QIN Xiwei
1 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 2 Key Laboratory of Salt Lake Geology and Environment of Qinghai Province, Qinghai Institute of Salt Lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 3 University of Chinese Academy of Sciences, 100049 Beijing, ChinaMA Haizhou
1 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 2 Key Laboratory of Salt Lake Geology and Environment of Qinghai Province, Qinghai Institute of Salt Lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, ChinaZHANG Xiying
1 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 2 Key Laboratory of Salt Lake Geology and Environment of Qinghai Province, Qinghai Institute of Salt Lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, ChinaCHENG Huaide
1 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 2 Key Laboratory of Salt Lake Geology and Environment of Qinghai Province, Qinghai Institute of Salt Lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, ChinaHAN Jibin
1 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 2 Key Laboratory of Salt Lake Geology and Environment of Qinghai Province, Qinghai Institute of Salt Lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China；4 School of Environmental Studies, China University of Geosciences, 430074 Wuhan, ChinaLI Yongshou
1 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 2 Key Laboratory of Salt Lake Geology and Environment of Qinghai Province, Qinghai Institute of Salt Lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, ChinaMIAO Weiliang
1 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 2 Key Laboratory of Salt Lake Geology and Environment of Qinghai Province, Qinghai Institute of Salt Lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, ChinaHAI Qingyu
1 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 2 Key Laboratory of Salt Lake Geology and Environment of Qinghai Province, Qinghai Institute of Salt Lakes, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 810008 Xining, China 3 University of Chinese Academy of Sciences, 100049 Beijing, ChinaThis work was funded by the National Key Basic Research Project of China (973 program, No.2011CB403004). We thank Ma Yunqi, associate research fellow, for providing valuable suggestions and help during lab experiments.
Chemical and isotopic data were measured for 51 leached brine springs in the Changdu-Lanping-Simao Basin (CD-LP-SM), China. The predominance of Cl and Na, saturation indices of carbonate minerals, and Na/Cl and Ca/SO4 ratios of ~1 suggest that halite, sulphate, and carbonate are the solute sources. Integration of geochemical, δ18O, and δD values suggests that springs are mainly derived from meteoric water, ice-snow melt, and water-rock interactions. B concentrations range from 0.18 to 11.9 mg/L, with δ11B values of ?4.37‰ to +32.39‰, indicating a terrestrial source. The δ11B-B relationships suggest B sources of crustal origin (marine carbonates with minor crust-derived volcanics); we did not identify a marine or deep mantle origin. The δ11B values of saline springs (+4.61‰ to +32.39‰) exceed those of hot (?4.37‰ to +4.53‰) and cold (?3.47‰ to +14.84‰) springs; this has contributed to strong water-rock interactions and strong saturation of dissolved carbonates. Conversely, the global geothermal δ11B-Cl/B relationship suggests mixing of marine and non-marine sources. The δ11B-Cl/B relationships of the CD-LP-SM are similar to those of the Tibet geothermal belt and the Nangqen Basin, indicating the same B origin. These differ from thermal waters controlled by magmatic fluids and seawater, suggesting that B in CD-LP-SM springs has a crustal origin.
QIN Xiwei, MA Haizhou, ZHANG Xiying, CHENG Huaide, HAN Jibin, LI Yongshou, MIAO Weiliang, HAI Qingyu.2019. Geochemical Constraints on the Origin and Evolution of Spring Waters in the Changdu-Lanping-Simao Basin, Southwestern China[J]. Acta Geologica Sinica(),93(4):1097-1112
Copy
