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Martin Cramer

Cramer, Martin

Phone:

Office: CLAP 105

Email: martin.cramer@umontana.edu

M.S. Candidate

Curriculum Vitae

Current Office Hours

Thursday 10:00am-12:00pm



Education

M.S., Geoscience                                                                        Anticipated Graduation: Summer 2014

University of Montana, Missoula

 

Bachelor of Science, Geoscience                                                                                        May 2011

Bachelor of Science, Outdoor Education                           

Northland College—Ashland, Wisconsin

GPA: 3.82/4.0

 



Courses Taught

Geo 429, Field Geology: Summer 2013 teaching assistant

Geo 226, Minerals, Rocks and Resources: Spring 2013 teaching assistant

Geo 102 ,Physical Geology Lab: Fall 2012 teaching assistant



Research Interests

    The Ruby Range, located in southwestern Montana, records key aspects of the assembly and stabilization of the Laurentian craton from the Archean to the Paleoproterozoic. Two major periods of tectonothermal activity have been documented within the basement exposures of southwestern Montana: 1) a high-temperature, high-pressure ~1.8 Ga metamorphic event that may record ocean basin closure and continent-continent collision, and 2) a more cryptic metamorphic event at ~2.5 Ga that may be related to rift activity or an older tectonic event. Within the Ruby Range, the P-T-t paths of these events have yet to be determined. Additionally, while historically considered entirely reworked Archean cratonic lithosphere, recent evidence suggests that the Ruby Range may include accreted Proterozoic lithosphere and/or passive margin sediments (O’Neill and Christiansen, 2002; Alcock and Muller, 2012).

My hypothesis is that the Ruby Range represents a mid-crustal window during continental assembly at ~1.8 Ga that will aid us in understanding Proterozoic tectonics and crustal evolution. A combination of structural mapping, metamorphic phase equilibria, and in situ monazite laser ablation split stream inductively coupled plasma mass spectrometry (LASS-ICPMS) petrochronology will: 1) determine the structural history and pressure-temperature (P-T) paths of metamorphic rocks within the Ruby Range, 2) place constraints on the timing of metamorphic events that have occurred in this region, 3) potentially confirm the presence of Proterozoic lithosphere and/or passive margin sediments in this region, and 4) use the P-T-t data to make estimates on the nature and timescales of Proterozoic tectonic processes. These data will result in an improved understanding of the metamorphic evolution of rocks in the Ruby Range as well as provide important constraints on the evolution of continental crust during the assembly of Laurentia.



Field of Study

Metamorphic petrology



Affiliations

Geological Society of America, member since 2010



Specialized Skills

Wilderness First Responder,    Aerie Backcountry Medicine                                                 Expiration: January 2015

         



Honors / Awards

National Park Service, STAR Award                                                                                           August 2012

Northland College, Wallace C. Hitchcock Award                                                                           April 2011

Northland College, Natural Sciences Award                                                                                  April 2011

Northland College, Dean’s Hall of Recognition                                                                               May 2010