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| Creator | Title | Description | Subject | Date | ||
|---|---|---|---|---|---|---|
| 1 |
 | Chapman, David S. | Exhumation of the central Wasatch Mountains, Utah: 1, Patterns and timing of exhumation deduced from low-temperature thermochronology data | The Wasatch Mountains are often cited as an example of normal fault growth and footwall flexure. They represent a tilted footwall at the edge of the Basin and Range extensional province, a major rift basin. Thus understanding the detailed spatial and elevation changes in coupled thermochronometer da... | Uplift; exhumation; Wasatch fault; Wasatch Mountains; Utah; helium dating; fission track; tectonophysics; Extensional tectonics; geothermal observations | 2002 |
| 2 |
 | Chapman, David S. | Exhumation of the central Wasatch Mountains, Utah: 2, thermokinematic model of exhumation, erosion, and thermochronometer interpretation | The Wasatch fault is a ~370 km long normal fault in Utah that marks the boundary between the stable Colorado Plateau to the east and the extending Basin and Range to the west. Understanding the thermokinematic evolution of this fault can provide insights into intracontinental extensional tectonics a... | Uplift; exhumation; Wasatch Fault; Wasatch Mountains; Utah; helium dating; fission track; tectonophysics; extensional tectonics; geothermal observations | 2002 |
| 3 |
 | Chapman, David S.; Allis, Richard George | Late Neogene exhumation patterns in Taranaki Basin (New Zealand): evidence from offset porosity-depth trends | Taranaki Basin, New Zealand, is located adjacent to the Australian-Pacific Plate boundary where the tectonic regime changes from dominantly subduction-related to the north to transpression-related along the Alpine Fault to the south. During the Neogene, burial and exhumation varied extensively, in ... | Neogene; uplift; exhumation; Taranaki Basin; New Zealand | 1998 |
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