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    PAN Ming-chen, WANG Yong-mei, WANG Hai-peng, WANG Fu-jun, LIANG You-wei, LU Hong-feng, SUN Hai-long, LI Hong-mei, HU Hai-yan, MU Ya-nan, HONG Yan, XU Gui-yan. THE DERIWULANHADA CENTER-TYPE VOLCANIC EDIFICE IN HORQIN YOUYI ZHONGQI, INNER MONGOLIA[J]. Geology and Resources, 2015, 24(5): 414-417. DOI: 10.13686/j.cnki.dzyzy.2015.05.004
    Citation: PAN Ming-chen, WANG Yong-mei, WANG Hai-peng, WANG Fu-jun, LIANG You-wei, LU Hong-feng, SUN Hai-long, LI Hong-mei, HU Hai-yan, MU Ya-nan, HONG Yan, XU Gui-yan. THE DERIWULANHADA CENTER-TYPE VOLCANIC EDIFICE IN HORQIN YOUYI ZHONGQI, INNER MONGOLIA[J]. Geology and Resources, 2015, 24(5): 414-417. DOI: 10.13686/j.cnki.dzyzy.2015.05.004
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    THE DERIWULANHADA CENTER-TYPE VOLCANIC EDIFICE IN HORQIN YOUYI ZHONGQI, INNER MONGOLIA

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    • The Deriwulanhada center-type caldera edifice is the product of Late Jurassic volcanic activity, with periclinal introversion and developed annular and radial faults. The annular fractures are filled with a variety of dikes. The volcanic vent is occupied by trachyte, which is dated by isotopic age of 140.8 ±2.0 Ma.
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