| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4722738 | Precambrian Research | 2015 | 15 Pages |
Abstract
Highlights
- Wilhelm II Land experienced ca 1480Â Ma, 980-920Â Ma (high-grade) and locally 500Â Ma events.
- It was conjugated with neighboring blocks of Antarctica at least in late Mesoproterozoic.
- It bears features in common with the largely Palaeoproterozoic Mawson Palaeo Continent.
- The suspect Cambrian collisional suture likely ran offshore Wilhelm II Land.
- Wilhelm II Land experienced ca 1480Â Ma, 980-920Â Ma (high-grade) and locally 500Â Ma events.
- It was conjugated with neighboring blocks of Antarctica at least in late Mesoproterozoic.
- It bears features in common with the largely Palaeoproterozoic Mawson Palaeo Continent.
- The suspect Cambrian collisional suture likely ran offshore Wilhelm II Land.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
E.V. Mikhalsky, B.V. Belyatsky, S.L. Presnyakov, S.G. Skublov, V.P. Kovach, N.V. Rodionov, A.V. Antonov, A.K. Saltykova, S.A. Sergeev,