|Table of Contents|

Geochronology of Huangmeijian Composite Pluton in Middle-lower Yangtze River Valley Metallogenic Belt, China: Implications on the Petrogenesis and Metallogeny(PDF)

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

Issue:
2022年第02期
Page:
220-242
Research Field:
基础地质与矿床地质
Publishing date:

Info

Title:
Geochronology of Huangmeijian Composite Pluton in Middle-lower Yangtze River Valley Metallogenic Belt, China: Implications on the Petrogenesis and Metallogeny
Author(s):
ZHANG Shu1; 2; 3;  ZHOU Tao-fa3*;  ZHANG Zan-zan2;  LYU Bo2;  SHI Li-sheng4;  WANG Jing2;  WU Ming-an1; 2
(1. MNR Technology Innovation Center of Coverage Area Deep Resource Exploration Engineering, Geological Survey of Anhui Province, Hefei 230001, Anhui, China; 2. Anhui Institute of Geological Sciences, Hefei 230001, Anhui, China; 3. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, Anhui, China; 4. Anhui Nuclear Exploration Technology Central Institute, Wuhu 241000, Anhui, China)
Keywords:
composite pluton;  A-type granite;  zircon U-Pb age;  geochronology;  uranium deposit;  intrusive rock;  Middle-lower Yangtze River valley metallogenic belt;  Anhui
PACS:
P571; P597
DOI:
10.19814/j.jese.2021.10002
Abstract:
Huangmeijian composite pluton is a uranium-bearing A-type granite in Middle-lower Yangtze River valley metallogenic belt. Huangmeijian composite pluton can be divided into four emplacement stages from earliest to latest, including stage Ⅰ biotite quartz syenite, stage Ⅱ syenite porphyry, stage Ⅲ quartz syenite and stage Ⅳ alkali feldspar granite. The vein-type uranium mineralization predominantly occurs along the contacts between the stage Ⅰ biotite quartz syenite and the clastic rocks. The study on the micro-textures, REE characteristics and U-Pb dating of zircons in Huangmeijian composite pluton was carried out. The results show that the zircons of biotite quartz syenite, syenite porphyry and quartz syenite are of magmatic genesis, and yield zircon U-Pb ages of(131.8±1.1),(129.7±1.6),(124.7±1.6)Ma, respectively. The cores of zircons in alkali feldspar granite are of magmatic genesis and undergo metamictization, while the rims of zircons in alkali feldspar granite are altered by hydrothermal fluid, and probably undergo recrystallization. The zircon U-Pb dating of alkali feldspar granite yields the crystallization age of(111.5±1.3)Ma and the hydrothermal activity age of(107.6±2.1)Ma. Based on the previous geochronological studies, the A-type granites in Middle-lower Yangtze River valley metallogenic belt can be divided into three periods. The early period is represented by biotite quartz syenite and syenite porphyry with crystallization age of 132-129 Ma; the main period is represented by quartz syenite and syenogranite with crystallization age of 128-124 Ma; the late period is represented by alkali feldspar granite with crystallization age of 115-110 Ma. The crystallization ages of alkali feldspar granite and hydrothermal activity time are close to the uranium mineralization ages; combining with the stable isotope studies, it probably indicates that stage Ⅳ alkali feldspar granite of Huangmeijian composite pluton has provided the ore-forming fluid and heat for the uranium mineralization.

References:

[1] 常印佛,刘湘培,吴言昌.长江中下游铜铁成矿带[M].北京:地质出版社,1991.
CHANG Yin-fo,LIU Xiang-pei,WU Yan-chang.The Copper-iron Belt of the Lower and Middle Reaches of the Changjiang River[M].Beijing:Geological Publishing House,1991.
[2] 翟裕生,姚书振,林新多,等.长江中下游地区铁铜(金)成矿规律[M].北京:地质出版社,1992.
ZHAI Yu-sheng,YAO Shu-zhen,LIN Xin-duo,et al.Fe-Cu-Au Metallogeny of the Middle-lower Chang-jiang Region[M].Beijing:Geological Publishing Hou-se,1992.
[3] 周涛发,范 裕,王世伟,等.长江中下游成矿带成矿规律和成矿模式[J].岩石学报,2017,33(11):3353-3372.
ZHOU Tao-fa,FAN Yu,WANG Shi-wei,et al.Me-tallogenic Regularity and Metallogenic Model of the Middle-lower Yangtze River Valley Metallogenic Belt[J].Acta Petrologica Sinica,2017,33(11):3353-3372.
[4] 周涛发,范 裕,袁 峰,等.庐枞盆地侵入岩的时空格架及其对成矿的制约[J].岩石学报,2010,26(9):2694-2714.
