期刊文献+

海底蚀变玄武岩中次生组分去除实验研究 被引量:3

Leaching Experiments of Secondary Components in Altered Submarine Basalts
原文传递
导出
摘要 选择有大量次生方解石沉淀的海底蚀变玄武岩为研究对象,研磨、均一化后将粉末样品分为49份,其中48份分别以0.25,0.5,1.0,1.5,2.0,2.5 mol/L 6种浓度的足量HCl溶解0.5,1,2,4,8,16,32,64 h,选取溶解残渣测定其主要氧化物和特征微量元素含量,研究确定HCl溶解法去除海底玄武岩中次生组分的浓度—时间组合。结果表明,1.0 mol/L-0.5 h,1.0 mol/L-1 h,1.0 mol/L-2 h,1.0 mol/L-4 h,1.5 mol/L-0.5 h,1.5 mol/L-1 h,2.0 mol/L-0.5 h,2.0 mol/L-1 h和2.5 mol/L-0.5 h等9种HCl浓度—时间组合是可供去除海底蚀变玄武岩中次生碳酸盐的理想方案。 Altered submarine basalts with rich secondary calcites were graded,homogenized,and divided into 49 subsamples.48 subsamples were leached with hydrochloric acid(HCl) of different concentrations(0.25 mol/L,0.5 mol/L,1.0 mol/L,1.5 mol/L,2.0 mol/L,2.5 mol/L) for different time periods(0.5 hour,1 hour,2 hours,4 hours,16 hours,32 hours and 64 hours).The main oxides and trace elements in the leached residuals were analyzed to determine the preferred HCl concentration-time combinations for leaching secondary components in altered submarine basalts.The result indicates that there are 9 optimal schemes as preferred HCl concentration-time combinations to leach secondary components in altered submarine basalts,which are 1.0 mol/L-0.5 hours,1.0 mol/L-1 hour,1.0 mol/L-2 hours,1.0 mol/L-4 hours,1.5 mol/L-0.5 hours,1.5 mol/L-1 hour,2.0 mol/L-0.5 hours,2.0 mol/L-1 hour and 2.5 mol/L-0.5 hour.
出处 《地球科学进展》 CAS CSCD 北大核心 2012年第10期1167-1172,共6页 Advances in Earth Science
基金 国家海洋局第一海洋研究所基本科研业务费专项资金项目"海底玄武岩次生碳酸盐去除实验研究"(编号:2007G22) 国际海底区域研究开发"十一五"项目"海底多金属成矿系统及矿集区初步研究"(编号:DYXM-115-01-2-1)资助
关键词 蚀变玄武岩 次生组分 去除实验 Altered submarine basalts Secondary components Leaching experiments.
  • 相关文献

参考文献16

  • 1Guy C, Daux V, Schott J. Behaviour of rare earth elements during seawater/basalt interactions in the Mururoa Massif [ J ]. Chemical Geology, 1999, 158: 21-35. 被引量:1
  • 2Alta J C, Teagle D A H. Hydrothermal alteration of upper oceanic crust formed at a fast-spreading ridge : Mineral, chemical, and iso- topic evidence from ODP Site 801 [ J]. Chemical Geology, 2003, 201 : 191-211. 被引量:1
  • 3朱克超.麦哲伦海山区MA、MC、MD、ME、MF海山结壳基岩的岩石学[J].海洋地质与第四纪地质,2002,22(1):49-56. 被引量:7
  • 4Bach W, Garrido C J, Paulick H, et al. Seawater-peridotite inter- actions: First insights from ODP Leg 209, MAR 15°N [J]. Geo- chemistry Geophysics Geosystems,2004, 5 (9) : 1-22. 被引量:1
  • 5BU Wenrui,SHI Xuefa,PENG Jiantang,LIU Jihua,Zhang Mingjie,QI Liang.Low-temperature alteration of oceanic island basalts and their contribution to transition metal circulation of the ocean[J].Acta Oceanologica Sinica,2008,27(2):35-54. 被引量:1
  • 6Meurer W P, Sturm M A, Klein E M, et al. Basalt compositions from the Mid-Atlantic Ridge at the SMARK area (22°30′N to 22°50′N) implications for parental liquid variability at isotopically homogeneous spreading centers [ J ]. Earth and Planetary Science Letters, 2001, 186: 451-469. 被引量:1
  • 7Kamenetsky V S, Everard J L, Crawford A J, et al. Enriched end-member of primitive MORB Melts : Petrology and geochemis- try of glasses from Maequarie Island (SW Pacific) [J]. Journal of Petrology, 2000, 41(3): 411-430. 被引量:1
  • 8Hannigan R E, Basu A R, Teichmann F. Mantle reservoir gee- chemistry from statistical analysis of ICP-MS trace element data of equatorial mid-Atlantic MORB glasses [ J ]. Chemical Geology, 2001, 175 : 397-428. 被引量:1
  • 9Cooper K M, Eiler J M, Asimow P D. Oxygen isotope evidence for the origin of enriched mantle beneath the mid-Atlantic ridge [ J]. Earth and Planetary Science Letters, 2004, 220 : 297-316. 被引量:1
  • 10Chan L, Lassiter J C, Hauri E H. Lithium isotope systematics of lavas from the Cook-Austral Islands: Constraints on the origin of HIMU mantle [ J ]. Earth and Planetary Science Letters, 2009, 277 : 433-442. 被引量:1

二级参考文献19

  • 1党志,侯瑛.玄武岩-水相互作用的溶解机理研究[J].岩石学报,1995,11(1):9-15. 被引量:24
  • 2王焕夫.海山区铁锰结壳基座的起源及其成因分类方案[J].海洋地质与第四纪地质,1997,17(2):83-91. 被引量:6
  • 3朱佛宏.太平洋玄武岩的岩石化学类型及岩石蚀变[J].海洋地质地质,1989,(7):4-6. 被引量:3
  • 4D. A. Clague,E. D. Jackson,T. L. Wright.Petrology of Hualalai volcano, Hawaii: Implication for mantle composition[J].Bulletin Volcanologique.1980(4) 被引量:1
  • 5Akiho Miyashiro,Fumiko Shido,Maurice Ewing.Diversity and origin of abyssal tholeiite from the Mid-Atlantic Ridge near 24° and 30° North latitude[J].Contributions to Mineralogy and Petrology.1969(1) 被引量:1
  • 6Hein J R,Koschinsky A,Bau M, et al.Cobalt-richferromanganese crusts in the Pacific[].Handbook of Marine Mineral Deposits.1999 被引量:1
  • 7Hein J R,Manheim F T,Schwab W C, et al.Ferro-manganese crusts from Necker ridge, Horizon Guyot andS. P. Lee Guyot: geological considerations[].Marine Geology.1985 被引量:1
  • 8Hein J R,Morgan C L.Influence of substrate rocks onFerromanganese crust composition[].Deep Sea Research.1999 被引量:1
  • 9Hofmann A W,Jochum K P.Source characteristicsderived from very incompatible trace elements in MaunaLoa and Mauna Kea basalts, Hawaii Scientific DrillingPro-ject[].Geophys Res B.1996 被引量:1
  • 10Honnorez J.The aging of the oceanic crust at lowtem-perature[].The Sea v: The Oceanic Lithosphere.1981 被引量:1

共引文献6

同被引文献60

引证文献3

二级引证文献6

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部