text\">Field Trip Details<\/h2><\/div>\n\n\n\n<p><strong>Contact person:<\/strong><br>Nevenka Djeri\u0107 (<a href=\"mailto:nevenka.djeric@rgf.bg.ac.rs\">nevenka.djeric@rgf.bg.ac.rs<\/a>)<\/p>\n\n\n\n<p><strong>Leaders:<\/strong><br>Hans-J\u00fcrgen Gawlick (Leoben\/Austria), Milan Sudar (Belgrade\/Serbia), Milica Mrdak (Belgrade\/Serbia), Nevenka Djeri\u0107 (Belgrade\/Serbia), Divna Jovanovi\u0107 (Belgrade\/Serbia), Martin \u0110akovi\u0107 (Podgorica\/Montenegro)<\/p>\n\n\n\n<p><strong>Duration\/Date:<\/strong><br>4 days<br>19 September 2026 &#8211; 22 September 2026<\/p>\n\n\n\n<p><strong>Departure \/ final point:<\/strong><br>Vrdnik \u2013 Zlatar \u2013 Bistrica \u2013 Pljevlja \u2013 Durmitor \u2013 \u017dabljak \u2013 Vrdnik (Belgrade)<\/p>\n\n\n\n<p><strong>Price:<\/strong><br>460 EUR (single room), 410 EUR (double room)<\/p>\n\n\n\n<p><strong>Deadline:<\/strong> 30 April 2026<\/p>\n\n\n\n<p><strong>Participants:<\/strong><br>Minimum 20, maximum 50<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"400\" height=\"300\" src=\"https:\/\/alpshop.rgf.bg.ac.rs\/wp-content\/uploads\/2025\/12\/FT2-FT-2-Poros.jpg\" alt=\"\" class=\"wp-image-3040\" srcset=\"https:\/\/alpshop.rgf.bg.ac.rs\/wp-content\/uploads\/2025\/12\/FT2-FT-2-Poros.jpg 400w, https:\/\/alpshop.rgf.bg.ac.rs\/wp-content\/uploads\/2025\/12\/FT2-FT-2-Poros-300x225.jpg 300w\" sizes=\"auto, (max-width: 400px) 100vw, 400px\" \/><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-uagb-advanced-heading uagb-block-48076506\"><h2 class=\"uagb-heading-text\">Description<\/h2><\/div>\n\n\n\n<p>This excursion explores the Triassic\u2013Jurassic depositional history of the Dinarides, with a particular emphasis on the relationship between shallow-water carbonate production and coeval deep-water sedimentary successions. A central objective is to understand the Mesozoic\u2014primarily Triassic to Jurassic\u2014geodynamic evolution of the Western Tethys Realm, in which the Dinarides represent a key orogenic system.<\/p>\n\n\n\n<p>The field trip will focus on the deep-water sedimentary rocks during the Triassic-Jurassic geodynamic history in different basins: rift-basins, shelf areas, oceanic domains, trench-like basins, foreland basins.<\/p>\n\n\n\n<p>Special focus will be the so-called Lim zone in the Triassic (Lim deep-water intra-plattform basin) with the Zlatar and Cehotina deep-water subbasins between the Drina-Ivanjica unit (shallow-water Golija zone) and the shallow-water Durmitor zone with the shallow-water Mihajlovici ridge in the central part, all of them interpreted as Ladinian to Rhaetian shallow-water platforms (Wetterstein and Dachstein).<\/p>\n\n\n\n<p>We will visit:<\/p>\n\n\n\n<p>&#8211; Middle Triassic to Middle Jurassic passive margin evolution: all depositional realms from the continental slope to the the central shelf.<\/p>\n\n\n\n<p>-The Middle Triassic continental break-up: Anisian demise of shallow-water carbonate production, horst-and-graben formation, and deposition of deep-marine sediments elsewhere.<\/p>\n\n\n\n<p>-Restart of shallow-water carbonate production in the Middle and Late Triassic: the sedimentary sequences in the deep-water depositional realm as mirror of platform progradation (Sequence stratigraphy, highstand shedding, carbonate production potential).<\/p>\n\n\n\n<p>-Reasons for the demise of the Triassic shallow-water platforms and the expression of these events in deep-water settings.<\/p>\n\n\n\n<p>-Condensed Early-Middle Jurassic deep-water sedimentary rocks.