A snapshot of the transition from monogenetic  volcanoes to composite volcanoes: case study on  the Wulanhada Volcanic Field (northern China)

Luo, Diao; Reichow, Marc K.; Hou, Tong; Santosh, M.; Zhang, Zhaochong; Wang, Meng; Qin, Jingyi; Yang, Daoming; Pan, Ronghao; Wang, Xudong; Holtz, François; Botcharnikov, Roman

doi:https://doi.org/10.5194/ejm-34-469-2022

Articles | Volume 34, issue 5

Eur. J. Mineral., 34, 469–491, 2022

https://doi.org/10.5194/ejm-34-469-2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Eur. J. Mineral., 34, 469–491, 2022

https://doi.org/10.5194/ejm-34-469-2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 34, issue 5

Research article

20 Oct 2022

Research article | 20 Oct 2022

A snapshot of the transition from monogenetic volcanoes to composite volcanoes: case study on the Wulanhada Volcanic Field (northern China)

Diao Luo et al.

Supplement

https://doi.org/10.5194/ejm-34-469-2022-supplement

Data sets

Supplementary information of Tables S1–S5 Diao Luo https://doi.org/10.5281/zenodo.7188369

Short summary

Volcanoes on Earth are divided into monogenetic and composite volcanoes based on edifice shape. Currently the evolution from monogenetic to composite volcanoes is poorly understood. There are two distinct magma chambers, with a deeper region at the Moho and a shallow mid-crustal zone in the Wulanhada Volcanic Field. The crustal magma chamber represents a snapshot of transition from monogenetic to composite volcanoes, which experience more complex magma processes than magma stored in the Moho.