HYDROTHERMAL REMOBILIZATION OF SUBSEAFLOOR SULFIDE MINERALIZATION ALONG MID-OCEAN RIDGES CONTRIBUTES TO THE GLOBAL OCEANIC ZINC ISOTOPIC MASS BALANCE Back August 24, 2026 by emily chan MetadataShare TitleHYDROTHERMAL REMOBILIZATION OF SUBSEAFLOOR SULFIDE MINERALIZATION ALONG MID-OCEAN RIDGES CONTRIBUTES TO THE GLOBAL OCEANIC ZINC ISOTOPIC MASS BALANCEAuthorLIAO, SHILI | TAO, CHUNHUI | WEN, HANJIE | YANG, WEIFANG | LIU, JIA | JAMIESON, JOHN W. | DIAS, ÁGATA ALVEIRINHO | ZHU, CHUANWEI | LIANG, JIN | LI, WEI | DING, TENG | LI, XIAOHU | ZHANG, HUICHAOPUBLISH YEAR2022FACULTY / RESEARCH UNITINSTITUTE OF SCIENCE AND ENVIRONMENTSUBJECTSHYDROTHERMAL ACTIVITY,MID OCEAN RIDGE,SUBSURFACE REMOBILIZATION,ZINC ISOTOPIC MASS BALANCEDOCUMENT TYPEJournal ArticlePart ofGEOCHIMICA ET COSMOCHIMICA ACTADOI10.1016/j.gca.2022.08.022ISSN0016-7037LANGUAGEENGLISHLink to Publisherhttps://www.sciencedirect.com/science/article/pii/S0016703722004410 Continue browsing MACAO AIR QUALITY FORECAST USING STATISTICAL METHODS MATERIAL SOURCE OF SEDIMENTS FROM WEST CLARION–CLIPPERTON ZONE (PACIFIC): EVIDENCE FROM RARE EARTH ELEMENT GEOCHEMISTRY AND CLAY MINERALS COMPOSITIONS Back to items list