ZHAO Xia, HUANG Peng, HU Ningjing, KONG Juanjuan, LIAO Renqiang, WANG Xiong. CHARACTERISTICS AND INFLUENCE FACTORS OF ELEMENT MIGRATION OF HYDROTHERMAL ALTERED ROCK IN EASTERN MANUS BASIN[J]. Marine Geology & Quaternary Geology, 2017, 37(3): 86-101. DOI: 10.16562/j.cnki.0256-1492.2017.03.009
Citation: ZHAO Xia, HUANG Peng, HU Ningjing, KONG Juanjuan, LIAO Renqiang, WANG Xiong. CHARACTERISTICS AND INFLUENCE FACTORS OF ELEMENT MIGRATION OF HYDROTHERMAL ALTERED ROCK IN EASTERN MANUS BASIN[J]. Marine Geology & Quaternary Geology, 2017, 37(3): 86-101. DOI: 10.16562/j.cnki.0256-1492.2017.03.009
shu

CHARACTERISTICS AND INFLUENCE FACTORS OF ELEMENT MIGRATION OF HYDROTHERMAL ALTERED ROCK IN EASTERN MANUS BASIN

  • 1.

    Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences

  • 2.

    University of Chinese Academy of Sciences, Beijing 100049

  • 3.

    Key Laboratory of Marine Sedimentary and Environmental Geology, the First Institute of Oceanography, State Oceanic Administration, Qingdao 266061

