辽宁省八家子铅锌矿典型矿床研究及深部预测
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摘要
随着我国经济的快速发展,工业化进程的不断加快,重要的矿产资源愈发显得紧缺,其中也包括铅锌矿。加快铅锌矿产资源评价预测工作,增加矿区保有储量,提高危机矿山潜在储量,提高铅锌矿研究工作程度显得势在必行。
热液型铅锌矿是我国铅锌矿的一个主要类型,在我国铅锌矿石产出量占有重要位置。对八家子铅锌矿研究程度的高低,直接影响到辽宁省热液型铅锌矿产资源预测评价工作。八家子铅锌矿是辽西具有代表性的热液型铅锌矿,因此将八家子铅锌矿床作为典型矿床来研究热液型铅锌矿,有着很强的信服度。
本文运用典型矿床的研究方法及流程,对八家子铅锌矿床展开研究。在分析研究区地质特征的基础上,结合国内外学者对热液型铅锌矿、典型矿床、深部矿产预测的研究成果,建立八家子铅锌矿成矿模式,从中总结出成矿要素、预测要素,形成八家子铅锌矿典型矿床成矿模式图、成矿要素图、预测要素图及预测模型图。在文章的最后部分,利用典型矿床的研究成果,展开对八家子铅锌矿深部的预测研究工作、计算深部矿产资源量,从而实现典型矿床研究的目的,增加矿床的远景储量。
With the fast and steady development of economy in China, the mine-resource restrict the economy’s development more and more distinctly .If our country want to economy develop fast , we must heighten the reserves of mine. Hydrothermal-type lead-zinc mine is a magnitudedinous type of Lead-Zinc Ore , the reserves of which occupy a number of Lead-Zinc ore in China. Thereby the assessment and forecast about the potential of Lead-Zinc Ore in our country depend on the research of Ba Jia Zi Lead-Zinc ore. Ba Jia Zi Lead-Zinc ore, which is representative, is representative ore of Hydrothermal-type lead-zinc mine at Liao Ning province. By way of typical Hydrothermal-type lead-zinc mine , Ba Jia Zi Lead-Zinc ore is much more importance.
This article apply typical mineral theory and method to study Ba Jia Zi lead-zinc mine. It uses the research methods and processes of typical mineral deposit to research Ba Jia Zi Lead-Zinc ore. The article also pays more attention to the geological features of Ba Jia Zi Lead-Zinc ore, including stratum, geological structure, activity of magma, wall-rockalteration and the geological、physics characteristics of deposit, etc. Through the description to stratum of ChangCheng which include Da HongYu and Gao YuZhuang, we got the conclusion that the wall rock of Jia Zi Lead-Zinc ore are dolomite、fine-sandstone、sandyslate、dolomite-marble. The epoch of Gaoyuzhuang,transgression enlarged,BaJiaZi come into being tidal-flat facies sediment condition. For the reason of tidal-flat facies sediment condition gradually transport into semi-close lagoon bay sediment condition and beach form parallel with coastal. With result, Bajiaz‘is originality sediment condition become into impediment tidal-flat environment and the water in lagoon tidal-flat environment are much more steady、stagnancy and organic matter,the sediment condition become deoxidize condition which in the favor of mine element enrichment and form source bed. According to characterization of diggings fault and investigate diagnostic of area fault, we believe that fundus fault and deep and bigness fault control Bajiazi Lead-Zinc ore. Fundus fault control the aboriginal sediment condition and source bed forming ,deep and bigness fault control magmatic rock and interspace distributing of mineralization. Activity time of magma fasten on phase of YanShan and form Jian Chang and ShengZongMiao super-element rock mass. The activity of inrush magma bring not only mine substace—Pb、Zn but also essential element of mine—S, At the same time ,age-old seawater which seal up for keeping in the stratum and the rain water filter from the fault and rock crack ,which are heated up and the mine element ,which exist in the ource bed,that the activity is more violent. All these can come into the hot-liquid and form hot-liquid with mine element. Summarizing the geologic character of Bajiazi Lead-Zinc ore:1、The known mine ,which from Bei Shan to Bing Gou ,extend 5km along NW、strike 310°-330°, NE incline, obliquity is 35°-60°and the mine are lens and bedded or saccular; 2、Mesozoic is the