ZHOU Tao-fa,FAN Yu,YUAN Feng,et al.Temporal-spatial Framework of Magmatic Intrusions in Luzong Volcanic Basin in East China and Their Constrain to Mineralizations[J].Acta Petrologica Sinica,2010,26(9):2694-2714.
[5] 张赞赞,张 舒,吴明安,等.庐枞盆地小包庄铁矿床地质特征及40Ar-39Ar同位素年代学研究[J].矿床地质,2017,36(4):795-815.
ZHANG Zan-zan,ZHANG Shu,WU Ming-an,et al.Geological Characteristics and 40Ar-39Ar Geochrono-logy of Xiaobaozhuang Iron Deposit in Luzong Volcanic Basin[J].Mineral Deposits,2017,36(4):795-815.
[6] 范 裕,周涛发,袁 峰,等.安徽庐江—枞阳地区A型花岗岩的LA-ICP-MS定年及其地质意义[J].岩石学报,2008,24(8):1715-1724.
FAN Yu,ZHOU Tao-fa,YUAN Feng,et al.LA-ICP-MS Zircon U-Pb Ages of the A-type Granites in the Luzong(Lujiang-Zongyang)Area and Their Geologi-cal Significances[J].Acta Petrologica Sinica,2008,24(8):1715-1724.
[7] WU F Y,JI W Q,SUN D H,et al.Zircon U-Pb Geochronology and Hf Isotopic Compositions of the Me-sozoic Granites in Southern Anhui Province,China[J].Lithos,2012,150:6-25.
[8] 贾丽琼,徐文艺,吕庆田,等.庐枞盆地砖桥地区科学深钻岩浆岩LA-MC-ICP MS锆石U-Pb年代学和岩石地球化学特征[J].岩石学报,2014,30(4):995-1016.
JIA Li-qiong,XU Wen-yi,LV Qing-tian,et al.LA-MC-ICP MS Zircon U-Pb Geochronology and Petrological Geochemistry of Scientific Deep Drilling in Zhuanqiao,Lujiang-Zongyang Volcanic Basin[J].Acta Petrologica Sinica,2014,30(4):995-1016.
[9] 营俊龙.8412铀矿床沥青铀矿的稀土和锶、钕同位素研究[J].铀矿地质,1991,7(3):146-152.
YING Jun-long.A Study of Rare Earth Elements and Sr,Nd Isotopic Compositions of Pitchblende in Uranium Deposit No.8412[J].Uranium Geology,1991,7(3):146-152.
[10] 张祖还,沈渭洲,闵茂中.8411铀矿床成因的稳定同位素研究[J].放射性地质,1983(4):12-17.
ZHANG Zu-huan,SHEN Wei-zhou,MIN Mao-zhong.Study on the Stable Isotope of No.8411 Uranium Deposit[J].Rediation Geology,1983(4):12-17.
[11] 闵茂中.8411铀矿床的矿化特征[J].南京大学学报(自然科学版),1982,18(4):928-938.
MIN Mao-zhong.The Mineralization Feature of No.8411 Uranium Deposit[J].Journal of Nanjing University(Natural Science),1982,18(4):928-938.
[12] 朱杰辰,郑懋公,营俊龙,等.大龙山、昆山铀矿床稳定同位素地质特征研究[J].铀矿地质,1992,8(2):338-347.
ZHU Jie-chen,ZHENG Mao-gong,YING Jun-long,et al.A Study on Geological Characteristics of Stable Isotopes in Dalongshan and Kunshan Uranium Depo-sits[J].Uranium Geology,1992,8(2):338-347.
[13] 林冠英.苏皖沿江铀成矿地质特征及找矿方向探讨[J].铀矿地质,1990,6(5):279-286.
LIN Guan-ying.An Approach to Geological Characteristics of Uranium Metallogenesis and Prospecting Target Along the Yangtze River in Jiangsu and Anhui Provinces[J].Uranium Geology,1990,6(5):279-286.
[14] 郑永飞,傅 斌,龚 冰.安徽黄梅尖岩体热历史及其与成矿关系:同位素证据[J].地质学报,1995,69(4):337-348.
ZHENG Yong-fei,FU Bin,GONG Bing.The Thermal History of the Huangmeijian Intrusion in Anhui and Its Relation to Mineralization:Isotopic Evidence[J].Acta Geologica Sinica,1995,69(4):337-348.
[15] 郑永飞,魏春生,王峥嵘,等.大龙山岩体冷却史及其成矿关系的同位素研究[J].地质科学,1997,32(4):645-657.
ZHNEG Yong-fei,WEI Chun-sheng,WANG Zheng-rong,et al.An Isotope Study on the Cooling History of the Dalongshan Granite Massif and Its Bearing[J].Scientia Geologica Sinica,1997,32(4):645-657.
