Paleomagnetic evidence for a large rotation of the Yukon block relative to Laurentia: Implications for a low-latitude Sturtian glaciation and the breakup of Rodinia

Author:

Eyster Athena E.,Fu Roger R.,Strauss Justin V.,Weiss Benjamin P.,Roots Charlie F.,Halverson Galen P.,Evans David A.D.,Macdonald Francis A.

Publisher

Geological Society of America

Subject

Geology

Reference186 articles.

1. Abbott, J.G. , 1996, Implications of probable late Proterozoic dextral strike-slip movement on the Snake River fault, in Cook, F.A. , and Erdmer, P. , eds., Slave–Northern Cordillera Lithospheric Evolution (SNORCLE) Transect: Lithoprobe Report 50, p. 138–140.

2. Abbott, G. , 1997, Geology of the Upper Hart River Area, Eastern Ogilvie Mountains, Yukon Territory (116A/10, 116A/11): Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada Bulletin 9, 92 p.

3. Aitken, J.D. , 1981, Stratigraphy and sedimentology of the Upper Proterozoic Little Dal Group, Mackenzie Mountains, Northwest Territories, in Campbell, F.H.A. , ed., Proterozoic Basins of Canada: Geological Survey of Canada Paper 81-10, p. 47–71.

4. Uppermost Proterozoic Formations in Central Mackenzie Mountains, Northwest Territories;Aitken;Geological Survey of Canada Bulletin,1989

5. Aitken, J.D. , 1991a, The Ice Brook Formation and Post-Rapitan, Late Proterozoic Glaciation, Mackenzie Mountains, Northwest Territories: Geological Survey of Canada Bulletin 404, p. 1–43, doi:10.4095/132664.

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