File:Cratons West Gondwana IT.svg
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Size of this PNG preview of this SVG file: 629 × 599 pixels. Other resolutions: 252 × 240 pixels | 504 × 480 pixels | 806 × 768 pixels | 1,075 × 1,024 pixels | 2,149 × 2,048 pixels | 745 × 710 pixels.
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Italiano: Posizione approssimativa dei cratoni mesoproterozoici (età superiore a 1.3 Ga) in Sud America ed Africa. I continenti sono stati ruotati nella loro posizione durante il Triassico, per mostrare quale fosse la posizione realativa dei cratoni prima dell'apertura dell'Atlantico meridionale. |
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This is a retouched picture, which means that it has been digitally altered from its original version. Modifications: Traslation in italian language. The original can be viewed here: Cratons West Gondwana.svg:  . Modifications made by Ciaurlec.
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License. |
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Original upload log[edit]
This image is a derivative work of the following images:
- File:Cratons_West_Gondwana.svg licensed with Cc-by-sa-3.0,2.5,2.0,1.0, GFDL
- 2010-03-28T16:08:21Z Woudloper 745x710 (173677 Bytes) another try
- 2010-03-28T16:01:06Z Woudloper 745x710 (178529 Bytes) removed imported junk
- 2010-03-28T15:15:14Z Woudloper 744x710 (180374 Bytes) {{Information |Description={{en|1=Approximate location of Mesoproterozoic (older than 1.3 Ga) cratons in South America and Africa. These current two continents have been rotated back to their approximate positions during the
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 20:19, 19 October 2010 | | 745 × 710 (170 KB) | Ciaurlec (talk | contribs) | {{Information |Description={{it|1=Posizione approssimativa dei cratoni mesoproterozoici (età superiore a 1.3 Ga) in Sud America ed Africa. I continenti sono stati ruotati nella loro posizione durante il Triassico, per mostrare quale fosse la posizione re |
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