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- W772768549 abstract "INVESTIGATING THE ANISTOROPY OF MAGNETIC SUSCEPTIBILITY AND OTHER ROCK MAGNETIC PROPERTIES OF THE BEAVER RIVER DIABASE IN NORTHEASTERN MINNESOTA. by SAMER H. HARIRI December 2014 Advisor: Dr. Sarah Brownlee Major: Geology Degree: Master of Science The Beaver River Diabase (BRD) is a series of mafic dikes and sills within the Beaver Bay Complex (BBC) of northern Minnesota, which formed during the development of the ~1.1 Ga Midcontinent Rift (MCR). The BRD is one of the youngest and most extensive intrusive phases of the BBC. The BRD dikes and sills were emplaced into the medial levels of the 6-10 kilometer-thick North Shore Volcanic Group and occur over an arcuate area extending 120 by 20 kilometers. The BRD is composed of fineto medium-grained ophitic olivine gabbro and does not display obvious foliation or lineation features and rarely displays modal layering. Without obvious magmatic internal structures, it is difficult to determine emplacement properties such as flow direction using standard geologic mapping or petrographic techniques. For this reason, we measured the anisotropy of magnetic susceptibility (AMS), in conjunction with other rock magnetic properties, to better understand the BRD’s emplacement and deformation history in the context of the MCR." @default.
- W772768549 created "2016-06-24" @default.
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- W772768549 date "2014-01-01" @default.
- W772768549 modified "2023-09-26" @default.
- W772768549 title "Investigating The Anisotropy Of Magnetic Susceptibility And Other Rock Magnetic Properties Of The Beaver River Diabase In Northeastern Minnesota" @default.
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