Please wait a minute...
img img
高级检索
地球科学进展  2003, Vol. 18 Issue (4): 545-550    DOI: 10.11867/j.issn.1001-8166.2003.04.0545
研究论文     
天然矿物自然铝的研究进展
陈忠1,2,丘学林2,颜文2,杨惠宁3,古森昌2,陈木宏2
1.中国地质大学测试中心,湖北 武汉,430074;2.中国科学院南海海洋研究所与广州地球化学研究所边缘海地质重点实验室,广东 广州,510301;3.中国地质科学院地质研究所,北京 100037
RESEARCH ADVANCES ON NATIVE ALUMINIUM IN NATURAL MINERAL
Chen Zhong1,2,Qiu Xuelin2,Yan Wen2,Yang Huining3, Gu Senchang2,Chen Muhong2
1.Test Center, China University of Geosciences, Wuhan  430074, China;2.Open Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology & Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou  510301, China;3.Institute of Geology, Chinese Academy of Geological Sciences, Beijing  100037, China
 全文: PDF(75 KB)  
摘要:

综述了国内外自然铝的发现与研究史;自然铝的物理性质和颗粒形态、元素组成及含量、晶体结构参数等特征;自然铝的成因模式。自然铝主要见于老的火山和热液矿石中,或现代和中-新生代的海底活动构造带(如转换断层、中央海隆以及弧后扩张中心)的海洋沉积物中,有地幔碳热还原、海底热液内生和陆地表生置换等3种成因模式。

关键词: 内生模式南海热液流体自然铝地幔环境    
Abstract:

The paper reviewed advances on native aluminium research, including firstly process of finding and studying native aluminium, secondly physical property and morphology of metallic aluminium particles and their chemical composition, as well as crystal data, finally the models of the formation of native aluminium. In the geological environment native aluminium is usually found only in ancient volcanic rocks and hydrothermal ores, or in Recent and Meso-Cenozoic ocean sediments of the active tectonic regions of the ocean floor, including zones of transform faults, mid-ocean ridges and back-arc spreading centers. As a result of an accessory mineral involved mantle and high hydrothermal activity, there are three models of the formation of native aluminium, such as carbon deoxidization in the high temperature environment, endogenous processes of high hydrothermal activity in the submarine hydrothermal fluids, element replacement amond Al,S,K,Na.

Key words: Native aluminium    Mantle condition    Endogenous model    Hydrothermal fluid    South China Sea.
收稿日期: 2002-08-28 出版日期: 2003-08-01
:  P57  
基金资助:

中国科学院知识创新工程重要方向项目“南海西北部与红河地区的深部结构及其动力学机制研究”(编号:KZCX2-209)、“南海及邻区大地构造系统的组成、结构及演化”(编号:KZCX2-SW-117);科技部“十五”南沙综合专项“南砂群岛及珊瑚环境特征研究”(编号:2001D1A50041)资助.

通讯作者: 陈忠     E-mail: chzhsouth@scsio.ac.cn
作者简介: 陈忠(1970-),男,云南石屏县人,助理研究员,主要从事海洋矿物学与资源环境研究.E-mail:chzhsouth@scsio.ac.cn
服务  
把本文推荐给朋友
加入引用管理器
E-mail Alert
RSS
作者相关文章  
陈忠
颜文
陈木宏
古森昌
杨惠宁
丘学林

引用本文:

陈忠,丘学林,颜文,杨惠宁,古森昌,陈木宏. 天然矿物自然铝的研究进展[J]. 地球科学进展, 2003, 18(4): 545-550.

Chen Zhong,Qiu Xuelin,Yan Wen,Yang Huining, Gu Senchang,Chen Muhong. RESEARCH ADVANCES ON NATIVE ALUMINIUM IN NATURAL MINERAL. Advances in Earth Science, 2003, 18(4): 545-550.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2003.04.0545        http://www.adearth.ac.cn/CN/Y2003/V18/I4/545

[1] Novgorodova M I. Native Mentals in Hydrothermal Ores[M].Moscow:Nauka Press, 1983.288.

[2] Guilber J M, Park C F. The Geology of Ore Deposits[M]. San Franciso: Freeman Press, 1986.985.

[3] Pirajno F. Hydrothermal Mineral Deposits[M]. Berlin: Springer Press,1992.709.

