论徐州弧的北界与找煤

传统认为徐州弧止于原丰沛断层南，其北则为东西向构造，经研究后认为，该弧的北界不但通过原丰沛断层，而且延至鲁中一带，通过对徐州弧北界的探讨，为丰沛断层南北的构造推断及找煤提供了新的思路。

THE NORTHERN BOUNDARY OF THE XUZHOU ARC AND COAL PROSPECTING

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.