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Geothermal Energy

Science – Society – Technology

Fig. 4 | Geothermal Energy

Fig. 4

From: Geochemical and H–O–Sr–B isotope signatures of Yangyi geothermal fields: implications for the evolution of thermal fluids in fracture-controlled type geothermal system, Tibet, China

Fig. 4

Simplified diagram of B isotope distribution in Yangzi and sambaing high-temperature geothermal field (modified from Cao et al 2021). The B isotopes of Yangban geothermal fluids from Yuan et al. (2014); The B isotope of hydrothermal fluids from Aggarwal et al. (2000), Palmer (1991) and Vengosh et al. (1991, 1994); Submarine hydrothermal was referred to Palmer and Slack (1989); The B isotope composition of granitic tourmalines was referred to Jiang et al. (1998); the B isotope composition of metamorphic rocks and magmatic rocks was referred to Zhou et al. (2019)

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