Gravity anomalies and crustal thickness variations along the Mid-Atlantic Ridge between 33°N and 40°N

1995 ◽  
Vol 100 (B3) ◽  
pp. 3767-3787 ◽  
Author(s):  
Robert S. Detrick ◽  
H. D. Needham ◽  
V. Renard
Keyword(s):  
Gravity Anomalies ◽  
Crustal Thickness ◽  
Mid Atlantic Ridge ◽  
Thickness Variations

Crustal Thickness on the Mid-Atlantic Ridge: Bull's-Eye Gravity Anomalies and Focused Accretion

Science ◽  
1993 ◽  
Vol 262 (5134) ◽  
pp. 726-729 ◽  
Author(s):  
M. Tolstoy ◽  
A. J. Harding ◽  
J. A. Orcutt
Keyword(s):  
Gravity Anomalies ◽  
Crustal Thickness ◽  
Mid Atlantic Ridge ◽  
Bull's Eye

Crustal modeling from spectrally correlated free‐air and terrain gravity data—A case study of Ohio

Geophysics ◽  
2000 ◽  
Vol 65 (4) ◽  
pp. 1057-1069 ◽  
Author(s):  
Jeong Woo Kim ◽  
Ralph R. B. von Frese ◽  
Hyung Rae Kim
Keyword(s):  
Gravity Data ◽  
Gravity Anomalies ◽  
Crustal Thickness ◽  
Earthquake Hazards ◽  
Spectral Correlation ◽  
Free Air ◽  
Correlation Spectrum ◽  
Gravity Effects ◽  
Thickness Variations ◽  
Free Air Gravity

We investigate the use of spectral correlation theory to analyze terrain gravity effects and free‐air gravity anomalies of Ohio for possible constraints on the thickness variations and neotectonics of the crust. Terrain gravity effects are computed from the topography by Gauss‐Legendre quadrature integration and are compared against independent free‐air gravity anomaly observations for their wavenumber correlation spectrum. Spectral correlation filters are designed accordingly to extract terrain‐correlated free‐air gravity anomalies that are subtracted from the terrain gravity effects for estimates of the compensated terrain gravity effects. These effects are used to model the Moho by inversion, assuming they predominantly reflect crustal thickness variations. Our results characterize the middle third of Ohio as a broad zone of thickened Precambrian crust, which also may include rifted regions where the thickness of the prerift crust has been reduced greatly. Furthermore, we find that about 83% of the instrumentally determined earthquake epicenters are located within the inferred thinner regions of Ohio’s crust or at their margins where compressional stresses may dominate. In general, these crustal thickness variations provide new constraints on modeling the tectonic evolution and geotechnical parameters of the crust—constraints that are important for evaluating earthquake hazards, the distribution and extraction of crustal resources, and the storage of hazardous waste and other crustal engineering applications.

Regional crustal thickness variations of the Peninsular Ranges, southern California

Geology ◽  
2000 ◽  
Vol 28 (4) ◽  
pp. 303-306
Author(s):  
Jennifer L. Lewis ◽  
Steven M. Day ◽  
Harold Magistrale ◽  
Jennifer Eakins ◽  
Frank Vernon
Keyword(s):  
Southern California ◽  
Crustal Thickness ◽  
Peninsular Ranges ◽  
Thickness Variations

scholarly journals Causes of Oceanic Crustal Thickness Oscillations Along a 74‐M Mid‐Atlantic Ridge Flow Line

2019 ◽  
Vol 20 (12) ◽  
pp. 6123-6139 ◽  
Author(s):  
William J. Shinevar ◽  
Hannah F. Mark ◽  
Fiona Clerc ◽  
Emmanuel A. Codillo ◽  
Jianhua Gong ◽  
...  
Keyword(s):  
Flow Line ◽  
Crustal Thickness ◽  
Mid Atlantic Ridge
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