[16] 孙 洋,马昌前,刘园园.长江中下游燕山期最新的成岩成矿事件:来自宁镇地区的证据[J].科学通报,2014,59(8):668-678.
SUN Yang,MA Chang-qian,LIU Yuan-yuan.The La-test Yanshanian Magmatic and Metallogenic Events in the Middle-lower Yangtze River Belt:Evidences from the Ningzhen Region[J].Chinese Science Bulletin,2014,59(8):668-678.
[17] 刘建敏,闫 峻,李全忠,等.宁镇地区安基山岩体锆石LA-ICPMS U-Pb定年及意义[J].地质论评,2014,60(1):190-200.
LIU Jian-min,YAN Jun,LI Quan-zhong,et al.Zircon LA-ICPMS Dating of the Anjishan Pluton in Nanjing-Zhenjiang Area and Its Significance[J].Geological Re-view,2014,60(1):190-200.
[18] 关俊朋,韦福彪,孙国曦,等.宁镇中段中酸性侵入岩锆石U-Pb年龄及其成岩成矿指示意义[J].大地构造与成矿学,2015,39(2):344-354.
GUAN Jun-peng,WEI Fu-biao,SUN Guo-xi,et al.Zircon U-Pb Dating of Intermediate-acid Intrusive Rocks in the Middle Section of Ningzhen District and Their Metallogenic Implications[J].Geotectonica et Metallogenia,2015,39(2):344-354.
[19] 聂利青,周涛发,范 裕,等.长江中下游成矿带庐枞矿集区首例钨矿床成岩成矿时代及其意义[J].岩石学报,2016,32(2):303-318.
NIE Li-qing,ZHOU Tao-fa,FAN Yu,et al.LA-ICPMS U-Pb Zircon Age and Molybdenite Re-Os Dat-ing of Donggushan,the First Tungsten Deposit Found in the Luzong Orefield,Middle-lower Yangtze River Valley Metallogenic Belt[J].Acta Petrologica Sinica,2016,32(2):303-318.
[20] 张赞赞,吴明安,杜建国,等.庐枞矿集区与钨矿床有关的花岗岩的年代学及地球化学特征:岩石成因及其对长江中下游晚白垩世成矿的启示[J].岩石学报,2018,34(1):217-240.
ZHANG Zan-zan,WU Ming-an,DU Jian-guo,et al.Geochronology and Geochemistry of the Tungsten Deposit-related Granites in the Luzong Orefield:Pe-trogenesis and Insights for Late Cretaceous Metallo-geny in the Middle and Lower Reaches of Yangtze River Metallogenic Belt[J].Acta Petrologica Sinica,2018,34(1):217-240.
[21] 张祖还,沈渭洲,章邦桐.黄梅尖岩体成岩作用的锶同位素研究[J].岩石矿物及测试,1984,3(1):26-32.
ZHANG Zu-huan,SHEN Wei-zhou,ZHANG Bang-tong.Strontium Isotope Study of Petrogenetic Process on the Huangmeijian Body[J].Rock and Mineral Analysis,1984,3(1):26-32.
[22] 章邦桐,张富生,倪琦生,等.安庐石英正长岩带的地质和地球化学特征及成因探讨[J].岩石学报,1988,4(3):1-14.
ZHANG Bang-tong,ZHANG Fu-sheng,NI Qi-sheng,et al.Geology and Geochemical Characteristics of the Anqing-Lujiang Quartz Syenite Rock-belt and Its Ge-nesis[J].Acta Petrologica Sinica,1988,4(3):1-14.
[23] 周涛发,王 彪,范 裕,等.庐枞盆地与A型花岗岩有关的磁铁矿-阳起石-磷灰石矿床:以马口铁矿床为例[J].岩石学报,2012,28(10):3087-3098.
ZHOU Tao-fa,WANG Biao,FAN Yu,et al.Apatite-actinolite-magnetite Deposit Related to A-type Gra-nite in Luzong Basin:Evidence from Makou Iron Deposit[J].Acta Petrologica Sinica,2012,28(10):3087-3098.
[24] LI H,ZHANG H,LING M X,et al.Geochemical and Zircon U-Pb Study of the Huangmeijian A-type Gra-nite:Implications for Geological Evolution of the Lo-wer Yangtze River Belt[J].International Geology Review,2011,53(5/6):499-525.
[25] 周伟伟.郯庐断裂带晚中生代富碱侵入岩年代学、岩石地球化学及其地质意义[D].北京:中国地质大学,2014.
ZHOU Wei-wei.Chronological,Petrological and Geochemical Characteristics of the Late Mesozoic Alkaline-rich Intrusive Rocks Along Tanlu Fault Zone[D].Beijing:China University of Geosciences,2014.
