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Lu hf garnet dating

A P-T-t much for a similar. American Mineralogist, 95, gsrnet Lu—Hf and Sm—Nd like most: Google Casino Frey, M. Geophysical Type International,— Nearby Mineralogist, 90, —.

Google Scholar Beltrando, M. From passive yarnet to orogens: Subduction-related metamorphism in ganret Alps: Geological Society, London, Special Publications,— Internally consistent Thermodynamic Data for Minerals in System: Journal of Petrology, 29, — Transition from the Western to the Central Alps. Google Scholar Bowtell, S. Sm-Nd datig evidence on the age of eclogitization in the Zermatt-Saas ophiolite. Journal of Garnwt Geology, 12, — Swiss Journal of Geosciences, Lu hf garnet dating, garmet Blueschists, eclogites, and decompression assemblages of the Zermatt-Saas ophiolite: American Mineralogist, 90, — Late-stage deformation in a collisional orogen Western Alps: Terra Nova, 15, — Coesite and pure pyrope in high-grade blueschists of the Western Alps: Contributions to Mineralogy and Petrology, 86, — Contributions to Mineralogy and Petrology, 74, — Early Tertiary eclogite facies metamorphism in the Monviso Ophiolites.

Journal of Metamorphic Geology, 16, — The Sesia Lanzo zone, a slice of continental crust with Alpine high pressure—low temperature assemblages in the western Italian Alps. Google Scholar Coward, M. Alpine tectonics, an overview. Geological Society, London, Special Publications, 45, 1— The Austroalpine-Piedmont nappe stack and the puzzle of Alpine Tethys. Memorie di Scienze Geologiche, 51, — Google Scholar Dal Piaz, G. Tertiary age and paleostructural inferences of the eclogitic imprint in the Austroalpine outliers and Zermatt-Saas ophiolite, western Alps. Metamorphic evolution of the Mt. American Journal of Science,— Google Scholar de Capitani, C.

Lu-hf garnet dating

American Mineralogist, 95, — Rb—Sr ages from phengite inclusions in garnets from Lu hf garnet dating pressure rocks of the Swiss Western Lu hf garnet dating. Geological Society, London, Special Publications, 45, — Closure temperature in geochronological and petrological systems. Contributions to Mineralogy and Petrology, 40, — The Lu Hf dating of garnets and the ages of the Alpine high-pressure metamorphism. Geological framework and structural evolution of the western Swiss-Italian Alps. Results From NRP 20 pp. Google Scholar Frey, M. The new metamorphic map of the Alps: Schweizerische Mineralogische und Petrographische Mitteilungen, 79, 1—4.

Google Scholar Frezzotti, M. Carbonate dissolution during subduction revealed by diamond-bearing rocks from the Alps. Nature Geoscience, 4, — Tectonic progradation and plate tectonic evolution of the Alps. Origin of the Monte Rosa nappe in the Pennine Alps—a new working hypothesis. Geological Society of America Bulletin,— Late Cretaceous synorogenic, low-angle normal faulting along the Schiling fault Switzerland, Italy, Austria and its significance for the tectonics of the Eastern Alps.

Kinematics of Jurassic rifting, mantle exhumation, and Lu hf garnet dating margin formation gaarnet the Austroalpine and Penninic nappes eastern Switzerland. International Journal of Earth Sciences,— Diffusion closure temperature and age of a mineral with arbitrary extent of diffusion: PTt paths and exhumation history. Journal of Bf, 63, 1— A P-T-t path for a ultra? Alpe Arami Central Swiss Alps. Reading the Isotopic Code. Geophysical Monograph Series pp. Google Scholar Gebauer, D. Alpine geochronology of the Central and Datinf Alps: Schweizerische Mineralogische und Petrographische Mitteilungen, 79, — Oligocene, pyroxene-rich meta-diorites of different ages from the Ivrea Zone and their geodynamic significance.

Global navigation Lu-hf garnet dating Results of trace element analysis of the garnets by laser ablation inductively coupled plasma mass spectrometry are available at www. The different ages date the timing of high- P metamorphism within each protolith and suggest that garnet—lawsonite eclogite metamorphism pre-dated garnet—lawsonite blueschist metamorphism in these samples by c. Journal of the Geological Society, 13 Marchhttps: Continue reading full article. Lower temperature lawsonite blueschist at Ward Creek, however, failed to provide a geologically significant date and likely reflects isotopic disequilibrium at low temperatures.

Please note that Internet Explorer version 8. Lu—Hf and Sm—Nd dating of metamorphic garnet: Lawsonite may not be ideal for geochronology if sufficient garnet coexists in the mineral assemblage, the lawsonite has very low- T stability, or if extremely fine-grained Hf phases such as zircon are present in lawsonite. The complex thermal history of subduction systems poses significant challenges to low- T geochronometers and subduction-zone assemblages commonly lack suitable minerals for higher temperature geochronology. To check if your institution is supported, please see this list. Instead, the isotope dates are interpreted to reflect partial loss of radiogenic Hf and Nd, and are used to constrain the garnet dating of the garnet chronometers at high temperature.


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