Xie Hangqiang

Published:2017-07-31

Details of the Faculty or Staff

Xie Hangqiang

Address: Institute of Geology, Chinese Academy of Geological Sciences

Baiwanzhuang Road 26, Beijing, 100037 P.R. China

Email: rock@bjshrimp.cn

Tel:010-6899 4878

Education Experience

  • 11 / 2009 – now  Institute of Geology, CAGS.; Researcher
  • 7 / 2007 – 11 / 2009  post-doctoral research centers in CAGS.; Post-doctor
  • / 2008 – 9 / 2008  Kwazulu-Natal Univeristy, South Afica.; Visiting scholar
  • 9 / 2002 – 7 / 2007  Institute of Geology and Geophysics, Chinese Academy of Science.; MA and Ph.D student 
  • 9 / 2001 – 9 / 2002  Pengze No. 1 high school.; Teacher 
  • 9 / 1997 – 9 / 2001  Department of Geography, East China Normal University 

Professional Experience

Research interests

Early Precambrian Geology (North China Craton, Kaapvaal Craton in Southern Africa); Geochronology, Zirconology

The early Precambrian crustal evolution in North China Craton in China

Kaapvaal Craton in Southern Africa. 

Awards and Honors, Academic posts

Scientific Research Projects

(1)The tectono-thermal events and tectonoic setting during the late Neoarchean in western Shandong. National Natural Science Foundation of China (NSFC). 2015.01-2018.12

(2)Application Demonstration Project for the in-site REE and Ti analysis of lunar sample using TOF-SIMS-REE. Sub-project of the National Specific Fund for Valuable Instruments 2014.10-2017.10

(3)The crustal formation and evolution in Eastern Ancient Terrane in the North China Craton and 1:50 000 special mapping in representative area. Geological Survey project. 2016.01-2018.12(second researcher)

(4)Finding several Paleoarchean granitoid-greenstone belts in Kaapvaal Craton;

(5)Proving the Paleoproterozoic strata show the characteristic of continental rift but not subduction zone;

(6)Widespread muti-stage crustal evolution was found in Anshan area and Late-Neoarchean magmatic mingling was found in western Shandong area;

(7)Confirming the 2.6 Ga metamorphism in Limpopo belt record the collision event and the Limpopo belt is an Archean collision orogen. More than 30 articles were published in recently 5 years, including 4 SCI articles with the first author.

Publications

(1) Finding several Paleoarchean granitoid-greenstone belts in Kaapvaal Craton;

(2) proving the Paleoproterozoic strata show the characteristic of continental rift but not subduction zone;

(3) Widespread muti-stage crustal evolution was found in Anshan area and Late-Neoarchean magmatic mingling was found in western Shandong area;

(4) Confirming the 2.6 Ga metamorphism in Limpopo belt record the collision event and the Limpopo belt is an Archean collision orogen. More than 30 articles were published in recently 5 years, including 4 SCI articles with the first author.

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