Mass Spectrometry Laboratory
The Laboratory
The Mass Spectrometry laboratory is equipped with three mass spectrometers: a Thermo Scientific XSERIES 2 Quad, a Finnigan™ ELEMENT 2, and a Nu Plasma Multicollector with capacity for analysis of liquid samples and in-situ analysis of solid materials by coupling to an ESL NWRFemto Laser Ablation System).
How it works?
For solution analysis, the sample must be in liquid form. This is archived by dissolving the sample in ultra-pure acids. The sample material is then injected into the inductively coupled plasma (ICP) as an aerosol and transported by argon (carrier gas). Aerosol particles are generated by nebulizing the solution into the hot plasma, the sample is ionized, and the ions are transported to the mass spectrometer, where they are separated according to their mass and energy. This allows the determination of the intensity of individual masses (isotopes).
For solid materials, we use laser ablation-inductively coupled plasma mass spectrometry (LA-ICP-MS). LA-ICP-MS is a method for in-situ analyses of major, trace element concentrations and isotope ratios in solid materials. A pulsed-focused, high-energy laser beam removes (ablates) material from the sample, and the resulting aerosol is transported into the Inductively Coupled Mass Spectrometer (ICP-MS) for ionization and detection.
Instrumentation and applications:
The Thermo Scientific XSERIES 2 Quad mass spectrometer (MS) has dual collectors, allowing for a high-resolution analysis of a broad range of trace elements. At MCL we use the XSERIES 2 for rapid analysis of trace elements with masses from Li to U. The Finnigan Element 2 is a single collector mass spectrometer (MS) and allows for fairly precise analysis of both isotopes and trace elements. We typically use the Element 2 for U-Pb dating of minerals such as calcite, garnet, hematite, and fluorite. The Nu Plasma Multicollector mass spectrometer (MS) allows for high-resolution analysis of isotopes at a smaller mass range but with much more precision. The Nu Plasma is used for the isotopic characterization of material with elements such as Sr, Fe, and Pb.
Sample types and Preparation:
LA-ICP-MS can analyze almost any type of solid material. In contrast with other techniques, samples do not need to be coated or vacuum-resistant for LA-ICP-MS analysis. However, polishing samples is recommended for more precise results. We typically analyze thin and thick sections as well as epoxy/grain mounts.
For liquid samples, solutions must be dissolved with acid, then introduced via a 0.2 mL/m nebulizer in 2% HNO3.
Calibration and data reduction:
To determine elemental concentration (or isotopic ratios), unknown samples (samples of interest) are bracketed by standards with known elemental and/or isotopic ratios (external standards) and internal standards to account for instrumental drift where applicable. Standards are typically synthetic glasses containing trace elements (e.g., NIST 610, 612, and 614), synthetic glasses from natural rocks (USGS standards), in-house standards (e.g., U-Pb dated specular hematite from Chile), and certified mult-element solution standards.
Data quantification (reduction) is performed using iolite 4.
Contact Jason Kirk (lab manager) at jdkirk@arizona.edu.
Chernoff, C. B. (2002). Origin and redistribution of metals in sedimentary rocks. The University of Arizona. http://hdl.handle.net/10150/289837
Del Huggler, S. M. (2023). Metamorphism in IOCG Systems: Contact Metamorphism in the Candelaria-Punta Del Cobre District, Chile (Master's thesis, The University of Arizona). http://hdl.handle.net/10150/669840
Favorito, D. A. (2020). Laramide Crustal Shortening and Cenozoic Extensional Overprint in Southeastern Arizona: Insights from Structural Reconstructions and Relation to Porphyry Copper Systems (Doctoral dissertation, The University of Arizona). http://hdl.handle.net/10150/641361
Fitzpatrick, W. A. (2021). Development of the Texas Canyon Granite Magmatic-Hydrothermal System, Little Dragoon Mountains, Arizona (Master's thesis, The University of Arizona). http://hdl.handle.net/10150/660211
Girardi, J. D. (2014). Comparison of Mesozoic magmatic evolution and iron oxide (-copper-gold)('IOCG') mineralization, Central Andes and western North America. The University of Arizona. http://hdl.handle.net/10150/319881
Jensen, E. P. (2003). Magmatic and hydrothermal evolution of the Cripple Creek gold deposit, Colorado, and comparisons with regional and global magmatic-hydrothermal systems associated with alkaline magmatism. The University of Arizona. http://hdl.handle.net/10150/280422
King, C. A. (2017). Igneous petrology, geochronology, alteration, and mineralization associated with hydrothermal systems in the Battle Mountain district, Nevada (Doctoral dissertation, The University of Arizona). http://hdl.handle.net/10150/625475
Kreiner, D. C. (2011). Epithermal style iron oxide (-Cu-Au)(= IOCG) vein systems and related alteration. http://hdl.handle.net/10150/203504
Mizer, J. D. (2018). Early Laramide magmatism in southern Arizona; U-Pb geochronology of key igneous units and implications for the timing of regional porphyry copper mineralization (Doctoral dissertation, The University of Arizona). http://hdl.handle.net/10150/630212
Nickerson, P. A. (2012). Post-mineral normal faulting in Arizona porphyry systems (Doctoral dissertation, The University of Arizona). http://hdl.handle.net/10150/242354
Rader, S. (2018). The Natural Distribution and Geochemistry of Thallium. http://hdl.handle.net/10150/630192
Richardson, C. A. (2019). Extensional Deformation and Ore Deposits along a Transect Through Northern Nevada (Doctoral dissertation, The University of Arizona). http://hdl.handle.net/10150/634247
Runyon, S. E. (2017). Deep hydrothermal alteration in porphyry copper systems: Insights from the Laramide arc (Doctoral dissertation, The University of Arizona). http://hdl.handle.net/10150/625856
Runyon, S. E., Seedorff, E., Barton, M. D., Steele-MacInnis, M., Lecumberri-Sanchez, P., & Mazdab, F. K. (2019). Coarse muscovite veins and alteration in porphyry systems. Ore Geology Reviews, 113, 103045. https://doi.org/10.1016/j.oregeorev.2019.103045
Wodzicki, W. A. (1995). The evolution of Laramide igneous rocks and porphyry copper mineralization in the Cananea district, Sonora, Mexico. The University of Arizona. http://hdl.handle.net/10150/187049