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Research ArticleARTICLES

The Neoproterozoic Ottfjället dike swarm of the Middle Allochthon, traced geochemically into the Scandian Hinterland, Western Gneiss Region, Norway

Kurt Hollocher, Peter Robinson, Emily Walsh and Michael P. Terry
American Journal of Science June 2007, 307 (6) 901-953; DOI: https://doi.org/10.2475/06.2007.02
Kurt Hollocher
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Peter Robinson
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Emily Walsh
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Michael P. Terry
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Article Information

vol. 307 no. 6 901-953
DOI 
https://doi.org/10.2475/06.2007.02

Published By 
American Journal of Science
Print ISSN 
0002-9599
Online ISSN 
1945-452X
History 
  • Published online October 21, 2007.

Copyright & Usage 
American Journal of Science

Author Information

  1. Kurt Hollocher*,
  2. Peter Robinson**,
  3. Emily Walsh*** and
  4. Michael P. Terry§
  1. **Geological Survey of Norway, N-7491, Trondheim, Norway
  2. ***Geology Department, Cornell College, Mount Vernon, Iowa, 52314, USA
  3. §Department of Geology and Geological Engineering, South Dakota School of Mines and Technology, Rapid City, South Dakota, 57701, USA
  1. ↵*Department of Geology, Union College, Schenectady, New York, 12308, USA; hollochk{at}union.edu
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American Journal of Science
Vol. 307, Issue 6
1 Jun 2007
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The Neoproterozoic Ottfjället dike swarm of the Middle Allochthon, traced geochemically into the Scandian Hinterland, Western Gneiss Region, Norway
Kurt Hollocher, Peter Robinson, Emily Walsh, Michael P. Terry
American Journal of Science Jun 2007, 307 (6) 901-953; DOI: 10.2475/06.2007.02

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The Neoproterozoic Ottfjället dike swarm of the Middle Allochthon, traced geochemically into the Scandian Hinterland, Western Gneiss Region, Norway
Kurt Hollocher, Peter Robinson, Emily Walsh, Michael P. Terry
American Journal of Science Jun 2007, 307 (6) 901-953; DOI: 10.2475/06.2007.02
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  • Recent progress in Scandian ultrahigh-pressure metamorphism in the northernmost domain of the Western Gneiss Complex, SW Norway: continental subduction down to 180-200 km depth
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