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Geology; May 1998; v. 26; no. 5; p. 475-477; DOI: 10.1130/0091-7613(1998)026<0475:DAKPFD>2.3.CO;2
© 1998 Geological Society of America
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Dome-and-keel provinces formed during Paleoproterozoic orogenic collapse—Core complexes, diapirs, or neither?: Examples from the Quadrilátero Ferrífero and the Penokean orogen: Comment and Reply

Daniel Holm1, David Schneider2, Daniel Lux3, Stephen Marshak4, Douglas Tinkham4, Fernando F. Alkmim5, Hannes Brueckner6 and Theodore Bornhorst7

1 Department of Geology, Kent State University, Kent, Ohio 44242
2 Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania 18015
3 Department of Geological Sciences, University of Maine, Orono, Maine 04469
4 Department of Geology, University of Illinois, 1301 W. Green, Urbana, Illinois 61801
5 Departamento de Geologia, Universidade Federal de Ouro Preto, Ouro Preto, M.G., 35.400, Brazil
6 Department of Geology, Queens College, Flushing, New York 11367, and Lamont-Doherty Earth Observatory, Palisades, New York 10964
7 Department of Geological Engineering, Geology, and Geophysics, Michigan Technological University, Houghton, Michigan 49931

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