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Sr is split up off their ions because of the eluting an enthusiastic aliquot thanks to a great quartz cation change column full of Eichrom Sr-Specification resin. The brand new 87Sr/86Sr proportion dimension mistake try 2σ and relates to the past quantitative set. The brand new B isotopic well worth within study are expressed inside δ, as well as the reproducibility try 2σ to own δ11B. The brand new parallel test used in the test are D2811, the new relative error away from parallel samples are below 15%. Significant chemicals areas of liquid examples was computed at the Secret Laboratory out of Geothermal Tips Advancement and Usage, Sinopec. Levels from big cations (Na+, K+, Ca2+, Mg2+, B3+, Si4+, Sr2+and you will Li+) and you may significant anions (F−, Cl−, HCO3−and SO42−) were dependent on ion chromatography (Dionex ICS-1100) that have concerns of lower than 2%.

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Magnetotelluric questionnaire and you can seismic prospecting mirrored the fresh partly molten granite as the a low speed–high conductive covering close to the BSGZ northwest of the YHGF (The new Geothermal Geological People away from Tibet 1990). At the same time, with respect to the most recent mining of YHGF, the highest measured temperatures and you may restrict circulate skill from deep geothermal fluid were open from the chief creation well ZK208 within the BSGZ. Thus, the big heat source of YHGF try magmatic, provided with a leading-speed conductive level nearby the BSGZ found northwest of your YHGF. The fresh chemical compounds composition of one’s examined seas and you will physicochemical details such as the temperatures, pH, and you can total demolished solids (TDS) is actually placed in Dining table 1.

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Compared to the fresh conduction-kind of borehole, the fresh geothermal gradient beliefs of your conduction–convection-kind of borehole try relatively high and you may demonstrate the brand new trait away from vertical stratification. Such, the brand new geothermal gradient from ZK300 try 47.85 ℃/100 meters in the highest 0–349 m section and then decrease to one.72 ℃/100 yards between 349 and 407 m, to improve again in order to six.56 ℃/100 m ranging from 407 and you can 834 m. As a result of the apparently small thermal conductivity differences away from rock, it change in geothermal gradient is not caused by the change of thermal conductivity.

Also, K+ could be came from the fresh dissolution out of feldspars and you may micas throughout the water–material interaction. Also, From the YHGF, granitic rocks such as biotite granite porphyry, porphyritic biotite granite, and you may trachyandesite is actually generally delivered from the strong, that may render silicate vitamins. Some wells are affected by the fresh upwelling thermal drinking water, that have an excellent convex-kind of depth–temperatures curve, and you may get into a good conduction–convection-type borehole.