Cite
Partial melting mechanisms of peraluminous felsic magmatism in a collisional orogen: An example from the Khondalite belt, North China craton.
MLA
Huang, Guangyu, et al. “Partial Melting Mechanisms of Peraluminous Felsic Magmatism in a Collisional Orogen: An Example from the Khondalite Belt, North China Craton.” Journal of Metamorphic Geology, vol. 42, no. 6, Aug. 2024, pp. 817–41. EBSCOhost, https://doi.org/10.1111/jmg.12774.
APA
Huang, G., Liu, H., Guo, J., Palin, R. M., Zou, L., & Cui, W. (2024). Partial melting mechanisms of peraluminous felsic magmatism in a collisional orogen: An example from the Khondalite belt, North China craton. Journal of Metamorphic Geology, 42(6), 817–841. https://doi.org/10.1111/jmg.12774
Chicago
Huang, Guangyu, Hao Liu, Jinghui Guo, Richard M. Palin, Lei Zou, and Weilong Cui. 2024. “Partial Melting Mechanisms of Peraluminous Felsic Magmatism in a Collisional Orogen: An Example from the Khondalite Belt, North China Craton.” Journal of Metamorphic Geology 42 (6): 817–41. doi:10.1111/jmg.12774.