Comments on "Gravity field of the southern Colima graben" by W. L. Bandy, C. A. Mortera-Gutierrez and J. Urrutia
In a recent paper, Bandy et al. (1993) report the results of modeling marine gravity data for the continental margin of the Jalisco Block. In Figure 5 of its paper, one would expect line A-A' to be normal to the longest dimension of the anomaly, as they use a two-dimensional model, where densit...
| Author: | |
|---|---|
| Format: | article |
| Status: | Published version |
| Publication Date: | 1996 |
| Country: | México |
| Institution: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repository: | Geofísica Internacional |
| Language: | Spanish |
| OAI Identifier: | oai:revistagi.geofisica.unam.mx:article/549 |
| Online Access: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/549 |
| Access Level: | Open access |
| Keyword: | Gravedad campo meridional Colima México Gravity field southern graben |
| Summary: | In a recent paper, Bandy et al. (1993) report the results of modeling marine gravity data for the continental margin of the Jalisco Block. In Figure 5 of its paper, one would expect line A-A' to be normal to the longest dimension of the anomaly, as they use a two-dimensional model, where density does not change along strike. However, line A-A' actually runs parallel to strike, against the common usage in two-dimensional models. Gravity; field; southern; Colima; graben, México. |
|---|