2020
DOI: 10.1007/s00445-020-01410-7
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Eruptive history of La Poruña scoria cone, Central Andes, Northern Chile

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Cited by 8 publications
(1 citation statement)
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“…Parts of ignimbrites were highlighted by high silica percentages (~70%) according to ASTER, and the ignimbrite samples contained feldspar grains; however, although we did not find feldspar spectral signatures with Hyperion, we found moderate iron spectral signatures. In addition, the detection of high-iron-bearing mineral deposits at all three presented regions that were interpreted as basaltic-andesites is remarkable for research on mafic volcanism in the APVC [30,71,75].…”
Section: Re-emphasis Of the Apvc For Planetary Analog Usementioning
confidence: 77%
“…Parts of ignimbrites were highlighted by high silica percentages (~70%) according to ASTER, and the ignimbrite samples contained feldspar grains; however, although we did not find feldspar spectral signatures with Hyperion, we found moderate iron spectral signatures. In addition, the detection of high-iron-bearing mineral deposits at all three presented regions that were interpreted as basaltic-andesites is remarkable for research on mafic volcanism in the APVC [30,71,75].…”
Section: Re-emphasis Of the Apvc For Planetary Analog Usementioning
confidence: 77%