董杰，新葡的京集团35222vip博雅博士后获得者，新葡的京集团35222vip特聘副研究员

研究领域：

研究方向为变质相平衡与造山带演化，重点研究高压-超高压和高温-超高温岩石的变质相平衡关系和叠加变质作用过程

教育经历：

2015.09-2020.06新葡的京集团35222vip

2011.09-2015.06吉林大学地球科学学院

代表成果：

1.Dong, J., Wei, C. J., Clarke, G. L., & Zhang, J. X. (2018). Metamorphic evolution during deep subduction and exhumation of continental crust: insights from felsic granulites in South Altyn Tagh, West China. Journal of Petrology, 59, 1965-1990.

2.Dong, J., Wei, C., & Zhang, J. (2019). Ultra high temperature metamorphism of mafic granulites from South Altyn Orogen, West China: A result from the rapid exhumation of deeply subducted continental crust. Journal of Metamorphic Geology, 37(3), 315-338.

3.Dong, J., Wei, C., Chen, J., & Zhang, J. (2020). P-T-t path of garnetites in south Altyn Tagh, west China: a complete record of the ultradeep subduction and exhumation of continental crust. Journal of Geophysical Research: Solid Earth, e2019JB018881.

4.Dong, J.,&Wei, C. (2021). Multi-stage metamorphism of the South Altyn ultrahigh-pressure metamorphic belt, West China: insights into tectonic evolution from continental subduction to arc–backarc extension. Journal of Petrology.

5.Dong, J.,Wei, C., & Song, S. (2021). Deep subduction and exhumation of micro-continents in the Proto-Tethys realm: Evidence from metamorphism of HP-UHT rocks in the North Qinling Orogen, central China. Gondwana Research.

负责项目：

东昆仑造山带低压麻粒岩变质相平衡、年代学及其构造意义，国家自然科学青年基金，2022.01.01-2024.12.31，在研

东昆仑金水口低压麻粒岩变质作用及其构造意义，2021.11.08-2022.06.15，中国博士后科学基金，在研

获奖情况：

2020年10月，获李四光优秀博士研究生奖