[an error occurred while processing this directive] 世界地质 2018, 37(4) 1004-1017 DOI:   10.3969/j.issn.1004-5589.2018.04.002  ISSN: 1004-5589 CN: 22-1111/P

本期目录 | 下期目录 | 过刊浏览 | 高级检索                                                            [打印本页]   [关闭]
基础地质
扩展功能
本文信息
Supporting info
PDF(1077KB)
[HTML全文]
参考文献[PDF]
参考文献
服务与反馈
把本文推荐给朋友
加入我的书架
加入引用管理器
引用本文
Email Alert
文章反馈
浏览反馈信息
本文关键词相关文章
铼-锇同位素年龄
辉钼矿
成矿时代
热水
东昆仑
本文作者相关文章
朱德全
朱海波
李宝龙
李洪英
李国涛
PubMed
Article by Zhu D
Article by Zhu H
Article by Li B
Article by Li H
Article by Li G
青海省都兰县热水铜钼矿床辉钼矿Re-Os测年及成矿意义
朱德全1, 朱海波1, 李宝龙2,3, 李洪英2,3, 李国涛1
1. 山东省第八地质矿产勘查院, 山东 日照 276826;
2. 自然资源部成矿作用与资源评价重点实验室, 北京 100037;
3. 中国地质科学院矿产资源研究所, 北京 100037
摘要: 为了查明都兰县热水铜钼矿床的形成时间,笔者对其主要铜钼多金属矿体地表和岩芯的6件辉钼矿样品进行了Re-Os同位素分析,辉钼矿Re含量为(5.969±0.042)×10-6~(15.55±0.11)×10-6,Re-Os同位素模式年龄分布范围在(233.1±3.1~235.6±3.1)Ma,其年龄加权平均值为(234.2±1.3)Ma(MSWD=0.40),等时线年龄为(234.2±2.8)Ma(MSWD=1.09)。揭示该矿床的成矿时代为晚三叠世早期。结合区域地质特征、地球化学资料和同位素年代学数据,认为该矿床可能形成于东昆仑造山带的后碰撞背景。东昆仑成矿带在三叠纪存在一期广泛的构造-岩浆成矿事件,从祁漫塔格到鄂拉山等地均有出现。
关键词 铼-锇同位素年龄   辉钼矿   成矿时代   热水   东昆仑  
Re-Os geochronology of molybdenite from Reshui Cu-Mo deposit in Dulan, Qinghai and its geological significance
ZHU De-quan1, ZHU Hai-bo1, LI Bao-long2,3, LI Hong-ying2,3, LI Guo-tao1
1. The 8th Institute of Geology & Mineral Exploration of Shandong Province, Rizhao 276826, Shandong, China;
2. NLR Key Laboratory of Metallogeny and Mineral Assessment, Beijing 100037, China;
3. Institute of Mineral Resources, China Academy of Geological Sciences, Beijing 100037, China
Abstract: In order to identify the formation time of Reshui Cu-Mo deposit, six molybdenite samples from outcrops and core were used for Re-Os isotopic analysis. The dating results showed that Re content ranges from (5.969±0.042)×10-6~(15.55±0.11)×10-6, model ages is (233.1±3.1~235.6±3.1)Ma, the weighted average age is (234.2±1.3) Ma (MSWD=0.40), the isochron age is (234.2±2.8) Ma (MSWD=1.09).The data revealed that the metallogenic epoch was early Late Triassic. Combined with regional geology, geochemistry and isotopic geochronology data, the authors suggested that the Reshui Cu-Mo deposit was formed in a post-collisional background of east Kunlun Orogen during Mid-Late Triassic. There existed a widely occurred magmatic-tectonic mineralization event during Triassic in east Kunlun, from Qimantage in the west to Ngola in the east.
Keywords: Re-Os isotopic   molybdenite   metallogenic epoch   Reshui   eastern Kunlun  
收稿日期 2017-09-03 修回日期 2018-10-30 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2018.04.002
基金项目:

中国地质调查局调查项目(12120114034301)、中央级公益性科研院所基本科研业务费专项(K1309)联合资助.

