Age and deformation of early Proterozoic quartzites in the southern Lake Superior region: Implications for extent of foreland deformation during final assembly of Laurentia

Geology

Volumn 26, Issue 10, 1998, Pages 907-910

  Holm, Daniel ^a  

^a KENT STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BUILDINGS; DEFORMATION; METAMORPHIC ROCKS; SILICATE MINERALS; STRUCTURAL GEOLOGY; ZIRCON;

COMPRESSIONAL DEFORMATION; DETRITAL ZIRCON; FORELAND DEFORMATION; GEOLOGIC INFORMATION; METAMORPHIC EVENTS; MINERAL COOLING; STRUCTURAL EVIDENCE; THERMAL FRONTS;

LAKES;

DEFORMATION; GEOCHRONOLOGY; LAURENTIA; OROGENY; QUARTZITE;

NORTH AMERICA;

EID: 84879885878     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(1998)026<0907:AADOEP>2.3.CO;2     Document Type: Article

References (3)

1. Bowring, S. A., and Karlstrom, K. E., 1990, Growth, stabilization, and reactivation of Proterozoic lithosphere in the southwestern United States: Geology, v. 18, p. 1203-1206.
2. Dott, R. H., Jr., 1983, The Proterozoic red quartzite enigma in the north-central U.S. - Resolved by plate collision?, in Medaris, L. G., Jr., ed., Early Proterozoic geology of the Great Lakes region: Geological Society of America Memoir 160, p. 129-141.
3. Dott, R. H., Jr., Medaris, L. G., Jr., and Schott, R. C., 1997, Post-1760 Ma deposition of the Baraboo quartzite: Confirmation from detrital zircon ages and new field evidence: Geological Society of America Abstracts with Programs, v. 29, no. 4, p. 13.