[1]马万伟,黄小龙,于 洋.2020.栗木花岗岩中云母的特征: 对锡成矿热液作用过程的指示.大地构造与成矿学,44(6):1143-1142.doi:10.16539/j.ddgzyckx.2020.06.008
 MA Wanwei,HUANG Xiaolong,YU Yang.2020.Characteristics of Micas in the Limu Granites, South China: An Indicator of the Hydrothermal Processes Related to Tin Mineralization.Geotectonica et Metallogenia,44(6):1143-1142.doi:10.16539/j.ddgzyckx.2020.06.008
点击复制

栗木花岗岩中云母的特征: 对锡成矿热液作用过程的指示
分享到:

《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2020年44卷06期
页码:
1143-1142
栏目:
构造地质与成矿学
出版日期:
2020-12-20

文章信息/Info

Title:
Characteristics of Micas in the Limu Granites, South China: An Indicator of the Hydrothermal Processes Related to Tin Mineralization
文章编号:
1001-1552(2020)06-1143-017
作者:
马万伟1、2 黄小龙1* 于 洋1 尹 蓉1 贺鹏丽1
1.中国科学院 广州地球化学研究所, 同位素地球化学国家重点实验室, 广东 广州 510640; 2.中国科学院大学, 北京100049
Author(s):
MA Wanwei1、2 HUANG Xiaolong1* YU Yang1 YIN Rong1 and HE Pengli1
1. State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China; 2. University of Chinese Academy of Sciences, Beijing 100049, China
关键词:
云母 岩浆演化 热液作用 锡矿 稀有金属花岗岩 华南
Keywords:
mica magmatic evolution hydrothermal process tin mineralization rare-metal granite South China
分类号:
P575; P612
DOI:
10.16539/j.ddgzyckx.2020.06.008
文献标志码:
A
摘要:
南岭西段栗木锡铌钽矿的形成与花岗岩岩浆演化及热液作用过程密切相关。老虎头矿区的黑鳞云母花岗岩和锂白云母花岗岩具有高硅、富碱、强过铝质的特征, 其全岩稀土元素含量极低, 微量元素蛛网图显示强烈的Eu、Sr、Ba负异常, 指示均为高演化花岗岩, 经历了显著的长石结晶分异作用。老虎头花岗岩的稀土元素配分曲线呈现出明显的稀土四分组效应, 指示岩浆演化晚期强烈的热液作用。黑鳞云母花岗岩样品的云母从早阶段黑鳞云母变化至晚阶段锂白云母。锂白云母花岗岩的锂白云母普遍发育环带结构, 边部为白云母, 应与岩浆演化后期强烈的热液作用相关。黑鳞云母到锂白云母以及环带结构云母的核部到边部其F、Li、Rb、Cs含量均明显降低, 表明主要为外来流体参与了热液作用过程。稀有金属花岗岩的岩浆演化?热液作用过程中, W、Sn、Nb、Ta等稀有金属元素具有明显不同的地球化学行为, Sn的富集与岩浆高演化有关。老虎头矿区从黑鳞云母花岗岩到锂白云母花岗岩, 云母的Fe3+/Fe2+值升高, 且环带结构云母从核部到边部的Fe3+/Fe2+值明显升高, 表明热液作用下体系的氧逸度增加可能是导致Sn沉淀的重要机制。
Abstract:
The Limu Sn-Nb-Ta deposit is closely related to granitic magma evolution and hydrothermal processes. The protolithionite granite and lithium muscovite granite in Laohutou are high-silic, alkali-enriched and strongly peraluminous. They have extremely low whole-rock contents of rare earth elements, and show strong negative Eu, Sr and Ba anomalies on the upper crust-normalized trace element spider diagrams due to significant fractional crystallization of feldspars. In addition, they have strong REE tetrad effect, indicating the remarkable hydrothermal activities during the late stage magmatic evolution. Micas in the granite samples change in species from the early protolithionite to the late lithium muscovite, and those in the lithium muscovite granite samples commonly show zoning texture with muscovite rim, which should be related to strong hydrothermal activities during the late stage magmatic evolution. F, Li, Rb and Cs contents of the micas decrease notably from protolithionite to lithium muscovite in species and from core to rim in zoned micas, indicative of involvement of exotic hydrothermal fluids. During the magmatic evolution and hydrothermal processes of the rare-metal granites, W, Sn, Nb and Ta show distinct geochemical behaviors, and Sn was concentrated in the melt via high differentiation. In addition, the Fe3+/Fe2+ ratios of micas increase from the protolithionite granite to the lithium muscovite granite, while Fe3+/Fe2+ ratios of the zoned micas increase from core to rim, indicating that the rise of oxygen fugacity in the hydrothermal fluid is crucial to the final deposit of Sn minerals.

