世界地质 2017, 36(2) 346-360 DOI:   10.3969/j.issn.1004-5589.2017.02.003  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(6471KB)
[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
大兴安岭
内蒙古
索伦
玛尼吐组
锆石U-Pb
Lu-Hf同位素
本文作者相关文章
PubMed
大兴安岭中段索伦地区玛尼吐组火山岩年代学、地球化学及其构造背景
杜岳丹1, 和钟铧1, 隋振民2, 谭皓元1, 任子慧1
1. 吉林大学地球科学学院, 长春 130061;
2. 吉林农业大学 环境与资源学院, 长春 130118
摘要

索伦地区玛尼吐组火山岩岩相学鉴定为安山岩、粗安岩和英安岩,化学成分显示以玄武粗面安山岩、粗安岩为主,少量流纹岩。LA-ICPMS 锆石U-Pb定年结果显示其形成于130~132 Ma之间的早白垩世。地球化学特点上主要属高钾钙碱性系列。稀土总量较高(95.19~198.38)×10-6,轻重稀土分馏较明显(LREE/HREE=6.38~10.59),弱的负铕异常(δEu=0.68~1.01),富集大离子亲石元素(K、Rb、Th)和轻稀土元素,亏损高场强元素(Nb、Ta、P、Ti)。微量元素具高Sr(多>499×10-6)和低Yb(最大值为2.83×10-6<3.6×10-6)、Y(多<29.9×10-6)和高Sr/Y和低Rb/Sr比值,显示了弧火山岩的特征。正的εHft)值(7.3~13.7),锆石176Hf/177Hf 平均值为0.282 964,显示玛尼吐组安山质岩浆源区主要为岩石圈地幔和新增生下地壳的部分熔融,且岩浆形成的过程中受到了流体的改造作用。玛尼吐组火山岩形成于岛弧构造环境,该岛弧构造背景的产生可能与受古太平洋板块俯冲作用有关。

关键词 大兴安岭   内蒙古   索伦   玛尼吐组   锆石U-Pb   Lu-Hf同位素  
Zircon U-Pb ages, geochemical characteristics and tectonic implications of volcanic rocks from Manitu Formation of Suolun area in central Great Xing'an Range
DU Yue-dan1, HE Zhong-hua1, SUI Zhen-min2, TAN Hao-yuan1, REN Zi-hui1
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. College of Resources and Environmental Science, Jilin Agricultural University, Changchun 130118, China
Abstract:

The volcanic rocks in Manitu Formation of Suolun area are composed of andesite, trachy-andesite and dacite petrographically,but they are mainly basaltic andesite or trachy-andesite with minor rhyolite based on chemical composition. Zircon U-Pb dating results show that they formed in Early Cretaceous from 130 to 132 Ma. These volcanic rocks belong to high-K calc-alkaline series. They are high in total rare earth elements (∑REE=95.19×10-6~198.38×10-6), with high LREE/HREE(6.38~10.59) and negative Eu anomalies (δEu=0.68~1.01). The volcanic rocks are enriched in LILE(K, Rb, Th)and LREE, but depleted in HFSE(Nb, Ta, P, Ti). Trace elements are characterized by high Sr (>499×10-6), low Yb (the maximum is 2.83×10-6, <3.6×10-6) and Y (majority <29.9×10-6), and high ratio of Sr/Y and low ratio of Rb/Sr, indicating the characteristic of arc volcanic rocks. The volcanic rocks have positive values of εHf(t) (7.3~13.7), and the initial 176Hf/177Hf ratios for magmatic zircons is 0.282 964, suggesting that the andesitic magma of Manitu Formation was derived from the lithosphere mantle and partial melting of newly accreted lower crust, and is affected by the subduction fluid. Volcanic rocks of Manitu Formation formed in the island arc tectonic environment caused by the subductions of the Paleo-Pacific Plate beneath the Eurasian continent.

