Semicontinuous paleomagnetic record of the last 1 Ma from radiometrically dated igneous rocks (Trans-Mexican Volcanic Belt and surrounding areas)

Author:

García Rafael,Solano Cervantes Miguel,Goguitchaichvili Avto,Reyes Daniel Sebastián,Kravchinsky Vadim A.,Morales Juan,Cejudo Rubén,Elguera Rosas José

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference58 articles.

1. Geology of the northern Colima and Zacoalco grabens, southwest Mexico: late cenozoic rifting in the Mexican volcanic belt;Allan;Geol. Soc. Am. Bull.,1986

2. Apparent and true polar wander and the geometry of the geomagnetic field over the last 200 Myr;Besse;J. Geophys. Res. Solid Earth,2002

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

4. Secular variation in Mexico during the Last 40 000 years;Bönhel;Phys. Earth Planet. In.,2002

5. Rock-Magnetic and Paleomagnetic results from the Tepic-Zacoalco rift region (western Mexico);Calvo;Studia Geophys. Geod.,2012

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