period of Bajiazi Lead-Zinc ore’s formed; 3、he wall rock of Bajiazi Lead-Zinc ore is GaoYuZhuang which is terrigenous clastic rocks; 4、The ore have a equality digit and a high digit at part of mine. Mine possess obvious zonation electrophoresis, There are thre types of skarn: Magnesium skarn、Calcium skarn、Calcium manganese skarn. At the different part of mine the mineralize electrophoresis and mineralize degree are different and the Lead-Zinc ore local in the Calcium manganese skarn.;5、With the investigation of ore and assort the ore configuration with three types—sediment configuration, hot-liquid configuration and stress configuration. This three configuration types show that come into being mine has distinctness time; 6、Compartmentalizing mine epoch、mine phase and comfirming the character of mine epoch which is confirmed by ore configuration. On the basis of Bajiazi Lead-Zinc ore’s geologic character, establish Mineralization pattern of Bajiazi Lead-Zinc ore. Proterozoic, after forming ledge and lean mine , magma heat up the stratum of Proterozoic and ground water, which is formed hot-liquid which get along the fault and cranny of rock and get reaction with rock. Along with the decreasing of temperature、pressure, the hot-liquid sedimence in the fault and form the Lead-Zinc ore. According to discuss the process of mineralization , we establish the Ba Jia Zi Lead-Zinc ore’s Mineralization pattern map. On the bases of geological features of Ba Jia Zi Lead-Zinc ore and mineralization pattern, firstly ;picking up Ba Jia Zi Lead-Zinc ore’s mineralization factors and ascertaining forecast factors. With these, we protract Ba Jia Zi Lead-Zinc ore’s mineralization factors and forecast factors map, and establish Ba Jia Zi Lead-Zinc ore’s forecast model map. At last I forecast on Ba Jia Zi Lead-Zinc ore with forecast factors.
The article’s conclusions :
1、On the basis of investigation of Ba JiaZi typical deposit, establishing the Mineralization pattern map of Ba JiaZi.
2、Extract Ba JiaZi Lead-Zinc Ore’s mineralization and forecast factors, and form the Ba JiaZi Lead-Zinc ore’s mineralization factors map. Picking up mineralization factors and forecast factors and extablishing the mineralization factors map、forecast factors map and forecast model map . In this area, all these don’t do before.
3. Deep forecast in Ba Jia Zi Lead-Zince ore. Putting forward 10 forecast principle and three forecast zone and calculate the reserves, there is effects and significance for next phase work this area.
热液型铅锌矿是我国铅锌矿的一个主要类型,在我国铅锌矿石产出量占有重要位置。对八家子铅锌矿研究程度的高低,直接影响到辽宁省热液型铅锌矿产资源预测评价工作。八家子铅锌矿是辽西具有代表性的热液型铅锌矿,因此将八家子铅锌矿床作为典型矿床来研究热液型铅锌矿,有着很强的信服度。
本文运用典型矿床的研究方法及流程,对八家子铅锌矿床展开研究。在分析研究区地质特征的基础上,结合国内外学者对热液型铅锌矿、典型矿床、深部矿产预测的研究成果,建立八家子铅锌矿成矿模式,从中总结出成矿要素、预测要素,形成八家子铅锌矿典型矿床成矿模式图、成矿要素图、预测要素图及预测模型图。在文章的最后部分,利用典型矿床的研究成果,展开对八家子铅锌矿深部的预测研究工作、计算深部矿产资源量,从而实现典型矿床研究的目的,增加矿床的远景储量。
With the fast and steady development of economy in China, the mine-resource restrict the economy’s development more and more distinctly .If our country want to economy develop fast , we must heighten the reserves of mine. Hydrothermal-type lead-zinc mine is a magnitudedinous type of Lead-Zinc Ore , the reserves of which occupy a number of Lead-Zinc ore in China. Thereby the assessment and forecast about the potential of Lead-Zinc Ore in our country depend on the research of Ba Jia Zi Lead-Zinc ore. Ba Jia Zi Lead-Zinc ore, which is representative, is representative ore of Hydrothermal-type lead-zinc mine at Liao Ning province. By way of typical Hydrothermal-type lead-zinc mine , Ba Jia Zi Lead-Zinc ore is much more importance.
