δ13C, δ18O and deposition rate of tufa in Xiangshui River, SW China: Implications for land-cover change caused by climate and human impact during the late Holocene

Liu, Z.Z.LiuSun, H.H.SunLi, H.H.LiHONGCHUN LI2020-05-152020-05-152011https://scholars.lib.ntu.edu.tw/handle/123456789/493094[SDGs]SDG13δ13C, δ18O and deposition rate of tufa in Xiangshui River, SW China: Implications for land-cover change caused by climate and human impact during the late Holocenejournal article10.1144/SP352.72-s2.0-79951733686https://www.scopus.com/inward/record.uri?eid=2-s2.0-79951733686&doi=10.1144%2fSP352.7&partnerID=40&md5=b7912f7958c5c9a672be565508adb769