[26] 薛怀民,马 芳,曹光跃,等.长江中下游庐枞火山岩盆地南侧钾质侵入岩带的成因[J].地质学报,2016,90(9):2233-2257.
XUE Huai-min,MA Fang,CAO Guang-yue,et al.Petrogenesis of Potassic Intrusive Rocks Along the Southern Margin of the Luzong Volcanic Basin,Middle and Lower Yangtze River Reaches,China[J].Acta Geologica Sinica,2016,90(9):2233-2257.
[27] 谭正中,巩志根,梁才英.晚期小岩体归宿及其在找矿中的意义初探[J].铀矿地质,1993,9(5):280-288.
TAN Zheng-zhong,GONG Zhi-gen,LIANG Cai-ying.Preliminary Discussion on the Attribution of Late Sta-ge Small Massifs and Their Significance in Prospect-ing[J].Uranium Geology,1993,9(5):280-288.
[28] 朱 捌,凌洪飞,沈渭洲,等.粤北石土岭铀矿床同位素地球化学研究[J].矿床地质,2006,25(1):73-82.
ZHU Ba,LING Hong-fei,SHEN Wei-zhou,et al.Isotopic Geochemistry of Shituling Uranium Deposit,Northern Guangdong Province,China[J].Mineral Deposits,2006,25(1):73-82.
[29] 娄 峰,李宏卫,陈光明,等.花岗岩演化与铀钍元素富集的关系:以粤北贵东岩体为例[J].地学前缘,2011,18(1):110-117.
LOU Feng,LI Hong-wei,CHEN Guang-ming,et al.The Relationship Between Granite Evolution and Uranium-thorium Enrichment:An Example from the Guidong Granite Body,North Guangdong Province[J].Earth Science Frontiers,2011,18(1):110-117.
[30] ZHAO K D,JIANG S Y,DONG C Y,et al.Uranium-bearing and Barren Granites from the Taoshan Complex,Jiangxi Province,South China:Geochemical and Petrogenetic Discrimination and Exploration Significance[J].Journal of Geochemical Exploration,2011,110(2):126-135.
[31] 陈振宇,黄国龙,朱 捌,等.南岭地区花岗岩型铀矿的特征及其成矿专属性[J].大地构造与成矿学,2014,38(2):264-275.
CHEN Zhen-yu,HUANG Guo-long,ZHU Ba,et al.The Characteristics and Metallogenic Specialization of Granite-hosted Uranium Deposits in the Nanling Region[J].Geotectonica et Metallogenia,2014,38(2):264-275.
[32] 巫建华,郭国林,郭佳磊,等.中国东部中生代岩浆岩的时空分布及其与热液型铀矿的关系[J].岩石学报,2017,33(5):1591-1614.
WU Jian-hua,GUO Guo-lin,GUO Jia-lei,et al.Spatial-temporal Distribution of Mesozoic Igneous Rock and Their Relationship with Hydrothermal Uranium Deposits in Eastern China[J].Acta Petrologica Sinica,2017,33(5):1591-1614.
[33] 毛建仁,苏郁香,陈三元.长江中下游中酸性侵入岩与成矿[M].北京:地质出版社,1990.
MAO Jian-ren,SU Yu-xiang,CHEN San-yuan.The Intermediate-acid Intrusive Rocks in Middle and Lower Yangtze River and the Relationship with Mineralization[M].Beijing:Geological Publishing House,1990.
[34] 邢凤鸣,徐 祥.安徽两条A型花岗岩带[J].岩石学报,1994,10(4):357-369.
XING Feng-ming,XU Xiang.Two A-type Granite Belts from Anhui[J].Acta Petrologica Sinica,1994,10(4):357-369.
[35] LI H,LING M X,LI C Y,et al.A-type Granite Belts of Two Chemical Subgroups in Central Eastern China:Indication of Ridge Subduction[J].Lithos,2012,150:26-36.
[36] YAN J,LIU J M,LI Q Z,et al.In-situ Zircon Hf-O Isotopic Analyses of Late Mesozoic Magmatic Rocks in the Lower Yangtze River Belt,Central Eastern China:Implications for Petrogenesis and Geodynamic Evolution[J].Lithos,2015,227:57-76.
[37] 蔡煜琦,张金带,李子颖,等.中国铀矿资源特征及成矿规律概要[J].地质学报,2015,89(6):1051-1069.
CAI Yu-qi,ZHANG Jin-dai,LI Zi-ying,et al.Outline of Uranium Resources Characteristics and Metallogenetic Regularity in China[J].Acta Geologica Sinica,2015,89(6):1051-1069.