This article apply typical mineral theory and method to study Ba Jia Zi lead-zinc mine. It uses the research methods and processes of typical mineral deposit to research Ba Jia Zi Lead-Zinc ore. The article also pays more attention to the geological features of Ba Jia Zi Lead-Zinc ore, including stratum, geological structure, activity of magma, wall-rockalteration and the geological、physics characteristics of deposit, etc. Through the description to stratum of ChangCheng which include Da HongYu and Gao YuZhuang, we got the conclusion that the wall rock of Jia Zi Lead-Zinc ore are dolomite、fine-sandstone、sandyslate、dolomite-marble. The epoch of Gaoyuzhuang,transgression enlarged,BaJiaZi come into being tidal-flat facies sediment condition. For the reason of tidal-flat facies sediment condition gradually transport into semi-close lagoon bay sediment condition and beach form parallel with coastal. With result, Bajiaz‘is originality sediment condition become into impediment tidal-flat environment and the water in lagoon tidal-flat environment are much more steady、stagnancy and organic matter,the sediment condition become deoxidize condition which in the favor of mine element enrichment and form source bed. According to characterization of diggings fault and investigate diagnostic of area fault, we believe that fundus fault and deep and bigness fault control Bajiazi Lead-Zinc ore. Fundus fault control the aboriginal sediment condition and source bed forming ,deep and bigness fault control magmatic rock and interspace distributing of mineralization. Activity time of magma fasten on phase of YanShan and form Jian Chang and ShengZongMiao super-element rock mass. The activity of inrush magma bring not only mine substace—Pb、Zn but also essential element of mine—S, At the same time ,age-old seawater which seal up for keeping in the stratum and the rain water filter from the fault and rock crack ,which are heated up and the mine element ,which exist in the ource bed,that the activity is more violent. All these can come into the hot-liquid and form hot-liquid with mine element. Summarizing the geologic character of Bajiazi Lead-Zinc ore:1、The known mine ,which from Bei Shan to Bing Gou ,extend 5km along NW、strike 310°-330°, NE incline, obliquity is 35°-60°and the mine are lens and bedded or saccular; 2、Mesozoic is the period of Bajiazi Lead-Zinc ore’s formed; 3、he wall rock of Bajiazi Lead-Zinc ore is GaoYuZhuang which is terrigenous clastic rocks; 4、The ore have a equality digit and a high digit at part of mine. Mine possess obvious zonation electrophoresis, There are thre types of skarn: Magnesium skarn、Calcium skarn、Calcium manganese skarn. At the different part of mine the mineralize electrophoresis and mineralize degree are different and the Lead-Zinc ore local in the Calcium manganese skarn.;5、With the investigation of ore and assort the ore configuration with three types—sediment configuration, hot-liquid configuration and stress configuration. This three configuration types show that come into being mine has distinctness time; 6、Compartmentalizing mine epoch、mine phase and comfirming the character of mine epoch which is confirmed by ore configuration. On the basis of Bajiazi Lead-Zinc ore’s geologic character, establish Mineralization pattern of Bajiazi Lead-Zinc ore. Proterozoic, after forming ledge and lean mine , magma heat up the stratum of Proterozoic and ground water, which is formed hot-liquid which get along the fault and cranny of rock and get reaction with rock. Along with the decreasing of temperature、pressure, the hot-liquid sedimence in the fault and form the Lead-Zinc ore. According to discuss the process of mineralization , we establish the Ba Jia Zi Lead-Zinc ore’s Mineralization pattern map. On the bases of geological features of Ba Jia Zi Lead-Zinc ore and mineralization pattern, firstly ;picking up Ba Jia Zi Lead-Zinc ore’s mineralization factors and ascertaining forecast factors. With these, we protract Ba Jia Zi Lead-Zinc ore’s mineralization factors and forecast factors map, and establish Ba Jia Zi Lead-Zinc ore’s forecast model map. At last I forecast on Ba Jia Zi Lead-Zinc ore with forecast factors.
The article’s conclusions :
1、On the basis of investigation of Ba JiaZi typical deposit, establishing the Mineralization pattern map of Ba JiaZi.
2、Extract Ba JiaZi Lead-Zinc Ore’s mineralization and forecast factors, and form the Ba JiaZi Lead-Zinc ore’s mineralization factors map. Picking up mineralization factors and forecast factors and extablishing the mineralization factors map、forecast factors map and forecast model map . In this area, all these don’t do before.
3. Deep forecast in Ba Jia Zi Lead-Zince ore. Putting forward 10 forecast principle and three forecast zone and calculate the reserves, there is effects and significance for next phase work this area.
引文
[1].裴荣富.中国矿床模式[M]地质出版社.1995.06.