[4] Hollister C D,Ewing J I. Shipboard Scientists Site 105: Lower continental rise hills[R]. Initial Reports of the Deep Sea Drilling Project, 1972,11:219-312.

[5] Lazur Yu M,Varentsov I M,Ermilov V V. Copper-zinc regions of the northwestern part of the Pacific Ocean(DSDP leg 62,1984)[J].Geochemistry, 1984,:1 718-1 725(in Russian).

[6] Arsamakov H I, Kruglyakov V V, Marushkin A I. Native metals and alloys in the pelagic sediments of the Pacific Ocean [J]. Lithology of Ore Deposits,1988,4:122-126(in Russian).

[7] Shterenberg L E. On native metals at the seafloor[J]. Journal of Mineralology,1993,15: 79-85(in Russian).

[8] Qiu Zhuxian. Nature aluminium[J]. Light Mental,1999,2:34-37. [邱竹贤.自然铝[J].轻金属,1999,2:34-37.]

[9] Qiu Zhuxian. Nature aluminium[J]. World Sci-Tech R&D,1999,21(1):23-25.[邱竹贤.自然铝[J].世界科技研究与发展,1999,21(1):23-25.]

[10] Davydov M P, Aleksandrov P A. Native aluminium in metasomatized sediments of the East Pacific Rise, 13°N[J]. Doklady Earth Sciences , 2001,379 (5): 567-570.

[11] Oleynikov B V, Okrugin A V, Leskova N V. Petrological significance of native aluminium finds in basites[J]. Doklady Academii of Sciences of USSR,1978,243(1):191-194(in Russian).

[12] НовгородоваМИ.Докдадщакадемнннау[J].ДАН,CCCP (Союз Советских Социалистических Реслублик),1981,256:445-447(in Russian).

[13] Kovalski V V, Oleynikov O B. Native metals and natural polymineral alloys of copper, zink, lead, tin and antimony in the rocks of the kimberlite pipe “Leningrad”[J]. Doklady Academii of Sciences of USSR, 1985, 285: 203-208 (in Russian).

[14] Novgorodova M I, Minina E L, Trubkin N V. Native aluminium from collection of vernadsky state geological museum[J]. Doklady Akademii Nauk,1995,344(5): 677-680(in Russian).

[15] Gorshkov A I, Seliverstov V A, Sivtsov A V, et al. The first discovery of native aluminum in carbonado[J]. Geology of Ore Deposits,1996,38 (4): 341-343.

[16] Novgorodova M I, Generalov M E, Glavatskikh S F. Native Al from gas exhalations of active volcanoes and from ancient basaltic diatremes: The similarity of composition and origin[J]. Doklady Akademii Nauk,1997,354 (4): 524-528 (in Russian).

[17] Shmulovich K I, Vakulenko A G, Shiryaev A A. Formation of nature aluminum and silicon in sublimates of Kudryavyi volcano, Iturup island, Kuril arc[J]. Doklady Akademii Nauk,1997,354(6):800-803(in Russian).

[18] Shterenberg L E, Vassileva G L. Native metals and intermetals in the sediment from the north-eastern Pacific Ocean[J]. Lithology of Ore Deposits,1979,2:133-139 (in Russian).

[19] Yushko-Zakharova O E, Zakharova V E, Golovina M S, et al. Native metals inn the iron-manganese nodules of the World Ocean[J]. Doklady Academii of Sciences of USSR,1984,275:465-467(in Russian).

[20] Shterenberg L E, Kuzmina O V, Laputina I P, et al. On the find of native in association with ZnO and ZnCl2 in the sediments of site 647(north-western Pacific Ocean)[J]. Lithology of Ore Deposits,1986,1:137-140 (in Russian).

[21] Butuzova G Yu, Shterenberg L E, Voronin B I, et al. Native metals in the ore-bearing sediments in the Red Sea[J]. Lithology of Ore Deposits,1987,2:122-125(in Russian).

[22] Vesselin M D, Elena D M, Kalin B D, et al. Native aluminium in metalliferous sediments from the east Pacific Rise axial zone(21°S)[J]. Marine Geology,1995,123(1/2):87-103.

[23] Новгородова M И,Мамедов Ю Г.Самородный а люминий из грязе воговулкана острова булла[J]. Литология и полезные ископаемые,1996,(4):339-349 (in Russian).