More Information
  • Received Date: July 17, 2016
  • Revised Date: November 21, 2016
    Graphical Abstract
    • Abstract
  • Five fresh and one altered volcanic rock samples from Eastern Manus Basin were chosen as research materials in this study. The major and trace elements of the bulk samples and the in-situ plagioclase of these rocks are analyzed. Comparative studies of altered rock and fresh rocks are carried out to explore the characteristics and influence factors of element migration during the hydrothermal alteration. As results, the hydrothermal sulfide of altered rock is a sort of copper-rich sulfide which mainly composed of chalcopyrite, sphalerite and ilmenite. Silicified alteration is the main type of alteration as the SiO2 content is extremely high in the altered area. The contents of major and trace elements of the altered rock change around the average of the content of basaltic andesite and dacite. Andesite is believed the protolith of the altered rock. During the process of hydrothermal alteration, the mass of the altered rock is increased by 150%. The altered rock is most enriched by the elements of Cu, Zn, Ga, Sr, Cd, Ba and Pb, enriched by Ti, V, Mn, Co, Ni, Mo and U, less enriched by Si and Fe, and least enriched by Sc, Cr, Nb, Ta, W and Bi. The altered rock is most depleted by Be and Ca, more depleted by Li, Na, Mg, K, Rb, REE and Y, and least depleted by Zr, Cs and Th. Al, P and Hf are immobile elements. The influence factors of element migration of the hydrothermal altered rock may include mineralization, metasomatism (such as chloritization and silicification) and the activity of elements in fluids.
    • FullText(HTML)
    • References (72)
  • [1]
    Yang K H, Scott S D.Possible contribution of a metal-rich magmatic fluid to a sea-floor hydrothermal system[J].Nature, 1996, 383(6599):420-423. doi: 10.1038/383420a0
    [2]
    Yang K H, Scott S D.Magmatic Fluids as a Source of Metals in Seafloor Hydrothermal Systems[M]//Christie D M, Fisher C R, Lee S M, et al. Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions. Washington, DC: American Geophysical Union, 2006: 163-184.
    [3]
    Sun W D, Arculus R J, Kamenetsky V S, et al.Release of gold-bearing fluids in convergent margin magmas prompted by magnetite crystallization[J].Nature, 2004, 431(7011):975-978. doi: 10.1038/nature02972
    [4]
    Simmons S F, Brown K L. Gold in magmatic hydrothermal solutions and the rapid formation of a giant ore deposit[J].Science, 2006, 314(5797):288-291. doi: 10.1126/science.1132866
    [5]
    Reeves E P, Seewald J S, Saccocia P, et al.Geochemistry of hydrothermal fluids from the PACMANUS, Northeast Pual and Vienna Woods hydrothermal fields, Manus Basin, Papua New Guinea[J].Geochimica et Cosmochimica Acta, 2011, 75(4):1088-1123. doi: 10.1016/j.gca.2010.11.008
    [6]
    de Ronde C E J. Fluid Chemistry and Isotopic Characteristics of Seafloor Hydrothermal Systems and Associated VMS Deposits: Potential for Magmatic Contributions[M]//Thompson J F H. Magmas, Fluids, and Ore Deposits. Canada: Mineralogical Association of Canada, 1995: 479-509.
    [7]
    Ishibashi J I, Urabe T. Hydrothermal Activity Related to Arc-backarc Magmatism in the Western Pacific[M]//Taylor B. Backarc Basins. New York, US: Springer, 1995: 451-495.
    [8]
    Kamenetsky V S, Binns R A, Gemmell J B, et al.Parental basaltic melts and fluids in eastern Manus backarc basin: implications for hydrothermal mineralisation[J].Earth and Planetary Science Letters, 2001, 184(3-4):685-702. doi: 10.1016/S0012-821X(00)00352-6
    [9]
    Park S H, Lee S M, Kamenov G D, et al.Tracing the origin of subduction components beneath the South East rift in the Manus Basin, Papua New Guinea[J].Chemical Geology, 2010, 269(3-4):339-349. doi: 10.1016/j.chemgeo.2009.10.008
    [10]
    Sinton J M, Ford L L, Chappell B, et al.Magma genesis and mantle heterogeneity in the Manus back-arc basin, Papua New Guinea[J].Journal of Petrology, 2003, 44(1):159-195. doi: 10.1093/petrology/44.1.159
    [11]
    Yang B J, Zeng Z G, Wang X Y, et al.Pourbaix diagrams to decipher precipitation conditions of Si-Fe-Mn-oxyhydroxides at the PACMANUS hydrothermal field[J].Acta Oceanologica Sinica, 2014, 33(12):58-66. doi: 10.1007/s13131-014-0572-9
    [12]
    Zeng Z G, Chen S, Wang X Y, et al.Mineralogical and micromorphological characteristics of Si-Fe-Mn oxyhydroxides from the PACMANUS hydrothermal field, Eastern Manus Basin[J].Science China Earth Sciences, 2012, 55(12):2039-2048. doi: 10.1007/s11430-012-4536-7
    [13]
    Zeng Z G, Ouyang H G, Yin X B, et al.Formation of Fe-Si-Mn oxyhydroxides at the PACMANUS hydrothermal field, Eastern Manus Basin: mineralogical and geochemical evidence[J].Journal of Asian Earth Sciences, 2012, 60: 130-146. doi: 10.1016/j.jseaes.2012.08.009
    [14]
    杨宝菊.东马努斯海盆PACMANUS热液区Si-Fe-Mn氧化物的形成机制及其对热液活动的指示[D].中国科学院(海洋研究所)硕士学位论文, 2015.

    YANG Baoju.The forming mechnism of Si-Fe-Mn oxides and implications for hydrothermal activity at the PACMANUS hydrothermal field, Eastern Manus Basin[D].Master's Thesis of Institute of Oceanology, Chinese Academy of Sciences, 2015.
    [15]
    杨宝菊, 曾志刚, 殷学博, 等.PACMANUS热液区Fe-Si-Mn羟基氧化物的成因及地球化学特征[J].海洋地质与第四纪地质, 2016, 36(3):69-80. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201603010

