Other10.3133/OFR81846
Colored gravity anomaly and terrain maps of the east-central United States
Robert W. Simpson,Richard H. Godson +1 more
- 01 Jan 1981
About: The article was published on 01 Jan 1981. The article focuses on the topics: Gravity anomaly & Terrain.
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Citations
Interpretation Theory in Applied Geophysics Grant (McGraw-Hill, 140s.)
TL;DR: Interpretation theory in applied geophysics: Grant, F S as mentioned in this paper, Unknown Binding, January 1, 1965 5.0 out of 5 stars 1 rating. Read it now.
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Identification of a Precambrian Rift through Missouri by digital image processing of geophysical and geological data
Edward A. Guinness,Raymond E. Arvidson,J. W. Strebeck,K. J. Schulz,Geoffrey F. Davies,C. Leff +5 more
TL;DR: In this paper, a newly discovered feature in the mid-continent -a gravity low that begins at a break in a midcontinent gravity high in SE Nebraska, extends across Missouri in a NW-SE direction, and intersects the Mississippi Valley graben to form the Pascola arch -is discussed.
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References
Machine contouring using minimum curvature
TL;DR: In this article, Finite difference equations are deduced from a principle of minimum total curvature, and an iterative method of solution is outlined, based on which the spline fit has well defined smoothness properties.
1.1K
Interpretation Theory in Applied Geophysics Grant (McGraw-Hill, 140s.)
TL;DR: Interpretation theory in applied geophysics: Grant, F S as mentioned in this paper, Unknown Binding, January 1, 1965 5.0 out of 5 stars 1 rating. Read it now.
1.1K
State of stress in the conterminous United States
Mary Lou Zoback,Mark D. Zoback +1 more
TL;DR: In this article, a major variation in principal stress orientation is observed between the Atlantic Coast and mid-continent areas, and the authors suggest that these transitions can be abrupt, occurring over <75 km in places.
Implications of regional gravity for state of stress in the Earth's crust and upper mantle
TL;DR: In this paper, the authors used gravity anomalies and surface deformation produced by these features to demonstrate that the upper 30-40 km of the oceanic lithosphere is capable of regionally supporting stress differences in the 100-MPa range.
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Gravitationally induced stresses at structural boundaries
A. K. Goodacre,H. S. Hasegawa +1 more
TL;DR: In this article, the authors describe a set of gravity anomalies, consisting of paired positive-negative belts, which occur in Canada at structural boundaries between geological provinces and produce what are referred to as anomalous masses.
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