Paleomagnetic study of the Late Miocene volcanic sequence in Sonora, Mexico: clockwise vertical axis rotation related to the oblique rifting in the Pacific-North American plate boundary. Supporting information.

Published: 23 December 2021| Version 1 | DOI: 10.17632/jxj8bn2vyf.1
Contributors:
luis velderrain,
Jesus Vidal-Solano,
Luis Alva-Valdivia

Description

This supporting information included here contains the table files of the paleomagnetic data used for constrain the age of the magmatic units from late Miocene distributed in the eastearn marging of the Gulf of California (coastal Sonora), characterized their magnetic properties and calculate their vertical axis rotation that suggest a transtensional deformation during the developmen of the Pacific-North American transform plate boundary.

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Paleomagnetism

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