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Laboratory for Crustal Petrology |
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Michael Brown, Director Sarah Penniston-Dorland Co-Director ![]() View of 1493 m peak from Umanap Suvdlua
to show upper zone in the mountain peak and the intermediate zone in the
fjord wall; Qorqut Granite Complex, Greenland.
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RESEARCH GOALS OF THE LABORATORY FOR CRUSTAL PETROLOGYResearch in the Laboratory for Crustal Petrology is concerned with the origin and evolution of the earth’s crust, including crust-mantle interactions, processes of mass transfer within the crust and intracrustal differentiation during orogenesis. To understand crustal evolution, faculty and students investigate the pressure-temperature-time-deformation (P-T-t-d) history of metamorphic belts through detailed study of metamorphic rocks and interpretation of microstructures, phase petrology and geochemistry; we investigate the role of fluids and the generation, segregation, transfer and emplacement of granite within orogens. Currently, we have a particular interest in granulite facies metamorphism, particularly high-pressure granulite and ultrahigh-temperature metamorphism, and the relationship between metamorphism, mass transfer and mineralization in the Platreef of the Bushveld Complex, South Africa. In the Laboratory for Crustal Petrology, our interests span the fields of mineralogy and petrology, structural geology and tectonics, and geochemistry. Our work involves integration between field studies and laboratory studies [CSS 2259, CHEM 1211A, the Geochemistry Laboratories and the Electron Probe Microanalyzer Facility within the Nanoscale Imaging, Spectroscopy, and Properties Lab (http://www.nanocenter.umd.edu/labs/nisplab.php)], and theoretical analysis and modeling (e.g. phase petrology using THERMOCALC and the Holland & Powell internally consistent thermodynamic dataset). Areas of active work include: the northern Appalachians of New England, particularly Vermont, New Hampshire and western Maine; Southern Brittany in the Variscides of France; the Neoproterozoic Brasília fold belt in Brazil; the contact aureole of the Bushveld Complex in South Africa; and, the Fosdick Migmatitic Gneiss Dome, Fosdick Mountains, Antarctica. |
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EXAMPLES OF RESEARCH SUPPORTED BY THE LABAnimated
CT Images of Migmate Samples
Click on the image to view an animated gif of gray scale inverted images of 112 HR X-ray CT scans of the migmatitic garnet amphibolite. First and last slices are outlined in white. Animation cycles from first to last slice (Movie 10 Mb; GIF). |
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Animation of projection of false-color three-dimensional image of stromatic migmatite, derived from the stack of two-dimensional representations of the HR X-ray CT scans, created using VoxBlast® . A scale bar is not presented because these are projections of a three-dimensional image (Fig. 4(b) contains the scale for the first image in the stack). The leucosome is rendered transparent in this image. The color of the solid part of the image is brighter for material with higher mineral density, with garnet appearing yellow (Movie: 115 Mb, AVI).