[24] Deng Yanhua,Zhang Lekai,Ou Jinxiu,et al. Discovery native aluminium in beresitization vein[J].Journal of Gulin Institute of Technology, 1983,3(1):1-6.[邓燕华,张乐凯,欧锦秀,.黄铁绢英岩中发现的罕见天然矿物——自然铝[J].桂林冶金地质学报,1983,3(1):1-6.]

[25] Jiang Xinshun,Li Wenkang,Zhang Shuxin,et al. Discover of native aluminium in the oxidation zone in Getang, Anlong county,Guizhou province[J]. Bulletin of the Chinese Academy of Geological Sciences,1985,11:79-84. [姜信顺,李文亢,张树新,.贵州安龙戈塘氧化带中自然铝的发现[J].中国地质科学院院报,1985,11:79-84.]

[26] He Shuangmei,Cao Fenyuan,Liu Yanzhong. The native aluminium discovered in the Lianhuashan Tungsten deposit,Guangdong province[J] .Geology and Prospecting,1990,26(9): 32-34.[何双梅,曹芬元,刘燕忠.广东莲花山钨矿床中发现自然铝[J].地质与勘探,1990,26(9):32-34.]

[27] Yang Huining,Chen Zhong, Yan Wen,et al. Solid mineral resource and its distribution in South China Sea area[A].In:The Papers on Investigation of Special Economic Zones and Continental Shelf of China[C]. Beijing:China Ocean Press,2002.102-109.[杨慧宁,陈忠,颜文,.南海海域固体矿产资源与分布[A].:我国专属经济区和大陆架勘测研究论文集[C].北京:海洋出版社,2002.102-109.]

[28] Gao Shan,Jin Qingmin. Delamination and its geodynamical significance for crust-mantle evolution[J].Geological Science and Technology Information, 1997,16(1):1-9. [高山,金庆民.拆沉作用及其壳—幔演化动力学意义[J].地质科技情报,1997,16(1):1-9.]

[29] Li X H, Zhou H W, Liu Y, et al. Shoshonitic intrusive suite in SE Guangxi: Petrology and geochemistry[J]. Chinese Science Bulletin,2000,45(7):653-658.

[30] Guo Xinsheng,Chen Jiangfeng,Zhang Xun,et al. Nd isotopic ratios of K-enriched magmatic complexes from southeastern Guangxi province: Implications for the mantle in southeastern China during the Mesozoic[J]. Acta Petrologica Sinica,2001,17(1):19-27.[郭新生,陈江峰,张巽,.桂东南富钾岩浆岩的Nd同位素组成:华南中生代地幔物质上涌事件[J].岩石学报,2001,17(1):19-27.]

[31] Fei Yingwei. Phase transition in the Earths mantle and mantle mineralogy[A]. In: Zhang Youxue, Yin An,eds.Struture Evolution and Dynamics of the Earth[C]. Beijing:Higher Education Press, 2002.49-90.[费英伟.地幔中的相变和地幔矿物[A].:张有学,尹安编.地球的结构、演化和动力学[C].北京:高等教育出版社,2002.49-90.]

[32] Lukanin O A ,Kadik A A. The possible role of the partial melting in the formation of the oxi-reducing and fluid conditions of the upper mantle[J]. Doklady Academii of Sciences of USSR, 1984,275: 996-998(in Russian).

[33] Lissitzin A P, Bogdanow Yu A, Gurvich E G. Hydrothermal Formations of the Rift Ocean Zones[M]. Moscow: Nauka Press ,1990.256

[34] Osadchii E G, Alekhin Yu V. On the origin of native aluminium [J]. 27th International Geological Congress, Moscow, USSR, Abstracts ,1984,5:131.

[35] Korzhinskii M A, Tkachenko S I, Bulgakov R F, et al. Condensate compositions and native metals in sublimates of high-temperature gas streams of Kudryavyi volcano, Iturup island, Kuril islands[J]. Geokhimiya,1996(12):1 175-1 182.

[36] Howard K J, Fisk M R. Hydrothermal alumina-rich clay and beohmite on the Gorda Ridge[J]. Geochimica et Cosmochimica Acta,1988,52:2 269-2 279.

