摘要
本文根据邓家山地区构造分区、分段和空间形态与结构的研究，得出该区的地质构造主要是多期自南向北挤压作用的结果，并受到后期岩浆侵入作用的影响。在此基础上分析得出，有利的成矿地段和成矿构造部位与隐伏岩体、矿体的埋深向南逐渐加深的结论。
Based on study of the spacial forms and structures in subdistricts and subsections of the Dengjiashan area,this paper comes to a conclusion that the geological structures in this area were formed mainly by multistage comperssion from south to north and were subsequently influenced by post-magmatic intrusion. On this basis another conclusion may also be drawn that the ore potential locations , the orecontrolling structures, the orerelated magmatic rocks and the potential ore bodies are buried deeper and deeper southward.
出处
《江西地质》
1997年第2期25-31,共7页
Jiangxi Geology
