The role of subduction channel mélanges and convergent subduction systems in the petrogenesis of post-collisional K-rich mafic magmatism in NW Tibet

2014/03/28 by Zhengfu Guo, Marjorie Wilson, Lihong Zhang +3 · 1 citation
Earth and Planetary Sciences · #Geological and Geochemical Analysis #earthquake and tectonic studies #High-pressure geophysics and materials

paper · doi:10.1016/j.lithos.2014.03.020

Citations

• Major and trace element composition of the depleted MORB mantle (DMM)
• Post-collision, Shoshonitic Volcanism on the Tibetan Plateau: Implications for Convective Thinning of the Lithosphere and the Source of Ocean Island Basalts
• A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram
• Nature of the Source Regions for Post-collisional, Potassic Magmatism in Southern and Northern Tibet from Geochemical Variations and Inverse Trace Element Modelling
• Geochemical Constraints on Leucogranite Magmatism in the Langtang Valley, Nepal Himalaya

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