Keywords: central Great Xingan Range   Inner Mongolia   Suolun   Manitu Formation   zircon U-Pb dating   geochronology   Hf isotope  
收稿日期 2016-11-02 修回日期 2017-05-03 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2017.02.003
基金项目:

中国地质调查局区域地质调查项目(12120114012901).

通讯作者: 和钟铧(1968),男,教授,主要从事构造地质方面的研究.E-mail:hezhonghua@126.com
作者简介:
作者Email: hezhonghua@126.com

参考文献:

[1] 林强, 葛文春, 曹林, 等. 大兴安岭中生代双峰式火山岩的地球化学特征[J]. 地球化学, 2003, 32(3):208-222. LIN Qiang, GE Wen-chun, CAO Lin, et al. Geochemistry of Mesozoic volcanic rocks in Da Hinggan Ling: the bimodal volcanic rocks[J]. Geochimica, 2003, 32(3):208-222.
[2] 葛文春, 林强, 孙德有, 等. 大兴安岭中生代玄武岩的地球化学特征:壳幔相互作用的证据[J]. 岩石学报, 1999, 15(3):396-406. GE Wen-chun, LIN Qiang, SUN De-you, et al. Geochemical characteristics of the Mesozoic basalts in Da Hinggan Ling: evidence of the mantle crust interaction [J]. Acta Petrologica Sinica, 1999, 15(3):396-406.
[3] 葛文春, 吴福元, 周长勇, 等. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J]. 岩石学报, 2005,21(3):749-762. GE Wen-chun, WU Fu-yuan, ZHOU Chang-yong, et al. Zircon U-Pb ages and its significance of the Mesozoic granites in the Wulanhaote region, central Da Hinggan Mountain[J]. Acta Petrologica Sinica, 2005, 21(3):749-762.
[4] Wang F, Zhou X H, Zhang L C, et al. Late Mesozoic volcanism in the Great Xing'an Range (NE China): timing and implications for the dynamic setting of NE Asia[J]. Earth & Planetary Science Letters, 2006, 251(1/2):179-198.
[5] 张连昌, 陈志广, 周新华, 等. 大兴安岭根河地区早白垩世火山岩深部源区与构造-岩浆演化:Sr-Nd-Pb-Hf同位素地球化学制约[J]. 岩石学报, 2007, 23(11):2823-2835. ZHANG Lian-chang, CHEN Zhi-guang, ZHOU Xin-hua, et al. Characteristics of deep sources and tectonic-magmatic evolution of the Early Cretaceous volcanics in Genhe area, Da-Hinggan Mountains: constraints of Sr-Nd-Pb-Hf isotopic geochemistries [J]. Acta Petrol Sinica, 2007, 23(11):2823-2835.
[6] Zhang J H, Ge W C, Wu F Y, et al. Large-scale Early Cretaceous volcanic events in the northern Great Xing'an Range, northeastern China [J]. Lithos, 2008, 102(1):138-157.
[7] Zhang J H, Gao S, Ge W C, et al. Geochronology of the Mesozoic volcanic rocks in the Great Xing'an Range, northeastern China: implications for subduction-induced delamination [J]. Chemical Geology, 2010, 276(3):144-165.
[8] 周新华, 英基丰, 张连昌, 等. 大兴安岭晚中生代火山岩成因与古老地块物质贡献:锆石U-Pb年龄及多元同位素制约[J]. 地球科学, 2009, 34(1):1-10. ZHOU Xin-hua, YING Ji-feng, ZHANG Lian-chang, et al. The petrogenesis of Late Mesozoic volcanic rock and the contributions from ancient micro-continents:constraints from the zircon U-Pb dating and Sr-Nd-Pb-Hf isotopic systematics [J]. Earth Science, 2009, 34(1):1-10.
