辽宁排山楼金矿T4矿体Au元素富集规律及其对找矿的指示意义

doi:10.11872/j.issn.1005-2518.2021.03.070

摘要/Abstract

摘要：

排山楼金矿位于华北地台北缘，为受控于韧性剪切带的大型金矿床。该矿床成因与韧性剪切带密切相关，矿区成矿地质条件优越，具有很好的找矿潜力。通过总结排山楼金矿地质特征及其主要控矿因素，认为区内韧性剪切带为控岩（控矿）构造，控制着赋矿糜棱岩和金矿体的空间展布，向矿区深部赋矿岩石变薄，找矿空间变小。通过分析T4矿体的品位和厚度分布规律发现，矿体厚度及品位分布规律在空间上表现出高度一致性，根据金品位等值线图判断矿体向南西侧伏。研究认为T4矿体在南西深部其厚度及品位降低趋势明显，向深部工业价值不大，应重点加强对其他韧性剪切带找矿潜力的研究。

关键词: 韧性剪切带, 成矿地质条件, 控矿因素, Au元素富集规律, 深部找矿潜力, 排山楼金矿, 辽宁省

Abstract:

The Paishanlou gold deposit is located in the gold province of northern margin of North China Craton，which is the third largest gold province in China.The deposit is mainly hosted in metamorphic rocks of the Jianping Group of Archean and it is structurally controlled by two sets of ductile shear zones.Both the Paishanlou gold deposit in Liaoning Province and Hetai gold deposit in Guangdong Province were firstly been confirmed as ductile shear zone type gold deposits in China.The main orebody T4 in the mining area is controlled by the northeast trending ductile shear zone，and the host rocks are the biotite-plagioclase mylonite and felsic mylonite from Late Archean Jianping Group.The orebody lies in the most strongly deformed rocks in the ductile shear zone，and its hanging wall is dolomitic mylonite.Previous studies have shown that dolomitic mylonite plays a role as a geochemical barrier in the mineralizing process.The Yanshanian granite intruded into the ore-bearing Jianping Group.In this study，by summarizing the geological characteristics and main ore-controlling factors of the Paishanlou gold deposit，it is believed that the ductile shear zone in the area is a rock-controlling and ore-controlling structure，which controls the spatial distribution of the ore-bearing mylonite and gold ore bodies.Granite intrusion causes thinning of ore-bearing rocks which reduced prospecting space.The grade and thickness data of the ore-body T4 were collected in this study.By using the Surfer software to compile the grade and thickness contour maps，the distribution characteristics of the grade and thickness of the ore-body T4 were analyzed.It is considered that the grade and thickness of the ore-body T4 from the east end near the surface to the deep end of the west end can be divided into three obvious gradient zones，and the grade and thickness gradually decrease.The thickness and grade of the orebody shows spatially high consistency.According to the gold grade contour map，we judge that the orebody is leaning to the south and west，with a side leaning angle of 53°.It indicates that the thickness and grade of the orebody T4 in the southwest of the deep have a significant decrease.Therefore，there is no great potential to find economically important orebody in the southwest of the deep.It’s proposed to analyze and research the prospecting potential of other ductile shear zones in the mining area.

Key words: ductile shear zone, ore-forming geological conditions, ore-controlling factors, enrichment regularities of Au element, prospecting potential of deep area, Paishanlou gold deposit, Liaoning Province

中图分类号:

P618.51

刘彦兵,屈海浪,胡博心,缪广,滕俊伟,武昌胜,王睿鹏. 辽宁排山楼金矿T4矿体Au元素富集规律及其对找矿的指示意义[J]. 黄金科学技术, 2021, 29(3): 325-333.

Yanbing LIU,Hailang QU,Boxin HU,Guang MIAO,Junwei TENG,Changsheng WU,Ruipeng WANG. Enrichment Regularities of Au Element in T4 Orebody of the Paishanlou Gold Deposit in Liaoning Province and Its Indicative Significance for Prospecting[J]. Gold Science and Technology, 2021, 29(3): 325-333.

