EH-4在本溪大台沟地区隐伏铁矿探测的研究
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摘要
目前,铁矿石作为国民经济发展必须的大宗矿产是不可替代的。钢铁工业发展对铁矿石的需求也将有较大增长。我国的自产铁矿石远不能满足钢铁工业的需求,进口铁矿石量逐年增长,1991年的1855.9万吨增加到2000年的6997.2万吨。2003年,我国共进口1.48亿吨铁矿石,占世界总贸易量的26.43%,首次超过日本位居世界第一位。2006年进口铁矿石3.26亿吨,2007年我国进口铁矿石3.83亿吨。随着我国经济的快速发展进口铁矿石的量还要增加。
随着表层与浅层铁矿体的开采,一些矿山出现相对的危机。面对这样的问题,用以前的找矿方法已经不能迅速找到深部的隐伏矿体。如何迅速、准确的发现深部矿体是一个急待研究的课题。
面对这样的问题,我们用EH-4进行探测研究,通过对大台沟隐伏矿床的探测研究,得出以下结论：矿体的总体走向为北西向,南西倾,倾角较陡,矿体从矿头向下延伸约500米,这为矿山开发新的资源基地提供了科学依据。该方法对本区的航磁特征有很好的验证,特别是深部铁矿资源探测具有良好的借鉴意义。本次研究表明连续电导率测量系统对鞍本地区深部铁矿资源具有良好的探矿效果,大台沟及邻区(小台沟)具有一定的铁矿资源潜力。研究采用的方法和技术手段方便快捷,科学准确,直观有效,且不受地形地物的影响。随着经济发展对铁矿石的需求,这一地区可为今后的铁矿开发提供资源储备,应进一步开展地质工作,但要考虑矿体埋藏深度对开采技术条件带来的影响。
At present, Stone of Iron is necessary and irreplaceable in the Process of development of economic. Development of Iron and steel industry on the demand for iron ore will also have greater growth. China's iron ore production for much of the iron and steel industry can not meet demand, iron of imports of will grow each year,18.559 million tons 1991 to 69.972 million tons of 2000. In 2003, China has imported 148 million tons of iron ore, in the world total trade volume of 26.43 percent.2006 imported 326 million tons of iron ore,2007 imported 383 million tons of iron ore. As development rapid economic of China's the iron ore import volume will increase.
As with the shallow surface of the iron ore mining, Some of mine will be crisis. Faced with such the problem, with the previous method can not quickly find the buried deep ore body.It is a priority research topic How quickly and accurately did find the deep ore body.
Faced with such the problem, We use the EH-4 detection research, Through concealed deposit detection research of the Da tai gou. Draw the following conclusions:Ore body of the overall direction to the North West, sw dumping, steep angle quickly. Ore from the mine head downward extension about 500 meters, This mine for the development of new resource base to provide a scientific basis. The method of the district aeromagnetic characteristics is a good verification. Especially deep iron ore resources exploration has a good reference. This study shows that the conductivity measurement system for the saddle in the region of deep iron ore resources prospecting has a good effect. Areas of Dataigou and xiaotaigou is a potential iron ore resources. On the methodology and technical means to facilitate fast and accurate science, visual effective, and the terrain features from the impact of. We should be further geological work, but to consider mining ore bodies buried on the depth of the impact of technical conditions.
随着表层与浅层铁矿体的开采,一些矿山出现相对的危机。面对这样的问题,用以前的找矿方法已经不能迅速找到深部的隐伏矿体。如何迅速、准确的发现深部矿体是一个急待研究的课题。
面对这样的问题,我们用EH-4进行探测研究,通过对大台沟隐伏矿床的探测研究,得出以下结论：矿体的总体走向为北西向,南西倾,倾角较陡,矿体从矿头向下延伸约500米,这为矿山开发新的资源基地提供了科学依据。该方法对本区的航磁特征有很好的验证,特别是深部铁矿资源探测具有良好的借鉴意义。本次研究表明连续电导率测量系统对鞍本地区深部铁矿资源具有良好的探矿效果,大台沟及邻区(小台沟)具有一定的铁矿资源潜力。研究采用的方法和技术手段方便快捷,科学准确,直观有效,且不受地形地物的影响。随着经济发展对铁矿石的需求,这一地区可为今后的铁矿开发提供资源储备,应进一步开展地质工作,但要考虑矿体埋藏深度对开采技术条件带来的影响。
At present, Stone of Iron is necessary and irreplaceable in the Process of development of economic. Development of Iron and steel industry on the demand for iron ore will also have greater growth. China's iron ore production for much of the iron and steel industry can not meet demand, iron of imports of will grow each year,18.559 million tons 1991 to 69.972 million tons of 2000. In 2003, China has imported 148 million tons of iron ore, in the world total trade volume of 26.43 percent.2006 imported 326 million tons of iron ore,2007 imported 383 million tons of iron ore. As development rapid economic of China's the iron ore import volume will increase.