    YANG Baoju, ZENG Zhigang, YIN Xuebo, et al.The origin and geochemical characteristics of Fe-Si-Mn oxyhydroxides at PACMANUS hydrothermal field[J]. Marine Geology and Quaternary Geology, 2016, 36(3):69-80. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201603010
    [16]
    Beaudoin Y, Scott S D, Gorton M P, et al. Effects of hydrothermal alteration on Pb in the active PACMANUS hydrothermal field, ODP Leg 193, Manus Basin, Papua New Guinea: a LA-ICP-MS study[J].Geochimica et Cosmochimica Acta, 2007, 71(17):4256-4278. doi: 10.1016/j.gca.2007.06.034
    [17]
    Beaudoin Y, Scott S D. Pb in the PACMANUS sea-floor hydrothermal system, eastern Manus Basin: numerical modeling of a magmatic versus leached origin[J].Economic Geology, 2009, 104(5):749-758. doi: 10.2113/gsecongeo.104.5.749
    [18]
    Craddock P R, Bach W, Seewald J S, et al.Rare earth element abundances in hydrothermal fluids from the Manus Basin, Papua New Guinea: indicators of sub-seafloor hydrothermal processes in back-arc basins[J].Geochimica et Cosmochimica Acta, 2010, 74(19):5494-5513. doi: 10.1016/j.gca.2010.07.003
    [19]
    Pašava J, Vymazalová A, Petersen S, et al. PGE distribution in massive sulfides from the PACMANUS hydrothermal field, eastern Manus basin, Papua New Guinea: implications for PGE enrichment in some ancient volcanogenic massive sulfide deposits[J].Mineralium Deposita, 2004, 39(7):784-792. doi: 10.1007/s00126-004-0442-z
    [20]
    Moss R, Scott S D. Geochemistry and mineralogy of gold-rich hydrothermal precipitates from the eastern Manus Basin, Papua New Guinea[J].The Canadian Mineralogist, 2001, 39(4):957-978. doi: 10.2113/gscanmin.39.4.957
    [21]
    Sun W D, Binns R A, Fan A C, et al. Chlorine in submarine volcanic glasses from the eastern Manus basin[J].Geochimica et Cosmochimica Acta, 2007, 71(6):1542-1552. doi: 10.1016/j.gca.2006.12.003
    [22]
    马瑶.东马努斯弧后盆地岩浆岩地球化学特征及其对热液活动中Cu的物质供给研究[D].中国科学院(海洋研究所)博士学位论文, 2016.

