"Olivine Variability of the Nickel Lake Macrodike of Northern Minnesota" by Katelyn Boege
 

Honors Program Theses

Award/Availability

Open Access Honors Program Thesis

First Advisor

Chad Heinzel

Abstract

This project is looking at the mineralogy of olivine crystals found in an igneous formation called the Nickel Lake Macrodike. This formation is from 1.1 billion years ago and is a part of the Midcontinent Rift System that extends from Kansas to Michigan. Olivine crystals are typically only found in ultramafic and mafic rocks which are associated with the mantle of the Earth. Knowing more about the original composition of the magma that formed these crystals can give information about the consistency of the magma and can give more information about the formation of other rocks in the area. Given the results presented in the figures, there is evidence for morphological and chemical changes within Nickel Lake Macrodike. This means that as the dike formed, the magma likely changed in composition and the morphology indicates a change in cooling rates.

Year of Submission

2024

Department

Department of Environmental Science

University Honors Designation

A thesis submitted in partial fulfillment of the requirements for the designation University Honors

Date Original

12-2024

Object Description

1 PDF (18 pages)

Language

en

File Format

application/pdf

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