摘要
新测得TAG热液区中 5件海底块状硫化物样品的锇含量及其同位素组成 ,187Os/ 186Os比值在 2 .30 5～7.879之间 ,均值为 5 .986 ,介于现代海水和上部洋壳岩石的锇同位素组成之间 ,表明该区海底块状硫化物中锇是海水和上部洋壳来源锇混合的产物。在海底热液循环过程中 。
New data on osmium isotopic compositions of four seafloor massive sulfide samples from the TAG hydrothermal field has been got, the 187 Os/ 186Os ratios of massive sulfide samples vary from 2.305 to 7.879, with a mean of 5.986, these ratios are between that of modern seawater and upper oceanic crust, and this range of Os isotopic compositions is likely the result of mixing of seawater with upper oceanic crust, maybe about 56% of osmium in the massive sulfides is from the seawater, and 44% is from the upper oceanic crust. The mixing of seawater with hydrothermal fluid have an obvious effect on the Os concentration and isotope composition of massive sulfide during the seafloor hydrothermal activity.
出处
《沉积学报》
CAS
CSCD
北大核心
2002年第3期394-398,共5页
Acta Sedimentologica Sinica
基金
国家大洋重大专项课题 (批准号 :DY1 0 5 0 1 0 3 1 )
国家自然科学基金项目 (批准号 :40 1 760 2 0 )资助
