The field is formed by twelve
basalticcinder cones.[1] Some of the cones formed on a
fault.[2] It may be of
Holocene age.[1] Young
lava flows from this field look much younger than these of
Quaternary volcanoes in the neighbourhood.[3] The volcanism may originate in the tectonic effects of the movement of the
Ordos Block.
Seismic tomography indicates the presence of a low velocity region at the volcano.[4]
^Whitford-Stark, J. L. (1987). "A survey of Cenozoic volcanism on mainland Asia". A Survey of Cenozoic Volcanism on Mainland Asia. Geological Society of America Special Papers. Vol. 213. pp. 1–74.
doi:
10.1130/SPE213-p1.
ISBN0-8137-2213-6.
ISSN0072-1077.
^Wei, H.; Sparks, R.S.J.; Liu, R.; Fan, Q.; Wang, Y.; Hong, H.; Zhang, H.; Chen, H.; Jiang, C.; Dong, J.; Zheng, Y.; Pan, Y. (February 2003). "Three active volcanoes in China and their hazards". Journal of Asian Earth Sciences. 21 (5): 516.
Bibcode:
2003JAESc..21..515W.
doi:
10.1016/S1367-9120(02)00081-0.