必须声明标量变量 "@Script_ID"。 西准噶尔巴音布拉克花岗斑岩成因:岩石地球化学、年代学与Sr-Nd-Hf同位素证据-《地球科学与环境学报》
|本期目录/Table of Contents|

[1]刘朕语,李光来*,刘晓东,等.西准噶尔巴音布拉克花岗斑岩成因:岩石地球化学、年代学与Sr-Nd-Hf同位素证据[J].地球科学与环境学报,2019,41(06):658-674.
 LIU Zhen-yu,LI Guang-lai*,LIU Xiao-dong,et al.Petrogenesis of Bayinbulake Granite Porphyry in West Junggar, China: Evidences from Petrogeochemistry, Geochronology and Sr-Nd-Hf Isotopes[J].Journal of Earth Sciences and Environment,2019,41(06):658-674.
点击复制

西准噶尔巴音布拉克花岗斑岩成因:岩石地球化学、年代学与Sr-Nd-Hf同位素证据(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第41卷
期数:
2019年第06期
页码:
658-674
栏目:
基础地质与矿产地质
出版日期:
2019-11-15

文章信息/Info

Title:
Petrogenesis of Bayinbulake Granite Porphyry in West Junggar, China: Evidences from Petrogeochemistry, Geochronology and Sr-Nd-Hf Isotopes
文章编号:
1672-6561(2019)06-0658-17
作者:
刘朕语1李光来1*刘晓东1陈光旭1王果2宋佳2
(1. 东华理工大学 核资源与环境国家重点实验室,江西 南昌 330013; 2. 核工业二一六大队,新疆 乌鲁木齐 830011)
Author(s):
LIU Zhen-yu1LI Guang-lai1*LIU Xiao-dong1 CHEN Guang-xu1WANG Guo2SONG Jia2
(1. State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, Jiangxi, China; 2. No.216 Geological Party, China Nuclear Geology, Urumqi 830011, Xinjiang, China)
关键词:
年代学 岩石地球化学 岩石成因 花岗斑岩 巴音布拉克岩体 杨庄岩体 雪米斯坦成矿带 西准噶尔
Keywords:
geochronology pretrogeochemistry petrogenesis granite porphyry Bayinbulake pluton Yangzhuang pluton Xuemisitan metallogenic belt West Jungger
分类号:
P588.12+1; P597
DOI:
-
文献标志码:
A
摘要:
西准噶尔雪米斯坦成矿带是中国重要的铀多金属成矿带,带内分布有大量古生代中酸性侵入岩体,这些岩体为探索雪米斯坦成矿带古生代岩浆活动及其构造演化提供了重要依据。巴音布拉克花岗斑岩岩体位于该成矿带东南部。对该花岗斑岩开展了系统的岩相学、锆石U-Pb年代学、岩石地球化学和Sr-Nd-Hf同位素研究。结果表明:该岩体形成于(393.7±1.7)Ma(MSWD值为1.3),属于早泥盆世,侵入于志留系雪米斯坦组地层中; 在主量元素组成上,巴音布拉克花岗斑岩具有高Si、贫水、高Al、富碱(特别是富K)以及低Mg和Ca的特征,属准铝质—过铝质A2亚型花岗岩; 微量元素组成上,岩石富集Rb、Th、U等,亏损Sr、P、Ti等,球粒陨石标准化稀土元素配分模式整体呈轻稀土元素相对富集的右倾模式,轻、重稀土元素分馏明显,稀土元素总含量较高且具有较为明显的Eu负异常; εNd(t)为4.3~6.7,变化范围很小,说明岩浆相对均一,二阶段Nd模式年龄为591~788 Ma,εHf(t)为3.98~9.35,二阶段Hf模式年龄为794~1 130 Ma,成岩物质可能来自于新元古代的亏损地幔。综上所述,巴音布拉克花岗斑岩是在俯冲环境下地幔发生部分熔融,并在沿俯冲带上升过程中混入了少量古老地壳物质形成的。通过与雪米斯坦成矿带西部杨庄岩体对比,巴音布拉克岩体具有形成工业性铀矿的前景。
Abstract:
Xuemisitan metallogenic belt in West Junggar is an important Chinese uranium polymetallic metallogenic belt with the massively distributed Paleozoic intermediate-acid intrusive plutons. These plutons provide an important basis for the exploration of Paleozoic magmatism and tectonic evolution of Xuemisitan metallogenic belt. The petrography, zircon U-Pb geochronology, petrogeochemistry and Sr-Nd-Hf isotopes of Bayinbulake granite porphyry in the southeastern margin of Xuemisitan metallogenic belt were studied systematically. The results show that the granite porphyry is formed in(393.7±1.7)Ma(MSWD is 1.3), belonging to Early Devonian, and invades into Silurian Xuemisitan Formation; the granite porphyry is characterized by high Si, poor H2O, high Al, rich alkali(especially K), low Mg and Fe, belonging