中太平洋海山富钴结壳与基岩关系的研究
Research on the relationships between cobalt-rich crusts and substrate rocks in the Mid-Pacific Mountains
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摘要: 对我国首次取得的中太平洋海山基岩和富钴结壳样品的结构构造、矿物和化学组成特征的研究表明,该区主要基岩类型为碱性玄武岩、磷块岩、磷酸盐化碳酸盐岩和燧石等,碱性玄武岩分布最广,并均有不同程度的风化.观察表明,富钴结壳的载体可以是各种岩性的基岩.玄武岩、风化火山岩和磷块岩上的结壳厚度比燧石的大,有较高的经济价值,是选矿冶炼的主要对象.对于调查区内富钴结壳形态总体上可分为三种类型:板状、砾状和结核状结壳.从以下四个方面探讨结壳与基岩之间的关系:(1)海水、基岩和结壳中主要金属元素含量特点;(2)通过聚类分析方法探讨结壳与基岩之间的亲疏程度;(3)结壳的分布特征;(4)不同基岩类型对结壳生长的影响.分析结果表明,调查区内的火山岩及磷块岩对结壳形成的贡献大(比其他类型岩石).Abstract: The features of texture and structures,mineral and chemical compositions of substrate rocks and cobaltcrusts in the Mid-Pacific Mountains are identified and analysed.The results indicate that the major types of substrate rocks are alkaline basalt,phosphorite,phosphatized carbonate rocks and cherts in this area.In the above-mentioned rocks,the alkaline basalt is the most widespread one,and has been weathered to some extent.The observation has shown that the carrier of cobaltcrust can be all kinds of rocks.The thickness of crusts on basalts,weathered volcanic rocks,etc.is greater than that of cherts.The thicker crusts have more economic value and are major objects for dressing and smelting.The cobal-trich crusts in the research area can be divided into three types according to the shape:plate,gravel-like and nodule-like crust.The relationships between crusts and substrate rocks have been probed from the following four aspects:(1) the characteristics of major metallic elements content in seaw ater,substrate rocks and crusts;(2) the different close relations between different bedrocks and crusts by cluster analysis; (3) the distribution characteristics of crusts;(4) the influence of rock types on the growth of crusts.The conclusion is that volcanic rock,phosphorite,etc.contribute to the formation of the crust.
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Key words:
- central Pacific Ocean /
- cobaltcrust /
- substrate rock
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HALBACH P,MACHEIM F T,OTTEN P.Co-rich ferromanganese deposits in the marginal seamount regions of the Central Pacific Basin-results of the Midpac.'81[J].Erzmetall,1982,35(9):447-453. JAMES R Hein,WILLIAM C Schwab,ALICE S Davis.Cobalt and platinum-rich ferromanganese crusts and associated substrate rock from the Marshall Island[J].Marine Geology,1988,78:255-283. TAKEMETSU N,et al.控制海洋锰结核的结壳化学组成的因素——回顾与综述[J].地质地球化学,1991,(4):54-58. 许东禹.中太平洋锰结壳地球化学特征[J].海洋地质与第四纪地质,1990,10(4):1-9. 朱克超,李扬,赵祖斌.麦哲伦海山区MA,MC海山玄武岩基岩的岩石学特征[J].海洋地质与第四纪地质,1999,19(4):11-19. БАТУРИНΓИ.大洋铁锰矿形成的模式[J].陈颐亨译.海洋地质译丛,1989,(2):53-56. ДМ.ИТРИЕВЮИ.太平洋西北部海山的玄武岩,Fe-Mn结核和结壳的化学成分[J].朱佛宏译.海洋地质,1994,(1):80-91. 张尧庭,方开泰.多元统计分析引论[M].北京:科学出版社,1997.393-397. 丁士晟.多元分析方法及其应用[M].长春:吉林人民出版社,1981.362-370. 刘英俊,曹励明,李兆麟,等.元素地球化学[M].北京:科学出版社,1984.50-112. 林承毅,边立曾,张富生,等.深海锰结核中微生物的分类及串珠状超微生物化石的研究[J].科学通报,1996,41(9):821-824. 张富生,边立曾,林承毅,等.深海锰结核中螺旋状超微生物化石的发现及其意义[J].高校地质学报,1995,1(1):109-116. 陈建林,张富生,边立曾.超微生物是大洋多金属结核成矿的建造者[J].科学通报,1997,42(4):337-343. 陈建林,张富生,林承毅,等.太平洋中国开辟区锰结核生物成因研究[J].地质学报,2001,75(2):228-233. 陈建林,张富生,林承毅,等.锰质核形石——大洋多金属结核[M].北京:海洋出版社,2002.
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