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金属矿山 ›› 2009, Vol. 39 ›› Issue (08): 87-90+96.

• 地质与测量 • 上一篇    下一篇

铁山矿床铁山庙和石门郭矿段的构造关系

文启付,王海军   

  1. 河南安钢集团舞阳矿业有限责任公司
  • 出版日期:2009-08-17 发布日期:2011-04-26

Structural Relation between Tieshanmiao and Shimenguo Ore Sections in Tieshan Deposit

Wen Qifu,Wang Haijun   

  1. Henan AnGang Group Wuyang Mining Co., Ltd.
  • Online:2009-08-17 Published:2011-04-26

摘要: 铁山矿床铁山庙、石门郭2矿段的构造关系多属推断,构造地质依据尚不充分,直接影响到地采设计方案。为此,分析矿床地质,找出原地质报告对2矿段构造关系认识存在的问题,确定研究2矿段构造关系的方法。首先,运用反射波地震勘探和电测深确定构造关系由原F13逆冲断层调整为F13正断层;其次,用钻探直接控制2矿段的衔接部位,证实F13断层为正断层,同时在F13的北部附近又新发现F701正断层。F13、F701正断层和铁山庙矿段南部基底正断层F4共同形成了田洛庄地堑。

关键词: 构造关系, 地堑, 地震勘探, 电测深, 补充勘探

Abstract: The structural relation between Tieshanmiao and Shimenguo ore sections in Tieshan deposit was mostly deduced with insufficient structural geological data, directly affecting the underground mining design.Therefore, the deposit geology was analyzed, the problems in understanding the structural relation between the two ore sections in the original geological report were found out and the method for studying their relation was determined.Firstly, reflected wave seismic exploration and electrical depth sounding were used to found that the original F13 thrust fault was in fact F13 normal fault; secondly, the drilling was used to directly control the connecting site of the two sections, founding that F13  fault was a normal fault.Meanwhile, a new F701 normal fault was found to the north of F13.F13 and F701 normal faults and F4 normal fault in the south base of the Tieshanmiao ore section have jointly formed Tianluozhuang faulted graben.

Key words: Structural relation, Faulted graben, Seismic exploration, Electrial depth sounding, Supplementary exploration