The origin of large local uplift in extensional regions
January 1, 1990
Large localized uplift is commonly observed in continental regions undergoing extension. These observations can be modelled by planar, high-angle normal faulting of an elastic upper crust overlying an inviscid lower crust. Isostasy provides the necessary driving force. The model quantifies the role of flexural rigidity, density variations in the crust, and erosion and deposition of sediment.
Citation Information
| Publication Year | 1990 |
|---|---|
| Title | The origin of large local uplift in extensional regions |
| Authors | G. King, M. Ellis |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Nature |
| Index ID | 70015827 |
| Record Source | USGS Publications Warehouse |