Earth:Honggeertu volcanic field
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Revision as of 18:11, 19 April 2022 by imported>Steve Marsio (update)
Template:Coord/display/intitle Honggeertu is a volcanic field in China , in the Nei Mongol Province.[1]
The field is formed by twelve basaltic cinder 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]
References
- ↑ 1.0 1.1 1.2 "Honggeertu". Smithsonian Institution. https://volcano.si.edu/volcano.cfm?vn=305010.
- ↑ 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. 213. pp. 1–74. doi:10.1130/SPE213-p1. ISBN 0-8137-2213-6.
- ↑ Wei, H.; Sparks, R.S.J.; Liu, R.; Fan, Q.; Wang, Y.; Hong, H.; Zhang, H.; Chen, H. et al. (February 2003). "Three active volcanoes in China and their hazards". Journal of Asian Earth Sciences 21 (5): 516. doi:10.1016/S1367-9120(02)00081-0. Bibcode: 2003JAESc..21..515W.
- ↑ 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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