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Abstract
A SEEMING paradox has puzzled investigators of the crustal structure of the Gulf of Mexico since Ewing et al.1 calculated that a unit area of the rather thick crust in the gulf contains less mass than does a combination of the crust and enough of the upper mantle to make a comparable thickness in the Atlantic Ocean. They also noted that the free-air gravity of the gulf is essentially normal and fails by a large factor to be low enough to reflect the mass difference that they calculated. We propose a solution to this problem.
Study Area
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Crust and mantle of the Gulf of Mexico |
Series title | Nature |
DOI | 10.1038/238452b0 |
Volume | 238 |
Issue | 5365 |
Year Published | 1972 |
Language | English |
Publisher | Nature |
Description | 2 p. |
First page | 452 |
Last page | 453 |
Country | Mexico, United States |
Other Geospatial | Gulf of Mexico |
Google Analytic Metrics | Metrics page |