参考文献/References:

陈骏. 2000. 锡的地球化学. 南京: 南京大学出版社: 1- 320.
陈骏, 陆建军, 陈卫锋, 王汝成, 马东升, 朱金初, 张文兰, 季峻峰. 2008. 南岭地区钨锡铌钽花岗岩及其成矿作用. 高校地质学报, 14(4): 459-473.
陈骏, 王汝成, 朱金初, 陆建军, 马东升. 2014. 南岭多时代花岗岩的钨锡成矿作用. 中国科学: 地球科学, 44(1): 111-121.
董业才, 丁汝福. 2016. 广西栗木矿田花岗岩体地球化学特征制约因素及其动力学背景. 矿产与地质, 30(6): 998-1005.
董业才, 庄晓蕊. 2014. 广西栗木花岗岩岩石地球化学特征及其构造环境. 矿产与地质, 28(5): 596-604.
甘晓春, 朱金初, 沈渭洲. 1992. 广西栗木水溪庙稀有金属花岗岩成因. 地质找矿论丛, 7(2): 35-45.
韩丽, 黄小龙, 李洁, 贺鹏丽, 姚军明. 2016. 江西大湖塘钨矿花岗岩的磷灰石特征及其氧逸度变化指示. 岩石学报, 32(3): 746-758.
胡欢, 王汝成, 张爱铖, 黄小龙, 刘昌实, 徐士进. 2003. 江西雅山黄玉锂云母花岗岩中铯矿物的电子探针研究. 地球化学, 32(1): 63-75.
蒋少涌, 赵葵东, 姜耀辉, 凌洪飞, 倪培. 2006. 华南与花岗岩有关的一种新类型的锡成矿作用矿物化学、元素和同位素地球化学证据. 岩石学报, 22(10): 2509-2516.
康志强, 冯佐海, 杨锋, 廖家飞, 潘会彬. 2012. 广西桂林地区东部栗木花岗岩体SHRIMP锆石U-Pb年龄. 地质通报, 31(8): 1306-1312.
李洁. 2015. 华南中生代稀有金属花岗岩岩浆演化与热液过程的矿物学约束. 北京: 中国科学院大学博士学位论文: 51-54.
李洁, 黄小龙. 2013. 江西雅山花岗岩岩浆演化及其Ta-Nb富集机制. 岩石学报, 29(12): 4311-4322.
李胜虎, 李建康, 张德会, 万贵龙. 2015. 广西栗木钽铌锡多金属矿床的成矿流体演化及其对成矿过程的制约. 岩石学报, 31(4): 954-966.
梁玲慧, 彭振安, 汪明, 长尾敬介, 蔡明海, 郭腾飞, 刘虎, 程柳. 2013. 广西栗木锡铌钽矿田成矿物质来源的惰性气体同位素示踪. 矿床地质, 32(2): 397-404.
梁玲慧, 彭振安, 汪明, 张芳, 刘虎, 郭腾飞, 黄敦杰. 2012. 广西栗木锡铌钽多金属矿床成矿流体包裹体特征. 矿产与地质, 26(6): 502-510.
林文蔚, 彭丽君. 1994. 由电子探针分析数据估算角闪石、黑云母中的Fe3+、Fe2+. 吉林大学学报, 24(2): 155- 162.
刘昌实, 陈小明, 王汝成, 张文兰, 胡欢. 2005. 广东南昆山A型花岗岩定年和环带云母研究. 地质论评, 51(2): 193-200.
刘翔, 彭振安, 庞文聪, 曹江帅, 张文兵, 李强, 薛彦萍, 韦干华. 2016. 广西栗木钨锡铌钽矿区流体包裹体及氢氧同位素研究. 地质与勘探, 52(6): 1016-1028.
刘颖, 刘海臣, 李献华. 1996. 用ICP-MS准确测定岩石样品中的40余种微量元素. 地球化学, 25(6): 552-558.
娄峰, 伍静, 陈国辉. 2014. 广西栗木泡水岭印支期岩体LA-ICP-MS锆石U-Pb年龄及其地质意义. 地质通报, 33(7): 960-965.
