Heat flow from eastern Panama and northwestern Colombia
Earth and Planetary Science Letters
By: J. H. Sass, R. J. Munroe, and T. H. Moses Jr.
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Abstract
Heat flows were determined at 12 sites in four distinct areas between longitude 77° and 80°W in eastern Panama and northwestern Colombia. Evidently, most of the region is underlain by mafic oceanic crust so that the crustal radiogenic component of heat flow is very small (∼ 0.1 μcal cm−2 sec−1). Low heat-flow values (∼ 0.7 μcal cm−2 sec−1) in northwestern Colombia may reflect thermal transients associated with shallow subduction. The normal values (∼ 1) at about 78°W are consistent with the mean heat flow from the western Caribbean and the Gulf of Mexico. At 80°W, a fairly high value of 1.8 may define the easterly limit of thermal transients due to Cenozoic volcanic activity in Central America.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Heat flow from eastern Panama and northwestern Colombia |
| Series title | Earth and Planetary Science Letters |
| DOI | 10.1016/0012-821X(74)90046-6 |
| Volume | 21 |
| Issue | 2 |
| Year Published | 1974 |
| Language | English |
| Publisher | Elsevier |
| Description | 9 p. |
| First page | 134 |
| Last page | 142 |
| Country | Columbia, Panama |
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