@article{oai:u-ryukyu.repo.nii.ac.jp:02004843,
 author = {木村, 政昭 and 林, 正雄 and 大森, 保 and Kimura, Masaaki and Hayashi, Masao and Oomori, Tamotsu},
 issue = {40},
 journal = {琉球大学理学部紀要, Bulletin of the College of Science. University of the Ryukyus},
 month = {Oct},
 note = {A geochemical study on hot spring gush out of the sea bottom of 22 meters deep off Taketomi-jima reveals that the spring water at well mouth is 17.8-18.1 % of chlorinity and 37.5℃ in temperature which is considerably higher than the temperature of the water column in the vicinity (about 25℃). Based upon the result of the simple mixing  ratios between sea water and fresh spring water, temperature and depth of the subground water reservoir could be \nestimated as 191℃ and 130 m beneath sea level. This is thought to be active thermal source which gives good cause for hope., 紀要論文},
 pages = {137--144},
 title = {竹富島海底温泉の貯留層についての一考察},
 year = {1985}
}