[9] 苟军, 孙德有, 赵忠华, 等. 满洲里南部白音高老组流纹岩锆石U-Pb定年及岩石成因[J]. 岩石学报, 2010, 26(1):333-344. GOU Jun, SUN De-you, ZHAO Zhong-hua, et al. Zircon LA-ICPMS U-Pb dating and petrogenesis of rhyolites in Baiyingaolao Formation from the southern Manzhouli, Inner-Mongolia [J]. Acta Petrol Sinica, 2010, 26(1):333-344.
[10] 孙德有, 苟军, 任云生, 等. 满洲里南部玛尼吐组火山岩锆石U-Pb年龄与地球化学研究[J]. 岩石学报, 2011, 27(10):3083-3094. SUN De-you, GOU Jun, REN Yun-sheng, et al. Zircon U-Pb dating and study on geochemistry of volcanic rocks in Manitu Formation from southern Manchuria, Inner Mongolia [J]. Acta Petrol Sinica, 2011, 27(10):3083-3094.
[11] 李永飞, 郜晓勇, 孙守亮. 大兴安岭中段突泉盆地玛尼吐组火山岩地球化学特征与40Ar/39Ar测年[J]. 地质与资源, 2013, 22(6):444-451. LI Yong-fei, GAO Xiao-yong, SUN Shou-liang. Geochemical characteristics and Laser 40Ar/39Ar dating of the volcanics from the Manitu Formation of Tuquan Basin in central Daxing'anling [J]. Geology and Resources, 2013, 22(6):444-451.
[12] Dong Y, Ge W C, Yang H, et al. Geochronology and geochemistry of Early Cretaceous volcanic rocks from the Baiyingaolao Formation in the central Great Xing'an Range, NE China, and its tectonic implications [J]. Lithos,2014, 205:168-184.
[13] 郭锋, 范蔚茗, 王岳军, 等. 大兴安岭南段晚中生代双峰式火山作用[J]. 岩石学报, 2001, 17(1):161-168. GUO Feng, FAN Wei-ming, WANG Yue-jun, et al. Petrogenesis of the Late Mesozoic bimodal volcanic rocks in the southern Da Hinggan Mts [J]. Acta Petrologica Sinica, 2001, 17(1):161-168.
[14] 吕志成, 段国正, 郝立波, 等. 大兴安岭中南段中生代中基性火山岩岩石学地球化学研究[J]. 高校地质学报, 2004, 10(2):186-198. LÜ Zhi-cheng, DUAN Guo-zheng, HAO Li-bo, et al. Petrological and geochemical studies on the intermediate-basic volcanic rocks from the Middle-South part of the Da Hinggan Mountains [J]. Geolgica Journal of China Universities, 2004, 10(2):186-198.
[15] 高晓峰, 郭锋, 范蔚茗, 等. 南兴安岭晚中生代中酸性火山岩的岩石成因[J]. 岩石学报, 2005, 21(3):737-748. GAO Xiao-feng, GUO Feng, FAN Wei-ming, et al. Origin of late Mesozoic intermediate-felsic volcanic rocks from the northern Da Hinggan Mountain, NE China [J]. Acta Petrol Sinica, 2005, 21(3):737-748.
[16] 高晓峰, 郭锋, 李超文. 南兴安岭晚中生代火山岩的岩石成因(Ⅱ): Pb同位素制约[J]. 中山大学学报:自然科学版, 2009, 48(6):121-126. GAO Xiao-feng, GUO Feng, LI Chao-wen, et al. Origin of Late Mesozoic volcanic rocks from the southern Da Hinggan Mountain, NE China (Ⅱ): constraints of Pb isotope [J]. Journal of Sun Yatsen University: Natural Science Edition, 2009, 48(6):121-126.
[17] 吴华英, 张连昌, 周新华, 等. 大兴安岭中段晚中生代安山岩年代学和地球化学特征及成因分析[J]. 岩石学报, 2008, 24(6):1339-1352. WU Hua-ying, ZHANG Lian-chang, ZHOU Xin-hua, et al. Geochronology and geochemical characteristics of the Late Mesozoic andesites in the central Da-Hinggan Mountains, and its genesis [J]. Acta Petrologica Sinica, 2008, 24(6):1339-1352.
