41°28′N 113°00′E / 41.47°N 113°E / 41.47; 113 Honggeertu is a volcanic field in China, in the Nei Mongol Province.
The field is formed by twelve basaltic cinder cones. Some of the cones formed on a fault. It may be of Holocene age. Young lava flows from this field look much younger than these of Quaternary volcanoes in the neighbourhood. 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.
References
- ^ "Honggeertu". Global Volcanism Program. Smithsonian Institution.
- 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. ISBN 0-8137-2213-6. ISSN 0072-1077.
- 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.
- Zheng, Yong; Shen, Weisen; Zhou, Longquan; Yang, Yingjie; Xie, Zujun; Ritzwoller, Michael H. (2011). "Ambient Noise Tomography of North east ern China, the Korean Peninsula, and the Sea of Japan". Journal of Geophysical Research: 18–19. doi:10.1029/2011JB008637.
External links
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