to metaluminous-peraluminous series A2 sub-type granite; the granite porphyry is enriched in Rb, Th, U, etc., and depleted in Sr, P, Ti, etc., chondrite-normalized REE pattern is a right-leaning type with relative rich LREE, and the granite porphyry has the characteristics of obvious LREE and HREE fractionation, higher contents of total REE, and apparent Eu negative anomaly; the variation range of Nd isotopic composition is small, εNd(t)is 4.3-6.7 with the two-stage Nd model age of 591-788 Ma, indicating that the magma is relatively homogeneous, and εHf(t)is 3.98-9.35 with the two-stage Hf model age of 794-1 130 Ma, indicating that the diagenetic material maybe come from Neoproterozoic depleted mantle. In general, Bayinbulake pluton is formed in subduction setting, which causes partial melting of the mantle, and is mixed with a small amount of ancient crustal material during the rising along the subduction zone. Compared with Yangzhuang pluton, Bayinbulake pluton has the prospect of forming industrial uranium deposits.

参考文献/References:

[1] 胡霭琴,张国新,陈义兵,等.新疆大陆基底分区模式和主要地质事件的划分[J].新疆地质,2001,19(1):12-19.
HU Ai-qin,ZHANG Guo-xin,CHEN Yi-bing,et al.A Model of Division of the Continental Crust Basement and the Time Scales of the Major Geological Events in the Xinjiang[J].Xinjiang Geology,2001,19(1):12-19.
[2] 陈家富,韩宝福,张 磊.西准噶尔北部晚古生代两期侵入岩的地球化学、Sr-Nd 同位素特征及其地质意义[J].岩石学报,2010,26(8):2317-2335.
CHEN Jia-fu,HAN Bao-fu,ZHANG Lei.Geochemi-stry,Sr-Nd Isotopes and Tectonic Implications of Two Generations of Late Paleozoic Plutons in Northern West Junggar,Northwest China[J].Acta Petrologica Sinica,2010,26(8):2317-2335.
[3] 高 睿,肖 龙,王国灿,等.西准噶尔晚古生代岩浆活动和构造背景[J].岩石学报,2013,29(10):3413-3434.
GAO Rui,XIAO Long,WANG Guo-can,et al.Paleozoic Magmatism and Tectonic Setting in West Junggar[J].Acta Petrologica Sinica,2013,29(10):3413-3434.
[4] 李锦轶,何国琦,徐 新,等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报,2006,80(1):148-168.
LI Jin-yi,HE Guo-qi,XU Xin,et al.Crustal Tectonic Framework of Northern Xinjiang and Adjacent Regions and Its Formation[J].Acta Geologica Sinica,2006,80(1):148-168.
[5] 王 谋,李晓峰,王 果,等.新疆雪米斯坦火山岩带白杨河铍铀矿床地质特征[J].矿产勘查,2012,3(1):34-40.
WANG Mou,LI Xiao-feng,WANG Guo,et al.Geological Characteristics of Baiyanghe Beryllium-uranium Deposits in Xuemisitan Volcanic Belt,Xinjiang[J].Mineral Exploration,2012,3(1):34-40.
[6] 尹继元,陈 文,袁 超,等.新疆西准噶尔晚古生代侵入岩的年龄和构造意义:来自锆石LA-ICPMS定年的证据[J].地球化学,2013,42(5):414-429.
YIN Ji-yuan,CHEN Wen,YUAN Chao,et al.Ages and Tectonic Implication of Late Paleozoic in the West Junggar,North Xinjiang:Evidence from LA-ICPMS Zircon Geochronology[J].Geochimica,2013,42(5):414-429.
[7] MAO W,LI X F,WANG G,et al.Petrogenesis of the Yangzhuang Nb- and Ta-rich A-type Granite Porphyry in West Junggar,Xinjiang,China[J].Lithos,2014,198/199:172-183.
