O,H,and Sr isotope evidence for origin and mixing processes of the Gudui geothermal system,Himalayas

• 作 者: Chenguang Wang Mianping Zheng
• 机 构: MLRKeyLaboratoryofSalineLakeResourcesandEnvironments,HydrochemistryandEnvironmentalLaboratory,StateK
• 出 处: 地学前缘:英文版
• 发表日期: 2020年4期
• 关键词: Geothermal fluid Oxygen-18 and deuterium isotope 87Sr/86Sr ratio Origin and mixi
• 基金项目: This work was financially supported by the China Geological Survey(Grant No.DD20160054),the National Natural Science Foundation of China(Grant No.U1407207),the National Key Research and Development Pr

Tho Gudui geothermal field records the highest temperature at equivalent borehole depths among the lainland hydrothermal systems in mainland China.Located about 150 km southeast of Lhasa City,the capital of Tibet,the Gudui geothermal field belongs to the