Award Abstract # 1039797
MRI: Acquistion of Integrated Energy Dispersive X-Ray, Electron Backscatter Diffraction and Panchromatic Cathodoluminescence Imaging System

NSF Org: EAR
Division Of Earth Sciences
Recipient: COLGATE UNIVERSITY
Initial Amendment Date: September 20, 2010
Latest Amendment Date: September 20, 2010
Award Number: 1039797
Award Instrument: Standard Grant
Program Manager: Russell Kelz
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: October 1, 2010
End Date: September 30, 2012 (Estimated)
Total Intended Award Amount: $187,937.00
Total Awarded Amount to Date: $187,937.00
Funds Obligated to Date: FY 2010 = $187,937.00
History of Investigator:
  • Bruce Selleck (Principal Investigator)
    bselleck@mail.colgate.edu
  • William Peck (Co-Principal Investigator)
  • Martin Wong (Co-Principal Investigator)
Recipient Sponsored Research Office: Colgate University
13 OAK DR
HAMILTON
NY  US  13346-1386
(315)228-7457
Sponsor Congressional District: 22
Primary Place of Performance: Colgate University
13 OAK DR
HAMILTON
NY  US  13346-1386
Primary Place of Performance
Congressional District:
22
Unique Entity Identifier (UEI): D4P7H8NWZER7
Parent UEI:
NSF Program(s): Major Research Instrumentation
Primary Program Source: 01001011DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s):
Program Element Code(s): 118900
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

1039797
Selleck

This Major Research Instrumentation (MRI) Program grant supports acquisition of an integrated energy dispersive X-ray (EDS), electron backscatter diffraction (EBSD) and panchromatic cathodoluminescence (CL) imaging system for the Department of Geology at Colgate University. The integrated package will be mated to an existing JEOL 6360LV scanning electron microscope (SEM) that was acquired by Colgate with previous NSF/MRI support (EAR-0320639). The enhanced capabilities of the SEM will support PI and student research including rock fabric investigations of footwall mylonites from Cordilleran core complexes using EBSD to infer the kinematics and temperature of their formation, CL-SEM analysis of lower Paleozoic quartz sandstones of the Appalachian basin to infer the diagenetic history of micron-scale cement fabrics, and studies of the biomineralization of barnacle exoskeletons. Colgate University is a non-Ph.D. granting institution. The instrumentation will support undergraduate student training in state-of-the-art electron microscopy research methods with applications to structural geology and sedimentary, igneous and metamorphic petrology.

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PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Brown, LL, McEnroe, SA, Peck, WH, Peterson, LP "Anorthosites as Sources of Magnetic Anomalies, in Earthâ��s Magnetic Interio" E. Petrovsk�½, D Ivers, T Harinarayana, and E. Herrero-Bervera, Eds.), Springer-Verlag, p. 321-342 , 2011
J. Levine, M.A. Segreti, and K.D. Heylman "Weathering of H-Chondrite Roosevelt County 037" 42nd Lunar and Planetary Science Conference, abstract 1241 , 2011
McLelland, J. and Selleck, B "Megacrystic Gore Mountain-type garnets in the Adirondack Highlands: Age, origin and tectonic implications" Geosphere , 2011
Peck, W. "Reconnaissance geochronology and geochemistry of the Mont-Tremblant gneiss of the Morin terrane" Geosphere , v.8 , 2012 , p.1356
Wong, M., Peck, W., Selleck, B., Catalano, J., Hochman, S. and Maurer, J. "The Black Lake Shear Zone: a boundary between terranes in the Adirondack Lowlands, Grenville Province;" PreCambrian Research , 2011 10.1016/j.precamres.2011.04.001

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

This report summarizes the outcomes of an National Science Major Research Instrumentation (NSF-MRI) grant.  The grant funding was used to purchase detectors for a Scanning Electron (SEM) system in the Department of Geology at Colgate University.   This facility is used by faculty and students in the departments of Geology, Physics and Astronomy, Biology and Chemistry at Colgate, and faculty and student users from nearby colleges and universities.  SEM is used to examine very small samples of natural and artificial materials, using magnifications up to 50,000X.The new detectors purchased with these funds include (1) an Energy Dispersive X-Ray Analyzer (EDS) system which determines the chemical composition of materials, and supports mapping of the distribution of elements in samples; (2) an Electron Backscatter Diffraction dectector (EBSD), to determine the crystal structure and orientation of mineral and metal grains; and (3) a Polychromatic Cathodoluminescence dectector (PCL), which supports imaging of component grains based on the visible light produced by the electron beam of the SEM. PCL patterns reveal growth patterns and damage to crystal structures in natural and artificial materials.

Examples of research projects making use of this new facility are described below.

Rebecca Metzler, of the Colgate Department of Physics and Astronomy has used the new EBSD system to examine barnacle shell microstructure. Barnacles are arthropods dating back ~400 million years. Her undergraduate research students have begun to explore the micro-structure of both fossilized and modern barnacle exoskeletons, allowing for an exploration into the structure changes that have occurred over time.


“By combining EBSD with synchrotron techniques (XANES and X-PEEM) andmicro-hardness testing, we have been able to explore the structure,
composition, and materials properties of barnacle cement at an unprecedented scale, allowing us to identify two distinct regions within the cement.”

Co-PI Martin Wong has integrated the EBSD into his undergraduate structural geology course through the use of a lab where students analyze shear zone rocks petrographically and then collect EBSD data on those same samples as a way to learn about slip systems and ductile deformation mechanisms. In addition, many undergraduate research projects that Wong has supervised over the past two years have integrated both the CL and EBSD detectors, including EBSD investigations of mylonites in the
Harcuvar, Sierra Mazatan, and Snake Range metamorphic core complexes and CL investigations of zircons dated by LA-ICPMS from the Harcvuar core
complex. 

Co-William Peck notes that the SEM/EDS isthe primary instrument used in Geology 320, taught by William Peck.Students use the system to examine the paragenesis of example ore deposits. and for a final ore deposit project. Senior thesis student Max Ephraim is currently using the SEM-EDS-CL to
characterize newly-discovered zircon veins in the Pikes Peak Batholith (CO),and independent study student Avalon Bunge is working on an SEM-EDS project examining the petrology of Fe-Ti oxides in metamorphosed anorthosites.

PI Bruce Selleck, Department of Geology, and undergraduate
research students have used the SEM system to determine the mineralogy and geochemistry of the Marcellus and Utica gas shales.  Currently, Spencer Staley is using the SEM-EDS to quantify mineralogy using phase-component software on the new Oxford EDS system. Recent students have used the EDS to examine the mineralogy and chemistry of sulfide mineral phases in the organic-rich intervals of the Uticaand Marcellus.  Selleck and co-workersat the University of Massachusetts have used the SEM-CL system to characterize mineral phases used in radiometric dating.

Jonathan Levin...

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