Assessment of Chaves Low-Temperature CO<sub>2</sub>-Rich Geothermal System (N-Portugal) Using an Interdisciplinary Geosciences Approach

<div>Hydrogeological conceptual circulation model of Chaves low-temperature CO<sub>2</sub>-rich geothermal system. B stands for granitic and metasedimentary rocks; C stands for cover deposits; CLTGW stands for Chaves low-temperature CO<sub>2</sub>-rich geothermal waters; GR stands for geothermal reservoir; (−54; −8.1) stands for the isotopic composition (<i>δ</i><sup>2</sup>H; <i>δ</i><sup>18</sup>O) of the waters. Taken from [<a href="/journals/geofluids/2019/1379093/#B27">27</a>].</div>

Geofluids

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Figure 13

Figure 13: Assessment of Chaves Low-Temperature CO<sub>2</sub>-Rich Geothermal System (N-Portugal) Using an Interdisciplinary Geosciences Approach 

Geofluids

Assessment of Chaves Low-Temperature CO2-Rich Geothermal System (N-Portugal) Using an Interdisciplinary Geosciences Approach

Figure 13

Assessment of Chaves Low-Temperature CO₂-Rich Geothermal System (N-Portugal) Using an Interdisciplinary Geosciences Approach