[8] LI X F,WANG G,MAO W,et al.Fluid Inclusions,Muscovite Ar-Ar Age,and Fluorite Trace Elements at the Baiyanghe Volcanic Be-U-Mo Deposit,Xinjiang,Northwest China:Implication for Its Genesis[J].Ore Geology Reviews,2015,64:387-399.
[9] 陈光旭,李光来,刘晓东,等.西准噶尔白杨河矿床沥青铀矿的矿物特征及形成环境[J].地质学报,2019,93(4):865-878.
CHEN Guang-xu,LI Guang-lai,LIU Xiao-dong,et al.Mineralogical Characteristic and Formation Environment of Pitchblende in the Baiyanghe Uranium Depo-sit in West Junggar[J].Acta Geologica Sinica,2019,93(4):865-878.
[10] 孙远强,范洪海,薛春纪,等.新疆谢米斯台成矿带火山岩型铀矿预测[J].矿床地质,2017,36(3):611-622.
SUN Yuan-qiang,FAN Hong-hai,XUE Chun-ji,et al.Metallogenic Prediction of Volcanic Type Uranium Re-sources in Xiemisitai Metallogenic Belt,Xinjiang[J].Mineral Deposits,2017,36(3):611-622.
[11] CHEN J F,HAN B F,JI J Q,et al.Zircon U-Pb Ages and Tectonic Implications of Paleozoic Plutons in Northern West Junggar,Nouth Xinjiang,China[J].Lithos,2009,115(1/2/3/4):137-152.
[12] 童 英,王 涛,洪大卫,等.北疆及邻区石炭—二叠纪花岗岩时空分布特征及其构造意义[J].岩石矿物学杂志,2010,29(6):619-641.
TONG Ying,WANG Tao,HONG Da-wei,et al.Spatial and Temporal Distribution of the Carboniferous-Permian Granitoids in Northern Xinjiang and Its Adjacent Areas,and Its Tectonic Significance[J].Acta Petrologica et Mineralogica,2010,29(6):619-641.
[13] 宋 佳.2015年巴音布拉克地区铀-多金属矿预查年度报告[R].乌鲁木齐:核工业二一六大队,2015.
SONG Jia.2015 Annual Report on Uranium-polymetallic Deposits in the Bayinbulake Area[R].Urumqi:No.216 Geological Party,China Nuclear Geology,2015.
[14] LIU Y S,HU Z C,ZONG K Q,et al.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS[J].Chinese Science Bulletin, 2010,55(15):1535-1546.
[15] LUDWIG K R.User's Manual for Isoplot 4.15:A Geochronological Toolkit for Microsoft Excel[R].Berkeley:Berkeley Geochronology Center,2012.
[16] VERVOORT J D,PATCHETT P J,SODERLUND U,et al.Isotopic Composition of Yb and the Determination of Lu Concentrations and Lu/Hf by Isotope Dilution Using MC-ICPMS[J].Geochemistry,Geophysics,Geosystems,2004,DOI:org/10.1029/2004GC000721.
[17] 陈光旭.西准噶尔白杨河铀矿床地质特征及成因探讨[D].南昌:东华理工大学,2018.
CHEN Guang-xu.Discussion on Geological Characte-ristics and Genesis of the Baiyanghe Uranium Deposit in Western Junggar[D].Nanchang:East China University of Technology,2018.
[18] 苏 晔.赣中聚源钨矿花岗斑岩地球化学特征及其地质意义[D].南昌:东华理工大学,2017.
SU Ye.Geochemical Characteristics of Granite Porphyry from Juyuan Tungsten Deposit in Central of Jiangxi Province and Its Geological Implications[D].Nanchang:East China University of Technology,2017.
[19] 陈瑞莉,潘家永,伍俊杰,等.皖南泾县茂林岩体锆石U-Pb年龄和Hf同位素特征[J].地质通报,2019,38(7):1219-1227.
CHEN Rui-li,PAN Jia-yong,WU Jun-jie,et al.A Study of Zircon U-Pb Age and Characteristics of Hf Isotopes of the Maolin Granodiorite in Jingxian County,Southern Anhui Province[J].Geological Bulletin of China,2019,38(7):1219-1227.
[20] IRBER W.The Lanthanide Tetrad and Its Correlation with K/Rb,Eu/Eu*,Sr/Eu,Y/Ho,and Zr/Hf of Evo-lving Peraluminous Granites[J].Geochimica et Cosmochimica Acta,1999,63(3/4):489-508.