通讯作者: 李宝龙(1982-),男,副研究员,主要从事成矿规律和资源勘查工作.E-mail:xinzhongguolong@163.com
作者简介:
作者Email: xinzhongguolong@163.com

参考文献:
[1] 潘彤. 青海祁漫塔格地区铁多金属矿成矿特征及找矿潜力[J]. 矿产与地质,2008, 22(3):232-235. PAN Tong. Metallogenic characteristics and prospecting potential of the Fe polymetallic deposits in Qimantage area, Qinghai Province[J]. Mineral Resources and Geology, 2008, 22(3):232-235.
[2] 宋忠宝,杜玉良,李智明,等. 青海省矿产资源发育特征概述[J]. 地球科学与环境学报,2009, 33(1):30-47. SONG Zhong-bao, DU Yu-liang, LI Zhi-ming, et al. Characteristics of mineral resources in Qinghai Province[J]. Journal of Earth Sciences and Environment, 2009, 33(1):30-47.
[3] 宋忠宝,张雨莲,陈向阳,等. 东昆仑哈日扎含矿花岗闪长斑岩LA-ICP-MS锆石U-Pb定年及地质意义[J]. 矿床地质,2013, 32(1):157-168. SONG Zhong-bao, ZHANG Yu-lian, CHEN Xiang-yang, et al. Geochemical characteristics of Harizha granite diorite-porphyry in East Kunlun and their geological implications[J]. Mineral Deposits, 2013, 32(1):157-168.
[4] 丰成友,马圣钞,李国臣,等. 青海景忍-迎庆沟多金属矿床成因的成岩成矿年代学约束[J]. 矿物学报,2011(增刊1):576-577. FENG Cheng-you, MA Sheng-chao, LI Guo-chen, et al. The chronology constraint on the diagenetic metallogenic of Jingren-Yingqinggou polymetallic deposit, Qinghai Province[J]. Acta Mineralogica Sinica, 2011(Suppl.1):576-577.
[5] 丰成友,王雪萍,舒晓峰,等. 青海祁漫塔格虎头崖铅锌多金属矿床年代学研究及地质意义[J]. 吉林大学学报(地球科学版),2011, 41(6):1806-1817. FENG Cheng-you, WANG Xue-ping, SHU Xiao-feng, et al. Isotopic chronology of the Hutouya skarn lead-zic polymetallic ore district in Qimantage area of Qinghai Province and its geological significance[J]. Journal of Jilin University(Earth Science Edition), 2011, 41(6):1806-1817.
[6] 丰成友,赵一鸣,李大新,等. 青海西部祁漫塔格地区矽卡岩型铁铜多金属矿床的矽卡岩类型和矿物学特征[J]. 地质学报,2011,85(7):1108-1115. FENG Cheng-you, ZHAO Yi-ming, LI Da-xin, et al. Skarn types and mineralogical characteristics of the Fe-Cu-polymetallic skarn deposits in the Qimantage area, West Qinghai Province[J]. Acta Geologica Sinica, 2011, 85(7):1108-1115.
[7] 丰成友,王松,李国臣,等. 青海祁漫塔格中晚三叠世花岗岩:年代学、地球化学及成矿意义[J]. 岩石学报,2012, 28(2):665-678. FENG Cheng-you, WANG Song, LI Guo-chen, et al. Middle to Late Triassic granitoids in the Qimantage area, Qinghai Province, China:chronology, geochemistry and metallogenic significances[J]. Acta Petrologica Sinica, 2012, 28(2):665-678.
[8] 尹利君,刘继顺,杨立功,等. 青海都兰白石崖矿区花岗岩年代学、地球化学特征及地质意义[J]. 新疆地质,2013,31(3):248-255. YIN Li-jun, LIU Ji-shun, YANG Li-gong, et al. Geochronology, geochemistry and geological significance of granites from the Baishiya skarn iron-polymetallic deposit, Dulan, Qinghai Province[J]. Xinjiang Geology, 2013, 31(3):248-255.
[9] 许长坤,刘世宝,赵子基,等.青海省东昆仑成矿带铁矿成矿规律与找矿方向研究[J]. 地质学报,2012,86(10):1621-1678. XU Chang-kun, LIU Shi-bao, ZHAO Zi-ji, et al. Metallogenic law and prospecting direction of iron deposits in the East Kunlun metallogenic belt in Qinghai[J]. Acta Geologica Sinica, 2012, 86(10):1621-1678.
