{"id":12689,"date":"2021-06-29T09:00:30","date_gmt":"2021-06-29T07:00:30","guid":{"rendered":"https:\/\/physik.nawi.at\/?p=12689"},"modified":"2021-06-29T12:05:45","modified_gmt":"2021-06-29T10:05:45","slug":"einladung-zum-vera-seminar-von-stephanie-neuhuber-zum-thema-numerical-age-dating-of-cave-sediments-quantify-vertical-movement-at-the-alpine-carpathian-transition","status":"publish","type":"post","link":"https:\/\/physik.nawi.at\/index.php\/einladung-zum-vera-seminar-von-stephanie-neuhuber-zum-thema-numerical-age-dating-of-cave-sediments-quantify-vertical-movement-at-the-alpine-carpathian-transition\/","title":{"rendered":"Einladung zum Vera-Seminar zum Thema “Numerical age dating of cave sediments quantify vertical movement at the Alpine-Carpathian transition”"},"content":{"rendered":"

E I N L A D U N G<\/span>
\n<\/span>zum<\/span><\/p>\n

V E R A – S E M I N A R<\/span><\/p>\n

von<\/span><\/p>\n

 <\/p>\n

Stephanie NEUHUBER<\/span><\/p>\n

 <\/p>\n

Institut f\u00fcr Angewandte Geologie, Labor f\u00fcr kosmogene Nuklide,\u00a0<\/span><\/p>\n

Universit\u00e4t f\u00fcr Bodenkultur Wien<\/span><\/p>\n

 <\/p>\n

Numerical age dating of cave sediments<\/span><\/p>\n

quantify vertical movement at the<\/span><\/p>\n

Alpine-Carpathian transition<\/span><\/p>\n

 <\/p>\n

 <\/p>\n

The paleoenvironmental and tectonic history at the southwestern end of the Mal\u00e9 Karpaty Mountains close to Hainburg an der Donau was reconstructed using sediment analysis, mineralogy, and numerical age dating. Numerical ages were constrained by <\/span>26<\/span><\/span>Al\/<\/span>10<\/span><\/span>Be burial age dating, <\/span>230<\/span><\/span>Th\/U ages and luminescence age dating to infer the Pliocene and Pleistocene development of the Hainburg Hills region. This study investigated sediments from two caves separated by a height difference of 92 m as well as aeolian cover sands from a fissure. The cave deposits are very different as one is a carbonate precipitate and the other sediment infill. Both preserve information on the uplift\/incision at the Alpine-Carpathian border. The minerals hematite and smectite as well as traces of poorly crystallized iron oxides found in the matrix of the upper (older) cave, suggest formation during warm and humid climate. This is a remnant from the late Miocene or Early Pliocene where soil formed in a subtropical climate.<\/span><\/p>\n

 <\/p>\n

 <\/p>\n

Mittwoch,<\/span> 30. Juni 2021, 16:30 Uhr<\/span><\/p>\n

Zoom-Meeting <\/span>\/ ab<\/span> 16:15 Uhr offen<\/span><\/p>\n

\u00a0<\/b><\/p>\n

https:\/\/univienna.zoom.us\/j\/98385461923?pwd=L0s2dUJLSmkwS040aStiNCtnOUNTdz09<\/span><\/a><\/p>\n

 <\/p>\n

Die Zugangsdaten: Meeting ID: 983 8546 1923 \u00a0 Passwort: 458365<\/span><\/p>\n

\u00a0<\/span><\/div>\n","protected":false},"excerpt":{"rendered":"

E I N L A D U N G zum V E R A – S E M I N A R von   Stephanie NEUHUBER   Institut f\u00fcr Angewandte Geologie, Labor f\u00fcr kosmogene Nuklide,\u00a0 Universit\u00e4t f\u00fcr Bodenkultur Wien   Numerical age dating of cave sediments quantify vertical movement at the Alpine-Carpathian transition     […]<\/p>\n","protected":false},"author":86,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"wds_primary_category":0,"_wpscppro_dont_share_socialmedia":false,"_wpscppro_custom_social_share_image":0,"_facebook_share_type":"","_twitter_share_type":"","_linkedin_share_type":"","_pinterest_share_type":"","_linkedin_share_type_page":"","_instagram_share_type":"","_medium_share_type":"","_threads_share_type":"","_google_business_share_type":"","_selected_social_profile":[],"_wpsp_enable_custom_social_template":false,"_wpsp_social_scheduling":{"enabled":false,"datetime":null,"platforms":[],"status":"template_only","dateOption":"today","timeOption":"now","customDays":"","customHours":"","customDate":"","customTime":"","schedulingType":"absolute"},"_wpsp_active_default_template":true},"categories":[20],"tags":[],"_links":{"self":[{"href":"https:\/\/physik.nawi.at\/index.php\/wp-json\/wp\/v2\/posts\/12689"}],"collection":[{"href":"https:\/\/physik.nawi.at\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/physik.nawi.at\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/physik.nawi.at\/index.php\/wp-json\/wp\/v2\/users\/86"}],"replies":[{"embeddable":true,"href":"https:\/\/physik.nawi.at\/index.php\/wp-json\/wp\/v2\/comments?post=12689"}],"version-history":[{"count":0,"href":"https:\/\/physik.nawi.at\/index.php\/wp-json\/wp\/v2\/posts\/12689\/revisions"}],"wp:attachment":[{"href":"https:\/\/physik.nawi.at\/index.php\/wp-json\/wp\/v2\/media?parent=12689"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/physik.nawi.at\/index.php\/wp-json\/wp\/v2\/categories?post=12689"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/physik.nawi.at\/index.php\/wp-json\/wp\/v2\/tags?post=12689"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}