17 Undergraduate Research II (Posters)

Thursday, 20 March 2025
1:00 PM - 5:00 PM
Shenandoah ABC


BED FLUIDIZATION EXPERIMENTS AS MAGMA CHAMBER ANALOGS

Paper number: 17-17
Program: Theme Sessions
Time: 1:00 PM – 5:00 PM


Authors


Abstract

The concept of a magma chamber has undergone an evolution over recent decades. Magma chambers are not giant vats of crystal-free magma, and instead, there is a growing body of evidence in support of many magmatic bodies containing significant volume fractions of solids throughout their emplacement history. If this is the case, then new phenomena need to be considered when inferring magmatic processes from product. In this study, we consider one such process--bed fluidization. Bed fluidization occurs when melt percolation through a packed granular bed is sufficient to unpack grains, converting the mass into a mobile slurry. Our model investigates the effects of bed fluidization in a system scaled to represent a mafic slurry with melt percolation from below. The analogs selected are styrene butadiene (plagioclase), polycarbonate (pyroxene), and water (basaltic melt). We allow for these particles to range in sizes, approximating a polydisperse, straight line CSD, by calculating the mass required for each size fraction. Additionally, we utilize particle sizes that have low Particle Reynold’s Number to better approximate grains in magmatic systems. These analog particles are loaded into a Hele-Shaw cell, and water is injected at a controlled flux rate. Repeating the experiment for different flux rates allows for the mapping of resulting features across a range of conditions. These experimental results are extrapolated to magmatic systems through the Ergun Number—a dimensionless parameter that can be used to predict under what conditions bed fluidization occurs. Specifically, we compare the results of these experiments to features observed in the Basement Sill of the McMurdo Dry Valleys, Antarctica, where spectacular unmixing of plagioclase and orthopyroxene have occurred.

Geological Society of America Abstracts with Programs. Vol. 57, No. 2

doi: 10.1130/abs/2025SE-408892

© Copyright 2025 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.