[21] AURISICCHIO C,DEVITO C,FERRINI V,et al.Nb-Ta Oxide Minerals from Miarolitic Pegmatites of the Baveno Pink Granite,NW Italy[J].Mineralogical Magazine,2001,65(4):509-522.
[22] ERLANK A J,SMITH H S,MARCHANT J W,et al.Zirconium,Abundance in Rock Forming Minerals,Phase Equilibria,Zirconium Minerals[M]∥WEDEPOHL K H.Handbook of Geochemistry.Berlin:Springer-Verlag,1978:40-51.
[23] MIDDLERMOST E A K.Namin Materials in the Magma/Igneous Rock System[J].Earth-science Reviews,1994,37:215-224.
[24] MANIAR P D,PICCOLI P M.Tectonic Discrimination of Granitoids[J].Geological Society of America Bulletin,1989,101(5):635-643.
[25] COLLINS W J,BEAMS S D,WHITE A J R,et al.Nature and Origin of A-type Granites with Particular Reference to Southeastern Australia[J].Contributions to Mineralogy and Petrology,1982,80(2):189-200.
[26] PECCERILLO A,TAYLOR S R.Geochemistry of Eocene Calcalkaline Volcanic Rocks from the Kast Amonu Area,Northern Turkey[J].Contributions to Mineralogy and Petrology,1976,58(1):63-81.
[27] MCDONOUGH W F,SUN S S.The Composition of the Earth[J].Chemical Geology,1995,120(3/4):223-253.
[28] TAYLOR S R,MCLENNAN S M.The Continental Crust:Its Composition and Evolution[M].London:Blackwell,1985.
[29] 吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589-1604.
WU Yuan-bao,ZHENG Yong-fei.Study on Zircon in Mineralogy and the Constraints on the Interpretation of U-Pb Ages[J].Chinese Science Bulletin,2004,49(16):1589-1604.
[30] 黄鹏辉,陈宣华,王志宏,等.西准噶尔成矿带晚古生代花岗岩类岩浆活动及其构造意义[J].大地构造与成矿学,2016,40(1):145-160.
HUANG Peng-hui,CHEN Xuan-hua,WANG Zhi-hong,et al.Late Paleozoic Granitic Magmatism in West Junggar Metallogenic Belt(Xinjiang),Central Asia,and Its Tectonic Implication[J].Geotectonica et Metallogenia,2016,40(1):145-160.
[31] 吴福元,李献华,郑永飞,等.Lu-Hf同位素体系及其岩石学应用[J].岩石学报,2007,23(2):185-220.
WU Fu-yuan,LI Xian-hua,ZHENG Yong-fei,et al.Lu-Hf Isotopic Systematics and Their Applications in Petrology[J].Acta Petrologica Sinca,2007,23(2):185-220.
[32] 杨 钢,肖 龙,王国灿,等.西准噶尔谢米斯台西段花岗岩年代学、地球化学、锆石Lu-Hf同位素特征及大地构造意义[J].地球科学,2015,40(3):548-562.
YANG Gang,XIAO Long,WANG Guo-can,et al.Geo-chronology,Geochemistry and Zircon Lu-Hf Study of Granites in Western Section of Xiemisitai Area,Western Junggar[J].Earth Science,2015,40(3):548-562.
[33] LOISELLE M C,WONES D R.Characteristics and Origin of Anorogenic Granites[J].Abstracts with Programs,Geological Society of America,1979,11(7):468.
[34] WHALEN J B,CURRIE K L,CHAPPELL B W.A-type Granites:Geochemical Characteristics,Discrimination and Petrogenesis[J].Contributions to Minera-logy and Petrology,1987,95(4):407-419.
[35] EBY G N.Chemical Subdivision of the A-type Grani-toids:Petrogenetic and Tectonic Implications[J].Geo-logy,1992,20(7):641-644.
[36] 洪大卫,王式洸,韩宝福,等.碱性花岗岩的构造环境分类及其鉴别标志[J].中国科学:B辑,1995,25(4):418-426.
HONG Da-wei,WANG Shi-guang,HAN Bao-fu,et al.Classification and Identification of the Tectonic Environment of Alkaline Granite[J].Science in China:Series B,1995,25(4):418-426.
[37] PEARCE J A,HARRIS N B W,TINDLE A G.Trace Element Discrimination Diagrams for the Tecronic Interpretation of Granitic Rocks[J].Journal of Petrology,1984,25(4):956-983.
[38] 刘昌实,陈小明,陈培荣,等.A型岩套的分类、判别标志和成因[J].高校地质学报,2003,9(4):573-591.
