It was generally considered that the Xuzhou arc probally terminated on the southern side of the original Feng-Pei fault and that north of it may be an E-W-trending structure. Through a study the author holds that the northern boundary of the arc not only runs across the original Feng-Pei fault but also possibly extends as far as the vicinity of central Shandong. The study of the northern boundary of the Xuzhou arc may provided a new idea for the inference of the structures north and south of the Feng-Pei fault and coal finding.
参考文献
相似文献
引证文献
引用本文
李桂春.1995.论徐州弧的北界与找煤[J].地质论评,41(6):509-516,[DOI]. Li Guichun.1995. THE NORTHERN BOUNDARY OF THE XUZHOU ARC AND COAL PROSPECTING[J]. Geological Review,41(6):509-516.