    MA Yao. Geochemistry of igneous rocks and material contribution of Cu to seafloor hydrothermal system in eastern Manus Basin[D].Doctoral Dissertation of Institute of Oceanology, Chinese Academy of Sciences, 2016.
    [23]
    Fourre E, Jean-Baptiste P, Charlou J L, et al. Helium isotopic composition of hydrothermal fluids from the Manus back-arc Basin, Papua New Guinea[J].Geochemical Journal, 2006, 40(3):245-252. doi: 10.2343/geochemj.40.245
    [24]
    Kim J, Lee I, Lee K Y. S, Sr, and Pb isotopic systematics of hydrothermal chimney precipitates from the Eastern Manus Basin, western Pacific: evaluation of magmatic contribution to hydrothermal system[J].Journal of Geophysical Research, 2004, 109(B12), doi: 10.1029/2003JB002912.
    [25]
    Roberts S, Bach W, Binns R A, et al. Contrasting evolution of hydrothermal fluids in the PACMANUS system, Manus Basin: the Sr and S isotope evidence[J].Geology, 2003, 31(9):805-808. doi: 10.1130/G19716.1
    [26]
    Wilckens F, Kasemann S A, Bach W, et al. Boron and lithium isotope compositions of acid-sulfate fluids from the Eastern Manus Basin, Papua New Guinea[C]//Goldschmidt, 2015.
    [27]
    Scott S D, Binns R A. Hydrothermal processes and contrasting styles of mineralization in the western Woodlark and eastern Manus basins of the western Pacific[J]. Geological Society, London, Special Publications, 1995, 87(1):191-205. doi: 10.1144/GSL.SP.1995.087.01.16
    [28]
    Gemmell J B, Binns R A, Parr J M. Submarine, high sulfidation alteration within DESMOS caldera, Manus Basin, PNG[C]//Mineral Deposits: Processes to Processing: Fifth Biennial SGA Meeting and the Tenth Quadrennial IAGOD Symposium. Rotterdam: Balkema, 1999: 503-506.
    [29]
    Lackschewitz K S, Devey C W, Stoffers P, et al. Mineralogical, geochemical and isotopic characteristics of hydrothermal alteration processes in the active, submarine, felsic-hosted PACMANUS field, Manus Basin, Papua New Guinea[J].Geochimica et Cosmochimica Acta, 2004, 68(21):4405-4427. doi: 10.1016/j.gca.2004.04.016
    [30]
    Taylor B. Bismarck Sea: evolution of a back-arc basin[J].Geology, 1979, 7(4):171-174. doi: 10.1130/0091-7613(1979)7<171:BSEOAB>2.0.CO;2
    [31]
    Phinney E J, Mann P, Coffin M F, et al. Sequence stratigraphy, structure, and tectonic history of the southwestern Ontong Java Plateau adjacent to the North Solomon Trench and Solomon Islands Arc[J].Journal of Geophysical Research, 1999, 104(B9):20449-20466. doi: 10.1029/1999JB900169
    [32]
    Exon N F, Stewart W D, Sandy M J, et al. Geology and offshore petroleum prospects of the eastern New Ireland Basin, northeastern Papua New Guinea[J].BMR Journal of Australian Geology & Geophysics, 1986, 10(1):39-51.
    [33]
    Woodhead J D, Eggins S M, Johnson R W. Magma genesis in the New Britain island arc: further insights into melting and mass transfer processes[J].Journal of Petrology, 1998, 39(9):1641-1668. doi: 10.1093/petroj/39.9.1641
    [34]
    Martinez F, Taylor B. Backarc spreading, rifting, and microplate rotation, between transform faults in the Manus Basin[J].Marine Geophysical Researches, 1996, 18(2-4):203-224. doi: 10.1007/BF00286078
    [35]
    Both R, Crook K, Taylor B, et al. Hydrothermal chimneys and associated fauna in the Manus Back-Arc Basin, Papua New Guinea[J].EOS, Transactions American Geophysical Union, 1986, 67(21):489-490. doi: 10.1029/EO067i021p00489
    [36]
    Tufar W. Modern hydrothermal activity, formation of complex massive sulfide deposits and associated vent communities in the Manus back-arc basin (Bismarck Sea, Papua New Guinea)[J].Mitteilungen der österreichischen Geologischen Gesellschaft, 1989, 82:183-210.
    [37]
    Lisitsyn A P, Crook K A W, Bogdanov Y A, et al. A hydrothermal field in the rift zone of the Manus Basin, Bismarck Sea[J].International Geology Review, 1993, 35(2):105-126. doi: 10.1080/00206819309465517
    [38]
    Binns R A, Scott S D. Actively forming polymetallic sulfide deposits associated with felsic volcanic rocks in the eastern Manus back-arc basin, Papua New Guinea[J].Economic Geology, 1993, 88(8):2226-2236. doi: 10.2113/gsecongeo.88.8.2226
    [39]
    Binns R A, Barriga F J A S, Miller D J. Leg 193 synthesis: anatomy of an active felsic-hosted hydrothermal system, eastern Manus basin, Papua new guinea[C]//Proceedings of the Ocean Drilling Program Scientific Results.College Station, TX: Ocean Drilling Program, 2007: 1-71.
    [40]
    Gamo T, Sakai H, Ishibashi J, et al. Hydrothermal plumes in the eastern Manus Basin, Bismarck Sea: CH4, Mn, Al and ph anomalies[J].Deep Sea Research Part Ⅰ: Oceanographic Research Papers, 1993, 40(11-12):2335-2349. doi: 10.1016/0967-0637(93)90108-F
    [41]
    Gamo T, Okamura K, Charlou J L, et al. Acidic and sulfate-rich hydrothermal fluids from the Manus back-arc basin, Papua New Guinea[J].Geology, 1997, 25(2):139-142. doi: 10.1130/0091-7613(1997)025<0139:AASRHF>2.3.CO;2
    [42]
    Gamo T, Ishibashi J, Tsunogai U, et al. Unique geochemistry of submarine hydrothermal fluids from arc-back-arc settings of the Western Pacific[M]//Christie D M, Fisher C R, Lee S M, et al. Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions. Washington D C: American Geophysical Union, 2006: 147-161.
    [43]
    Auzende J M, Hashimoto J, Fiala-Médioni A, et al. In situ geological and biological study of two hydrothermal zones in the Manus Basin (Papua New Guinea)[J].Comptes Rendus de l'Académie des Sciences Séries IIA Earth and Planetary Sciences, 1997, 325(8):585-591.
    [44]
    Binns R A, Scott S D, Gemmell J B, et al. The SuSu Knolls hydrothermal field, eastern Manus Basin, Papua New Guinea[J].EOS, Transactions American Geophysical Union, 1997, 78:46. doi: 10.2113-gsecongeo.102.1.55/
    [45]
    Auzende J M, Ishibashi J, Beaudoin Y, et al. The eastern and western tips of Manus Basin (Papua, New Guinea) explored by submersible: MANAUTE cruise[J].Comptes Rendus de l'Académie des Sciences Séries IIA Earth and Planetary Sciences, 2000, 331(2):119-126.
    [46]
    Douville E, Bienvenu P, Charlou J L, et al. Yttrium and rare earth elements in fluids from various deep-sea hydrothermal systems[J].Geochimica et Cosmochimica Acta, 1999, 63(5):627-643. doi: 10.1016/S0016-7037(99)00024-1
    [47]
    黄朋.冲绳海槽火山活动及其构造意义[D].中国科学院(海洋研究所)博士学位论文, 2005.