[18] 杨扬, 高福红, 陈井胜, 等.赤峰地区中生代火山岩锆石U-Pb年代学证据[J]. 吉林大学学报: 地球科学版, 2012,42(增刊2):257-268. YANG Yang, GAO Fu-hong, CHEN Jing-sheng, et al. Zircon U-Pb ages of Mesozoic volcanic rocks in Chifeng area [J].Journal of Jilin University: Earth Science Edition, 2012, 42(Suppl.2):257-268.
[19] 邵济安, 张履桥, 牟保磊,等. 大兴安岭中生代伸展造山过程中的岩浆作用[J]. 地学前缘, 1999, 6(4):339-346. SHAO Ji-an, ZHANG Lü-qiao, MU Bao-lei. Magmatism in the Mesozoic extending orogenic process of Da Hinggan MTS[J].Earth Science Frontiers, 1999, 6(4):339-346.
[20] 葛文春, 林强, 孙德有, 等. 葛文春, 林强, 孙德有,等. 大兴安岭中生代两类流纹岩成因的地球化学研究[J]. 地球科学, 2000, 25(2):172-178. GE Wen-chun, LIN Qiang, SUN De-you, et al. Geochemical resarch into origins of two types of Mesozoic rhyolites in Daxing'anling [J]. Acta Geoscientica Sinica, 2000, 25(2):172-178.
[21] 高晓峰. 东北地区中生代火成岩Sr-Nd-Pb同位素填图及其对区域构造演化的制约:博士学位论文[D]. 广州:中国科学院研究生院, 2007. GAO Xiao-feng. Sr-Nd-Pb isotope mapping of Mesozoic igneous rocks in NE China: constraints on tectonic evolution of the eastern CAOB: doctor's degree thesis [D]. Guangzhou:Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, 2007.
[22] 范蔚茗, 郭锋, 高晓峰, 等.东北地区中生代火成岩Sr-Nd同位素区划及其大地构造意义[J]. 地球化学, 2008, 37(4):361-372. FAN Wei-ming, GUO Feng, GAO Xiao-feng, et al. Sr-Nd isotope mapping of Mesozoic igneous rocks in NE China: constraints on tectonic framework and crustal growth [J]. Geochimica, 2008, 37(4):361-372.
[23] Ying J F, Zhou X H, Zhang L C, et al. Geochronological framework of Mesozoic volcanic rocks in the Great Xing'an Range, NE China, and their geodynamic implications[J]. Journal of Asian Earth Sciences, 2010, 39(6):786-793.
[24] 许文良, 王枫, 裴福萍, 等.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J]. 岩石学报, 2013, 29(2):339-353. XU Wen-liang, WANG Feng, PEI Fu-ping, et al. Mesozoic tectonic regimes and regional ore-forming background in NE China: constraints from spatial and temporal variations of Mesozoic volcanic rock associations [J]. Acta Petrol Sinica, 2013, 29(2):339-353.
[25] 孟凡超, 刘嘉麒, 崔岩, 等.中国东北地区中生代构造体制的转变:来自火山岩时空分布与岩石组合的制约[J]. 岩石学报, 2014, 30(12):3569-3586. MENG Fan-chao, LIU Jia-qi, CUI Yan, et al. Mesozoic tectonic regimes transition in the Northeast China: constriants from temporal-spatial distributions of volcanic rocks [J]. Acta Petrologica Sinica, 2014, 30(12):3569-3586.
[26] Wu B Y, Niu H C, Cheng L R, et al. Geochronology, geochemistry and geodynamic implications of the Late Mesozoic volcanic rocks in the southern Great Xing'an Mountains, NE China [J]. Journal of Asian Earth Sciences, 2015, 113:454-470.