[38] 毛景文,段 超,刘佳林,等.陆相火山-侵入岩有关的铁多金属矿成矿作用及矿床模型——以长江中下游为例[J].岩石学报,2012,28(1):1-14.
MAO Jing-wen,DUAN Chao,LIU Jia-lin,et al.Me-tallogeny and Corresponding Mineral Deposit Model of the Cretaceous Terrestrial Volcanic-intrusive Rocks Related Polymetallic Iron Deposits in Middle-lower Yangtze River Valley[J].Acta Petrologica Sinica,2012,28(1):1-14.
[39] 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.
[40] LIU Y S,GAO S,HU Z C,et al.Continental and Ocea-nic Crust Recycling-induced Melt-peridotite Interactions in the Trans-North China Orogen:U-Pb Dating,Hf Isotopes and Trace Elements in Zircons of Mantle Xenoliths[J].Journal of Petrology,2010,51(1/2):537-571.
[41] LUDWIG K R.User's Manual for Isoplot 3.00:A Geo-chronological Toolkit for Microsoft Excel[R].Berkely:Berkeley Geochronology Center,2003.
[42] ANDERSEN T.Correction of Common Lead in U-Pb Analyses That Do Not Report 204Pb[J].Chemical Geo-logy,2002,192(1/2):59-79.
[43] VAVRA G,GEBAUER D,SCHMID R.Multiple Zircon Growth and Recrystallization During Polyphase Late Carboniferous to Triassic Metamorphism in Gra-nulites of the Ivrea Zone(Southern Alps):An Ion Microprobe(SHRIMP)Study[J].Contributions to Mi-neralogy and Petrology,1996,122:337-358.
[44] 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.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age[J].Chinese Science Bulletin,2004,49(16):1589-1604.
[45] EWING R C,MELDRUM A,WANG L M,et al.Radiation Effects in Zircon[J].Reviews in Mineralogy and Geochemistry,2003,53(1):387-425.
[46] CORFU F,HANCHAR J M,HOSKIN P W O,et al.Atlas of Zircon Textures[J].Reviews in Mineralogy and Geochemistry,2003,53(1):469-500.
[47] FARNAN I,BALAN E,PICKARD C J,et al.The Effect of Radiation Damage on Local Structure in the Crystalline Fraction of ZrSiO4:Investigating the 29Si NMR Response to Pressure in Zircon and Reidite[J].American Mineralogist,2003,88(11/12):1663-1667.
[48] SUN S S,MCDONOUGH W F.Chemical and Isoto-pic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society,London,Special Publications,1989,42:313-345.
[49] HOSKIN P W O,IRELAND T R.Rare Earth Element Chemistry of Zircon and Its Use as a Provenance Indicator[J].Geology,2000,28(7):627-630.
[50] HANCHAR J M,WESTENEN W.Rare Earth Element Behavior in Zircon-melt Systems[J].Elements,2007,3(1):37-42.
[51] KEAY S,LISTER G,BUICK I.The Timing of Partial Melting,Barrovian Metamorphism and Granite Intrusion in the Naxos Metamorphic Core Complex,Cyclades,Aegean Sea,Greece[J].Tectonophysics,2001,342(3/4):275-312.
[52] 刘小驰,吴元保,彭 敏,等.桐柏造山带深熔作用:混合岩LA-ICP-MS锆石U-Pb年代学证据[J].岩石学报,2011,27(4):1163-1171.
LIU Xiao-chi,WU Yuan-bao,PENG Min,et al.Crustal Anatexis in the Tongbai Orogen:Evidence from LA-ICP-MS Zircon U-Pb Age of Migmatite[J].Acta Petrologica Sinica,2011,27(4):1163-1171.
[53] 向 华,钟增球,李 晔,等.北秦岭造山带早古生代多期变质与深熔作用:锆石U-Pb年代学证据[J].岩石学报,2014,30(8):2421-2434.
XIANG Hua,ZHONG Zeng-qiu,LI Ye,et al.Early Paleozoic Polymetamorphism and Anatexis in the North Qinling Orogen:Evidence from U-Pb Zircon Geochronology[J].Acta Petrologica Sinica,2014,30(8):2421-2434.
[54] FRASER G,ELLIS D,EGGINS S.Zirconium Abundance in Granulite-facies Minerals with Implications for Zircon Geochronology in High-grade Rocks[J].Geology,1997,25(7):607-610.
[55] GINGEN B,AUSTRHEIM H,WHITEHOUSE M.Ilmenite as a Source for Zirconium During High-grade Metamorphism? Textural Evidence from the Caledonides of Western Norway and Implications for Zircon Geochronology[J].Journal of Petrology,2001,42(2):355-375.