[37] Oudin E. Hydrothermal sulfide deposits of the east Pacific Rise (21°N), Party: Descriptive mineralogy[J]. Marine Geology, 1983,4:39-72.

[38] Li Hongyang,Niu Shuyin. Oxidation of common sulfide minerals and its environmental effects[J]. Beijing Geology,2001,13(2) :6-11.[李红阳,牛树银.常见硫化物的氧化作用及其环境效应[J].北京地质,2001,13(2):6-11.]

[39] Yao Baichu,Zeng Weijun,Hayes D E,et al. The Geological Memoir of South China Sea Surveyed Jointly by China & USA [M]. Wuhan: China University of Geosciences Press, 1994.191-194.[姚伯初,曾维军,Hayes D E,.中美合作调研南海地质专报[M].武汉:中国地质大学出版社,1994.191-194.]

[40] Zou Heping. Continental marginal rifting along the northern South China Sea: The crustal response to the lower lithospheric delamination[J]. Marine Geology & Quaternary Geology,2001,21(1):39-44.[邹和平.南海北部陆缘张裂——岩石圈拆沉的地壳响应[J].海洋地质与第四纪地质,2001,21(1):39-44.]

[1] 张江勇, 王志敏, 廖志良, 王金莲, 李小穗. 南海深海平原柱状样QD189磁化率、非磁滞剩磁、粒度、碎屑矿物丰度之间的主要关系[J]. 地球科学进展, 2015, 30(9): 1050-1062.
[2] 韩钦臣, 康建成, 王国栋, 朱炯. 基于海洋分析资料的吕宋海峡水交换的月际变化特征[J]. 地球科学进展, 2015, 30(5): 609-619.
[3] 蔡树群, 刘统亚, 何映晖, 吕海滨, 陈植武, 刘军亮, 谢皆烁, 许洁馨. 南海东北部剪切流场对内波影响的研究进展[J]. 地球科学进展, 2015, 30(4): 416-424.
[4] 卢汐, 宋金明, 袁华茂, 李宁. 黑潮与毗邻陆架海域的碳交换[J]. 地球科学进展, 2015, 30(2): 214-225.
[5] 孙枢. 10年来中国IODP专家委员会工作简要回顾[J]. 地球科学进展, 2014, 29(3): 317-321.
[6] 邵勰, 黄平, 黄荣辉. 南海夏季风爆发的研究进展[J]. 地球科学进展, 2014, 29(10): 1126-1137.
[7] 贺子丁,刘志飞,李建如,谢昕. 南海西部54万年以来元素地球化学记录及其反映的古环境演变[J]. 地球科学进展, 2012, 27(3): 327-336.
[8] 汪鹏,钟广法. 南海ODP1144站深海沉积牵引体的岩石物理模型研究[J]. 地球科学进展, 2012, 27(3): 359-366.
[9] 李琪,李前裕,王汝建. 20万年来南海古海洋研究的主要进展[J]. 地球科学进展, 2012, 27(2): 224-239.
[10] 蔡树群,何建玲,谢皆烁. 近10年来南海孤立内波的研究进展[J]. 地球科学进展, 2011, 26(7): 703-710.
[11] 杜岩,方国洪. 印度尼西亚海与印度尼西亚贯穿流研究概述[J]. 地球科学进展, 2011, 26(11): 1131-1142.
[12] 李春峰,苏 新,姜 涛,Ujiie K, Fabbri O, Yamaguchi A,Chester F M,Kimura G. 日本南海海槽俯冲增生楔前缘的构造变形特征[J]. 地球科学进展, 2010, 25(2): 203-211.
[13] 高金耀,吴招才,王健,杨春国,张涛. 南海北部陆缘磁静区及与全球大洋磁静区对比的研究评述[J]. 地球科学进展, 2009, 24(6): 577-588.
[14] 李春峰, 汪品先, Dieter Franke, 李家彪, Randell Stephenson, 许树坤,Peter Michael, 周祖翼,等. 南海张裂过程及其对晚中生代以来东南亚构造的启示-IODP建议书735-Full介绍[J]. 地球科学进展, 2009, 24(12): 1339-1351.
[15] 鲍颖,兰健,王毅. 南海在1997/1998年El Niño事件后的异常变化[J]. 地球科学进展, 2008, 23(10): 1027-1036.