As with the shallow surface of the iron ore mining, Some of mine will be crisis. Faced with such the problem, with the previous method can not quickly find the buried deep ore body.It is a priority research topic How quickly and accurately did find the deep ore body.
Faced with such the problem, We use the EH-4 detection research, Through concealed deposit detection research of the Da tai gou. Draw the following conclusions:Ore body of the overall direction to the North West, sw dumping, steep angle quickly. Ore from the mine head downward extension about 500 meters, This mine for the development of new resource base to provide a scientific basis. The method of the district aeromagnetic characteristics is a good verification. Especially deep iron ore resources exploration has a good reference. This study shows that the conductivity measurement system for the saddle in the region of deep iron ore resources prospecting has a good effect. Areas of Dataigou and xiaotaigou is a potential iron ore resources. On the methodology and technical means to facilitate fast and accurate science, visual effective, and the terrain features from the impact of. We should be further geological work, but to consider mining ore bodies buried on the depth of the impact of technical conditions.
引文
[1]杜春林.我国铁矿资源的概况与展望.地质出版社[J].1996
[2]郎一环,容洞谷.我国矿产资源态势与对策.自然资源学报.[J]2001,4
[3]李文虎,李奋雄等.矿山企业持续稳定发展问题研究(1).冶金经济分析.[J]1993,3
[4]沈通生.我国铁矿资源形势与对策.[J]West-china Exploration Engineering.1995,7
[5]魏文博.我国大地电磁测新进瞻及展望[J],地球物理学进展,2002年6月(245-254)
[6]鞍钢地质勘探公司四0二队.鞍山地区鞍山群基底构造特征及找矿方向探讨.[J]
[7]郑峻庆,张宝华,蔡一廷等.辽宁本溪地区北台—歪头山带太古宙鞍山群主要构造特征.地质找矿论从.[J]1986,3
[8]曹飞.本溪地区矿产资源优化利用的研究.[D]2005,12
[9]王守伦.鞍本地区鞍山群铁矿成因类型的讨论.矿床地质.[J]1986,5,
[10]沈其韩.华北地台早期寒武纪地质研究论文集.北京：地质出版社,[J]1998
[11]李鸿业.鞍山地区前震旦纪花岗岩问题[J].地质知识,1957,5
[12]程浴淇.中国东北部前寒武纪条带铁矿中富铁矿的成因问题[J].地质学报,1957
[13]李鸿业,赵秀德.鞍本地区鞍山式铁矿去地质构造[J].前寒武纪研究进展.1999
[14]曹代勇.物探资料在构造地质中的应用[J],中国煤炭地质,1993,6
[15]张建奎.可控源音频大地电磁测深在寻找隐伏矿体中的应用[J].甘肃地质,2002
[16]王东方.辽东地块的构造分解[J].辽宁地质,1992,6
[17]欧阳承新, 王时平,全德辉,曾建华等.高频大地电磁测深在断层构造探测中的应用研究[J].世界地震工程,2007,9
[18]陈乐寿,王光锷.大地电磁测深法,地质出版社,1990
[19]吴功建、林清.地球物理方法在地质和找矿中的应用[M].北京：地质出版社,1988.
[20]倪芬明,刘泰生.EH-4电磁仪的原理及应用.石油器材,1999,13(1)32-34
[21]漆新民,电磁场论.武汉大学出版社,1998
[22]王家映.我国大地电磁测深研究新进展[J].地球物理学报,1997,40(4)：206—211
[23]石应骏.大地电磁测深法教程[M].地质出版社,1987.
[24]胡健伟,汤怀民,微分方程数值方法,科学出版社,1999
[25]陈小斌,张翔,胡文宝.有限元直接迭代算法在MT二维正演计算中的应用[J].石油地球物理勘探,2000,35(4)：487496
[26]周熙襄,钟本善,严警琼,等.点源二维电法正演的有限单元法
[27]Jones A G. On the equivalence of the'Niblett'and'Bo2stick'transformations in the magnetotelluric method[J] Journal of Geophysics,1983,53:72～73.
[28]Fischer G. Some remarks on the behavior of the magne2totelluric phase[J]. Geophysical Prospecting,1985,33:716-722.
[29]EH-4电磁仪操作与技术手册.Electromagnetic Instruments Inc. Copyright c January,1996(information)
[30]D.F.Pridmore, G..W.Hohmann, S.H.Ward, and W.R.Sill, An investigation of finite-element modeling for electrical and electromagnetic data in three dimensions, Geophysics,46,1009-1024
[31]朴化荣.电磁测深法原理[M].北京：地质出版社,1990.[J].物探化探计算技术,1983,16(3)：19
[32]纪宏金,林瑞庆, 周永昶.关于若干化探数据处理方法的讨论
[33]史明娟,徐世浙,刘斌,大地电磁二次函数插值的有限元法正演模拟,1997,40(3),地球物理学报[J].地质与勘探,2001,37(4)：56-59.
