Paleomagnetic investigation of quaternary sediment at Tlapacoya, México and at Valsequillo, Puebla, México

Resultados paleomagnéticos para sedimentos del Pleistoceno y Holoceno de dos localidades en el Eje Transversal Mexicano indican una polaridad normal durante ese período. No obstante que los resultados para Tlapacoya, México son detallados para el periodo de 25 000 - 5 000 años antes del presente, la...

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Bibliographic Details
Published in:	Geofísica Internacional
Main Authors:	J.C. Liddicoat, R. S. Coe, P. W. Lambert, H. E. Malde, V. Steen-Mcintyre
Format:	Article
Language:	English
Published:	Universidad Nacional Autónoma de México, Instituto de Geofísica 1981-07-01
Subjects:	paleomagnetismo sedimentos cuaternario eje transversal mexicano tlapacoya valsequillo puebla (méxico)
Online Access:	http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/45

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