ASU Electronic Theses and Dissertations
This collection includes most of the ASU Theses and Dissertations from 2011 to present. ASU Theses and Dissertations are available in downloadable PDF format; however, a small percentage of items are under embargo. Information about the dissertations/theses includes degree information, committee members, an abstract, supporting data or media.
In addition to the electronic theses found in the ASU Digital Repository, ASU Theses and Dissertations can be found in the ASU Library Catalog.
Dissertations and Theses granted by Arizona State University are archived and made available through a joint effort of the ASU Graduate College and the ASU Libraries. For more information or questions about this collection contact or visit the Digital Repository ETD Library Guide or contact the ASU Graduate College at gradformat@asu.edu.
- Lynda, Williams B
- 1 Amanda, Clarke B
- 1 Arizona State University
- 1 Donald, Burt M
- 1 Guggino, Steve Nelson
- 1 Hervig, Richard L
- 1 Stanley, Williams N
- 1 English
- 1 Public
- Geochemistry
- 1 Fluorine
- 1 Fluorine Partitioning
- 1 Microanalytical Reference Materials
- 1 Mineralogy
- 1 Nominally Anhydrous Minerals
- 1 Partition Coefficient
- more
- 1 Petrology
- 1 Secondary Ion Mass Spectrometry
- Dwarf Galaxies as Laboratories of Protogalaxy Physics: Canonical Star Formation Laws at Low Metallicity
- Evolutionary Genetics of CORL Proteins
- Social Skills and Executive Functioning in Children with PCDH-19
- Deep Domain Fusion for Adaptive Image Classification
- Software Defined Pulse-Doppler Radar for Over-The-Air Applications: The Joint Radar-Communications Experiment
Fluorine (F) is a volatile constituent of magmas and hydrous mantle minerals. Compared to other volatile species, F is highly soluble in silicate melts, allowing F to remain in the melt during magma differentiation and rendering F less subject to disturbance during degassing upon magma ascent. Hence, the association between fluorine in basalts and fluorine in the mantle source region is more robust than for other volatile species. The ionic radius of F- is similar to that of OH- and O2-, and F may substitute for hydroxyl and oxygen in silicate minerals and melt. Fluorine is also incorporated at trace …
- Contributors
- Guggino, Steve Nelson, Hervig, Richard L, Donald, Burt M, et al.
- Created Date
- 2012