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Deciphering viscous flow of frictional melts with the mini-AMS method

Ferré, Eric C.; Chou, Yu Min; Kuo, Ruo Lin; Yeh, En Chao; Leibovitz, Natalie R.; Meado, Andrea L.; Campbell, Lucy; Geissman, John W.

Authors

Eric C. Ferré

Yu Min Chou

Ruo Lin Kuo

En Chao Yeh

Natalie R. Leibovitz

Andrea L. Meado

Lucy Campbell

John W. Geissman



Abstract

The anisotropy of magnetic susceptibility (AMS) is widely used to analyze magmatic flow in intrusive igneous bodies including plutons, sills and dikes. This method, owing its success to the rapid nature of measurements, provides a proxy for the orientation of markers with shape anisotropy that flow and align in a viscous medium. AMS specimens typically are 25 mm diameter right cylinders or 20 mm on-a-side cubes, representing a volume deemed statistically representative. Here, we present new AMS results, based on significantly smaller cubic specimens, which are 3.5 mm on a side, hence∼250 times volumetrically smaller than conventional specimens. We show that, in the case of frictional melts, which inherently have an extremely small grain size, this small volume is in most cases sufficient to characterize the pseudotachylyte fabric, particularly when magnetite is present. Further, we demonstrate that the mini-AMS method provides new opportunities to investigate the details of frictional melt flow in these coseismic miniature melt bodies. This new method offers significant potential to investigate frictional melt flow in pseudotachylyte veins including contributions to the lubrication of faults at shallow to moderate depths.

Citation

Ferré, E. C., Chou, Y. M., Kuo, R. L., Yeh, E. C., Leibovitz, N. R., Meado, A. L., Campbell, L., & Geissman, J. W. (2016). Deciphering viscous flow of frictional melts with the mini-AMS method. Journal of Structural Geology, 90, 15-26. https://doi.org/10.1016/j.jsg.2016.07.002

Journal Article Type Article
Acceptance Date Jul 11, 2016
Online Publication Date Jul 15, 2016
Publication Date 2016-09
Deposit Date Apr 3, 2022
Publicly Available Date May 26, 2022
Journal Journal of Structural Geology
Print ISSN 0191-8141
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 90
Pages 15-26
DOI https://doi.org/10.1016/j.jsg.2016.07.002
Keywords Pseudotachylyte; Anisotropy of magnetic susceptibility; Fabric; Frictional melt; Fault; Magma flow
Public URL https://hull-repository.worktribe.com/output/3963898

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