11 Recent Advances in Basin-and-Range and Proterozoic Geology of the Western U.S.: A Session Honoring Ernie Duebendorfer (Posters)

Tuesday, 15 May 2018
8:30 AM - 6:30 PM
Outdoor Tents


CRYSTALLOGRAPHICALLY ORIENTED RUTILE NEEDLES IN GARNET FROM THE TAOS RANGE OF NORTHERN NEW MEXICO SUGGEST (ULTRA) HIGH TEMPERATURE PROTEROZOIC METAMORPHISM

Paper number: 11-7
Program: Symposia Sessions
Time: 8:30 AM – 6:30 PM


Authors


Abstract

Uplifts in northern New Mexico and southern Colorado expose high grade metamorphic rocks that represent significant crustal thickening during Proterozoic tectonism. Metamorphic garnet from the northern Taos Range, New Mexico contains two types of rutile inclusions: rounded coarse rutile and crystallographically oriented rutile needles. The several micrometer wide rutile needles only occur within garnet core domains in two pelitic schist samples. The samples include the assemblage garnet + biotite + quartz + K–feldspar + muscovite + plagioclase + sillimanite ± tourmaline + accessory minerals. Garnet cores are almandine-rich (~0.85) with low pyrope (near 0.07) and spessartine (0.03–0.07), plus very low grossular (~0.01–0.03). All garnets show shifts in composition near the rims, consistent with the disappearance of the rutile needle inclusions. Ti solubility in garnet is known to increase with temperature. Similar oriented rutile crystals in metamorphic garnet in other orogens are interpreted to represent exsolution/precipitation of TiO2 from high Ti garnet in response to a decrease in Ti solubility in garnet due to cooling. Garnet with Ti contents leading to rutile exsolution/precipitation during cooling are estimated to represent metamorphic temperatures over 900ºC in other localities, in many cases representing extreme UHT/UHP metamorphic conditions. The timing of granulite facies or UHT metamorphism in these samples is not directly constrained but based on U-Pb monazite ages from nearby samples likely took place during the Mesoproterozoic Picuris Orogeny.

Geological Society of America Abstracts with Programs. Vol. 50, No. 5

doi: 10.1130/abs/2018RM-314357

© Copyright 2018 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.