LIU Chang-shi,CHEN Xiao-ming,CHEN Pei-rong,et al.Subdivision,Discrimination Criteria and Genesis for A-type Rock Suites[J].Geological Journal of China Universities,2003,9(4):573-591.
[39] VERVOORT J D,PATCHETT P J,BLICHERT-TOFT J,et al.Relationships Between Lu-Hf and Sm-Nd Isotopic Systems in the Global Sedimentary System[J].Earth and Planetary Science Letters,1999,168(1/2):79-99.
[40] BARTH M G,MCDONOUGH W F,RUDNICK R L.Tracking the Budget of Nb and Ta in the Continental Crust[J].Chemical Geology,2000,165(3/4):197-213.
[41] GREEN T H,PEARSON N J.An Experimental Study of Nb and Ta Partitioning Between Ti-rich Minerals and Silicate Liquids at High Pressure and Temperature[J].Geochimica et Cosmochimica Acta,1987,51(1):55-62.
[42] CHEN B,ARAKAWA Y.Elemental and Nd-Sr Isotopic Geochemistry of Granitoids from the West Junggar Foldbelt(NW China),with Implications for Phanerozoic Continental Growth[J].Geochimica et Cosmochimica Acta,2005,69(5):1307-1320.
[43] 徐 新,何国琦,李华芹,等.克拉玛依蛇绿混杂岩带的基本特征和锆石SHRIMP年龄信息[J].中国地质,2006,33(3):470-475.
XU Xin,HE Guo-qi,LI Hua-qin,et al.Basic Characteristics of the Karamay Ophiolitic Melange,Xinjiang,and Its Zircon SHRIMP Dating[J].Geology in China,2006,33(3):470-475.
[44] 韩宝福,季建清,宋 彪,等.新疆准噶尔晚古生代陆壳垂向生长:后碰撞深成岩浆活动的时限[J].岩石学报,2006,22(5):1077-1086.
HAN Bao-fu,JI Jian-qing,SONG Biao,et al.Late Paleozoic Vertical Growth of Continental Crust Around the Junggar Basin,Xinjiang,China:Timing of Post-collisional Plutonism[J].Acta Petrologica Sinica,2006,22(5):1077-1086.
[45] 刘朕语.西准噶尔巴音布拉克花岗斑岩地质地球化学特征及其指示意义[D].南昌:东华理工大学,2018.
LIU Zhen-yu.Geological and Geochemical Characte-ristics of the Bayinbulake Granite Porphyry in West Junggar and Its Indicative Significance[D].Nanchang:East China University of Technology,2018.
[46] 刘朕语,陈光旭.西准噶尔地区主要金属矿床概论[J].世界有色金属,2018(4):163-165.
LIU Zhen-yu,CHEN Guang-xu.An Introduction to the Main Metal Deposits in West Junggar Region[J].World Nonferrous Metals,2018(4):163-165.
[47] 陈光旭,李光来,刘晓东,等.西准噶尔白杨河铀矿床沥青铀矿矿物特征及形成环境[J].地质学报,2019,93(4):865-878.
CHEN Guang-xu,LI Guang-lai,LIU Xiao-dong,et al.Mineralogical Characteristics and Formation Environment of Pitchblende in the Baiyanghe Uranium Depo-sit in West Junggar[J].Acta Geologica Sinica,2019,93(4):865-878.
[48] XIAO W J,HAN C M,YUAN C,et al.Middle Cambrian to Permian Subduction-related Accretionary Orogenesis of Northern Xinjiang,NW China:Implications for the Tectonic Evolution of Central Asia[J].Journal of Asian Earth Sciences,2008,32(2/3/4):102-117.
[49] 徐 新,周可法,王 煜.西准噶尔晚古生代残余洋盆消亡时间与构造背景研究[J].岩石学报,2010,26(11):3206-3214.
XU Xin,ZHOU Ke-fa,WANG Yu.Study on Extinction of the Remnant Oceanic Basin and Tectonic Setting of West Junggar During Late Paleozoic[J].Acta Petrologica Sinica,2010,26(11):3206-3214.
[50] 杨 维,王国灿,纵瑞文,等.西准噶尔志留纪—泥盆纪弧盆格局的确定及其区域构造演化意义[J].地球科学,2015,40(3):448-503.
YANG Wei,WANG Guo-can,ZONG Rui-wen,et al.Determination of Silurian-Devonian Arc-basin Pattern in Western Jungger and Its Regional Tectonic Significance[J].Earth Science,2015,40(3):448-503.
