Paleomagnetic study of the Valle de Santiago volcanics, Michoacán-Guanajuato volcanic field, Mexico

The Valle de Santiago area of the Michoacán-Guanajuato volcanic field is characterized by a 7 km by 50 km NNW-SSEtrending cluster of 20 maars, 13 in a smaller sub-area. This volcanic lineament may be associated with a pre-existing fault or zoneof structural weakness, which is approximately normal to...

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Kaydedildi:
Detaylı Bibliyografya
Yayımlandı:Geofísica Internacional
Asıl Yazarlar: Rosa María Uribe Cifuentes, Jaime Urrutia Fucugauchi
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Universidad Nacional Autónoma de México 1999
Konular:
Ciencias de la Tierra
Plio
Michoacan
Tectonics
Quaternary
Paleomagnetism
Online Erişim:https://www.redalyc.org/articulo.oa?id=56838402
Etiketler: Etiketle
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