    HUANG Peng. The volcanic activities and their implications in the Okinawa Trough[D]. Doctoral Dissertation of Institute of Oceanology, Chinese Academy of Sciences, 2005.
    [48]
    McDonough W F, Sun S S. The composition of the Earth[J]. Chemical Geology, 1995, 120(3-4):223-253. doi: 10.1016/0009-2541(94)00140-4
    [49]
    张德玉, 陈穗田, 王冠荣, 等.马里亚纳海槽热液硅质烟囱矿物学及地球化学研究[J].海洋学报, 1992, 14(4):61-68. doi: 10.1007/BF02677081

    ZHANG Deyu, CHEN Suitian, WANG Guanrong, et al.Mineralogy and geochemistry characteristic of silica chimney from hydrotherm area in Mariana Trench[J].Acta Oceanologica Sinica, 1992, 14(4):61-68. doi: 10.1007/BF02677081
    [50]
    曾志刚, 陈代庚, 殷学博, 等.东太平洋海隆13° N附近热液硫化物中的元素, 同位素组成及其变化[J].中国科学D辑:地球科学, 2009, 39(12):1780-1794. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd200912014

    ZENG Zhigang, CHEN Daigeng, YIN Xuebo, et al.Elemental and isotopic compositions of the hydrothermal sulfide on the East Pacific Rise near 13°N[J].Science China Earth Sciences, 2010, 53(2):253-266. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd200912014
    [51]
    陈永权, 蒋少涌, 周新源, 等.塔里木盆地寒武系层状硅质岩与硅化岩的元素, δ30Si, δ18O地球化学研究[J].地球化学, 2010, 39(2):159-170.

    CHEN Yongquan, JIANG Shaoyong, ZHOU Xinyuan, et al. δ30Si, δ18O and elements geochemistry on the bedded siliceous rocks and cherts in dolostones from Cambrian strata, Tarim Basin[J].Geochimica, 2010, 39(2):159-170.
    [52]
    赵珊茸.结晶学及矿物学[M].北京:高等教育出版社, 2004:385-392.