[51] GILL J B.Orogenic Andesites and Plate Tectonics[M].Berlin:Springer-Verlag,1981.
[52] THIRLWALL M F,SMITH T E,GRAHAM A M,et al.High Field Strength Element Anomalies in Arc Lavas:Source or Process?[J].Journal of Petrology,1994,35(3):819-838.

相似文献/References:

[1]周争艳,杨家喜,徐涛,等.西秦岭天水地区早中生代草川铺花岗岩年代学、地球化学特征及其地质意义[J].地球科学与环境学报,2015,37(02):11.
 ZHOU Zheng-yan,YANG Jia-xi,XU Tao,et al.Geochronological and Geochemical Characteristics of Early Mesozoic Caochuanpu Granitoids in Tianshui Area of West Qinling and Their Geological Significance[J].Journal of Earth Sciences and Environment,2015,37(06):11.
[2]高景刚,梁婷,李文渊,等.新疆额尔齐斯韧性剪切带新生锆石及其年代学意义[J].地球科学与环境学报,2015,37(04):15.
 GAO Jing-gang,LIANG Ting,LI Wen-yuan,et al.Neogenic Zircons in Ertix Ductile Shear Zone of Xinjiang and Their Geochronological Significance[J].Journal of Earth Sciences and Environment,2015,37(06):15.
[3]孙会一,石玉若,赵希涛,等.北京密云地区早白垩世花岗岩SHRIMP锆石U-Pb年龄及其地质意义[J].地球科学与环境学报,2016,38(01):43.
 SUN Hui-yi,SHI Yu-ruo,ZHAO Xi-tao,et al.SHRIMP Zircon U-Pb Ages of Early Cretaceous Granites in Miyun Area of Beijing and Their Geological Significance[J].Journal of Earth Sciences and Environment,2016,38(06):43.
[4]肖荣,李晓峰,王翠云,等.江西德兴地区朱砂红斑岩铜矿成岩成矿年代学特征及其地质意义[J].地球科学与环境学报,2016,38(01):55.
 XIAO Rong,LI Xiao-feng,WANG Cui-yun,et al.Diagenetic and Metallogenic Geochronological Characteristics of Zhushahong Porphyry Copper Deposit in Dexing Area of Jiangxi and Its Implications[J].Journal of Earth Sciences and Environment,2016,38(06):55.
[5]侯晨阳,杨天水,石玉若.大别超高压变质带榴辉岩中金红石SHRIMP原位U-Pb定年及其年代学意义[J].地球科学与环境学报,2016,38(03):334.
 HOU Chen-yang,YANG Tian-shui,SHI Yu-ruo.In-situ SHRIMP U-Pb Dating of Rutiles in Eclogite from Dabie UHP Metamorphic Belt and Its Geochronological Significance[J].Journal of Earth Sciences and Environment,2016,38(06):334.
[6]师震,陈宏骏,钱壮志*,等.东天山红石岗镁铁—超镁铁质岩体成因及铜镍成矿潜力[J].地球科学与环境学报,2019,41(02):156.
 SHI Zhen,CHEN Hong-jun,QIAN Zhuang-zhi*,et al.Genesis and Cu-Ni Metallogenetic Potential of Hongshigang Mafic-ultramafic Intrusion in East Tianshan, China[J].Journal of Earth Sciences and Environment,2019,41(06):156.
[7]张忠利,杨成栋*,张斌,等.新疆阿尔泰克兰盆地泥盆纪花岗岩年代学特征及其地质意义[J].地球科学与环境学报,2019,41(04):414.
 ZHANG Zhong-li,YANG Cheng-dong*,ZHANG Bin,et al.Geochronological Characteristics of Devonian Granitoids in Kelan Basin of Altay, Xinjiang, China and Their Geological Implications[J].Journal of Earth Sciences and Environment,2019,41(06):414.

备注/Memo

备注/Memo:
收稿日期:2019-05-31; 修回日期:2019-07-18投稿网址:http:∥jese.chd.edu.cn/
基金项目:中国核工业地质局研究项目(2110400024); 国家自然科学基金项目(41862004,41972071)
作者简介:刘朕语(1992-),男,山东菏泽人,理学硕士研究生,E-mail:liuzhenyuldd@sina.com。
*通讯作者:李光来(1983-),男,江苏连云港人,副教授,工学博士,E-mail:liguanglaia886@163.com。
更新日期/Last Update: 2019-11-19