Paper No. 6
Presentation Time: 9:00 AM-6:30 PM


ROMANOSKI, Anthony M.1, HETHERINGTON, Callum J.2, ARENDALE, Avery H.3, BARNES, Calvin G.2 and COTTLE, John4, (1)Geosciences, Texas Tech University, Box 41053, Lubbock, TX 79409-1053, (2)Department of Geosciences, Texas Tech University, Box 41053, Lubbock, TX 79409-1053, (3)Department of Geosciences, Texas Tech University, Box 41053, Lubbock, TX 79410-1053, (4)Department of Earth Science, University of California, Santa Barbara, Santa Barbara, CA 93106,

U-Pb geochronology, Hf isotope analysis, trace element geochemistry and zircon imaging concludes that emplacement of peraluminous pegmatitic granitic gneiss in the Ruby Mountains-East Humboldt metamorphic core complex, Nevada, occurred during two discrete, short-lived magmatic events during Cretaceous and Paleocene times. A third period of zircon crystallization is evident in pegmatitic gneiss occurring during Eocene times in response to partial melting of the older pegmatitic gneiss. This migmitization may have occurred in response to a thermal influx resulting from extensional deformation and emplacement of Eocene magmas.

Zircon from magmatic pegmatitic gneiss reveals two periods of crystallization at 70.7 ± 0.5 Ma and 60.6 ± 0.2 Ma. The older gneiss has an average εHf value of -30 (± 8 ε units). Heavy rare earth element (HREE) ratios range between (LuCN/GdCN) ~15 and ~33. Pegmatitic gneiss dated at 60.6 Ma has an average εHf value of -46.3 ± 2.4 (± 8 ε units). Heavy REE abundances are an order of magnitude higher than the older unit, with HREE ratios from (LuCN/GdCN) ~54 to ~83. Biotite monzogranite from the same field area gives a crystallization age of 33.7 ± 0.3. Hf analyses gave a mean εHf value of -40.1 ± 3.2 (± 6 ε unit). U-Pb analysis of zircon cores from very coarse-grained gneiss give ages of ~71 Ma, whereas rims yield a crystallization age of 34.2 ± 2.7 Ma. Hf analysis of the 34.2 Ma zircon rims give average εHf values of -27.1 ± 2.2 (± 6 ε unit). The U-Pb and Hf values overlap with those of the Late Cretaceous pegmatitic gneiss but show a more restricted range. Heavy REE ratios (LuCN/GdCN = ~39 to ~88) are similar to those from Late Cretaceous pegmatitic gneiss. It is proposed that partial melting of Late Cretaceous pegmatitic gneiss was the result of an increased thermal input, possibly from intruding magmas, during extensional deformation and core complex formation to produce migmatites.

These new data, when combined with εHf values of -14 in zircon from a 91-92 Ma equi-granular granitic gneiss suggest that Cretaceous to Eocene peraluminous granites in the Ruby Mountains have distinctly crustal, but unique, sources as well as temporally short-lived emplacement histories. The data support a model that requires refertilization of the lower crust, which is compatible with channel flow beneath an elevated plateau.