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    万永平, 王根厚, 郭春影, 于海亮, 张静. 2007: 京西房山岩体南侧青白口系下马岭组构造片岩中红柱石的变形特征及其地质意义. 地质通报, 26(2): 200-205.
    引用本文: 万永平, 王根厚, 郭春影, 于海亮, 张静. 2007: 京西房山岩体南侧青白口系下马岭组构造片岩中红柱石的变形特征及其地质意义. 地质通报, 26(2): 200-205.
    shu
    WAN Yong-ping, WANG Gen-hou, GUO Chun-ying, YU Hai-liang, ZHANG Jing. 2007: Deformation features of andalusite in tectonic schist of the Xiamaling Formation of the Qingbaikouan System on the southern side of the Fangshan pluton in the Western Hills, Beijing, Chian. Geological Bulletin of China, 26(2): 200-205.
    Citation: WAN Yong-ping, WANG Gen-hou, GUO Chun-ying, YU Hai-liang, ZHANG Jing. 2007: Deformation features of andalusite in tectonic schist of the Xiamaling Formation of the Qingbaikouan System on the southern side of the Fangshan pluton in the Western Hills, Beijing, Chian. Geological Bulletin of China, 26(2): 200-205.
    shu

    京西房山岩体南侧青白口系下马岭组构造片岩中红柱石的变形特征及其地质意义

    Deformation features of andalusite in tectonic schist of the Xiamaling Formation of the Qingbaikouan System on the southern side of the Fangshan pluton in the Western Hills, Beijing, Chian

      摘要
    • 摘要: 在房山岩体南侧下马岭组构造片岩中发现红柱石横截面上发育一组共扼裂隙和“环带状”构造，环带形状与红柱石变斑晶横截面的形状相似，均压扁为长方形，红柱石的变形是同构造递进变形的结果。裂隙及环带均被流体包裹体所充填，流体包裹体的热爆温度为604-685℃，利用黑云母-石榴子石温度计得出变质温度为592℃。计算出变质发生深度为2．69-3．11km。

       

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