More information on these migmate images is available in the article:
Representative Poster Presentations
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MARYLAND RESEARCHERS AFFILIATED WITH THE LABORATORY FOR CRUSTAL PETROLOGYHier-Majumder, Saswata ( |
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RESEARCH ASSOCIATEKorhonen, Fawna J. ( |
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GRADUATE STUDENTS (current)Advisor: Brown, Michael Reno, Barry ( Chen, Yan ( Advisor: Penniston-Dorland, Sarah Potter, Rachel (
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Undergraduate Interns (current)
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OPPORTUNITIES FOR UNDERGRADUATESThere is a variety of opportunities for undergraduate geology students
to participate in research with members of the LCP. These include the
possibility of fieldwork and potential GEOL 393/394 projects. Interested
students are encouraged to contact Michael Brown ( |
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VISITING RESEARCHERSBaldwin, Julia A. (University of Montana) Johnson, Timothy (Graz, Austria) Moraes, Renato (University of Sao Palo, Brazil) |
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COMPLETED THESES (1994-present)Advisor: Brown, Michael Burgess, J.L., Metamorphic studies in the Port aux Basques Area, SW Newfoundland,
Canada. Pressley, R.A., Petrogenesis of the Phillips pluton, west-central Maine. Solar, G.S., Structural and petrologic investigations in the Central
Maine Belt, west-central Maine, with special reference to the migmatites. Tian, J., A geological and geochemical study of the Mooselookmeguntic
composite pluton, west-central Maine and east-central New Hampshire. Advisor: Penniston-Dorland, Sarah
RECENT PUBLICATIONS (2003-present)Johnson, T.E., Brown, M. and Solar, G.S., 2003. Low-pressure subsolidus and suprasolidus phase equilibria in the MnNCKFMASH system: Constraints on conditions of regional metamorphism in western Maine, northern Appalachians. American Mineralogist, 88, 624-638. Johnson, T.E., Gibson, R.L., Brown, M., Buick, I.S. and Cartwright, I., 2003. Partial melting of metapelitic rocks beneath the Bushveld Complex, South Africa. Journal of Petrology, 44, 789-813. Marchildon, N. and Brown, M., 2003. Spatial distribution of melt-bearing structures in anatectic rocks from Southern Brittany: implications for melt-transfer at grain- to orogen-scale. Tectonophysics, 364, 215-235. Brown, M., 2003. Hot orogens, tectonic switching, and creation of continental crust: Comment and Reply. Geology: On-Line Forum. June 2003, doi:10.1130/0091-7613(2003)31<e9:HOTSAC>2.0.CO;2. Johnson, T. and Brown, M., 2004. Quantitative Constraints on Metamorphism in the Variscides of Southern Brittany - a Complementary Pseudosection Approach. Journal of Petrology, 45, 1237-1259; doi:10.1093/petrology/ehg012. Johnson, T., Brown, M., Gibson, R. and Wing, B., 2004. Spinel-cordierite symplectites replacing andalusite: Evidence for melt-assisted diapirism in the Bushveld Complex, South Africa. Journal of Metamorphic Geology, 22, 529-545; doi:10.1111/j.1525-1314.2004.00531.x. Brown, M., 2004. The mechanism of melt extraction from lower continental crust of orogens. Transactions of the Royal Society of Edinburgh: Earth Sciences, 95, 35-48. Invited Contribution Invited Contribution Baldwin, J.A., Powell, R., Brown, M., Moraes, R. and Fuck, R.A., 2005. Mineral equilibria modeling of ultrahigh-temperature metamorphism: an example from the Anápolis-Itauçu Complex, central Brazil. Journal of Metamorphic Geology, 23, 511-531. Penniston-Dorland, S.C. and Ferry, J.M., 2005. Coupled dichotomies of apatite and fluid composition during contact metamorphism of siliceous carbonate rocks. American Mineralogist, 90, 1606-1618. Ferry, J.M., Rumble, D. III, Wing, B.A. and Penniston-Dorland, S.C., 2005. A new interpretation of centimeter-scale variations in the progress of infiltration-driven metamorphic reactions: Case study of carbonated metaperidotite, Val d'Efra, Central Alps, Switzerland. Journal of Petrology, 46, 1725-1746. Brown, M., 2006. Duality of thermal regimes is the distinctive characteristic of plate tectonics since the Neoarchean. Geology, 34, 000-000. Baldwin, J.A., Brown, M. and Schmitz, M.D., 2007. First application of titanium-in-zircon thermometry to ultrahigh-temperature metamorphism. Geology, 35, 000-000. Brown, M., 2007a. Metamorphic conditions in orogenic belts: A record of secular change. International Geology Review, 00, 000-000. Brown 2007b. Metamorphism, plate tectonics and the supercontinent cycle. Earth Science Frontiers, 00, 000-000. Moraes, R., Fuck, R.A., Brown, M., Piccoli, P., Baldwin, J., Dantas, E.L., Laux, J.H. and Junges, S.L., 2007. Wollastonite-scapolite-clinopyroxene marble of the Anápolis-Itauçu Complex, Goiás: More evidence of ultrahigh-temperature metamorphism. Revista Brasileira de Geociências, 37, 000-000.
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