[10] 浙江省地质矿产研究所. 青海省都兰县热水矿区钼矿普查报告[R]. 青海:青海中鑫矿业有限公司,2008:1-80. Institute of Geology and Mineral Resources of Zhejiang Province. The census reports of Reshui molybdenum ore mining area, Dulan County, Qinghai Province[R]. Qinghai:Qinghai Zhongxin Co., Ltd, 2008:1-80.
[11] 王学良. 东昆仑东段香加南山花岗岩体地质特征及其形成年代研究:硕士学位论文[D].西安:长安大学, 2012. WANG Xue-liang. Studies on geological characteristics and forming age of southern Xiangjia Mountain granitic pluton at east section of East Kunlun orogenic belt:master's degree thesis[D]. Xi'an:Chang'an University, 2012.
[12] 王威,袁万明,郭娇,等. 东昆仑造山带都兰地区花岗岩类锆石U-Pb定年和地球化学特征[J]. 电子显微学报,2015,34(3):222-233. WANG Wei, YUAN Wan-ming, GUO Jiao, et al. Zircon U-Pb ages and geochemical features of granites in Dulan area, eastern Kunlun Mountains[J]. Journal of Chinese Electron Microscopy Society, 2015, 34(3):222-233.
[13] 国显正,贾群子,李金超,等. 东昆仑热水钼矿区似斑状黑云母二长花岗岩元素地球化学及年代学研究[J]. 中国地质,2016, 43(4):1164-1177. GUO Xian-zheng, JIA Qun-zi, LI Jin-chao, et al. Geochemical characteristics and geochronology of porphyroid biotite monzogranite from the Reshui Mo polymetallic deposit, East Kunlun Mountains[J]. Geology in China, 2016, 43(4):1165-1177.
[14] 杜安道,何红蓼,殷宁万,等. 辉钼矿的铼-锇同位素地质年龄测定方法研究[J].地质学报,1994,68(4):339-347. DU An-dao,HE Hong-lin,YIN Ning-wan,et al. A study on the rhenium-osmium geochronometry of molybdenites[J].Acta Geologica Sinica,1994, 68(4):339-347.
[15] 杜安道,屈文俊,王登红,等. 铼-锇法及其在矿床学中的应用[M]. 北京:地质出版社, 2012:1-182. DU An-dao,QU Wen-jun,WANG Deng-hong, et al. Re-Os and its application in economic geology[M].Beijing:Geological Publishing House,2012:1-182.
[16] Smoliar M I, Walker R J, Morgan J W. Re-Os ages of Group ⅡA, ⅢA, ⅣA, and ⅣB iron meteorites[J]. Science, 1996, 271:1099-1102.
[17] 孟健寅, 杨立强, 吕亮, 等. 滇西北红山铜钼矿床辉钼矿Re-Os同位素测年及其成矿意义[J]. 岩石学报, 2013, 4:1214-1222. MENG Jian-yin, YANG Li-qiang, LYU Liang, et al. Re-Os dating of molybdenite from the Hongshan Cu-Mo deposit in Northwest Yunnan and its implications for mineralization[J]. Acta Petrologica Sinica, 2013, 4:1214-1222.
[18] 殷鸿福,张克信. 东昆仑造山带的一些特点[J]. 地球科学,1997, 22(4):339-342. YIN Hong-fu, ZHANG Ke-xin. Characteristics of the eastern Kunlun orogenic belt[J]. Earth Science, 1997, 22(4):339-342.
[19] 李瑞保. 东昆仑造山带(东段)晚古生代-早中生代造山作用研究:博士学位论文[D].西安:长安大学,2012. LI Rui-bao. Research on the Late Paleozoic-Early Mesozoic orogeny in East Kunlun orogen:doctor's degree thesis[D]. Xi'an:Chang'an University,2012.
[20] 毛景文,周振华,丰成友,等. 初论中国三叠纪大规模成矿作用及其动力学背景[J]. 中国地质,2012, 39(6):1437-1471. MAO Jing-wen, ZHOU Zhen-hua, FENG Cheng-you, et al. A preliminary study of the Triassic large-scale mineralization in China and its geodynamic setting[J]. Geology in China, 2012, 39(6):1437-1471.
