马旭东 副研究员

来源:地调局资源所 发布时间:2017-10-24
 

 

姓名:

马旭东

性别:

 

职称:

副研究员

学位:

博士

 

电话:

010-68999049

传真:

 

 

Email

maxudong2011@126.com

邮编:

100037

 

地址:

北京市西城区百万庄大街26

 

 

说明: 证件照-白底

 

更多信息:

 

   

 

简历:

马旭东,1982年出生于辽宁省。现为中国地质科学院矿产资源研究所副研究员,硕士生导师。
   
长期从事早前寒武纪地壳增生与演化及相关矿产,碰撞造山过程中的岩浆与成矿作用研究。先后主持或参加自然科学基金,重大基础研究(973)等国家级项目10余项,中国地质大调查项目多项,目前,已发表论文26篇,其中第一作者/通讯作者在《Precambrian research》、《Ore geology review》、《Journal of geochemical exploration》、《International geology review》及《Geological journal》等国内外地质学、矿床学及岩石学领域刊物上发表SCIEI论文13篇。


学习、工作经历:

2001-2005年,西北大学 地质学专业,本科

2005-2011年,中国科学院地质与地球物理研究所,矿物学、岩石学、矿床学专业,博士

2011-2013年,中国科学院地质与地球物理研究所,地质工程与地质资源, 博士后

2013-至今,中国地质科学矿产资源研究所,助理研究员、副研究员

  

   

 

学科类别:

矿物学、岩石学、矿床学

前寒武纪地质学

 

研究方向:

1.早前寒武纪地壳增生与演化及相关金属非金属矿产

2.碰撞造山过程中的岩浆与成矿作用

 

职务:

   

 

 

承担科研项目情况:

家自然科学基金面上项目固阳花岗-绿岩地体 ~2.5Ga岩浆作用与地壳增生机制

(项目编号:41572174, 2016.01-2019.12,直接经费:70万元.

家自然科学基金青年项目华北克拉通西部晚太古代固阳高镁闪长岩成因与阴山地块演化

(项目编号:41202138, 2013.01-2015.12,经费:25万元.

中国博后基金“华北克拉通西部晚太古代固阳高镁闪长岩体中包体研究”(项目编号:2012M510539, 2012.01-2014.12,经费:5万元

中国地质调查工作项目大型矿集区时空结构与巨量金属富集机理研究” (项目编号:DD201901672019.01-2021.12,参与).

中国地质调查工作项目藏西北铜多金属资源基地综合调查评价” (项目编号:DD201901672019.01-2021.12,参与).

中国地质调查工作项目西藏申扎县雄梅1/5万四幅矿产地质调查” (项目编号:DD201600262016.01-2018.12,参与)

中国地质调查工作项目西藏班公湖-怒江成矿带中段铜矿调查评价” (项目编号:121201130373002014.01-2016.12,参与).

 

获奖及荣誉:

  

 

代表性论文:

第一作者及通讯作者:

1Ma, X*., Guo, J., Chen, L., Chu, Z. (2010). Re-Os isotopic constraint to the age of in komatiites in the Neoarchean Guyang greenstone belt, North China Craton. Chinese Science Bulletin, 55(27-28), 3197-3204.

2马旭东*,范宏瑞,郭敬辉,2013,阴山地块晚太古代岩浆作用、变质作用对地壳演化及

BIF 成因的启示,岩石学报,29(7)2329-2339

3Ma, X*., Guo, J., Liu, F., Qian, Q., Fan, H. (2013). Zircon U-Pb ages, trace elements and Nd-Hf isotopic geochemistry of Guyang sanukitoids and related rocks: Implications for the Archean crustal evolution of the Yinshan Block, North China Craton. Precambrian Research, 230, 61-78.

4Ma, X., Fan, H. R*., Santosh, M., Guo, J. (2013). Geochemistry and zircon U-Pb chronology of charnockites in the Yinshan Block, North China Craton: tectonic evolution involving Neoarchaean ridge subduction. International Geology Review, 55(13), 1688-1704.

5Ma, X., Fan, H. R*., Santosh, M., Liu, X., Guo, J. H. (2014). Origin of sanukitoid and hornblendite enclaves in the Dajitu pluton from the Yinshan Block, North China Craton: product of Neoarchaean ridge subduction?. International Geology Review, 56(10), 1197-1212.

6Ma, X., Fan, H. R*., Santosh, M., Guo, J. (2014). Chronology and geochemistry of Neoarchean BIF-type iron deposits in the Yinshan Block, North China Craton: Implications for oceanic ridge subduction. Ore Geology Reviews, 63, 405-417.

7Ma, X*., Fan, H. R., Santosh, M., Guo, J. (2016). Petrology and geochemistry of the Guyang hornblendite complex in the Yinshan block, North China Craton: Implications for the melting of subduction-modified mantle. Precambrian Research, 273, 38-52.