    ZHAO Shanrong. Crystallography and Mineralogy[M].Beijing: High Education Press, 2004:385-392.
    [53]
    祁冬梅, 周汉文, 宫勇军, 等.岩石热液蚀变作用过程元素的活动性——河南祁雨沟金矿Ⅳ号岩体蚀变花岗斑岩的研究[J].岩石学报, 2015, 31(9):2655-2673. http://www.ysxb.ac.cn/ysxb/ch/reader/key_query.aspx

    QI Dongmei, ZHOU Hanwen, GONG Yongjun, et al. Element mobility during the fluid-rock hydrothermal alteration: evidence from altered porphyritic granite in Ⅳ pipe of the Qiyugou gold deposit, Henan Province[J].Acta Petrologica Sinica, 2015, 31(9):2655-2673. http://www.ysxb.ac.cn/ysxb/ch/reader/key_query.aspx
    [54]
    Grant J A. The isocon diagram; a simple solution to Gresens' equation for metasomatic alteration[J].Economic Geology, 1986, 81(8):1976-1982. doi: 10.2113/gsecongeo.81.8.1976
    [55]
    Costa U R, Barnett R L, Kerrich R. The Mattagami Lake Mine Archean Zn-Cu sulfide deposit, Quebec; hydrothermal coprecipitation of talc and sulfides in a sea-floor brine pool; evidence from geochemistry, 18O/16O, and mineral chemistry[J].Economic Geology, 1983, 78(6):1144-1203. doi: 10.2113/gsecongeo.78.6.1144
    [56]
    Gong Q J, Deng J, Yang L Q, et al. Behavior of major and trace elements during weathering of sericite-quartz schist[J].Journal of Asian Earth Sciences, 2011, 42(1-2):1-13. doi: 10.1016/j.jseaes.2011.03.003
    [57]
    Troll V R, Sachs P M, Schmincke H U, et al. The REE-Ti mineral chevkinite in comenditic magmas from Gran Canaria, Spain: a SYXRF-probe study[J].Contributions to Mineralogy and Petrology, 2003, 145(6):730-741. doi: 10.1007/s00410-003-0475-9
    [58]
    Hynes A. Carbonatization and mobility of Ti, Y, and Zr in Ascot Formation metabasalts, SE Quebec[J].Contributions to Mineralogy and Petrology, 1980, 75(1):79-87. doi: 10.1007/BF00371891
    [59]
    陈子琪, 蒋少涌, 徐耀明, 等.江西九瑞矿集区郎君山第三纪玄武岩的成因与岩浆演化:来自辉石和长石的矿物学证据[J].岩石学报, 2015, 31(3):686-700. http://www.ysxb.ac.cn/ysxb/ch/reader/key_query.aspx

    CHEN Ziqi, JIANG Shaoyong, XU Yaoming, et al. Petrogenesis and magma evolution of Tertiary basalts from the Langjunshan area in the Jiurui mineralization district, Jiangxi Province: evidence from pyroxene and feldspar[J].Acta Petrologica Sinica, 2015, 31(3):686-700. http://www.ysxb.ac.cn/ysxb/ch/reader/key_query.aspx
    [60]
    MacLean W H, Kranidiotis P. Immobile elements as monitors of mass transfer in hydrothermal alteration; Phelps Dodge massive sulfide deposit, Matagami, Quebec[J].Economic Geology, 1987, 82(4):951-962. doi: 10.2113/gsecongeo.82.4.951
    [61]
    刘英俊.元素地球化学[M].北京:科学出版社, 1984.

