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Anisotropy of magnetic susceptibility analysis of the Cantera Ignimbrite, San Luis Potosi, México: flow source recognition

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Figure

Fig. 2.Stratigraphic column with position and relative thickness of theCantera Ignimbrite in relation to adjacent ignimbrite and rhyolitic unitsin the studied area
Fig. 3. Geologic map of SLPVF showing sampled sites and Cantera Ignimbrite outcropping, underlying and overlying volcanic units, the Cretaceousbasement and structural features
Fig. 4.Transmitted (A) and reflected (B and C) light microphotographs. (A) This photograph of PS site shows the fragmentary character of thephenocrystals: quartz (Q), sanidine (S) and plagioclase (P), englobed in a partially devitrified matrix (M)
Fig. 5. AMS structural corrected data and point density distribution circles plotted on equal-area projections—of lower hemisphere—
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