[27] 李世超, 徐仲元, 刘正宏, 等.大兴安岭中段玛尼吐组火山岩LA-ICP-MS锆石U-Pb年龄及地球化学特征[J]. 地质通报, 2013, 32(2):399-407. LI Shi-chao, XU Zhong-yuan, LIU Zheng-hong, et al. Zircon U-Pb dating and geochemical study of volcanic rocks in Manitu Formation of central Da Hinggan Mountains [J]. Geological Bulletin of China, 2013, 32(2):399-407.
[28] 陶传忠,李伫民,王大千,等.乌兰浩特地区玛尼吐组火山岩LA-ICP-MS锆石U-Pb定年及地球化学特征[J]. 地质与资源, 2015, 24(2):102-109. TAO Chuan-zhong, LI Zhu-min, WANG Da-qian, et al. LA-ICP-MS zircon U-Pb dating and geochemistry of the volcanic rocks from Manitu Formation in Ulanhot region of southern Daxing'anling [J]. Geology and Resources, 2015, 24(2):102-109.
[29] 孟宪锋, 张正平, 徐翠, 等.内蒙古东北部东乌珠穆沁旗乌兰哈德一带晚侏罗世满克头鄂博组的地质特征及岩性段划分[J]. 地质通报, 2010, 29(11):1649-1654. MENG Xian-feng, ZHANG Zheng-ping, XU Cui, et al. Geologic characteristics and lithologic member division in the Late Jurassic Manketou'ebo Formation in Wulanhade area, Dongwuzhumuqinqi, Inner Mongolia, China [J]. Geological Bulletin of China, 2010, 29(11):1649-1654.
[30] 张超, 杨伟红, 和钟铧, 等.大兴安岭中南段塔尔气地区满克头鄂博组流纹岩年代学和地球化学研究[J]. 世界地质, 2014, 33(2):255-265. ZHANG Chao, YANG Wei-hong, HE Zhong-hua, et al. Chronology and geochemistry of rhyolites in Manketou'ebo Formation from Ta'erqi area, southern-central Greater Xing'an Range [J]. Global Geology, 2014, 33(2):255-265.
[31] Ji Z, Ge W C, Wang Q H, et al. Petrogenesis of Early Cretaceous volcanic rocks of the Manketouebo Formation in the Wuchagou region, central Great Xing'an Range, NE China, and tectonic implications: geochronological, geochemical, and Hf isotopic evidence[J]. International Geology Review, 2015, 58(5):1-18.
[32] 张乐彤, 李世超, 赵庆英, 等.大兴安岭中段白音高老组火山岩的形成时代及地球化学特征[J]. 世界地质, 2015, 34(1):44-54. ZHANG Le-tong, LI Shi-chao, ZHAO Qing-ying, et al. Formation age and geochemical characteristics of volcanic rocks from Baiyingaolao Formation of middle Da Hinggan Mountains [J]. Global Geology, 2015, 34(1):44-54.
[33] 肖中军, 王振强, 吴煜, 等.内蒙古苏尼特左旗白音乌拉北部白音高老组时代重新厘定:来自LA-ICP-MS锆石U-Pb年龄的证据[J]. 地质通报, 2015, 34(9):1706-1714. XIAO Zhong-jun, WANG Zhen-qiang, WU Yu, et al. Redetermination of the age of Baiyingaolao Formation in Sonid Left Banner, Inner-Mongolia:evidence from LA-ICP-MS U-Pb dating of zircons [J]. Geological Bulletin of China, 2015, 34(9):1706-1714.
[34] 司秋亮, 崔天日, 王恩德, 等.大兴安岭柴河白音高老组流纹岩锆石U-Pb定年及成因探讨[J]. 东北大学学报:自然科学版, 2016, 37(3):412-415. SI Qiu-liang, CUI Tian-ri, WANG En-de, et al. Zircon U-Pb dating and petrogenesis of the Baiyingaolao Formation rhyolites in Chaihe area, Great Xing'an Range [J]. Journal of Northeastern University: Natural Science, 2016, 37(3):412-415.