毛景文, 谢桂青, 郭春丽, 陈毓川. 2007. 南岭地区大规模钨锡多金属成矿作用: 成矿时限及地球动力学背景. 岩石学报, 23(10): 2329-2338.
毛景文, 谢桂青, 郭春丽, 袁顺达, 程彦博, 陈毓川. 2008. 华南地区中生代主要金属矿床时空分布规律和成矿环境. 高校地质学报, 14(4): 510-526.
涂湘林, 张红, 邓文峰, 凌明星, 梁华英, 刘颖, 孙卫东. 2011. RESOlution激光剥蚀系统在微量元素原位微区分析中的应用. 地球化学, 40(1): 83-98.
张怀峰, 陆建军, 王汝成, 马东升, 朱金初, 章荣清. 2014. 广西栗木大岐岭隐伏花岗岩的成因及其构造意义: 岩石地球化学、锆石U-Pb年代学和Nd-Hf同位素制约. 中国科学: 地球科学, 44(5): 901-918.
张怀峰, 陆建军, 王汝成, 章荣清. 2013. 广西栗木矿区牛栏岭岩体印支期年龄的厘定及其意义. 高校地质学报, 19(2): 220-232.
Audétat A, Günther D and Heinrich C A. 2000. Magmatic- hydrothermal evolution in a fractionating granite: A microchemical study of the Sn-W-F-mineralized Mole Granite (Australia). Geochimica et Cosmochimica Acta, 64(19): 3373-3393.
Bai T B and Van Groos A K. 1999. The distribution of Na, K, Rb, Sr, Al, Ge, Cu, W, Mo, La, and Ce between granitic melts and coexisting aqueous fluids. Geochimica et Cosmochimica Acta, 63(7-8): 1117-1131.
Ballouard C, Branquet Y, Tartese R, Poujol M, Boulvais P and Vigneresse J L. 2016. Nb-Ta fractionation in peraluminous granites: A marker of the magmatic- hydrothermal transition. Geology, 44(7): 395.
Breiter K, ?uri?ová J, Hrstka T, Korbelová Z, Vaňková M H, Galiová M V, Kanick? V, Rambousek P, Knésl I, Dobe? P and Dosbaba M. 2017. Assessment of magmatic vs. metasomatic processes in rare-metal granites: A case study of the Cínovec/Zinnwald Sn-W-Li deposit, Central Europe. Lithos, 292-293: 198-217.
Chevychelov V Y, Zaraisky G P, Borisovskii S E and Borkov D A. 2005. Effect of melt composition and temperature on the partitioning of Ta, Nb, Mn, and F between granitic (alkaline) melt and fluorine-bearing aqueous fluid: Fractionation of Ta and Nb and conditions of ore formation in rare-metal granites. Petrology, 13(4): 305-321.
Cuney M, Marignac C and Weisbrod A. 1992. The Beauvoir topaz-lepidolite albite granite (Massif Central, France): The disseminated magmatic Sn-Li-Ta-Nb-Be mineralization. Economic Geology, 87(7): 1766-1794.
F?rster H J. 1999. The chemical composition of uraninite in Variscan granites of the Erzgebirge, Germany. Minera?lo-gical Magazine, 63(2): 239-252.
Foster M D. 1960. Interpretation of the composition of lithium micas. United States Geological Survey Professional Paper, 354-E: 115-147.
Fu M, Kwak T A P and Mernagh T P. 1993. Fluid inclusion studies of zoning in the Dachang tin-polymetallic ore field, People’s Republic of China. Economic Geology, 88(2): 283-300.
Gysi A and Williams J A. 2013. Hydrothermal mobilization of pegmatite-hosted REE and Zr at Strange Lake, Canada: A reaction path model. Geochimica et Cosmo?chimica Acta, 122: 324-352.
Heinrich C A. 1990. The chemistry of hydrothermal tin(-tungsten) ore deposition. Economic Geology, 85(3): 457-481.
Heinrich C A and Eadington P J. 1986. Thermodynamic predictions of the hydrothermal chemistry of arsenic, and their significance for the paragenetic sequence of some cassiterite-arsenopyrite-base metal sulfide deposits. Economic Geology, 81(3): 511-529.
Henry D J, Guidotti X V and Thomson J A. 2005. The Ti-saturation surface for low-to-medium pressure metapelitic biotites: Implications for geothermometry and Ti-substitution mechanisms. American Mineralogist, 90(2-3): 316-328.
Hu R Z and Zhou M F. 2012. Multiple Mesozoic mineralization events in South China — An intro?du?ction to the thematic issue. Mineralium Deposita, 47(6): 579-588.
Irber W. 1999. The lanthanide tetrad effect and its correlation with K/Rb, Eu/Eu*, Sr/Eu, Y/Ho, and Zr/Hf of evolving peraluminous granite suites. Geochimica et Cosmochi?mica Acta, 63(3-4): 489-508.
Kelly W C and Turneaure F S. 1970. Mineralogy, paragenesis and geothermometry of the tin and tungsten deposits of the eastern Andes, Bolivia. Economic Geology, 65(6): 609-680.
Kempe U, G?tze J, Dandar S and Habermann D. 1999. Magmatic and metasomatic processes during formation of the Nb-Zr-REE deposits Khaldzan Buregte and Tsakhir (Mongolian Altai): Indications from a combined CL-SEM study. Mineralogical Magazine, 63(2): 165-177.
Keppler H and Wyllie P J. 1991. Partitioning of Cu, Sn, Mo, W, U, and Th between melt and aqueous fluid in the systems haplogranite-H2O-HCl and haplogranite-H2O- HF. Contributions to Mineralogy and Petrology, 109(2): 139-150.
Legros H, Marignac C, Mercadier J, Cuney M, Richard A, Wang R C, Charles N and Lespinasse M Y. 2016. Detailed paragenesis and Li-mica compositions as recorders of the magmatic-hydrothermal evolution of the Maoping W-Sn deposit (Jiangxi, China). Lithos, 264: 108-124.
Legros H, Marignac C, Tabary T, Mercadier J, Richard A, Cuney M, Wang R C, Charles N and Lespinasse M Y. 2018. The ore-forming magmatic-hydrothermal system of the Piaotang W-Sn deposit (Jiangxi, China) as seen from Li-mica geochemistry. American Mineralogist, 103(1): 39-54.
Legros H, Richard A, Tarantola A, Kouzmanov K, Mercadier J, Vennemann T, Marignac C, Cuney M, Wang R C, Charles N, Bailly L and Lespinasse M Y. 2019. Multiple fluids involved in granite-related W-Sn deposits from the world-class Jiangxi province (China). Chemical Geology, 508: 92-115.
Lehmann B. 1982. Metallogeney of tin: Magmatic differentiation versus geochemical heritage. Economic Geology, 77(1): 50-59.
Lehmann B. 1987. Tin granites, geochemical heritage, magmatic differentiation. Geologische Rundschau, 76(1): 177-185.
Lehmann B. 1990. Large-scale tin depletion in the Tanjung-pandan tin granite, Belitung Island, Indonesia. Economic Geology, 85(1): 99-111.
Li J, Huang X L, He P L, Li W X, Yu Y and Chen L L. 2015. In situ analyses of micas in the Yashan granite, South China: Constraints on magmatic and hydrothermal evolutions of W and Ta-Nb bearing granites. Ore Geology Reviews, 65: 793-810.
Li Z X, Li X H, Wartho J A, Clark C, Li W X, Zhang C L and Bao C D. 2010. Magmatic and metamorphic events during the early Paleozoic Wuyi-Yunkai orogeny, southeastern South China: New age constraints and pressure-temperature conditions. Geological Society of America Bulletin, 122(5-6): 772-793.
Van Lichtervelde M, Grégoire M, Linnen R L, Béziat D and Salvi S. 2008. Trace element geochemistry by laser ablation ICP-MS of micas associated with Ta mineralization in the Tanco pegmatite, Manitoba, Canada. Contributions to Mineralogy and Petrology, 155(6): 791-806.
Linnen R L and Cuney M. 2005. Granite-related rare-element deposits and experimental constraints on Ta-Nb-W-Sn- Zr-Hf mineralization. Rare-element geochemistry and mineral deposits. Geological Association of Canada Short Course Notes, 17: 45-67.
Linnen R L, Pichavant M and Holtz F. 1996. The combined effects of fO2 and melt composition on SnO2 solubility and tin diffusivity in haplogranitic melts. Geochimica et Cosmochimica Acta, 60(24): 4965-4976.
Linnen R L, Pichavant M, Holtz F and Burgess S. 1995. The effect of ?O2 on the solubility, diffusion, and speciation of tin in haplogranitic melt at 850 ℃ and 2 kbar. Geochimica et Cosmochimica Acta, 59(8): 1579-1588.
Linnen R L, Samson I, Williams-Jones A and Chakhmouradian A R. 2014. Geochemistry of the rare-earth element, Nb, Ta, Hf, and Zr deposits // Treatise on Geochemistry (Second Edition): 543-568.
