The Estimation of Reservoir Temperature for Thermal Springs Using the Integrated Multicomponent Geothermometry Method at Changbai Mountain, Northeastern Songliao Basin, China

Table 3

Geothermal deep circulation characteristics of different thermal springs in the Changbai Mountain region.

Thermal springs	Sample no.	(°C)	(°C)	(°C)	(°C/100 m)		(m)	(km)	(km)
Julong springs	G01	4	167	5	3.4	29.41	30	4.76	4.82
	G02	4	172	5	3.4	29.41	30	4.91	4.97
Jinjiang springs	G03	4	170	5	3.4	29.41	30	4.85	4.91
	G04	4	153	5	3.4	29.41	30	4.35	4.41
	G05	4	162	5	3.4	29.41	30	4.62	4.68
	G06	4	162	5	3.4	29.41	30	4.62	4.68
Shibadaogou springs	G07	4	130	5	2.8	35.71	30	4.46	4.53
	G08	4	110	5	2.8	35.71	30	3.75	3.82
	G09	4	118	5	2.8	35.71	30	4.36	4.42
Xianrenqiao springs	G010	4	127	5	3.0	33.33	30	4.07	4.13