Paleomagnetic and magnetic fabric studies of the San Gaspar ignimbrite, western Mexico—constraints on emplacement mode and source vents-Reference-Cited by-同舟云学术

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Paleomagnetic and magnetic fabric studies of the San Gaspar ignimbrite, western Mexico—constraints on emplacement mode and source vents

Published:2005-10 Issue:1-2 Volume:147 Page:68-80
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Alva-Valdivia L.M.,Rosas-Elguera J.,Bravo-Medina T.,Urrutia-Fucugauchi J.,Henry B.,Caballero C.,Rivas-Sanchez M.L.,Goguitchaichvili A.,López-Loera H.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference35 articles.

1. Turbulent transport and deposition of the Ito pyroclastic flow: determinations using anisotropy of magnetic susceptibility;Baer;J. Geophys. Res.,1997

2. Iron–titanium oxide minerals and synthetic equivalents;Buddington;J. Petrol.,1964

3. The anisotropy of magnetic susceptibility of lava flows: an experimental approach;Cañon-Tapia;J. Volcanol. Geotherm. Res.,2000

4. Hysteresis properties of titanomagnetites: grain-size and compositional dependence;Day;Phys. Earth Planet. Inter.,1977

5. Estimates of flow direction for calc–alkaline welded tuffs and paleomagnetic data reliability from anisotropy of magnetic susceptibility measurements: Central San Juan Mountains, southwest Colorado;Ellwood;Earth Planet. Sci. Lett.,1982

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