Liu Y, Cheng Q M, Xia Q L and Wang X Q. 2014. Mineral potential mapping for tungsten polymetallic deposits in the Nanling metallogenic belt, South China. Journal of Earth Science, 25(4): 689-700.
Liu Y S, Hu Z C, Gao S, Günther D, Xu J, Gao C G and Chen H H. 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology, 257(1): 34-43.
Mao J W, Cheng Y B, Chen M H and Pirajno F. 2013. Major types and time-space distribution of Mesozoic ore deposits in South China and their geodynamic settings. Mineralium Deposita, 48(3): 267-294.
Masuda A, Kawakami O, Dohmoto Y and Takenaka T. 1987. Lanthanide tetrad effects in nature: Two mutually opposite types, W and M. Geochemical Journal, 21(3): 119-124.
Monier G and Robert J L. 1986. Evolution of the miscibility gap between muscovite and biotite solid solutions with increasing lithium content: An experimental study in the system K2O-Li2O-MgO-FeO-Al2O3-SiO2-H2O-HF at 600 ℃, 2 kbar PH2O: Comparison with natural lithium micas. Mineralogical Magazine, 50: 641-651.
Munoz J L. 1984. F-OH and Cl-OH exchange in micas with applications to hydrothermal ore deposits. Mineralogical Society of America Reviews in Mineralogy, 13: 469- 493.
Neiva A M R. 2013. Micas, feldspars and columbite-tantalite minerals from the zoned granitic lepidolite-subtype pegmatite at Namivo, Alto Ligonha, Mozambique. European Journal of Mineralogy, 25(6): 967-985.
Pouchou J L and Pichoir F. 1991. Quantitative analysis of homogeneous or stratified microvolumes applying the model “PAP” // Electron Probe Quantitation: 31-75.
Roda E, Keller P, Pesquera A and Fontan F. 2007. Micas of the muscovite-lepidolite series from Karibib pegmatites, Namibia. Mineralogical Magazine, 71(1): 41-62.
Rudnick R L and Gao S. 2003. Composition of the continental crust // Rudnick R L. Treatise on Geochemistry. Oxford: Elsevier, 3: 1-64.
Schmidt C. 2018. Formation of hydrothermal tin deposits: Raman spectroscopic evidence for an important role of aqueous Sn(IV) species. Geochimica et Cosmochimica Acta, 220: 499-511.
Stepanov A, Mavrogenes J A, Meffre S and Davidson P. 2014. The key role of mica during igneous concentration of tantalum. Contributions to Mineralogy and Petrology, 167(6): 1009.
Taylor S R and Mclennan S M. 1985. The continental crust: Its composition and evolution, an examination of the geochemical record preserved in sedimentary rocks. Journal of Geology, 94(4): 632-633.
Tindle A G and Webb P C. 1990. Estimation of lithium contents in trioctahedral micas using microprobe data: Application to micas from granitic rocks. European Journal of Mineralogy, 2(5): 595-610.
Tischendorf G, Gottesmann B, Forster H J and Trumbull R B. 1997. On Li-bearing micas: Estimating Li from electron microprobe analyses and an improved diagram for graphical representation. Mineralogical Magazine, 61: 809-834.
Wilson G A and Eugster H P. 1990. Cassiterite solubility and tin speciation in supercritical chloride solutions. Fluid- Mineral Interactions: A tribute to HP Eugster, 2: 179-195.
Wu F Y, Liu X C, Ji W Q, Wang J M and Yang L. 2017. Highly fractionated granites: Recognition and research. Science China: Earth Sciences, 60(7): 1201-1219.
Xie L, Wang R C, Che X D, Huang F F, Erdmann S and Zhang W L. 2016. Tracking magmatic and hydrothermal Nb-Ta-W-Sn fractionation using mineral textures and composition: A case study from the late Cretaceous Jiepailing ore district in the Nanling Range in South China. Ore Geology Reviews, 78: 300-321.
Xie L, Wang R C, Chen J and Zhu J C. 2010. Mineralogical evidence for magmatic and hydrothermal processes in the Qitianling oxidized tin-bearing granite (Hunan, South China): EMP and (MC)-LA-ICPMS investigations of three types of titanite. Chemical Geology, 276: 53-68.