[21] 高永宝. 东昆仑祁漫塔格地区中酸性侵入岩浆活动与成矿作用:博士学位论文[D].西安:长安大学,2013. GAO Yong-bao. The intermediate-acid intrusive magmatism and mineralization in Qimantage, East Kunlun Mountains:doctor's degree thesis[D]. Xi'an:Chang'an University,2013.
[22] DING Qing-feng, JIANG Shao-yong, SUN Feng-yue. Zircon U-Pb geochronology, geochemical and Sr-Nd-Hf isotopic compositons of the Trassic granite and diorite dikes from the Wulonggou mining area in the eastern Kunlun Orogen, NW China:petrogenesis and tectonic implications[J]. Lithos, 2014, 205:266-283.
[23] 陈永福,张栋,路英川,等. 青海鄂拉山北段耗牛沟铜金矿辉钼矿Re-Os年龄及其地质意义[J]. 地球学报,2016, 37(1):69-78. CHEN Yong-fu, ZHANG Dong, LU Ying-chuan, et al. Re-Os dating of molybdenite from the Maoniugou Cu-Au ore deposit in the northern part of the Ngola Mountain, Qinghai Province, and its geological significance[J]. Acta Geoscientica Sinica, 2016, 37(1):69-78.
[24] 奎明娟,柏红喜,古凤宝,等. 东昆仑构造岩浆带的划分及晚华力西期-燕山期岩石构造组合[J]. 青海大学学报(自然科学版),2010,28(5):49-55. KUI Ming-juan, BAI Hong-xi, GU Feng-bao, et al. Division of East Kunlun tectonic magmatic belt and the rock tectonic combination in the Late Variscan-Yanshanian period[J]. Journal of Qinghai University (Nature Science), 2010, 28(5):49-55.
[25] Liegeois L P. Preface:some words on the post-collisional magmatism[J]. Lithos, 1998, 45:15-17.
[26] Crawford A J, Corbett K D, Everard J. Geochemistry and tectonic setting of a Cambrian VMS-rich volcanic belt:the Mount Read volcanic, W Tasmania[J]. Economic Geology, 1992, 87:597-619.
[27] HOU Zeng-qian, WANG Li-quan, Khin Z, et al. Post-collisonal crustal extension setting and VHMS mineralization in the Jinshajiang orogenic belt, SW China[J]. Ore Geology Review, 2003, 22:177-199.
[28] 孙延贵. 西秦岭-东昆仑造山带的衔接转换与共和坳拉谷:博士学位论文[D].西安:西北大学,2004. SUN Yan-gui. Gonghe Aulaeogen and conjugate and transfer between the West Qinling and East Kunlun orogens:doctor's degree thesis[D]. Xi'an:Northwest University,2004.
[29] 王松,丰成友,李世金,等. 青海祁漫塔格卡尔却卡铜多金属矿区花岗闪长岩锆石SHRIMP U-Pb测年及其地质意义[J]. 中国地质,2009, 36(1):74-84. WANG Song, FENG Cheng-you, LI Shi-jin, et al. Zircon SHRIMP U-Pb dating of granodiorite in the Kaerqueka polymetallic ore deposit, Qimantage Mountain, Qinghai Province, and its geological implications[J]. Geology in China, 2009, 36(1):74-84.
[30] 李世金,孙丰月,丰成友,等. 青海东昆仑鸭子沟多金属矿的成矿年代学研究[J].地质学报,2008,82(7):949-955. LI Shi-jin, SUN Feng-yue, FENG Cheng-you, et al. Geochronological study on Yazigou polymetallic deposit in Eastern Kunlun, Qinghai Province[J]. Acta Geologica Sinica, 2008, 82(7):949-955.
[31] 高永宝,李文渊,钱兵,等. 东昆仑野马泉铁矿相关花岗岩体年代学、地球化学及Hf同位素特征[J]. 岩石学报,2014, 30(6):1647-1665. GAO Yong-bao, LI Wen-yuan, QIAN Bing, et al. Geochronology, geochemistry and Hf isotopic compositions of the granitic rocks related with iron mineralization in Yemaquan deposit, East Kunlun, NW China[J].Acta Petrologica Sinica, 2014, 30(6):1647-1665.
[32] 佘宏全,张德全,景向阳,等. 青海省乌兰乌珠尔斑岩铜矿矿床地质特征与成因[J]. 中国地质,2007, 34(2):306-314. SHE Hong-quan, ZHANG De-quan, JING Xiang-yang, et al. Geological characteristics and genesis of the Ulan Uzhur porphyry copper deposit in Qinghai[J]. Geology in China, 2007, 34(2):306-314.
