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HONGGEERTU Latitude and Longitude:

41°28′N 113°00′E / 41.47°N 113°E / 41.47; 113 [1]
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41°28′N 113°00′E / 41.47°N 113°E / 41.47; 113 [1] 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. ^ a b c d "Honggeertu". Global Volcanism Program. Smithsonian Institution.
  2. ^ 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.
  3. ^ 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.
  4. ^ 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.

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