Xie L, Wang R C, Groat L A, Zhu J C, Huang F F and Cempírek J. 2015. A combined EMPA and LA-ICP-MS study of Li-bearing mica and Sn-Ti oxide minerals from the Qiguling topaz rhyolite (Qitianling District, China): The role of fluorine in origin of tin mineralization. Ore Geology Reviews, 65: 779-792.
Xie Y W. 2002. Petrogenic implication of the characteristics of micas in shoshonitic rocks in eastern Qinghai-Tibet Plateau. Acta Petrologica Sinica, 18: 205-211.
Yin L, Pollard P J, Hu S X and Taylor R G. 1995. Geologic and geochemical characteristics of the Yichun Ta-Nb-Li deposit, Jiangxi Province, South China. Economic Geology, 90(3): 577-585.
Yin R, Han L, Huang X L, Li J, Li W X and Chen L L. 2019. Textural and chemical variations of micas as indicators for tungsten mineralization: Evidence from highly evolved granites in the Dahutang tungsten deposit, South China. American Mineralogist, 104(7): 949-965.
Zajacz Z, Halter WE, Pettke T and Guillong M. 2008. Determination of fluid/melt partition coefficients by LA-ICPMS analysis of co-existing fluid and silicate melt inclusions: Controls on element partitioning. Geochimica et Cosmochimica Acta, 72(8): 2169-2197.
Zaraisky G P, Korzhinskaya V and Kotova N. 2010. Experimental studies of Ta2O5 and columbite-tantalite solubility in fluoride solutions from 300 to 550 C and 50 to 100 MPa. Mineralogy and Petrology, 99(3-4): 287-300.
Zhao Z H, Xiong X L, Han X D, Wang Y X, Wang Q, Bao Z W and Jahn B. 2002. Controls on the REE tetrad effect in granites: Evidence from the Qianlishan and Baerzhe Granites, China. Geochemical Journal, 36(6): 527-543.
Zhu J C, Li R K, Li F C, Xiong X L, Zhou F Y and Huang X L. 2001. Topaz-albite granites and rare-metal mineralization in the Limu district, Guangxi Province, Southeast China. Mineralium Deposita, 36(5): 393-405.

相似文献/References:

[1]王亚磊,李文渊,张照伟.新疆圪塔山口含铜镍岩体锆石SHRIMP U-Pb年龄、岩石地球化学特征及其地质意义.大地构造与成矿学,2016.4(6):1275.doi:10.16539/j.ddgzyckx.2016.06.014
 WANG Yalei,LI Wenyuan,ZHANG Zhaowei.Geochronological and Geochemical Characteristics of Getashankou Cu-Ni Bearing Intrusion in Eastern Tianshan, Xinjiang and its Geological Significance.Geotectonica et Metallogenia,2016.44(6):1275.doi:10.16539/j.ddgzyckx.2016.06.014
[2]焦建刚,马泽民,鲁浩.阿拉善地块南缘野芨里镁铁-超镁铁质岩体锆石U-Pb年龄及其地质意义.大地构造与成矿学,2017.41(5):950.doi:10.16539/j.ddgzyckx.2017.05.011
 JIAO Jiangang,MA Zemin,LU Hao.Zircon U-Pb Dating of Yejili Mafic-ultramafic Intrusion in Southern Margin of Alxa Block, and its Geological Implication.Geotectonica et Metallogenia,2017.44(6):950.doi:10.16539/j.ddgzyckx.2017.05.011
[3]丁 一,刘吉强,李正刚.橄榄石及其熔体包裹体地球化学约束冲绳海槽岩浆水含量.大地构造与成矿学,2020.44(6):1208.doi:10.16539/j.ddgzyckx.2020.06.012
 DING Yi,LIU Jiqiang,LI Zhenggang.Geochemical Constraints on the H2O Contents of Magmas from the Okinawa Trough: A Study of Olivine and Melt Inclusions.Geotectonica et Metallogenia,2020.44(6):1208.doi:10.16539/j.ddgzyckx.2020.06.012

备注/Memo

备注/Memo:
收稿日期: 2019-08-28; 改回日期: 2019-10-21
项目资助: 国家重点研发计划课题(2016YFC600204)和国家自然科学基金项目(41625007、U1701641)联合资助。
第一作者简介: 马万伟(1993-), 男, 硕士研究生, 矿物学、岩石学、矿床学专业。Email: mawanwei@gig.ac.cn
通信作者: 黄小龙(1972-), 研究员, 博士生导师, 从事岩石地球化学研究。Email: xlhuang@gig.ac.cn
更新日期/Last Update: 2020-12-20