Paleosecular variation and time-averaged field recorded in late Pliocene-Holocene lava flows from Mexico

Author:

Mejia V.1,Böhnel H.2,Opdyke N. D.1,Ortega-Rivera M. A.2,Lee J. K. W.3,Aranda-Gomez J. J.2

Affiliation:

1. Department of Geological Sciences; University of Florida; 241 Williamson Hall,; Gainesville; Florida; 32611-2120; USA

2. Centro de Geociencias; Universidad Nacional Autónoma de México, Campus Juriquilla; Querétaro; 76230; Mexico

3. Department of Geological Sciences and Geological Engineering; Queen's University; Kingston, Ontario; Canada; K7L 3N6

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference60 articles.

1. Effect of strain rate in the distribution of monogenetic and polygenetic volcanism in the Transmexican volcanic belt;Alaniz-Alvarez;Geology,1998

2. Further constraints for the Plio-Pleistocene geomagnetic field strength: New results from the Los Tuxtlas volcanic field;Alva-Valdivia;Earth Planets Space,2001

3. Aranda-Gomez , J. J. J. F. Luhr A. F. Nieto-Samaniego 1993 Localidades recien descubiertas de xenolitos del manto de la base de la corteza en el estado de San Luis Potosí, Mexico Boletín 106 25 36 Inst. de Geol., Univ. Nacl. Autonoma de Mexico Ciudad Universitaria, Mexico

4. Secular variation in Mexico during the last 40000 years;Böhnel;Phys. Earth Planet. Inter.,2002

5. Preliminary results of palaeomagnetic measurements of Tertiary and Quaternary igneous rocks from the eastern part of the Trans Mexican volcanic belt;Böhnel;Geofis. Int.,1981

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