File:BlessingAd3.jpg
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| Description |
English: Development of an orogenic wedge showing the exhumation of an extruding channel (Blue colured). At greater depth the temperature is higher but as the rock becomes cooler as it approaches the surface. OSL cooling ages ages of the bedrock mineral (e.g. Quartz) aids in the determination the exhumation age and rate of the rock in a convergent tectonic system. |
| Date | |
| Source | Own work |
| Author | BlessingAdeoti |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 12:40, 9 October 2018 | | 3,377 × 2,584 (460 KB) | BlessingAdeoti (talk | contribs) | Cross-wiki upload from en.wikipedia.org |
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