- [1]15. Co. P.I., Robert Bosch Fund from Germany（Science Bridge: Asia Grant Request for Support for an Initiation Project）, Grant No.：32.5.8003.0105.0, P.I., Prof. Joern Kruhl, Technique University of Munich, Germany, 2011.9-2012.4
- [2]14. Co. P.I., National Science Foundation of China, Key Project from the Key Research Program, Global comparison between North China craton and world classical craton: Implications to the decratonization and continental growth. 2011.1-2014.12, P.I. Prof. Timothy Kusky, Grant No.: 91014002.
- [3]13. P.I., Opening fund from Three Gorges Geohazards Research Center, Ministry of Education, China University of Geosciences, Wuhan, China. Microstructures characters and tectonic significances of ultramafic rocks (Miaowan Ophiolite rocks) in Southwestern Huangling anticline, Three Gorges reservoir area. 2010. 1-2011.12. Grant No.: TGRC201024
- [4]12. P.I., Special Fund for Outstanding Postdoctoral Research, Geometry and geneisis of In-situ partial melting of UHP eclogite in Sulu belt, China; 2011.1-2012.12; Grant No.: 201104495
- [5]11. P.I., China Postdoctoral Science Foundation, Microstructures characters and tectonic significances of Miaowan ophiolite rocks in Southwestern Huangling anticline. 2010.7-2011.12; Grant No.: 20100471203
- [6]10. P.I., Natural Science Foundation of Shandong Province. Structural Evolution and High precision structural analysis of multistage overprinted folding events in UHP-HP metamorphic terrain, Yangkou. 2009.1-2011.12，Grant No：Q2008E03.
- [7]9. P.I., National Natural Science Foundation of China, High precision structural analysis and rheology study on multistage overprinted folding events in UHP-HP metamorphic terrain, Yangkou. 2009.1-2011.12，Grant No：40802045
- [8]8. P.I., National Natural Science Foundation of China, Partial melting of deep subducted eclogite and its rheological significance to the continental collision, 2013.1-2016.12, Grant No.: 41272225
- [9]7. P.I., the Fundamental Research Funds for the Central Universities, 2012219279-CUG120818, Preservation of intergranular coesite and deformation mechanism within UHP eclogite from Yangkou Bay, Sulu orogen. 2013.1-2014.12
- [10]6. P.I., the Fundamental Research Funds for the Central Universities, "Tengfei Program", G1323511572, Partial melting of HP-UHP metamorphic rocks within subduction zone, 2015.1-2017.12
- [11]5. P.I., National Natural Science Foundation of China, P-T-t-Deformation-Melting evolution process of UHP eclogite and its rheological significance, 2016.1-2019.12, Grant No.: 41572182，
- [12]4. Co. P.I., National Science Foundation of China, Key Project from the Key Research Program “Geodynamic Systems of the Tethys”, Lateral escape and the Formation of New Plate Boundaries During Continental Collision. 2018.1-2021.12, Grant No.: 91755213.
- [13]3. Co. P.I., National Science Foundation of China, China-Mongolia Science and Technology Collaboration Fund, Accretionary tectonics in the SE Mongolia: implications for correlation with the Chinese segment of CAOB, 2020.1-2022.12, Grant No.: 41961144020
- [14]2. P.I., National Natural Science Foundation of China, Partial melting of meta-basic rocks in the northern Sulu orogen: correlations among structural geology, P-T-t path and melt-fluid evolution, 2021.1-2024.12, Grant No.: 40272228
- [15]1. P.I., GPMR MOST Special Fund, Record of geological process at the rigid plate boundaries of early earth: implications to ore-deposit resources and habitable earth, 2022.1-2024.12, MSFGPMR2022-7
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