[56] 胡芳芳,范宏瑞,杨进辉,等.胶东乳山含金石英脉型金矿的成矿年龄:热液锆石SHRIMP法U-Pb测定[J].科学通报,2004,49(12):1191-1198.
HU Fang-fang,FAN Hong-rui,YANG Jin-hui,et al.The Ore-forming Age of Gold-bearing Quartz Vein in Rushan,Jiaodong:Dating by Hydrothermal Zircon U-Pb SHRIMP[J].Chinese Science Bulletin,2004,49(12):1191-1198.
[57] 李长民,邓晋福,陈立辉,等.华北北缘张宣地区东坪金矿中的两期锆石:对成矿年龄的约束[J].矿床地质,2010,29(2):265-275.
LI Chang-min,DENG Jin-fu,CHEN Li-hui,et al.Two Periods of Zircon from Dongping Gold Deposit in Zhangjiakou-Xuanhua Area,Northern Margin of Nor-th China:Constraints on Metallogenic Chronology[J].Mineral Deposits,2010,29(2):265-275.
[58] GEISLER T,ULONSKA M,SCHLEICHER H,et al.Leaching and Differential Recrystallization of Meta-mict Zircon Under Experimental Hydrothermal Conditions[J].Contributions to Mineralogy and Petrology,2001,141:53-65.
[59] 陈道公,DELOULE E,夏群科,等.大别山双河超高压榴辉岩中变质锆石:离子探针和微区结构研究[J].岩石学报,2002,18(3):369-377.
CHEN Dao-gong,DELOULE E,XIA Qun-ke,et al.Metamorphic Zircon from Shuanghe Ultra-high Pressure Eclogite,Dabieshan:Ion Microprobe and Internal Micro-structure Study[J].Acta Petrologica Sinica,2002,18(3):369-377.
[60] 陈仁旭,郑永飞.大陆俯冲带变质过程中熔/流体活动的锆石学记录[J].科学通报,2013,58(22):2227-2232.
CHEN Ren-xu,ZHENG Yong-fei.Zirconological Records of Fluid/Melt Action During Continental Subduction-zone Metamorphism[J].Chinese Science Bulletin,2013,58(22):2227-2232.
[61] 唐 勇,张 辉,吕正航.不同成因锆石阴极发光及微量元素特征:以新疆阿尔泰地区花岗岩和伟晶岩为例[J].矿物岩石,2012,32(1):8-15.
TANG Yong,ZHANG Hui,LV Zheng-hang.Cha-racteristics of Zircon Cathodoluminescence and Trace Elements of Granite and Pegmatite from Altai Moun-tains,Northwest China[J].Journal of Mineralogy and Petrology,2012,32(1):8-15.
[62] RIZCANOVA N G,LEVCHENKOV O A,BELOUS A E,et al.Zircon Reaction and Stability of the U-Pb Isotope System During Interaction with Carbonate Fluid:Experimental Hydrothermal Study[J].Contributions to Mineralogy and Petrology,2000,139:101-114.
[63] PIDGEON R T.Recrystallization of Oscillatory-zoned Zircon:Some Geochronological and Petrological Implications[J].Contributions to Mineralogy and Petrology,1992,110:463-472.
[64] VAVRA G,SCHMID R,GEBAUER D.Internal Morphology,Habit and U-Th-Pb Microanalysis of Amphibole to Granulite Facies Zircon:Geochronology of the Ivren Zone(Southern Alps)[J].Contributions to Mineralogy and Petrology,1999,134:380-404.
[65] HOSKIN P W O,BLACK L P.Metamorphic Zircon Formation by Solid-state Recrystallization of Protolith Igneous Zircon[J].Journal of Metamorphic Geology,2000,18(4):423-439.
[66] 李秋立.离子探针锆石U-Pb定年的“高U效应”[J].矿物岩石地球化学通报,2016,35(3):405-412.
LI Qiu-li.“High-U Effect” During SIMS Zircon U-Pb Dating[J].Bulletin of Mineralogy,Petrology and Geochemistry,2016,35(3):405-412.
[67] KROUGH T E.Improved Accuracy of U-Pb Zircon Ages by the Creation of More Concordant Systems Using an Air Abrasion Technique[J].Geochimica et Cosmochimica Acta,1982,46(4):637-649.
[68] 王 强,赵振华,简 平,等.华南腹地白垩纪A型花岗岩类或碱性侵入岩年代学及其对华南晚中生代构造演化的制约[J].岩石学报,2005,21(3):795-808.
WANG Qiang,ZHAO Zhen-hua,JIAN Ping,et al.Geochronology of Cretaceous A-type Granitoids or Alkaline Intrusive Rocks in the Hinterland,South China:Constrains for Late-Mesozoic Tectonic Evolution[J].Acta Petrologica Sinica,2005,21(3):795-808.
