{"id":751,"date":"2018-11-10T11:08:27","date_gmt":"2018-11-10T10:08:27","guid":{"rendered":"https:\/\/wp.ux.uis.no\/julocra\/?p=751"},"modified":"2018-12-11T10:31:02","modified_gmt":"2018-12-11T09:31:02","slug":"751","status":"publish","type":"post","link":"https:\/\/wp.ux.uis.no\/julocra\/2018\/11\/10\/751\/","title":{"rendered":"JuLoCra annual meeting- Preliminary agenda"},"content":{"rendered":"

Date: <\/strong>07.12.2018<\/p>\n

Time: <\/strong>9:00<\/p>\n

Place:\u00a0<\/strong>Odin meeting room at NPD<\/p>\n

 <\/p>\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n
\n

Time<\/h4>\n
\n

 <\/th>\n

Speaker<\/p>\n
\n

 <\/th>\n

Presentation<\/p>\n
\n

\n<\/th>\n<\/tr>\n

\u00a0 \u00a0 9:00-9:20<\/th>\nAlejandro Escalona and Snorre Olaussen<\/span><\/th>\nIntroduction to the project and database<\/span><\/th>\n<\/tr>\n
9:20-9:40<\/span><\/th>\nMorten Smelror<\/span><\/th>\nBiostratigraphic subdivision of the Bathonian to Base Cretaceous Unconformity (BCU succession in the Barents Sea and Svalbard)<\/span><\/th>\n<\/tr>\n
9:40-10:00<\/span><\/th>\nSnorre Olaussen <\/span><\/th>\nTectonism, depositional environment of the Bathonian to Base Cretaceous Unconformity (BCU succession in Northern most Barents Sea\u00a0 and Svalbard)<\/span><\/th>\n<\/tr>\n
10:00-10:20<\/span><\/th>\nJ\u00f8rn Hurum<\/span><\/th>\nJurassic Cretaceous reptiles in Svalbard – current status\u00a0 <\/span><\/th>\n<\/tr>\n
10:20-10:40<\/span><\/th>\n\u00d8yvind Hammer<\/span><\/th>\nMethane hydrocarbon seeps in Spitsbergen<\/span><\/th>\n<\/tr>\n
10:40-11:00<\/span><\/th>\n— Break —<\/span><\/b><\/th>\n—<\/th>\n<\/tr>\n
11:00-11:20<\/span><\/th>\nAnna Suslova<\/span><\/th>\nBarents Sea basin analysis overview: techniques and key attributes<\/span><\/th>\n<\/tr>\n
11:20-11:40<\/span><\/th>\nAlina Mordasova<\/th>\nGeological structure and distribution of the Jurassic-Lower Cretaceous strata of the Western Arctic shelf<\/span><\/th>\n<\/tr>\n
11:40-12:00<\/span><\/th>\nCarita Augustsson<\/th>\nMiddle to Upper Jurassic facies and depositional settings in the Hammerfest Basin<\/span><\/th>\n<\/tr>\n
12:00-12:30<\/span><\/th>\nBj\u00f8rn K\u00e5re Bryn<\/span><\/th>\nScarecrow \u2013 Exploring the Lower Cretaceous of the Fingerdjupet Sub-basin<\/span><\/th>\n<\/tr>\n
12:30-12:50<\/span><\/th>\nDora Mar\u00edn<\/span><\/th>\nUnraveling the lateral variation in the Middle Jurassic to earliest Cretaceous succession in the SW Barents Sea <\/span><\/th>\n<\/tr>\n
12:50-13:20<\/span><\/th>\n— Light lunch —<\/span><\/b><\/th>\n—<\/th>\n<\/tr>\n
13:20-13:30<\/span><\/th>\nSolveig Helleren<\/span><\/th>\nCan the prominent gamma ray spikes in the Upper Jurassic source rock disclose lateral changes the deposition in the southwestern Barents Sea? (Thesis proposal)<\/span><\/th>\n<\/tr>\n
13:30-13:40<\/span><\/th>\nOlav Josefsen<\/span><\/th>\nOrigin of folds in hangingwalls of the southern Hammerfest Basin and their impact in coarse-grained sediment distribution (thesis proposal)<\/span><\/th>\n<\/tr>\n
13:40-14:00<\/span><\/th>\nElizaveta Krasnova<\/th>\nGeochemical evaluation and the work progress on the Upper\u00a0Jurassic-Lower Cretaceous\u00a0samples of the Barents Sea basin<\/span><\/th>\n<\/tr>\n
14:00-14:20<\/span><\/th>\nSverre Ohm<\/th>\nSource rock variation within the Hekkingen Formation. <\/span>Part I: Background material.<\/th>\n<\/tr>\n
14:20-14:40<\/span><\/th>\nAndres Cede\u00f1o<\/th>\nSource rock variation within the Hekkingen Formation. <\/span>Part II: Application and visualization.<\/th>\n<\/tr>\n
14:40-15:00<\/span><\/th>\nChristian Bjerrum<\/th>\nPaleoceanographic modelling of the Late Jurassic – quality and distribution of source rock in frontier basins. R&D project proposal by University of Copenhagen (KU) and GEUS<\/span><\/th>\n<\/tr>\n
15:00-15:20<\/span><\/th>\nAlejandro Escalona and Snorre Olaussen<\/th>\nDiscussion and future work<\/span><\/th>\n<\/tr>\n<\/tbody>\n<\/table>\n","protected":false},"excerpt":{"rendered":"

Date: 07.12.2018 Time: 9:00 Place:\u00a0Odin meeting room at NPD   Time   Speaker   Presentation \u00a0 \u00a0 9:00-9:20 Alejandro Escalona and Snorre Olaussen Introduction to the project and database 9:20-9:40 Morten Smelror Biostratigraphic subdivision of the Bathonian to Base Cretaceous Unconformity (BCU succession in the Barents Sea and Svalbard) 9:40-10:00 Snorre Olaussen Tectonism, depositional environment […]<\/p>\n","protected":false},"author":5,"featured_media":788,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3],"tags":[],"class_list":["post-751","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-latest-events-news"],"_links":{"self":[{"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/posts\/751","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/users\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/comments?post=751"}],"version-history":[{"count":9,"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/posts\/751\/revisions"}],"predecessor-version":[{"id":789,"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/posts\/751\/revisions\/789"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/media\/788"}],"wp:attachment":[{"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/media?parent=751"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/categories?post=751"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/wp.ux.uis.no\/julocra\/wp-json\/wp\/v2\/tags?post=751"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}