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back to Faculty Glen R. Himmelberg email: HimmelbergG@missouri.edu |
![]() Heintzleman Ridge, Juneau Ice Field, southeastern Alaska |
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Glen Himmelberg's research is currently focused on understanding the thermal and structural evolution of the earth's crust through studies of the metamorphism of orogenic belts. This is accomplished through integrated field, laboratory and theoretical studies. Studies include
Current studies are concentrated in the Cordilleran orogen in southeastern Alaska, which includes 14 distinct metamorphic belts that make up three major metamorphic complexes (Brew and others, 1992). Each of these complexes is related to a major subduction event. Detailed investigations are underway in the Western and Central metamorphic belts of the Coast Mountains Complex, the Admiralty Island metamorphic belt and the Baranof Island metamorphic belt. The Western and Central metamorphic belts exhibit multiple deformational, metamorphic, and plutonic events that span the interval of about 120 to 50 Ma. Detailed studies of the Western metamorphic belt near Juneau have been published (Himmelberg and others, 1991; 1995) and investigations of the belt to the south are underway. Little detailed petrology has been published on the Central metamorphic belt which consists of amphibolite facies pelitic schists, gneiss, migmatite, marble and metaperidotite. The Admiralty Island metamorphic
belt consists of sub-belts of subgreenschist to amphibolite facies rocks
that were produced during Triassic and post-Late Triassic regional metamorphism
and deformation. The Baranof Island metamorphic belt consists of regionally
thermally metamorphosed rocks exposed over at least 1200 km2, making it
one of the largest such regions reported to date. These rocks were metamorphosed
to albite-epidote hornfels, hornblende hornfels, and amphibolite facies
assemblages by granitic plutons 47 to 42 Ma. Emplacement of the plutons
and the associated thermal metamorphism were superposed on regional subgreenschist
to country rocks of the greenschist facies. |
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Himmelberg, G. R., Haeussler, P. J., and Brew, D. A., 2004, Emplacement, rapid burial, and exhumation of 90-Ma plutons in southeastern Alaska. Canadian Journal of Earth Sciences, 41, p. 87-102. Zumsteg, C. L., Himmelberg, G. R., Karl,
S. M., and Haeussler, P. J., 2003, Metamorphism within the Chugach accretionary
complex on southern Baranof Island, southeastern Alaska,
in Sisson, V.B., Roeske, S.M., and Pavlis, T.L., eds., Geology
of a transpressional orogen developed during ridge-trench interaction
along the North Pacific margin. Geological Society
of America Special Paper 371, p. 253-267. Himmelberg, G.R., Brew, D.A., and Ford, A.B., 1995, Low-grade, M1 metamorphism of the Douglas Island Volcanics, western metamorphic belt near Juneau, Alaska, in Schiffman, Peter and Day, Howard W. (eds.), Low-grade metamorphism of mafic rocks: GSA Sp. Paper 296. Brew, D.A., Himmelberg, G.R., Loney, R.A., and Ford, A.B., 1992, Distribution and characteristics of metamorphic belts in the south-eastern Alaskan part of the North American Cordillera: J. Met. Geol. v. 10, p. 465-482. Himmelberg, G.R., Brew, D.A., and Ford, A.B., 1991, Development of inverted metamorphic isograds in the western metamorphic belt, Juneau, Alaska: J. of Met. Geol., v. 9, p. 165-180. Brew, D.A., Ford, A.B., and Himmelberg, G.R., 1989, Evloution of the western part of the coast plutonic-metamorphic complex, south-eastern Alaskan, USA: a summary in Daly, J.S., Cliff, R.A., and Yardley, B.W.D. (eds.), Evolution of metamorphic belts: Geol. Soc. Sp. Publ. , v. 43, p. 447-452.
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