The origin of large local uplift in extensional regions
Nature
By: G. King and M. Ellis
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Abstract
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.
Suggested Citation
King, G., Ellis, M., 1990, The origin of large local uplift in extensional regions: Nature, v. 348, no. 6303, p. 689-693, https://doi.org/10.1038/348689a0.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | The origin of large local uplift in extensional regions |
| Series title | Nature |
| DOI | 10.1038/348689a0 |
| Volume | 348 |
| Issue | 6303 |
| Year Published | 1990 |
| Language | English |
| Publisher | Springer Nature |
| Description | 5 p. |
| First page | 689 |
| Last page | 693 |