The Yinshan Fold and Thrust Belt of Northern China--An Enigmatic Intraplate Orogen of Jura-Cretaceous Age

中国北方阴山褶皱和冲断带位于中生代华北板块内，与中生代活跃的华北板块的三个辐合边缘均无明显联系。这项研究的目的是了解这一带形成的原因如此远离这些边缘，以及大量的岩浆活动是否可能与如此遥远的俯冲过程有关。研究结果可能有助于理解其他神秘的造山带，这些造山带发生在板块内部，但距离板块边缘相当远。

9627909 Davis The Yinshan fold and thrust belt of northern China lies within the Mesozoic North China plate and is not clearly related to any of the three convergent margins of that plate that were active in Mesozoic time. This research is aimed at understanding the causes of this belt forming so far away from these margins, and whether the voluminous magmatism can be related to such distant subduction processes. Results may help understand other enigmatic orogenic belts that occur within plates but lie at considerable distances from the plate margin.