Magnetic Paleointensities in Fault Pseudotachylytes and Implications for Earthquake Lightnings

Magnetic Paleointensities in Fault Pseudotachylytes and Implications for Earthquake Lightnings

Fault pseudotachylytes commonly form by frictional melting due to seismic slip. These fine-grained clastic rocks result from melt quenching and may show a high concentration of fine ferromagnetic grains. These grains are potentially excellent recorders of the rock natural remanent magnetization (NRM...

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Bibliographic Details
Main Author: Leibovitz, Natalie Ruth
Format: Others
Published: OpenSIUC 2016
Subjects:
earthquake lightning
fault pseudotachylyte
magnetite
paleomagnetism
rock magnetism
Online Access:https://opensiuc.lib.siu.edu/theses/1980
https://opensiuc.lib.siu.edu/cgi/viewcontent.cgi?article=2994&context=theses

Internet

https://opensiuc.lib.siu.edu/theses/1980
https://opensiuc.lib.siu.edu/cgi/viewcontent.cgi?article=2994&context=theses

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