[33] 许庆林,孙丰月,李碧乐,等. 东昆仑莫河下拉银多金属矿床花岗斑岩年代学、地球化学特征及构造背景[J]. 大地构造与成矿学,2014, 38(2):421-433. XU Qing-lin, SUN Feng-yue, LI Bi-le, et al. Geochronological dating, geochemical characteristics and tectonic setting of the granite-porphyry in the Mohexiala silver polymetallic deposit, eastern Kunlun orogenic belt[J]. Geotectonica et Metallogenia, 2014, 38(2):421-433.
[34] 奚仁刚,校培喜,伍跃中,等. 东昆仑肯德可克铁矿区二长花岗岩组成、年龄及地质意义[J]. 西北地质,2010, 43(4):195-202. XI Ren-gang, XIAO Pei-xi, WU Yue-zhong, et al. The geological significances, composition and age of the monzonitic granite in Kendekeke iron mine[J]. Northwestern Geology, 2010, 43(4):195-202.
[35] 常有英,李建放,张军,等. 青海那陵郭勒河东晚三叠世侵入岩形成环境及年代学研究[J]. 西北地质,2009, 42(1):57-65. CHANG You-ying, LI Jian-fang, ZHANG Jun, et al. Study of environment and chronology of Late Triassic intrusive rocks in East Nalinggele River of Qinghai[J]. Northwestern Geology, 2009, 42(1):57-65.
[36] 刘云华,莫宣学,喻学惠,等. 东昆仑野马泉地区景忍花岗岩锆石SHRIMP U-Pb定年及其地质意义[J]. 岩石学报,2006, 22(10):2457-2463. LIU Yun-hua, MO Xuan-xue, YU Xue-hui, et al. Zircon SHRIMP U-Pb dating of the Jingren granite, Yemaquan region of the East Kunlun and its geological significance[J]. Acta Petrologica Sinica, 2006, 22(10):2457-2463.
[37] 瞿泓莹,丰成友,裴荣富,等. 青海祁漫塔格虎头崖多金属矿区岩体热年代学研究[J]. 地质学报,2015, 89(3):498-509. QU Hong-ying, FENG Cheng-you, PEI Rong-fu, et al. Thermochronology of Hutouya skarn type copper-lead-zinc polymetallic ore district in the Qimantage area, Qinghai Province[J]. Acta Geologica Sinica, 2015, 89(3):498-509.
[38] 周建厚,丰成友,沈灯亮,等. 新疆祁漫塔格维宝矿区西北部花岗闪长岩年代学、地球化学及其构造意义[J].地质学报,2015, 89(3):473-486. ZHOU Jian-hou, FENG Cheng-you, SHEN Deng-liang, et al. Geochronology, geochemistry and tectonic implications of granodiorite in the Northwest of Weibao deposit, Xinjiang Qimantage[J]. Acta Geologica Sinica, 2015, 89(3):473-486.
[39] 夏锐,卿敏,王长明,等. 青海东昆仑托克妥Cu-Au(Mo)矿床含矿斑岩成因:锆石U-Pb年代学和地球化学约束[J]. 吉林大学学报(地球科学版),2014, 44(5):1502-1524. XIA Rui, QING Min, WANG Chang-ming, et al. The genesis of the ore-bearing porphyry of the Tuoketuo porphyry Cu-Au (Mo) deposit in the East Kunlun, Qinghai Province:constraints from zircon U-Pb geochronological and geochemistry[J]. Journal of Jilin University(Earth Science Edition), 2014, 44(5):1502-1524.
[40] 刘建楠,丰成友,亓峰,等. 青海都兰县下得波利铜钼矿区锆石U-Pb测年及流体包裹体研究[J]. 岩石学报,2012, 28(2):679-690. LIU Jian-nan, FENG Cheng-you, QI Feng, et al. SIMS zircon U-Pb and fluid inclusion studies of Xiadeboli Cu-Mo ore district in Dulan County, Qinghai Province, China[J]. Acta Petrologica Sinica, 2012, 28(2):679-690.