    LIU Yingjun. Geochemistry of Elements[M].Beijing: Science Press, 1984.
    [62]
    杨超, 唐菊兴, 王艺云, 等.西藏铁格隆南浅成低温热液型-斑岩型Cu-Au矿床流体及地质特征研究[J].矿床地质, 2014, 33(6): 1287-1305. doi: 10.3969/j.issn.0258-7106.2014.06.009

    YANG Chao, TANG Juxing, WANG Yiyun, et al. Fluid and geological characteristics researches of Southern Tiegelong epithemal porphyry Cu-Au deposit in Tibet[J]. Mineral Deposits, 2014, 33(6): 1287-1305. doi: 10.3969/j.issn.0258-7106.2014.06.009
    [63]
    薛春纪, 赵晓波, 莫宣学, 等.西天山巨型金铜铅锌成矿带构造成矿演化和找矿方向[J].地质学报, 2014, 88(12):2490-2531. doi: 10.3969/j.issn.0001-5717.2014.12.025

    XUE Chunji, ZHAO Xiaobo, MO Xuanxue, et al. tectonic-metallogenic evolution of Western Tianshan Giant Au-Cu-Zn-Pb metallogenic belt and prospecting orietation[J].Acta Geologica Sinica, 2014, 88(12):2490-2531. doi: 10.3969/j.issn.0001-5717.2014.12.025
    [64]
    Humphris S E, Thompson G. Trace element mobility during hydrothermal alteration of oceanic basalts[J].Geochimica et Cosmochimica Acta, 1978, 42(1):127-136. doi: 10.1016/0016-7037(78)90222-3
    [65]
    Juteau T, Noack Y, Whitechurch H. Mineralogy and geochemistry of alteration products in holes 417a and 417d basement samples (Deep Sea Drilling Project Leg 51)[J].1979, 53(2): 1273-1297.
    [66]
    Ludden J N, Thompson G. An evaluation of the behavior of the rare earth elements during the weathering of sea-floor basalt[J].Earth and Planetary Science Letters, 1979, 43(1):85-92. doi: 10.1016/0012-821X(79)90157-2
    [67]
    Morgan J W, Wandless G A. Rare earth element distribution in some hydrothermal minerals: evidence for crystallographic control[J].Geochimica et Cosmochimica Acta, 1980, 44(7):973-980. doi: 10.1016/0016-7037(80)90286-0
    [68]
    Exley R A. Microprobe studies of REE-rich accessory minerals: implications for Skye granite petrogenesis and REE mobility in hydrothermal systems[J].Earth and Planetary Science Letters, 1980, 48(1):97-110. doi: 10.1016/0012-821X(80)90173-9
    [69]
    Vidal P, Cocherie A, Le Fort P. Geochemical investigations of the origin of the Manaslu leucogranite (Himalaya, Nepal)[J].Geochimica et Cosmochimica Acta, 1982, 46(11):2279-2292. doi: 10.1016/0016-7037(82)90201-0
    [70]
    Campbell I H, Coad P, Franklin J M, et al. Rare earth elements in volcanic rocks associated with Cu-Zn massive sulphide mineralization: a preliminary report[J].Canadian Journal of Earth Sciences, 1982, 19(3):619-623. doi: 10.1139/e82-049
    [71]
    Campbell I H, Lesher C M, Coad P, et al. Rare-earth element mobility in alteration pipes below massive Cu-Zn-sulfide deposits[J].Chemical Geology, 1984, 45(3-4):181-202. doi: 10.1016/0009-2541(84)90036-6
    [72]
    Lottermoser B G. Rare earth element study of exhalites within the Willyama supergroup, Broken Hill Block, Australia[J].Mineralium Deposita, 1989, 24(2):92-99. doi: 10.1007/BF00206309
    • Related Articles

