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Paleomagnetism of Plio-Quaternary basalts in the Jalisco block, western Mexico
The interior of the Jalisco block, western Mexico, is disrupted by several NW-SE to NESWoriented grabens and associated recent alkaline volcanics which are bounded byWNW oriented regional lineaments. The geometry of these features suggests deformationfrom a right-lateral shear couple, consistent wit...
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| Vydáno v: | Geofísica Internacional |
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| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universidad Nacional Autónoma de México
1997
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=56836103 |
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