[41] 罗明非,莫宣学,喻学惠,等. 东昆仑香日德地区晚三叠世花岗岩LA-ICP-MS锆石U-Pb定年、岩石成因和构造意义[J]. 岩石学报,2014, 30(11):3229-3241. LUO Ming-fei, MO Xuan-xue, YU Xue-hui, et al. Zircon LA-ICP-MS U-Pb age dating, petrogenesis and tectonic implications of the Late Triassic granites from the Xiangride area, East Kunlun[J]. Acta Petrologica Sinica, 2014, 30(11):3229-3241.
[42] 吴中楠,计文化,何世平,等. 青海省兴海县日龙沟花岗闪长岩LA-ICP-MS锆石U-Pb年龄及地球化学特征[J]. 地质通报,2015, 34(9):1677-1688. WU Zhong-nan, JI Wen-hua, HE Shi-ping, et al. LA-ICP-MS zircon U-Pb dating and geochemical characteristics of granodiorite in Rilonggou area, Xinghai County, Qinghai Province[J]. Geological Bulletin of China, 2015, 34(9):1677-1688.
[43] 刘建平,赖健清,谷湘平,等. 青海赛什塘铜矿区侵入岩体地球化学及锆石LA-ICP-MS U-Pb年代学[J]. 中国有色金属学报,2012, 22(3):622-632. LIU Jian-ping, LAI Jian-qing, GU Xiang-ping, et al. Geochemistry and zircon LA-ICP-MS U-Pb geochronology of intrusive body in Saishitang copper deposit, Qinghai Province, China[J]. The Chinese Journal of Nonferrous Metals, 2012, 22(3):622-632.
[44] 青海省地质调查院. 1:25万"兴海幅"区域地质调查报告[R]. 西宁:青海省地质调查院,2005. Qinghai Geological Survey Institute. The regional geological survey report of "Xinghai" at the sacle of 1:250000[R].Xining:Qinghai Geological Survey Institute,2005.
[45] 丰成友,李东生,屈文俊,等. 青海祁漫塔格索拉吉尔矽卡岩型铜钼矿床铼-锇同位素定年及其地质意义[J]. 岩矿测试,2009, 28(3):223-227. FENG Cheng-you, LI Dong-sheng, QU Wen-jun, et al. Re-Os isotopic dating of molybdenite from the Suolajier skarn type copper-molybdenum deposit of Qimantage Mountain in Qinghai Province and its geological significance[J]. Rock and Mineral Analysis, 2009, 28(3):223-227.
[46] 于淼,丰成友,刘洪川,等. 青海尕林格矽卡岩性铁矿金云母40Ar/39Ar年代学及成矿地质意义[J]. 地质学报,2015, 89(3):510-521. YU Miao, FENG Cheng-you, LIU Hong-chuan, et al. 40Ar/39Ar geochronology of the Galingge large skarn iron deposit in Qinghai Province and geological significance[J]. Acta Geolgocia Sinica, 2015, 89(3):510-521.
[47] 周建厚,丰成友,王辉,等. 新疆祁漫塔格于沟子铁多金属矿辉钼矿Re-Os年龄及其地质意义[J]. 地质与勘探,2014, 50(1):1-7. ZHOU Jian-hou, FENG Cheng-you, WANG Hui, et al. Re-Os dating of molybdenite from the Yugouzi Fe-Cu(Mo) deposit in Qimantage, Xinjiang and its geological implications[J]. Geology and Exploration, 2014, 50(1):1-7.
[48] 肖晔,丰成友,李大新,等. 青海果洛龙洼金矿区年代学研究与流体包裹体特征[J]. 地质学报,2014, 88(5):895-902. XIAO Ye, FENG Cheng-you, LI Da-xin, et al. Chronology and fluid inclusions of the Guoluolongwa gold deposit in Qinghai Province[J]. Acta Geologica Sinica, 2014, 88(5):895-902.
[49] 李文良,夏锐,卿敏,等. 应用辉钼矿Re-Os定年技术研究青海什多龙矽卡岩型钼铅锌矿床的地球动力学背景[J]. 岩矿测试,2014, 33(6):900-907. LI Wen-liang, XIA Rui, QING Min, et al. Re-Os molybdenite ages of the Shenduolong skarn Mo-Pb-Zn deposit and geodynamic framework, Qinghai Province[J]. Rock and Mineral Analysis, 2014, 33(6):900-907.
