J. Li

发表

Paleoproterozoic ultrahigh-temperature granulites in the North China Craton: Implications for tectonic models on extreme crustal metamorphism

M. Santosh, T. Tsunogae, Shuwen Liu, 2012 .

The variety of subaerial active salt deformations in the Kuqa fold-thrust belt (China) constrained by InSAR

François Renard, R. Lohman, M. Doin, 2016 .

First application of the revised Ti-in-zircon geothermometer to Paleoproterozoic ultrahigh-temperature granulites of Tuguiwula, Inner Mongolia, North China Craton

M. Santosh, Shiran Liu, J. Li, 2010 .

Phase equilibrium modelling of Palaeoproterozoic ultrahigh‐temperature sapphirine granulite from the Inner Mongolia Suture Zone, North China Craton: implications for counterclockwise P–T path

M. Santosh, T. Tsunogae, S. J. Liu, 2013 .

Ultrahigh-temperature metamorphism in Daqingshan, Inner Mongolia Suture Zone, North China Craton

M. Santosh, T. Tsunogae, Shuwen Liu, 2011 .

Carbonic metamorphism at ultrahigh-temperatures: Evidence from North China Craton

Kei Sato, M. Santosh, T. Tsunogae, 2008 .

Note on the paper by Guochun Zhao, Simon A. Wilde, Sanzhong Li, Min Sun, Matthew L. Grant and Xuping Li, 2007, “U–Pb zircon age constraints on the Dongwanzi ultramafic–mafic body, North China, confirm it is not an Archean ophiolite”

T. Kusky, J. Li, 2008 .

Active surface salt structures of the western Kuqa fold-thrust belt, northwestern China

A. Webb, D. He, C. Colón, 2014 .

Ultrahigh temperature metamorphism of Tuguiwula khondalite belt, Inner Mongolia; metamorphic reaction texture and P-T indication

S. Liu, M. Santosh, J. Li, 2008 .