[69] 楼亚儿,杜杨松.安徽繁昌中生代侵入岩的特征和锆石SHRIMP测年[J].地球化学,2006,35(4):333-345.
LOU Ya-er,DU Yang-song.Characteristics and Zircon SHRIMP U-Pb Ages of the Mesozoic Intrusive Rocks in Fanchang,Anhui Province[J].Geochimica,2006,35(4):333-345.
[70] 彭 戈,闫 峻,初晓强,等.贵池岩体的锆石定年和地球化学:岩石成因和深部过程[J].岩石学报,2012,28(10):3271-3286.
PENG Ge,YAN Jun,CHU Xiao-qiang,et al.Zircon U-Pb Dating and Geochemistry of Guichi Intrusive Rocks:Petrogenesis and Deep Dynamic Processes[J].Acta Petrologica Sinica,2012,28(10):3271-3286.
[71] 闫 峻,彭 戈,刘建敏,等.下扬子繁昌地区花岗岩成因:锆石年代学和Hf-O同位素制约[J].岩石学报,2012,28(10):3209-3227.
YAN Jun,PENG Ge,LIU Jian-min,et al.Petrogenesis of Granites from Fanchang District,the Lower Yangtze Region:Zircon Geochronology and Hf-O Isotopes Constrains[J].Acta Petrologica Sinica,2012,28(10):3209-3227.
[72] 刘 潇.安徽贵池—青阳地区中生代侵入岩岩石学和锆石U-Pb年代学研究[D].合肥:合肥工业大学,2013.
LIU Xiao.Studies on Petrology and Zircon U-Pb Geochronology of Mesozoic Intrusive Rocks in Guichi-Qingyang Region,Anhui Province[D].Hefei:Hefei University of Technology,2013.
[73] 褚 庚.安庆矿区中生代典型埃达克岩和A型花岗岩研究:多金属矿床成矿启示[D].合肥:中国科学技术大学,2016.
CHU Geng.Petrogenesis of the Mesozoic Classic Ada-kites and A-type Granites in the Anqing Orefield:Implications for Metallogenesis of Polymetallic Deposit[D].Hefei:University of Science and Technology of China,2016.
[74] 高 冉,闫 峻,李全忠,等.皖南谭山岩体成因:年代学和地球化学制约[J].高校地质学报,2017,23(2):227-243.
GAO Ran,YAN Jun,LI Quan-zhong,et al.Petroge-nesis of Tanshan Pluton in the Southern Anhui Pro-vince:Chronological and Geochemical Constraints[J].Geological Journal of China Universities,2017,23(2):227-243.
[75] 庞振山,高浮萍,朱晓强,等.安徽繁昌浮山钾长花岗岩成因及其构造意义——来自锆石U-Pb年龄、岩石地球化学和Hf同位素的证据[J].地质通报,2017,36(2/3):402-417.
PANG Zhen-shan,GAO Fu-ping,ZHU Xiao-qiang,et al.Petrogenesis and Tectonic Implications of the Fushan Moyite in the Fanchang Area,Anhui Pro-vince—Evidence from Zircon U-Pb Age,Geochemistry and Hf Isotopes[J].Geological Bulletin of China,2017,36(2/3):402-417.
[76] 赵 玲,陈志洪.皖南谭山岩体的锆石定年及地质意义[J].资源调查与环境,2014,35(3):185-191.
ZHAO Ling,CHEN Zhi-hong.Zircon LA-ICPMS Dating of the Tanshan Pluton in the Area of Southern Anhui Province and Its Geological Significances[J].Resources Survey and Environment,2014,35(3):185-191.
[77] 杜 欣,吴明安,周涛发,等.安徽庐枞盆地南部A型花岗岩成因探讨[J].地质科学,2018,53(2):678-696.
DU Xin,WU Ming-an,ZHOU Tao-fa,et al.Discussion on the Genesis of A-type Granites in Southern Lu-zong Basin,Anhui Province,China[J].Chinese Journal of Geology,2018,53(2):678-696.
[78] YANG C,YAN J,WANG S N,et al.Petrogenesis of the Late Mesozoic Bashan Complex in the Lower Yangtze River Belt,Eastern China:Implications for the Definition and Significance of A-type Granite[J].Lithos,2021,392/393:106144.
[79] 范 羽,周涛发,张达玉,等.皖南地区青阳—九华山复式岩体的成因[J].岩石学报,2016,32(2):419-438.
FAN Yu,ZHOU Tao-fa,ZHANG Da-yu,et al.Genesis of the Qingyang-Jiuhuashan Complex Pluton in South Anhui Province and Its Significance[J].Acta Petrologica Sinica,2016,32(2):419-438.
