T37 Geologic Fluids: Agents of Change (Posters)
Sunday, 15 October 2023
8:00 AM - 5:30 PM
Hall B
DATING SEDIMENTARY REACTIVE FLUID FLOW USING ZIRCON
Paper number: T37-6
Program: Technical Sessions
Time: 8:00 AM – 5:30 PM
Authors
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Erik SchoonoverThe Pennsylvania State University, University Park, PA
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Alex CerminaroThe Pennsylvania State University, University Park, PA
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Joshua GarberThe Pennsylvania State University, University Park, PA
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Max K. LloydThe Pennsylvania State University, University Park, PA
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Jesse ReiminkThe Pennsylvania State University, University Park, PA
Abstract
The Alta Stock is surrounded by a very well-studied metamorphic reaction aureole as a result, zircons in metamorphosed sediments experienced high and low-temperature fluid flow. Here, we present results from an attempt to use detrital zircon discordance to accurately quantify the age of lead (Pb) loss from rocks surrounding the Alta Stock in Utah. Using uranium-lead data from hydrothermally altered detrital zircon we accurately placed age constraints on hydrothermal alteration in Alta contact aureole. The Alta, Utah area experienced hydrothermal fluid from around 30-23 Ma. Our results agree well with other chronometric data from the area. We quantify the uncertainty in our analysis using detrital zircons, by applying a bootstrap resampling model that allows us to test the sensitivity of our technique for geochronology. We also examine the chemical effects of both fluid flow and metamorphism within zircons that have experienced Pb-loss. We evaluate whether metamorphism or fluid flow, or a combination, are drivers of Pb-loss and are therefore datable using our approach.
We will discuss the implications of the data for the applicability of our discordance dating technique for other fluid-flow and/or metamorphic settings.
Geological Society of America Abstracts with Programs. Vol. 55, No. 6
doi: 10.1130/abs/2023AM-395707
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