COOKIES: By using this website you agree that we can place Google Analytics Cookies on your device for performance monitoring. |
University of Cambridge > Talks.cam > Department of Earth Sciences Seminars (downtown) > Rift initiation in a continental setting: the western Balkan peridotites
Rift initiation in a continental setting: the western Balkan peridotitesAdd to your list(s) Download to your calendar using vCal
If you have a question about this talk, please contact John Maclennan. The Dinaride and Vardar zone ophiolite belts extend from the south-eastern margins of the Alps to the Albanian and Greek ophiolites. Detailed sampling of the Krivaja–Konjuh massif, one of the largest massifs in the Dinaride belt (> 600 km2), reveals fertile compositions and an extensive record of deformation at spinel peridotite facies conditions. High Na2O clinopyroxene and spinel–orthopyroxene symplectites after garnet, as well as cpx trace element patterns indicate a garnet facies (subcontinental) origin of the southern and western parts, similar to orogenic massifs such as Lherz, Ronda and the Eastern Central Alpine peridotites. In contrast to those massifs the peridotites from Krivaja are not refertilised. Clinopyroxene and spinel compositions from the eastern parts show similarities with fertile abyssal peridotite. In the central parts of the massif the spinel lherzolites contain locally abundant patches of plagioclase. The pyroxene abundances of the plagioclase peridotites range from similar to the fertile spinel peridotites to massive olivine-rich troctolites with no primary pyroxene. We infer that the olivine-rich troctolites are due to migrating melt dissolving pyroxene and then freezing, with interstitial plagioclase and cpx geometries similar to experimentally produced partial melts. Overall we infer that the massif represents the onset of continental rifting and early stages of formation of a new ocean basin. Combining our data with previously published analyses of other Balkan massifs we create a compositional map that suggests a simple tectonic setting for the Balkan massifs. This talk is part of the Department of Earth Sciences Seminars (downtown) series. This talk is included in these lists:
Note that ex-directory lists are not shown. |
Other listsRobinson College Seminars at the Department of Biochemistry What IS the deal with meat? Interesting talks- 1st try Cambridge Algorithms talks Social Psychology Seminar Series (SPSS)Other talksCellular recycling: role of autophagy in aging and disease Ethics for the working mathematician, seminar 8: Standing on the shoulders of giants. CPGJ Reading Group "Space, Borders, Power" Part IIB Poster Presentations Annual General Meeting Biomolecular Thermodynamics and Calorimetry (ITC) |