Helium evidences for mantle degassing in the groundwater of Madeira Island – Portugal
The Madeira Island is fed by an active hotspot, but there are no evidences of current volcanism and geothermal activity or, of a heat source at depth, which probably justifies why only low temperature and low TDS groundwater is found in Madeira. Nonetheless, Madeira is a relatively young island (≤7...
Published in: | Applied Geochemistry |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
2017
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Subjects: | |
Online Access: | https://doi.org/10.1016/j.apgeochem.2017.03.019 |