January 17, 2012,
1:00pm - 2:00pm
Location:
1-390
The origin of shale formations will be described. Source rock organic matter is clearly differentiated based on sedimentary origin. Following deposition, the organic matter matures in accord with its burial history, and this determines the nature of the resource. It will be seen that the distribution of shale resources on a continental scale can be explained by a few simple principles.