摘要
The high-mineral contents of some thermal waters are believed to have medicinal properties. Numerous spas and bathhouses might be built at these hot springs to take advantage of theses supposed healing properties such as skin diseases, rheumatism and so on. This paper is to find thermal reservoir and to classify the kinds of water. The majority of thermal springs are found discharging from igneous centers of Tertiary and Quaternary volcanic fields of the western Yemen (research area). Structurally these volcanisms are connected to N-NW faults that are parallel to the main Red Sea trend. Temperature and pH values of the thermal spring range 37℃～96℃, and 6.3～8.7 respectively. The Yemeni thermal waters indicate high variability in composition since they are of Na (K)-Cl, Na-HCO_3 and Ca (Mg) -SO_4 types, whereas the surficial waters have the typical worldwide Ca (Mg) -HCO_3 composition. Different liquid phase geothermometers, such as SiO_2, K^2/Mg and Na/K. Estimated reservoir temperatures ranging 70～140℃ perform equilibrium temperature evaluation of the thermal reservoirs.
The high-mineral contents of some thermal waters are believed to have medicinal properties. Numerous spas and bathhouses might be built at these hot springs to take advantage of theses supposed healing properties such as skin diseases, rheumatism and so on. This paper is to find thermal reservoir and to classify the kinds of water. The majority of thermal springs are found discharging from igneous centers of Tertiary and Quaternary volcanic fields of the western Yemen (research area). Structurally these volcanisms are connected to N-NW faults that are parallel to the main Red Sea trend. Temperature and pH values of the thermal spring range 37℃～96℃, and 6.3 ～8.7 respectively. The Yemeni thermal waters indicate high variability in composition since they are ofNa (K) -C1, Na-HCO3 and Ca (Mg) -SO4 types, whereas the surficial waters have the typical worldwide Ca (Mg) -HCO3 composition. Different liquid phase geothermometers,such as SiO2, K2/Mg and Na/K. Estimated reservoir temperatures ranging 70 ～ 140℃ perform equilibrium temperature evaluation of the thermal reservoirs.