[35] 司秋亮, 崔天日, 唐振, 等.大兴安岭中段柴河地区玛尼吐组火山岩年代学、地球化学及岩石成因[J]. 吉林大学学报: 地球科学版, 2015, 45(2):389-403. SI Qiu-liang, CUI Tian-ri, TANG Zhen, et al. Chronology, geochemistry and petrogenesis of the volcanic rocks in Manitu Formation in Chaihe area, central Great Xing'an Range [J]. Journal of Jilin University: Earth Science Edition , 2015, 45(2):389-403.
[36] 葛文春, 吴福元, 周长勇,等. 兴蒙造山带东段斑岩型Cu, Mo矿床成矿时代及其地球动力学意义[J]. 科学通报, 2007, 52(20):2407-2417. GE Wen-chun,WU Fu-yuan, ZHOU Chang-yong, et al. Porphyry Cu-Mo deposits in the eastern Xing'an Mongolian orogenic belt: mineralization ages and their geodynamic implications [J]. Chinese Bulletin, 2007, 52(20):2407-2417.
[37] 葛文春, 吴福元, 周长勇,等. 大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约[J]. 科学通报, 2005, 50(12):1239-1247. GE Wen-chun, WU Fu-yuan, ZHOU Chang-yong, et al. Emplacement age of Tahe granite and its constraints on the tectonic nature of the Erguna block in the northern part of the Da Hinggan Range [J].Chinese Science Bulletin, 2005, 50(12):1239-1247.
[38] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earthences, 2011, 41(1):1-30.
[39] 隋振民, 葛文春, 徐学纯, 等. 大兴安岭十二站晚古生代后造山花岗岩的特征及其地质意义[J]. 岩石学报, 2009, 25(10):2679-2686. SUI Zhen-min, GE Wen-chun, XU Xue-chun, et al. Characteristics and geological implications of the Late Paleozoic post-orogenic Shierzhan granite in the Great Xing'an Range [J]. Acta Petrological Sinica, 2009, 25(10):2679-2686.
[40] Andersen T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192(1/2):59-79.
[41] Yuan H, Gao S, Liu X, et al. Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma-mass spectrometry[J]. Geostandards & Geoanalytical Research, 2007, 28(3):353-370.
[42] Wu F Y, Yang Y H, Xie L W, et al. Hf isotopic compositions of the standard zircons and bad-deleyites used in U-Pb geochronology [J].Chemical Geology, 2006, 234(1/2):105-126.
[43] 郑吉林, 张文强, 徐立明, 等. 大兴安岭玻乌勒山地区玛尼吐组火山岩地球化学特征及成矿预测[J]. 黄金科学技术, 2015, 23(01):46-52. ZHENG Ji-lin, ZHANG Wen-qiang, XU Li-ming, et al. Geochemistry characteristics and metallogenic prognosis of the volcanic rocks from Manitu Formation of Bowule Mountain area in Da Hinggan Mountain [J]. Gold Science and Technology, 2015, 23(1):46-52.
[44] Xu W L, Pei F P, Wang F, et al. Spatial-temporal relationships of Mesozoic volcanic rocks in NE China: constraints on tectonic overprinting and transformations between multiple tectonic regimes [J]. Journal of Asian Earth Sciences, 2013, 74:167-193.
[45] 唐杰, 许文良, 王枫,等. 张广才岭帽儿山组双峰式火山岩成因:年代学与地球化学证据[J]. 世界地质, 2011, 30(04):508-520. TANG Jie, XU Wen-liang, WANG Feng, et al. Petrogenesis of bimodal volcanic rocks from Maoershan Formation in Zhangguangcai range: evidence from geochronology and geochemistry [J]. Global Geology, 2011, 30(4):508-520.