[50] 邓文兵,裴先治,刘成军,等. 东昆仑东段香日德地区察汗陶勒盖正长花岗岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 地质通报,2016, 35(5):687-699. DENG Wen-bing, PEI Xian-zhi, LIU Cheng-jun, et al. LA-ICP-MS zircon U-Pb dating of the Chahantaolegai syenogranites in Xiangride area of East Kunlun and its geological significance[J]. Geological Bulletin of China, 2016, 35(5):687-699.
[51] 潘桂堂,丁俊,姚东生,等. 1:150万青藏高原及邻区地质图[M]. 成都:成都地图出版社,2004:1-133. PAN Gui-tang, DING Jun, YAO Dong-sheng, et al. The geological map of Qinghai-Tibet Plateau and its adjacent areas[M]. Chengdu:Chengdu Map Publishing House,2004:1-133.
本刊中的类似文章
1.李小亮,杨乐,张松涛,张万辉,覃泽礼,严正平,赵俊芳,李良.青海东昆仑驼路沟钻矿的成矿时代与成因[J]. 世界地质, 2022,41(3): 483-497
2.李冬怀,程纪星,万汉平,谢迎春,郝伟林.西藏续迈地热田 “热水河”深部热源通道及其成因[J]. 世界地质, 2022,41(2): 334-341
3.郑振华,张勤山,何利,田滔,李生虎.东昆仑东段益克郭勒侵入岩 LA-ICP-MS锆石 U-Pb定年及其地质意义[J]. 世界地质, 2022,41(1): 56-71
4.陈海福,李小亮,严正平,张松涛,王生龙,赵俊芳,李良.青海东昆仑龙什更铁钴矿成矿时代与成因类型[J]. 世界地质, 2021,40(4): 830-846
5.王焕鑫,孙丰月,张涛,闫佳铭,刘承先.青海东昆仑德里特萤石矿成因探讨:来自流体包裹体和稳定同位素的证据[J]. 世界地质, 2021,40(4): 807-815
6.何泽宇, 申俊峰, 王来明, 李国武, 刘汉栋, 张华锋, 杜佰松, 吴晋超.胶东宋家沟金矿中基性脉岩锆石U-Pb年代学、地球化学及其地质意义[J]. 世界地质, 2020,39(3): 509-527
7.王琳琳, 王力, 霍亮, 李予晋.电感耦合等离子体质谱法测定辉钼矿中稀土元素[J]. 世界地质, 2020,39(3): 731-736
8.刘雷, 钱烨, 孙丰月, 李予晋, 顾焱, 张建平.东昆仑群力地区晚泥盆世A型花岗岩的年代学、地球化学和构造意义[J]. 世界地质, 2019,38(1): 34-45
9.齐成栋, 张永焕, 彭玉鲸, 陈尔臻, 牛军平, 屈旭钧, 靳克, 王春光.吉林省成矿规律与预测的新认识[J]. 世界地质, 2017,36(3): 850-861
10.刘大中, 郝宇杰, 杨群, 赵书跃, 任云生.大兴安岭中北段古中公路钼矿床形成时代与矿床成因[J]. 世界地质, 2017,36(2): 507-519
11.邵建波, 陈殿义, 潘月栋, 王洪涛.吉林省中东部季德屯及石马洞大型钼矿床辉钼矿 Re-Os 同位素年龄及地质意义[J]. 世界地质, 2016,35(3): 717-728
12.白宜娜, 孙丰月, 钱烨, 刘洪川, 张德明.青海东昆仑尕林格铁多金属矿床辉石闪长岩 U-Pb 年代学及地球化学特征[J]. 世界地质, 2016,35(1): 17-27
13.仇银江, 张元厚.新疆东天山成矿带成矿系统研究现状及存在问题[J]. 世界地质, 2015,34(3): 624-638
14.李金超, 杜玮, 孔会磊, 贾群子, 栗亚芝, 南卡俄吾, 张雨莲.Pyrite; characteristics of trace elements; geological significance; Qibaoshan; Shandong Province[J]. 世界地质, 2015,34(3): 664-674
15.施彬, 刘力.东昆仑灶火沟早志留世花岗岩岩石学、地球化学特征及地质意义[J]. 世界地质, 2014,33(4): 758-767

Copyright by 世界地质