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...
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| Tipo de documento: | artigo |
| Estado: | Versão publicada |
| Data de publicação: | 1996 |
| País: | México |
| Recursos: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repositório: | Geofísica Internacional |
| Idioma: | espanhol |
| OAI Identifier: | oai:revistagi.geofisica.unam.mx:article/549 |
| Acesso em linha: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/549 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Gravedad campo meridional Colima México Gravity field southern graben |
| Resumo: | 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. |
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