Ph.D. work
Images (left
to right): Phase
diagram for the
MSH system; NaCl recrystallization in the HDAC; Field work in Yosemite
Natl. Park, CA; Growth of fibrous talc in the HDAC; SEI image of
fibrous talc grown on magnesite; National Synchrotron Light Source
beamline map
My Ph.D. was conducted in the Laboratory of Mineral Deposits Research the Department of Geology at the University of Maryland - College Park under the supervision of Drs. Phil Candela and Phil Picooli
My Ph.D. research focused on
the
experimental
investigation of the
interaction of hot fluids and oceanic lithosphere, specifically the
kinetics of hydrothermal alteration of mafic and ultramafic rocks. My
Ph.D. work is on the system MgO-SiO2-H2O
(±
FeO, HCl, O2
and CO2)
to simulate the metasomatic alteration of ultramafic rocks by
silica-rich fluids in greenschist to amphibolite facies metamorphism.
For
my Ph.D. I had several specific
areas of
investigation:
- experimental determination of mineral dissolution/precipitation rates
- kinetics of the reactions of olivine with silica-rich fluids of varying acidity
- kinetics of the reactions of magnesite with silica-rich H2O-CO2 fluids
- the determination of conditions necessary for the growth of fibrous minerals
- Bassett-type hydrothermal diamond anvil cell (HDAC)
- in-situ weight loss determination
- spindle stage determination of index of refraction
- synchrotron radiation x-ray diffraction
- electron probe microanalyzer
- transmission electron microscope
Master's Degree
Images (left to right): Italian Mt., Gunnison Natl. Forest, CO; S+6-S-2-Cl- triangle plotting lazurite compositions; Hourglass selenite; Geologic Map of Italian Mt vicinity Gunnison Natl. Forest, CO; Single crystal of lazurite; WDS scan of K alpha sulfur peaksMy masters thesis was conducted in the Department of Earth Sciences at the University of Minnesota - Twin Cities under the supervision of Dr. James H. Stout.
My masters research focused on field mapping the Italian Mountian skarn deposit and lapis lazuli mine, along with identification of the chromophore for the blue mineral in lapis lazuli, lazurite. Our work indicated that the intenisty of blue within lazurite is attributed to the ratio of S+6 to S-2. Deeper darker blue lazurite contained more reduced sulfur (S-2) and lighter blue lazurite contained more oxidized sulfur (S+6).
Thesis Title:"The origin of color in lazurite from Italian Mountain, Colorado and other localities."