[34]周世泰.鞍本地质条带状铁矿地质[M].地质出版社1994,4
[35]孙中任,赵东亮.利用Surfers实现剖面平面图绘制[J].物探和化探,2006,4
[36]曹代勇.物探资料在地质构造中的应用[J].中国煤田地质,1993,6
[37]王红亮张远智等.一种应用Surfer软件快速进行地形绘制的方法[J].城市勘测,2007
[38]秦葆瑚,张昌达,朱文孝等高精度磁法勘探[M]长沙.中南工业大学出版社,1998
[39]张立军,高飞等.高精度磁法在大板金矿勘查中的应用[J].辽宁地质,2000,12
[2]郎一环,容洞谷.我国矿产资源态势与对策.自然资源学报.[J]2001,4
[3]李文虎,李奋雄等.矿山企业持续稳定发展问题研究(1).冶金经济分析.[J]1993,3
[4]沈通生.我国铁矿资源形势与对策.[J]West-china Exploration Engineering.1995,7
[5]魏文博.我国大地电磁测新进瞻及展望[J],地球物理学进展,2002年6月(245-254)
[6]鞍钢地质勘探公司四0二队.鞍山地区鞍山群基底构造特征及找矿方向探讨.[J]
[7]郑峻庆,张宝华,蔡一廷等.辽宁本溪地区北台—歪头山带太古宙鞍山群主要构造特征.地质找矿论从.[J]1986,3
[8]曹飞.本溪地区矿产资源优化利用的研究.[D]2005,12
[9]王守伦.鞍本地区鞍山群铁矿成因类型的讨论.矿床地质.[J]1986,5,
[10]沈其韩.华北地台早期寒武纪地质研究论文集.北京：地质出版社,[J]1998
[11]李鸿业.鞍山地区前震旦纪花岗岩问题[J].地质知识,1957,5
[12]程浴淇.中国东北部前寒武纪条带铁矿中富铁矿的成因问题[J].地质学报,1957
[13]李鸿业,赵秀德.鞍本地区鞍山式铁矿去地质构造[J].前寒武纪研究进展.1999
[14]曹代勇.物探资料在构造地质中的应用[J],中国煤炭地质,1993,6
[15]张建奎.可控源音频大地电磁测深在寻找隐伏矿体中的应用[J].甘肃地质,2002
[16]王东方.辽东地块的构造分解[J].辽宁地质,1992,6
[17]欧阳承新, 王时平,全德辉,曾建华等.高频大地电磁测深在断层构造探测中的应用研究[J].世界地震工程,2007,9
[18]陈乐寿,王光锷.大地电磁测深法,地质出版社,1990
[19]吴功建、林清.地球物理方法在地质和找矿中的应用[M].北京：地质出版社,1988.
[20]倪芬明,刘泰生.EH-4电磁仪的原理及应用.石油器材,1999,13(1)32-34
[21]漆新民,电磁场论.武汉大学出版社,1998
[22]王家映.我国大地电磁测深研究新进展[J].地球物理学报,1997,40(4)：206—211
[23]石应骏.大地电磁测深法教程[M].地质出版社,1987.
[24]胡健伟,汤怀民,微分方程数值方法,科学出版社,1999
[25]陈小斌,张翔,胡文宝.有限元直接迭代算法在MT二维正演计算中的应用[J].石油地球物理勘探,2000,35(4)：487496
[26]周熙襄,钟本善,严警琼,等.点源二维电法正演的有限单元法
[27]Jones A G. On the equivalence of the'Niblett'and'Bo2stick'transformations in the magnetotelluric method[J] Journal of Geophysics,1983,53:72～73.
[28]Fischer G. Some remarks on the behavior of the magne2totelluric phase[J]. Geophysical Prospecting,1985,33:716-722.
[29]EH-4电磁仪操作与技术手册.Electromagnetic Instruments Inc. Copyright c January,1996(information)
[30]D.F.Pridmore, G..W.Hohmann, S.H.Ward, and W.R.Sill, An investigation of finite-element modeling for electrical and electromagnetic data in three dimensions, Geophysics,46,1009-1024
[31]朴化荣.电磁测深法原理[M].北京：地质出版社,1990.[J].物探化探计算技术,1983,16(3)：19
[32]纪宏金,林瑞庆, 周永昶.关于若干化探数据处理方法的讨论
[33]史明娟,徐世浙,刘斌,大地电磁二次函数插值的有限元法正演模拟,1997,40(3),地球物理学报[J].地质与勘探,2001,37(4)：56-59.
[34]周世泰.鞍本地质条带状铁矿地质[M].地质出版社1994,4
[35]孙中任,赵东亮.利用Surfers实现剖面平面图绘制[J].物探和化探,2006,4
[36]曹代勇.物探资料在地质构造中的应用[J].中国煤田地质,1993,6
[37]王红亮张远智等.一种应用Surfer软件快速进行地形绘制的方法[J].城市勘测,2007
[38]秦葆瑚,张昌达,朱文孝等高精度磁法勘探[M]长沙.中南工业大学出版社,1998
[39]张立军,高飞等.高精度磁法在大板金矿勘查中的应用[J].辽宁地质,2000,12