作者: Zhiguan Shangguan , Yaqin Zheng , Jichuan Dong
DOI: 10.1007/BF02877570
关键词:
摘要: On the basis of chemical components and stable isotopic compositions escaped gases from Tianchi volcanic geothermal area, material sources these are discussed, presenting that they mainly derived residual mantle-derived magma in crust; Changbai area may be directly interlinked with eruption canal history; there is a reservoir water deep-seated under temperature being about (166 ± 9)°C.