التفاصيل البيبلوغرافية
| العنوان: |
The source of replenishment of geothermal water around Xi'an. |
| المؤلفون: |
Tao, Shuhua |
| المصدر: |
Science in China. Series E: Technological Sciences; Feb2001 Supplement, Vol. 44, p165-167, 3p |
| مستخلص: |
The meteoric origin of the geothermal water in Xi'an is evidenced by its H and O isotope composition. Based on the temperature dependence of isotopic composition, the temperature of meteoric water that replenishes the geothermal aquifers in Xi'an and its neighboring regions is calculated to be −13.28°C. The age of the geothermal water based on14C dating method is 10–30 kaBP, belonging to a secondary glacial period in Late Quaternary. The source of replenishment is considered to have mainly derived from glacial snow melt water from elevations higher than 2,000m (ASL) in Qinling Mountains. [ABSTRACT FROM AUTHOR] |
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| قاعدة البيانات: |
Complementary Index |
