潘明臣, 王咏梅, 王海鹏, 王福君, 梁有为, 鲁红峰, 孙海龙, 李红梅, 胡海彦, 穆亚男, 洪岩, 徐桂岩. 内蒙古科右中旗德日乌兰哈达中心式火山机构[J]. 地质与资源, 2015, 24(5): 414-417. DOI: 10.13686/j.cnki.dzyzy.2015.05.004
    引用本文: 潘明臣, 王咏梅, 王海鹏, 王福君, 梁有为, 鲁红峰, 孙海龙, 李红梅, 胡海彦, 穆亚男, 洪岩, 徐桂岩. 内蒙古科右中旗德日乌兰哈达中心式火山机构[J]. 地质与资源, 2015, 24(5): 414-417. DOI: 10.13686/j.cnki.dzyzy.2015.05.004
    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

    内蒙古科右中旗德日乌兰哈达中心式火山机构

    THE DERIWULANHADA CENTER-TYPE VOLCANIC EDIFICE IN HORQIN YOUYI ZHONGQI, INNER MONGOLIA

    • 摘要: 德日乌兰哈达中心式破火山机构是晚侏罗世时火山活动产物,围斜内倾,环状、放射状断裂发育,环状断裂以各种岩脉充填.火山通道为粗面岩所占据,测其同位素年龄140.8±2.0 Ma.

       

      Abstract: 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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