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Mineralogical and geochemical features of sulfide chimneys from the 49°39′E hydrothermal field on the Southwest Indian Ridge and their geological inferences
作者姓名:TAO ChunHui  LI HuaiMing  HUANG Wei  HAN XiQiu  WU GuangHai  SU Xin  ZHOU Ning  LIN Jian  HE YongHua  ZHOU JianPing
作者单位:[1]Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China [2]Qingdao Institute of Marine Geology, Qingdao 266071, China [3]China University ofGeosciences (Beijing), Beijing 100083, China [4]China Ocean Mineral Resources Research and DevelopmentAssociation, Beijing 100860, China [5]Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
基金项目:supported by the China Ocean Min-eral Resources Research and Development Association Program (DY115- 02-1-01); the State Oceanic Administration Youth Science Fund (2010318)
摘    要:During January–May in 2007,the Chinese research cruise DY115-19 discovered an active hydrothermal field at 49°39′E/37°47′S on the ultraslow spreading Southwest Indian Ridge (SWIR).This was also the first active hydrothermal field found along an ultraslow-spreading ridge.We analyzed mineralogical,textural and geochemical compositions of the sulfide chimneys obtained from the 49°39′E field.Chimney samples show a concentric mineral zone around the fluid channel.The mineral assemblages of the interiors consist ...

关 键 词:sulfide  chimneys  49°39′E  hydrothermal  field  Southwest  Indian  Ridge  mid-ocean  ridge  DY115-19  Chinese  cruise  
收稿时间:11 March 2005
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