Chapter 22 Evidence for Early and Mid-Cryogenian glaciation in the Northern Arabian-Nubian Shield (Egypt, Sudan, and western Arabia) - Photograph supplement
| dc.contributor.author | Mukherjee, Sumit K. | |
| dc.contributor.author | Stern, Robert J. | |
| dc.contributor.author | Ali, Kamal A. | |
| dc.date.accessioned | 2016-01-04T20:21:19Z | |
| dc.date.available | 2016-01-04T20:21:19Z | |
| dc.date.issued | 2011 | |
| dc.degree.department | School of Environmental Sciences | en |
| dc.description.abstract | Companion photographs to the book chapter Stern, Robert J., Johnson, Peter R., Ali, Kamal A., and Mukherjee, Sumit K. 2011. “Evidence for Early and Mid-Cryogenian glaciation in the Northern Arabian-Nubian Shield (Egypt, Sudan, and western Arabia).” In: Arnaud, E., Halverson, G. P. and Shields-Zhou, G. (eds) The Geological Record of Neoproterozoic Glaciations. Geological Society, London, Memoirs, 36, 277-284. | en_US |
| dc.identifier.uri | http://hdl.handle.net/10214/9443 | |
| dc.language.iso | en | en_US |
| dc.rights | Attribution-NonCommercial-NoDerivs 2.5 Canada | * |
| dc.rights.holder | The copyright of the photo rests with the author(s) of the chapter or, where stated, the person who took the photo. | |
| dc.rights.uri | https://creativecommons.org/licenses/by-nc-nd/2.5/ca/ | * |
| dc.subject | Neoproterozoic | en_US |
| dc.subject | Cryogenian glaciation | en_US |
| dc.subject | Northern Arabian-Nubian Shield | en_US |
| dc.subject | Egypt | en_US |
| dc.subject | Sudan | en_US |
| dc.subject | Western Arabia | en_US |
| dc.title | Chapter 22 Evidence for Early and Mid-Cryogenian glaciation in the Northern Arabian-Nubian Shield (Egypt, Sudan, and western Arabia) - Photograph supplement | en_US |
| dc.type | Image | en |
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- A) Neoproterozoic (~740 Ma) Banded Iron Formation from the Arabian-Nubian Shield. Field photograph showing folding of Sawawin (NW Arabia) BIF. Open fold with faulted hinges, suggesting deformation occurred after some consolidation of BIF (Photo credit: Dr. Sumit K. Mukherjee).
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- B) Neoproterozoic (~740 Ma) Banded Iron Formation from the Arabian-Nubian Shield. Field photograph showing folding of Sawawin (NW Arabia) BIF. Tightly folded BIF lacking axial-planar cleavage suggests deformation occurred prior to complete lithification, probably in association with slumping and soft-sediment deformation (Photo credit: Dr. Sumit K. Mukherjee).
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- C) Neoproterozoic (~740 Ma) Banded Iron Formation from the Arabian-Nubian Shield. Photomicrographs showing the typical banding in Sawawin BIF (NW Arabia) observed under the binocular microscope. The silica-rich bands are red (jasper) while the iron-rich bands are light colored (Photo credit: Dr. Sumit K. Mukherjee).
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- D) Neoproterozoic (~740 Ma) Banded Iron Formation from the Arabian-Nubian Shield. Photomicrograph showing a slab of disharmoniously folded BIF, orange jasper layers and dark hematitic layers, Wadi Dabbah, Eastern Desert of Egypt (Photo credit: Dr. Robert J. Stern).
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- Field photograph of Neoproterozoic (~740 Ma) Atud/Nuwaybah diamictite. A) General view of Atud Diamictite, ~740 Ma, outcrop showing strongly foliated diamictite, containing fractured clasts of granite, quartzite, marble, arkose, greywacke and conglomerate in Wadi Mubarak, Eastern Desert of Egypt (Photo credit: Dr. Kamal A. Ali).
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