• 薛家石梁地区 - 引用次数：2

  Changping Xuejiashiliang Region, located in the western segment of YanshanOrogenic Belt, underwent intensively tectonic deformation and magma activity inYanshan epoch.

  昌平薛家石梁地区位于燕山造山带西段,燕山期时发生了强烈的构造变形和岩浆活动。

  参考来源 - 昌平薛家石梁地区燕山期构造叠加探讨

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