[80] 薛怀民,汪应庚,马 芳,等.皖南太平—黄山复合岩体的SHRIMP年代学:由钙碱性向碱性转变对扬子克拉通东南部中生代岩石圈减薄时间的约束[J].中国科学:D辑,地球科学,2009,39(7):979-993.
XUE Huai-min,WANG Ying-geng,MA Fang,et al.Zircon U-Pb SHRIMP Ages of Taiping(Calc-alkaline)-Huangshan(Alkaline)Composite Intrusive:Con-straints on Mesozoic Lithospheric Thinning of the Southeastern Yangtze Craton,China[J].Science in China:Series D,Earth Sciences,2009,39(7):979-993.
[81] SONG G X,QIN K Z,LI G M,et al.Mesozoic Magmatism and Metallogeny in the Chizhou Area,Middle-lower Yangtze Valley,SE China:Constrained by Pe-trochemistry,Geochemistry and Geochronology[J].Journal of Asian Earth Sciences,2014,91:137-153.
[82] 华仁民,陈培荣,张文兰,等.华南中、新生代与花岗岩类有关的成矿系统[J].中国科学:D辑,地球科学,2003,33(4):335-343.
HUA Ren-min,CHEN Pei-rong,ZHANG Wen-lan,et al.The Metallogenesis Systems Related to Meso-zoic-Cenozoic Granitoids,South China[J].Science in China:Series D,Earth Sciences,2003,33(4):335-343.
[83] 张 龙,陈振宇,汪方跃.华南花岗岩型铀矿床主要特征与成矿作用研究进展[J].岩石学报,2021,37(9):2657-2676.
ZHANG Long,CHEN Zhen-yu,WANG Fang-yue.General Characteristics and Research Progresses in Metallogenesis of Granite-related Uranium Deposits in South China[J].Acta Petrologica Sinica,2021,37(9):2657-2676.
[84] 沈渭洲,张祖还,章邦桐.华南某些花岗岩型铀矿床的同位素地质研究[J].地质学报,1988,62(1):51-62.
SHEN Wei-zhou,ZHANG Zu-huan,ZHANG Bang-tong.A Study on Isotope Geology of Some Granite Type Uranium Deposits in South China[J].Acta Geologica Sinica,1988,62(1):51-62.
[85] 胡瑞忠.花岗岩型铀矿床成因讨论:以华南为例[J].地球科学进展,1994,9(2):41-46.
HU Rui-zhong.A Commentary on Genesis of Granite-type Uranium Deposits:As Exemplified by South China[J].Advance in Earth Sciences,1994,9(2):41-46.
[86] 陈培荣.华南东部中生代岩浆作用的动力学背景及其与铀成矿关系[J].铀矿地质,2004,20(5):266-270.
CHEN Pei-rong.Geodynamic Setting of Mesozoic Mag-matism and Its Relationship to Uranium Metalloge-nesis in Southeastern China[J].Uranium Geology,2004,20(5):266-270.
[87] 黄国龙,朱 捌,吴烈勤,等.华南花岗岩型铀矿勘查现状及找矿方向[J].铀矿地质,2006,22(6):345-349.
HUANG Guo-long,ZHU Ba,WU Lie-qin,et al.Exploration Situation and Direction of Granite Type Uranium Deposits in South China[J].Uranium Geology,2006,22(6):345-349.
[88] 胡瑞忠,毕献武,彭建堂,等.华南地区中生代以来岩石圈伸展及其与铀成矿关系研究的若干问题[J].矿床地质,2007,26(2):139-152.
HU Rui-zhong,BI Xian-wu,PENG Jian-tang,et al.Some Problems Concerning Relationship Between Me-sozoic-Cenozoic Lithospheric Extension and Uranium Metallogenesis in South China[J].Mineral Deposits,2007,26(2):139-152.
[89] 张国全,胡瑞忠,商朋强,等.华南花岗岩型铀矿床成矿机理研究进展[J].矿物岩石地球化学通报,2007,26(4):399-404.
ZHANG Guo-quan,HU Rui-zhong,SHANG Peng-qiang,et al.An Overview on the Ore-forming Mechanism of the Granite-type Uranium Deposit in South China[J].Bulletin of Mineralogy,Petrology and Geochemistry,2007,26(4):399-404.
[90] 凌洪飞.论花岗岩型铀矿床热液来源:来自氧逸度条件的制约[J].地质论评,2011,57(2):193-206.
LING Hong-fei.Origin of Hydrothermal Fluids of Granite-type Uranium Deposits:Constraints from Re-dox Conditions[J].Geological Review,2011,57(2):193-206.

Memo

Memo:
-
Last Update: 2022-04-30