[2].陈毓川、朱裕生等.中国矿床成矿模式[M].地质出版社.1993.10
[3].张景.西鞍山铁矿典型矿床研究及“鞍山式”铁矿深部预测.吉林大学[D].2009.06
[4].辽宁省地质矿产勘查局第三地质大队.辽西八家子矿区铅锌矿田控矿因素及成矿预测报告[R].辽宁.1994.12
[5].洪作民,杨雅君,朱金海.辽宁八家子铅锌矿田构造特征及其控矿作用[J].辽宁地质.1993.09
[6].王世家.辽西花岗岩类碱厂超单元成因及定位机制探讨[J].辽宁地质学报,1991.
[7].洪作民,白沿金,全秀杰,辽西地区逆冲断层和推覆构造[J].辽宁地质,1985.
[8].马永昌.辽西南部金属矿床分布规律及产出特征.矿床与地质[J],1999
[9].中国地质科学院矿产资源研究所.辽宁八家子银铅锌矿等大型危机矿山找矿示范研究阶段性总结报告[R].北京.2005.10.
[10] .朱建化、马永昌.八家子多金属矿矿床成因与找矿方向[J].地质与勘探.2000
[11].张耀华、崔笑梅.辽宁建昌八家子铅锌矿床的地球化学字特征及其成因探讨[J].辽宁地质,1986.
[12].杨占兴.辽西八家子多金属矿床的成因研究[J].辽宁地质,1994.
[13].辽宁省地质矿产局.辽宁省中下元古宙铅锌成矿控制因素[M].辽宁.1992.03.
[14].辽宁省地质矿产局.辽宁省成矿远景区划及“九五”找矿地质工作部署建议(金、银、铜、铅锌矿产)[R].辽宁.1994.12
[15].王世称,候惠群,王於天,刘少华等.内生矿床成矿系列中比例尺预测方法研究[M].地质出版社.1993.12.
[16].辽宁省地质矿产局第八地质大队.辽宁省锦西虹螺山-建昌五指山金、多金属成矿带IV级成矿远景区划报告[R].沈阳.1994.06
[17].J Riley J F. The tetrahedrite-freibergite eries, with reference to the Mount Pb-Zn-Ag ore body mineral Deposita[J]. 1974 ,09
[18]. Cox D P,Singer D A. Mineral deposit models. United States Geological Survey Bulletin[J].1986.
[2].陈毓川、朱裕生等.中国矿床成矿模式[M].地质出版社.1993.10
[3].张景.西鞍山铁矿典型矿床研究及“鞍山式”铁矿深部预测.吉林大学[D].2009.06
[4].辽宁省地质矿产勘查局第三地质大队.辽西八家子矿区铅锌矿田控矿因素及成矿预测报告[R].辽宁.1994.12
[5].洪作民,杨雅君,朱金海.辽宁八家子铅锌矿田构造特征及其控矿作用[J].辽宁地质.1993.09
[6].王世家.辽西花岗岩类碱厂超单元成因及定位机制探讨[J].辽宁地质学报,1991.
[7].洪作民,白沿金,全秀杰,辽西地区逆冲断层和推覆构造[J].辽宁地质,1985.
[8].马永昌.辽西南部金属矿床分布规律及产出特征.矿床与地质[J],1999
[9].中国地质科学院矿产资源研究所.辽宁八家子银铅锌矿等大型危机矿山找矿示范研究阶段性总结报告[R].北京.2005.10.
[10] .朱建化、马永昌.八家子多金属矿矿床成因与找矿方向[J].地质与勘探.2000
[11].张耀华、崔笑梅.辽宁建昌八家子铅锌矿床的地球化学字特征及其成因探讨[J].辽宁地质,1986.
[12].杨占兴.辽西八家子多金属矿床的成因研究[J].辽宁地质,1994.
[13].辽宁省地质矿产局.辽宁省中下元古宙铅锌成矿控制因素[M].辽宁.1992.03.
[14].辽宁省地质矿产局.辽宁省成矿远景区划及“九五”找矿地质工作部署建议(金、银、铜、铅锌矿产)[R].辽宁.1994.12
[15].王世称,候惠群,王於天,刘少华等.内生矿床成矿系列中比例尺预测方法研究[M].地质出版社.1993.12.
[16].辽宁省地质矿产局第八地质大队.辽宁省锦西虹螺山-建昌五指山金、多金属成矿带IV级成矿远景区划报告[R].沈阳.1994.06
[17].J Riley J F. The tetrahedrite-freibergite eries, with reference to the Mount Pb-Zn-Ag ore body mineral Deposita[J]. 1974 ,09
[18]. Cox D P,Singer D A. Mineral deposit models. United States Geological Survey Bulletin[J].1986.