<\/p>\n\n\n\n<p>-Active continental margin evolution: Middle to Late Jurassic radiolaritic\/argillaceous trench-like basin formation and nappe stacking in front of obducting ophiolites, large-scale mass movements. M\u00e9lange formation. The whole story is visible in one of the most beautiful areas of the Balkan Peninsula, the area between the Inner and Outer Dinarides in western Serbia and northern Montenegro. The field trip will provide beside geological highlights also special insights in culture and undisturbed nature in an area with increasing tourism.<\/p>\n<\/div>\n<\/div>\n\n\n\n<p><\/p>\n<\/div><\/div>\n<\/div><\/div>\n<\/div><\/div>\n<\/div><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Field Trips Post-Meeting Field Trip FT2: TRIASSIC-JURASSIC INTRAPLATFORM BASINS IN THE DINARIDES &#8211; MYTH OR REALITY? THE NEO-TETHYS GEODYNAMIC HISTORY ALONG A CROSS-SECTION THROUGH THE INNER TO OUTER DINARIDES Field Trip Details Contact person:Nevenka Djeri\u0107 (nevenka.djeric@rgf.bg.ac.rs) Leaders:Hans-J\u00fcrgen Gawlick (Leoben\/Austria), Milan Sudar (Belgrade\/Serbia), Milica Mrdak (Belgrade\/Serbia), Nevenka Djeri\u0107 (Belgrade\/Serbia), Divna Jovanovi\u0107 (Belgrade\/Serbia), Martin \u0110akovi\u0107 (Podgorica\/Montenegro) Duration\/Date:4 [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":2791,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_uag_custom_page_level_css":"","site-sidebar-layout":"no-sidebar","site-content-layout":"page-builder","ast-site-content-layout":"full-width-container","site-content-style":"unboxed","site-sidebar-style":"unboxed","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"disabled","ast-breadcrumbs-content":"","ast-featured-img":"disabled","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"enabled","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"set","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"class_list":["post-2796","page","type-page","status-publish","hentry"],"uagb_featured_image_src":{"full":false,"thumbnail":false,"medium":false,"medium_large":false,"large":false,"1536x1536":false,"2048x2048":false},"uagb_author_info":{"display_name":"alp_admin","author_link":"https:\/\/alpshop.rgf.bg.ac.rs\/?author=1"},"uagb_comment_info":0,"uagb_excerpt":"Field Trips Post-Meeting Field Trip FT2: TRIASSIC-JURASSIC INTRAPLATFORM BASINS IN THE DINARIDES &#8211; MYTH OR REALITY? THE NEO-TETHYS GEODYNAMIC HISTORY ALONG A CROSS-SECTION THROUGH THE INNER TO OUTER DINARIDES Field Trip Details Contact person:Nevenka Djeri\u0107 (nevenka.djeric@rgf.bg.ac.rs) Leaders:Hans-J\u00fcrgen Gawlick (Leoben\/Austria), Milan Sudar (Belgrade\/Serbia), Milica Mrdak (Belgrade\/Serbia), Nevenka Djeri\u0107 (Belgrade\/Serbia), Divna Jovanovi\u0107 (Belgrade\/Serbia), Martin \u0110akovi\u0107 (Podgorica\/Montenegro) Duration\/Date:4&hellip;","_links":{"self":[{"href":"https:\/\/alpshop.rgf.bg.ac.rs\/index.php?rest_route=\/wp\/v2\/pages\/2796","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/alpshop.rgf.bg.ac.rs\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/alpshop.rgf.bg.ac.rs\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/alpshop.rgf.bg.ac.rs\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/alpshop.rgf.bg.ac.rs\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=2796"}],"version-history":[{"count":17,"href":"https:\/\/alpshop.rgf.bg.ac.rs\/index.php?rest_route=\/wp\/v2\/pages\/2796\/revisions"}],"predecessor-version":[{"id":3247,"href":"https:\/\/alpshop.rgf.bg.ac.rs\/index.php?rest_route=\/wp\/v2\/pages\/2796\/revisions\/3247"}],"up":[{"embeddable":true,"href":"https:\/\/alpshop.rgf.bg.ac.rs\/index.php?rest_route=\/wp\/v2\/pages\/2791"}],"wp:attachment":[{"href":"https:\/\/alpshop.rgf.bg.ac.rs\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=2796"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}