8Ma, X*., Zhong, Y. (2017). Geochronology of the Guyang Granite-Greenstone Terrene and the Implications for Continental Crust Growth. Acta Geologica Sinica (English Edition), 91(4), 1499-1500.

9Ma, X*., Zhong, Y. (2018). Geochemistry and chronology of a diorite pluton in the Yinshan Block, implications for crustal growth and evolution of North China Craton. Geological Journal, 53(6), 2849-2862.

10Hou, K*., Ma, X*., Li, Y., Liu, F., Han, D. (2017). Chronology, geochemical, Si and Fe isotopic constraints on the origin of Huoqiu banded iron formation (BIF), southeastern margin of the North China Craton. Precambrian Research, 298, 351-364.

11Hou, K., Ma, X*., Li, Y., Liu, F., Han, D. (2019). Genesis of Huoqiu banded iron formation (BIF), southeastern North China Craton, constraints from geochemical and Hf-OS isotopic characteristics. Journal of Geochemical Exploration, 197, 60-69.

12Zhong, Y, Ma, X.*, Li, H-K., Zhai, M.G. (2019). Revisit and comparative analysis of the typical graphite deposits in the Paleoproterozoic khondalite series, western North China Craton: implications for genesis, depositional environment and prospecting potential, Ore Geology Reviews . 109, 370-380

13、王韵,马旭东*,陈伟,曾勇杰,曲晓明 (2018),班-怒带中段晚白垩世后碰撞岩浆钨矿化的发现及其意义,矿床地质,37(4)885-888.

14、王韵,马旭东*,陈伟,曲晓明,宋扬,唐菊兴 (2019),班公湖-怒江成矿带中早白垩世含铜岩体地球化学特征:以雄梅地区为例. 矿床地质,38 (1)181-196.

15马旭东*,钟焱,陈雅丽,曲晓明 (2019),华北克拉通孔兹岩带内孔兹岩系沉积过程对石墨矿床成矿的控制,大地构造与成矿学,10.16539/j.ddgzyckx.2019.02.015

 

合作论文:

16Zhao, L., Zhai, M., Zhou, X., Santosh, M., Ma, X. 2016, Thermal gradient and geochronology of a Paleozoic high-grade terrane in the northeastern Cathaysia block, South China. Tectonophysics, 691, 311-327.

17Zhong, Y., Zhai, M., Peng, P., Santosh, M., Ma, X. 2015, Detrital zircon U–Pb dating and whole-rock geochemistry from the clastic rocks in the northern marginal basin of the North China Craton: Constraints on depositional age and provenance of the Bayan Obo Group. Precambrian Research, 258, 133-145.

18Zhao, L., Zhai, M., Zhou, X., Santosh, M., Ma, X. 2015, Geochronology and geochemistry of a suite of mafic rocks in Chencai area, South China: Implications for petrogenesis and tectonic setting. Lithos, 236, 226-244.

19Zhao, L., Zhou, X., Zhai, M., Santosh, M., Ma, X., Shan, H., Cui, X. 2014, Paleoproterozoic tectonic transition from collision to extension in the eastern Cathaysia Block, South China: evidence from geochemistry, zircon U-Pb geochronology and Nd-Hf isotopes of a granite-charnockite suite in southwestern Zhejiang. Lithos, 184, 259-280.

20、陈伟,宋扬,曲晓明,孙渺,丁吉顺,马旭东2019,北拉萨块体唐江穷果岩体中由同源岩浆不同期次之间混合产生的暗色包体:一种新的暗色包体岩石成因.地球科学. http://kns.cnki.net/kcms/detail/42.1874.P.20180704.1739.006.html

21、孙渺,陈伟,曲晓明,马旭东,丁吉顺,2018.西藏雄梅地区晚白垩世江巴组火山岩岩石成因及对加厚地壳减薄的指示.地球科学,43(9): 3234-3251.

22、黎心远,陈伟,曲晓明,马旭东2018,西藏申扎县雄梅铜矿床的硫、铅同位素特征及其成矿意义. 矿床地质,37(3): 643-655.

23、王佳奇,曲晓明,马旭东,范淑芳,宋扬,2016,西藏雄梅铜矿区含矿斑岩与非含矿斑岩成因对比研究. 矿床地质,35(3): 437-455.

24、钟焱,陈雅丽,翟明国,马旭东2016,华北克拉通西部古元古代孔兹岩系的地层对比、岩相古地理特征及其地质意义,岩石学报,32(3) : 713-726.

25、曲晓明,范淑芳,马旭东,宋扬,2015,西藏班公湖-怒江成矿带上的碰撞后铜矿床,矿床地质,34 (3) : 431-448.

 

 

 

代表性专著: