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- W3152023866 abstract "中央内部蒙古的 Daqing 掸人(Mtns ) 的早白垩纪 Hohhot 变形核心建筑群(mcc ) 在暴露的最好和在北方中国 craton 的北边以内发展了的空间地孤立的 mccs 惊人的大多数之中。所有在一条晚古生代的 Andes 山脉风格的弧的地下室和可变年龄和构造 vergence 的到对面更旧的中生代 fold-and-thrust 带以内这些 mccs 被形成。主人 Hohhot 分开为至少 120 km 的沿着罢工距离在 Daqing 掸人的南部的边缘以内向南指责根。它在到北方的范围的几何学由干扰模式在之间是复杂的(1 ) 凸的主要、大规模 NW-SE-trending 和凹面指责折皱并且(2 ) 它的晚运动学的历史上合拢了分开的第二等的 ENE-WSW-trending antiforms 和 synforms。作为在 Whipple Mtns。加利福尼亚， Hohhot 主人分开不 Wernicke (1981 ) 是简单生根的类型；相反，它被孵化从一中间外壳砍地区，其顶在它的掘出的更低的板中在含碳的 metasedimentary 岩石以内作为 mylonitic 前面被保存。在现在的基础节硅质的暴烈的岩石标明日期的 40Ar39Ar 孤立 supradetachment 盆建议外壳的扩展在 ca 开始了。127 妈，尽管降低板的 mylonitic 岩石不暴露于侵蚀直到在 ca 以后。119 妈。在矿脉基卒下盘 mylonitic 片麻岩的角闪石，黑云母，和白云母的实质上同步的冷却显示很快速的发掘并且在 ca。122120 妈。与几份最近的报告相反，主人分开清楚地切到对面并且割下 Daqing 掸人低岬 fold-and-thrust 的更旧的、指导北方的戳表系上带子。合拢并且在它的 foredeep 阶层以内的指责戳的暗岩象 132.6 一样年轻 ??蔐 吗？？" @default.
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- W3152023866 date "2010-01-01" @default.
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- W3152023866 title "Early Cretaceous overprinting of the Mesozoic Daqing Shan fold-and-thrust belt by the Hohhot metamorphic core complex, Inner Mongolia, China" @default.
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