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Series: GSA Reviews in Engineering Geology
Published: 01 January 1990
DOI: 10.1130/REG8-p77
EISBN: 9780813758084
... Abstract Neotectonic movement in the United States east of the Rocky Mountains results from various superimposed intraplate adjustments related to movement in the North Atlantic Basin and glacial rebound. Some movements, such as slight southward tilt in the north from waning rebound...
Journal Article
Published: 01 August 1980
Quarterly Journal of Engineering Geology and Hydrogeology (1980) 13 (3): 133–152.
...T. C. Nichols, Jr Summary Rebound of rock masses, defined as the expansive recovery of surficial crustal material, either instantaneously, time-dependently, or both, initiated by the removal or relaxation of superincumbent loads, is found in most geological terrains. The applied loads resulting...
Journal Article
Journal: Geology
Published: 01 December 1976
Geology (1976) 4 (12): 797.
Journal Article
Published: 01 June 1976
Journal of Sedimentary Research (1976) 46 (2): 280–300.
... of laboratory values of density and porosity versus depth in the sea floor. To construct in situ profiles, the results of consolidation tests are used to estimate the amount of elastic rebound (increase in volume) which has occurred after removal of the samples from overburden pressure in the boreholes. In situ...
Journal Article
Journal: Geology
Published: 01 February 1976
Geology (1976) 4 (2): 73–75.
...J. T. Andrews; W. R. Peltier Abstract An ice-unloading model for Hudson Bay consistent with the rebound history of the Ottawa Islands requires collapse of the central dome of the Laurentide Ice Sheet between 12,000 and 10,000 B.P. Hudson Bay was then filled by a shallow ice shelf with ice streaming...
Journal Article
Journal: Geology
Published: 01 November 1975
Geology (1975) 3 (11): 617–620.
Journal Article
Journal: Geology
Published: 01 April 1975
Geology (1975) 3 (4): 169–171.
... channel coincide with the axis of the anticline. A model study based on the concept of finite elements shows that a possible mechanism for the folding of the Muav Limestone is elastic rebound caused by relief from overburden pressure as material was eroded to form the canyon. Geological Society...
Journal Article
Published: 01 June 1973
Canadian Journal of Earth Sciences (1973) 10 (6): 961–978.
... studies lead to the conclusion that, in large part, these features are due to elastic rebound of the rock into which the valley has been eroded. Rebound of the valley floor occurs due to vertical stress relief and gives rise to a gentle anticlinal structure. This structure and the upwarping of the beds...