J4 ›› 2011, Vol. 41 ›› Issue (2): 432-439.

• 地质与资源 • 上一篇    下一篇

劳盆地热液羽状流颗粒物微区特征及指示意义

雷吉江1,2|初凤友2|于晓果2|李小虎2|陶春辉2|杨克红2   

  1. 1.中国地质大学 资源学院|武汉430074;2.国家海洋局 海底科学重点实验室|杭州310012
  • 收稿日期:2010-07-12 出版日期:2011-03-26 发布日期:2011-03-26
  • 通讯作者: 初凤友(1964-),男,吉林四平人,研究员,博士,主要从事海洋地质方面的研究,Tel:0571-81963202 E-mail:chu@sio.org.cn
  • 作者简介:雷吉江(1983-)|男|湖北潜江人|博士研究生|主要从事海洋地质方面的研究|Tel:0571-81963162|E-mail:leijj@sio.org.cn
  • 基金资助:

    国家自然科学基金项目(40776035,40976039);国家自然科学基金青年基金项目(40906036);国家海洋局青年基金项目(1086-10);国家海洋局第二海洋研究所基本科研业务专项项目(JG0904)

Micro-Area Characteristics and Implications of Hydrothermal Plume-Derived Particles in Lau Basin

LEI Ji-jiang1,2, CHU Feng-you2, YU Xiao-guo2, LI Xiao-hu2, TAO Chun-hui2, YANG Ke-hong2   

  1. 1.Faculty of Resources, China University of Geosciences, Wuhan430074, China;
    2.Key Laboratory of Submarine Geosciences| State Oceanic Administration, Hangzhou310012, China
  • Received:2010-07-12 Online:2011-03-26 Published:2011-03-26

摘要:

以劳盆地热液羽状流水体为研究对象,对6个不同深度水层(海底以上50~500 m)的悬浮颗粒物(>0.45 μm)进行了扫描电镜观察和X射线能谱分析。通过颗粒物的微形貌将颗粒物分为生物碎屑、微生物成因颗粒、无定形颗粒和自形颗粒等类型。微生物成因颗粒包括丝状体和簇状体等形态类型;自形颗粒主要为黄铁矿和闪锌矿晶体;根据颗粒组分特征将无定形颗粒分为S-Zn-Ba-Ca、Fe氧化物+少量Ba-Zn-Ca、Fe-Mn-Ca-Ba+少量的Zn、硫化物颗粒及多金属颗粒5种不同类型。大量与热液活动有关的颗粒类型的出现以及无定形颗粒的尺寸分布特征反映了研究站位处于热液羽状流的早期发育阶段,推测在附近几百米范围内存在活动的热液喷口区。

关键词: 热液羽状流, 悬浮颗粒物, 喷口, 微区分析, 劳盆地

Abstract:

Particulate samples(>0.45 μm) from a hydrothermal plume in Lau basin are collected by filtering on deck and analyzed by scanning electron microscope(SEM) and X-ray energy dispersive spectroscopy(EDS). Four types of particles have been morphologically characterized. i)Biogenic detritus mainly device from background water. ii)Microbial particles include filamentous and clustered configuration; and these specific morphology suggest specific microorganism community. iii)Amorphous particles are divided into S-Zn-Ba-Ca phase, Fe-oxide phase containing trace of Ba-Zn-Ca, Fe-Mn-Ca-Ba phase containing trace of Zn, sulfide particles and polymetallic particles, and the amorphous forms should originate from precipitation in the external part of sulfide chimney or the fragmentation of chimney rocks. iv) Automorphic particles are probably formed in an area where the chemical conditions are homogeneous, i.e. the internal part of sulfide chimney. So many particles related to hydrothermal activity and the distributions of amorphous particles in different water layers indicate  that our study station locats at the incipient stage of formation of hydrothermal plumes, and during the several hundreds meters there may exist an active hydrothermal vent area.

Key words: hydrothermal plumes, buoyant particles, vents, micro-analyzed, Lau basin

中图分类号: 

  • P736
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