  • Related Articles

    [1]BI Yuntian, HU Rijun, CHEN Juanjuan, LI Yi, YI Zhaohan, CHEN Xiaoci, ZHU Longhai, YIN Yanjun, LIU Bo. Suspended sediment grain size and influencing factors in Funing Bay and its nearby sea areas[J]. Marine Geology & Quaternary Geology, 2024, 44(1): 15-29. DOI: 10.16562/j.cnki.0256-1492.2023010902
    [2]LEI Zhiyu, LIU Rongbo, HU Rijun, QIU Jiandong, ZHU Longhai, ZHU Feng, ZHANG Xiaodong. Controlling factors and distribution of geochemical characteristics of the surface sediments in the Yellow River Delta[J]. Marine Geology & Quaternary Geology, 2022, 42(6): 104-118. DOI: 10.16562/j.cnki.0256-1492.2022041301
    [3]QIU Yan, DU Wenbo, HUANG Wenkai, WANG Yingmin, NIE Xin. Stratigraphic features and controlling factors in the eastern Sub-basin of the Central Basin, South China Sea during the post-spreading period[J]. Marine Geology & Quaternary Geology, 2020, 40(5): 1-14. DOI: 10.16562/j.cnki.0256-1492.2020053001
    [4]CHENG Ke, WANG Qing, ZHENG Zhihui, ZHAN Chao, ZHOU Houyun, CHI Hong. Seasonal variations in trace elements and influencing factors in drip water from Kaiyuan Cave, Shandong Province[J]. Marine Geology & Quaternary Geology, 2019, 39(1): 154-162. DOI: 10.16562/j.cnki.0256-1492.2017032801
    [5]ZHANG Huaijing, ZHAI Shikui, ZHOU Yonghua, YU Zenghui. DISTRIBUTIONS OF MERCURY AND METHYLMERCURY IN SEDIMENTS OF MIN-ZHE COASTAL AREA AND INFLUENCING FACTORS[J]. Marine Geology & Quaternary Geology, 2016, 36(6): 163-174. DOI: 10.16562/j.cnki.0256-1492.2016.06.019
    [6]CHEN Zhiqiang, ZHOU Huaiyang, YAO Huiqiang, LIU Yang, YANG Qunhui, LI Jie, LI Jiwei, SUN Zhilei. THE INFLUENCE OF MAGMATIC PROCESS AND HYDROTHERMAL ALTERATION ON THE GEOCHEMICAL CHARACTERISTICS OF ABYSSAL PERIDOTITES[J]. Marine Geology & Quaternary Geology, 2013, 33(5): 73-80. DOI: 10.3724/SP.J.1140.2013.05073
    [7]SHAO Hebin, FAN Dejiang, MAI Xiaolei, ZHANG Jing, LI Qing. TYPES AND SIZE OF SUSPENDED PARTICLES IN A TYPICAL CROSS SECTION AT THE CHANGJIANG ESTUARY AND INFLUENCE FACTORS[J]. Marine Geology & Quaternary Geology, 2013, 33(3): 47-56. DOI: 10.3724/SP.J.1140.2013.03047
    [8]LIANG Jie, WEN Zhenhe, XIAO Guolin, ZHANG Yinguo, DONG Heping. RESERVOIR CHARACTERISTICS AND INFLUENTIAL FACTORS IN THE EASTERN DEPRESSION OF THE NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2013, 33(2): 111-119. DOI: 10.3724/SP.J.1140.2013.02111
    [9]JING Chunlei, ZHENG Yanpeng, LIU Baohua, CUI Yingchun. DISTRIBUTION PATTERN OF SUBMARINE HYDROTHERMAL SULFIDE DEPOSITS AND CONTROLLING FACTORS[J]. Marine Geology & Quaternary Geology, 2013, 33(1): 57-64. DOI: 10.3724/SP.J.1140.2013.01057
    [10]TIAN Qingchun, YANG Taibao, SHI Peihong, ZHU Heyong, ZHANG Shuxin. ENVIRONMENTAL IMPLICATION OF COLOR REFLECTANCE OF DRILL HOLE BDQ0608, KEKE XILI REGION AND ITS INFLUENCING FACTORS[J]. Marine Geology & Quaternary Geology, 2012, 32(1): 133-140. DOI: 10.3724/SP.J.1140.2012.01133

Catalog

    Get Citation
    PDF
    XML
    Article views (2705) PDF downloads (15) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return