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Paleomagnetism of the Acambay graben, central Trans-Mexican Volcanic Belt

✍ Scribed by Ana Marı́a Soler-Arechalde; J Urrutia-Fucugauchi


Book ID
117226480
Publisher
Elsevier Science
Year
2000
Tongue
English
Weight
663 KB
Volume
318
Category
Article
ISSN
0040-1951

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Geomorphic assessment of active tectonic
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Spatial variations of Quaternary deformation and tectonic activity of faults along the Acambay graben are assessed using geomorphic and morphometric approaches. The Acambay graben is an east-west trending structure of apparent Quaternary age, located in the central part of the Mexican Volcanic Belt,