Talk:Vaalbara

Geology Start‑class Mid‑importance

	Geology portal This article is within the scope of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. If you would like to participate, you can choose to edit this article, or visit the project page for more information.GeologyWikipedia:WikiProject GeologyTemplate:WikiProject GeologyGeology
Start	This article has been rated as Start-class on Wikipedia's content assessment scale.
Mid	This article has been rated as Mid-importance on the project's importance scale.

It is requested that a diagram or diagrams be included in this article to improve its quality. Specific illustrations, plots or diagrams can be requested at the Graphic Lab. Please replace this template with a more specific media request template where possible.
For more information, refer to discussion on this page and/or the listing at Wikipedia:Requested images.

Map needed

It is requested that a map or maps be included in this article to improve its quality.

Acasta Gneiss

Is there a connection with the Acasta Gneiss of the Slave craton? Vsmith 22:26, 26 July 2006 (UTC)[reply]

I cannot find any direct connection with the Acasta Gneiss in the Slave other than the corresponding Archaen time periods that do make such a connection highly probable. There might be some overlap with the Superior craton in other areas. It's a very complex tectonic stratigraphy in the Slave (see below):

"The Slave Province was not a simple continental rift as previously suggested, but represented a complex accretionary and collisional orogen with fragments of older ancient crust, juvenile arcs, mature arcs, and intervening accretionary prism material. All of these tectonostratigraphic units are cut by late granites and strike slip faults, and many are affected by late extensional collapse structures....Also of interest is the 3.0 Ga Steep Rock carbonate platform, one of the oldest most complete Archean platforms in the world. The Steep Rock platform preserves spectacular stromatolites and aragonite fans, and may be correlative with similar platforms disbursed across the Superior craton." Source: Kusky, Timothy M., Ph.D. "Homepage Research, Tectonics, Canada." Earth and Atmospheric Sciences Department, Saint Louis University. http://mnw.eas.slu.edu/People/TMKusky/canada.html

Acasta Gneiss Complex contains 4.03 Ga orthogneisses: the oldest rocks in the world. Slave craton has six distinct lithofacies and at least eight tectonothermal events." Source: Dr. Yuichiro Ueno, Assistant Professor, Research Center for the Evolving Earth and Planets, Department of Environmental Science and Technology, Tokyo Institute of Technology. Current Research Activities. Online: http://homepage.mac.com/yuee/H/research3.html

Compositional differences between Slave and other Archaen cratons (Superior, Siberian, Baltic, Kaaval): One study shows an extremely low electrical conductivity level of less than 1 Siemens in the lower crustal layer just beneath the Moho in the Slave craton which is "an order of magnitude smaller than other Archaen cratons....due to the highly anomalous composition....and absence of conducting material....In contrast, other mid- to late Archaen cratons (Superior, Siberian, Baltic, Kaavaal) have conducting material in their lower crust with a minimum conductance (conductivity-thickness product) of 20 Siemens compared to 1 Siemen for the Slave." Source: Jones, Alan J. and Ian J. Ferguson. (2001) "The Electric Moho." Nature, vol. 409, 18 January. Online: http://www.geophysics.dias.ie/~ajones/papers/74.pdf Valich 10:19, 29 July 2006 (UTC)[reply]

Improvement

How about a map John D. Croft 03:26, 14 April 2007 (UTC)[reply]

age

This article is contradicted by Ur (continent) as being the first supercontinent. 76.66.202.139 (talk) 15:14, 5 May 2009 (UTC)[reply]

Ditto. I noticed that, too. TeigeRyan (talk) 20:27, 15 August 2009 (UTC)[reply]

Reversal of SmartBot's efforts. Bettymnz4 (talk) 02:26, 6 March 2010 (UTC)

As I was working on my Saganagan Orogeny article, I wrote quite a bit about Vaalbara. I then decided that Vaalbara really didn't have anything to do with Saganagan (even though I wanted to "flesh" that article out).

I added my hyperlinks to the Saganagan article and was shocked to see that Vaalbara was not a red link. I was planning to copy and paste my information into a new article 'Vaalbara'.

Anyway, I did copy and paste my information into the existing 'Vaalbara' and then printed it out so I could work on combining the two articles.

SmartBot beat me to it!!!

I need to do more work on this.

Based on comments for my article "Rove region", to be moved to "Rove Formation", I need to do more work with citations especially.

I see in the comments for the special page intro, that a diagram of some sort is desired. I haven't found anything. Would a map of current-day South African Kaapvaal craton and/or of Western Australian Pilbara craton work? Bettymnz4 (talk) 18:47, 6 March 2010 (UTC)[reply]

I am finished.

I will apply a for peer review. Bettymnz4 (talk) 20:51, 7 March 2010 (UTC)[reply]