GSA Annual Meeting in Phoenix, Arizona, USA - 2019

Paper No. 274-5
Presentation Time: 9:00 AM-6:30 PM

CONSTRAINING THE TIMING OF PROGRADE METAMORPHISM IN THE SOLE OF THE SEMAIL OPHIOLITE: COUPLED ZIRCON TIMS U-PB DATING AND TRACE ELEMENT ANALYSES FROM THE MASAFI SOLE EXPOSURE, UNITED ARAB EMIRATES (U.A.E.)


STEVENS, Sally1, RIOUX, Matthew1, GARBER, Joshua M.2, SEARLE, Michael P.3, CROWLEY, Jim L.4 and KYLANDER-CLARK, Andrew R.C.1, (1)Department of Earth Science, University of California Santa Barbara, Santa Barbara, CA 93106, (2)Department of Geosciences, Penn State University, State College, PA 16801, (3)Department of Earth Sciences, University of Oxford, Oxford, OX1 3AN, United Kingdom, (4)Department of Geosciences, Boise State University, Boise, ID 83725

The Semail (Oman-U.A.E.) ophiolite is the largest and most extensively studied ophiolite in the world. Several lines of evidence suggest the ophiolite formed in a supra-subduction zone setting, potentially during subduction initiation. The ophiolite is underlain by an inverted metamorphic sole, consisting of greenschist- to granulite-facies metabasalts and metasediments. Geochronologic studies of these rocks can determine the timing of initial lower-plate burial relative to upper-plate extension, constraining the tectonic development of the ophiolite. Previous high-precision ID-TIMS zircon U-Pb dating of upper-level gabbros indicates rapid formation of the ophiolite crust from 96.12–95.50 Ma. In comparison, ID-TIMS zircons dates from leucocratic pods from the Sumeini and Wadi Tayin sole localities yield dates of 96.16 ± 0.022 Ma and 94.82 ± 0.035 Ma, respectively. Here we present new data from the Asimah-Masafi sole exposure at the northern end of the ophiolite in the U.A.E. To directly date peak metamorphism, we targeted garnet-clinopyroxene bearing amphibolites and used combined zircon ID-TIMS U-Pb dating and LA-ICP-MS trace-element analyses to link zircon dates to metamorphic processes. Zircons from five samples show a range from steep (Yb/Dy > 5) to shallow HREE (Yb/Dy < 5) slopes. We attribute spots with steep HREE slopes to pre-garnet zircon growth and spots with shallow HREE slopes to syn- or post-garnet zircon growth. In preliminary ID-TIMS data from two samples, HREE-enriched zircon have older TIMS U-Pb dates compared to HREE-depleted zircon from the same sample, which we interpret to bracket the timing of prograde garnet growth to ~96.6–96.2 Ma and ~95.6–95.3 Ma at the Khubakhib and Asimah localities, respectively. Our dates are similar to the previous U-Pb zircon dates from the sole, but significantly younger than recently reported Lu-Hf garnet dates (~104 Ma; Guilmette et al., 2018).