Geochemical exploration in Mesillas geothermal area, Mexico

Hydrogen sulphide (H2S) migration in groundwater of the Zechstein strata in the Legnica-Głogów Copper Basin and its vicinity, SW Poland

“…This gas is com monly found as so ci ated with sul phate and car bon ate rock units form ing sour nat u ral gas res er voirs (Worden and Smalley, 1996;Aali and Rahmani, 2012;Liu et al, 2014;Bilkiewicz and Kowalski, 2020;Kotarba et al, 2020;Torghabeh et al, 2021;Cheng et al, 2022). Be sides its oc currence in these nat u ral gas res er voirs, the or i gin, mi gra tion and ac cu mu la tion of H 2 S has been also stud ied in con nec tion with coal seams (Liu et al, 2012;Deng et al, 2014;Tan et al, 2020;Xie et al, 2021), pe tro leum fields (Kotarba et al, 2017b) and the ex plo ra tion, de sign and op er a tion of geo ther mal fa cil i ties (D'Amo re et al, 1990;Mayrhofer et al, 2014;Jácome Paz et al, 2022).…”

A Joint Method Based on Geochemistry and Magnetotelluric Sounding for Exploring Geothermal Resources in Sedimentary Basins and Its Application

“…The inversion of deep geothermal reservoirs' temperatures using geochemical methods (e.g., geothermometers) can be used to supplement and verify the results of geophysical exploration [21][22][23]. Geothermometers generally include cation and SiO 2 geothermometers and integrated multicomponent solute geothermometry, which are widely used in the estimation of geothermal reservoirs' temperatures [24][25][26][27][28][29][30][31][32][33]. Barcelona et al [33] estimated the temperature of the Gollette geothermal field using a cation geothermometer and the results obtained were consistent with those achieved using multiple mineral equilibrium diagrams.…”