[46] 纪政, 葛文春, 杨浩,等. 大兴安岭中段塔尔气地区早白垩世花岗岩成因及形成构造环境[J]. 世界地质, 2016, 35(2):283-296. JI Zheng, GE Wen-chun, YANG Hao, et al. Petrogenesis of Early Cretaceous granites in Taerqi area of central Great Xing'an Range and its tectonic setting [J]. Global Geology, 2016, 35(2):283-296.
[47] Yang W B, Niu H C, Cheng L R, et al. Geochronology, geochemistry and geodynamic implications of the Late Mesozoic volcanic rocks in the southern Great Xing'an Mountains, NE China[J]. Journal of Asian Earth Sciences, 2015, 113:454-470.

本刊中的类似文章
1. 李刚, 刘正宏.内蒙古西部狼山温更逆冲断层的地质特征[J]. 世界地质, 2009,28(4): 451-459
2. 于峻川, 韩振哲, 尹志刚, 李振德, 吕军, 李文龙, 李娟娟.大兴安岭东北部早白垩世秀山火山-侵入杂岩体特征及成因[J]. 世界地质, 2009,28(4): 414-423
3. 杨亮平, 查恩爽, 姜振蛟, 刘丽.内蒙古清水河水源地地下水允许开采量计算[J]. 世界地质, 2009,28(2): 233-236
4.葛玉辉,孙春林,王玉芬.内蒙古石拐盆地召沟组植物群及地质时代[J]. 世界地质, 2010,29(2): 175-182
5.赵春波,吕希华,吴国学.内蒙古乌努格吐山铜钼矿地质特征及找矿方向[J]. 世界地质, 2010,29(2): 234-239
6. 李吉焱, 杜金锐 , 叶水盛, 许亚明.SWOT 分析法在矿产资源开发利用中的探讨——以内蒙古锡林郭勒盟为例[J]. 世界地质, 2010,29(4): 677-682
7. 赵华雷, 郗爱华, 刘俊梅, 王守仁, 龚鹏辉.内蒙古西乌珠穆沁旗阿拉坦高勒钒钛磁铁矿矿床地质特征[J]. 世界地质, 2011,30(1): 39-45
8.隋振民,陈跃军.大兴安岭东部花岗岩类锆石饱和温度及其地质意义[J]. 世界地质, 0,(): 162-172
9.杨明春,刘永江,韩国卿,王长兵,温泉波,赵英利,梁琛岳,米晓楠.内蒙古伊敏地区下石炭统红水泉组砂岩物源分析及其构造意义[J]. 世界地质, 2011,30(2): 192-207
10.隋振民,陈跃军.大兴安岭东部花岗岩类锆石饱和温度及其地质意义[J]. 世界地质, 2011,30(2): 162-172
11. 于延秋, 郭守钰, 王立峰.内蒙古狼山浩日格山海西期花岗岩体特征与形成环境[J]. 世界地质, 2011,30(3): 345-351
12. 唐杰, 许文良, 王枫, 高福红, 曹花花.张广才岭帽儿山组双峰式火山岩成因: 年代学与地球化学证据[J]. 世界地质, 2011,30(4): 508-520
13. 张健, 陈井胜, 李泊洋, 高妍, 张彦龙.内蒙古塔尔气地区晚古生代花岗岩的锆石U--Pb 年龄及Hf 同位素特征[J]. 世界地质, 2011,30(4): 521-531
14. 唐臣, 杨帆, 孙景贵, 王清海, 陈行时.大兴安岭旁开门金银矿床赋矿围岩的锆石U--Pb 年龄及其地质意义[J]. 世界地质, 2011,30(4): 532-537
15. 庄云, 韦咏梅, 冯硕颖, 董永胜, 王可勇.内蒙古阿力奔铅多金属矿床地质特征及矿床成因[J]. 世界地质, 2011,30(4): 554-560

Copyright by 世界地质