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参考文献 0

	Bai Y，Zhang L C，Zhu M T，al et，2020.Mineralogy and He-Ar isotopic compositions of pyrites in the Paishanlou Au deposit on the northern margin of North China Craton［J］.Geological Journal，55（8）：5865-5884.
	Cai Xinming，2018.Mineralization evolution model of Paishanlou gold mine in Fumeng County［J］.Jilin Geology，37（1）：35-37.
	Chen Chong，Wei Junhao，Fu Lebing，2013.Geological characteristics study of the ductile shear zone type of gold deposits：With Paishanlou gold deposit and the Hetai gold deposit as examples［J］.Gold，34（10）：12-16.
	Dong Jun，2015.Analysis on the characteristics of Paishanlou of Liaoning ductile shear zone gold deposit and ore-controlling conditions［J］.Modern Industrial Economy and Informationization，5（5）：46-48.
	Fu Lebing，2012.The Mesozoic Tectonic-magmatic Evolution Process and Gold Metallogenesis in Chifeng-Chaoyang Region，Northern North China Craton［D］.Wuhan：China University of Geosiciences.
	Jia Sanshi，Fu Jianfei，Song Jianchao，al et，2010.Geochemical characteristics of trace elements and deep evaluation of the deposit in Paishanlou gold deposit，Fuxin，Liaoning［J］.Mineral Deposits，29（Supp.1）：947-948.
	Jia Sanshi，Wang Ende，Fu Jianfei，al et，2011.Geochemical characteristics of trace elements and deep prediction of the Paishanlou gold deposit，Fuxin，western Liaoning［J］.Geochimica，40（3）：266-279.
	Li Youquan，Song Yuchun.2015.Report on the verification of gold reserves in Paishanlou mining area，Fuxin Mongolian Autonomous County，Liaoning Province［R］.Fuxin：Liaoning Paishanlou Gold Mining Co.，Ltd.
	Liu J Z，Ouyang Z Y，Liu X S，al et，1999.Mineralization dynamics of Paishanlou gold deposit in Fuxin，Liaoning Province［J］.Chinese Science Bulletin，（Supp.2）：188-190.
	Luo Hui，Zhao Yunqi，1997.Geology and mineralization of Paishanlou gold deposit in Fuxin，Liaoning Province［J］.Progress in Precambrian Research，20（4）：13-24.
	Luo Zhenkuan，Miao Laicheng，Guan Kang，al et，2001.SHRIMP U-Pb zircon age of magmatic rock in Paishanlou gold mine district，Fuxin，Liaoning Province，China［J］.Geochimica，30（5）：483-490.
	Ma Bingqian，2020.The metallogenic mechanism and metallogenic regularity of Fuxin gold deposit in Liaoning Province［J］.World Nonferrous Metals，（22）：89-90.
	Meng Xiangang，2003.Mesozoic Structure Framework and Its Controls on Accumulation and Distribution of Gold Deposits in the Northern Part of Yiwulüshan Mts.，Western Liaoning Province［D］.Beijing：China University of Geosiciences（Beijing）.
	Meng Xiangang，Feng Xiangyang，Shao Zhaogang，al et，2002.Yiwulüshan metamorphic core complex system in western Liaoning and its control on gold deposits［J］.Geological Bulletin of China，（12）：841-847.
	Ni Jinlong，Liu Junlai，Tang Xiaoling，al et，2014.Evolution of the ductile shear zone of the Paishanlou gold deposits，Western Liaoning，China［J］.Science China（Earth Sciences），44（7）：1374-1387.
	Qu Yajun，Gao Diansheng，1990.Genesis and geological characteristics of gold deposits at Paishanlou in West Liaoning［J］.Liaoning Geology，（4）：304-313.
	Qu Yajun，Gao Diansheng，Jia Yunwei，al et，1992.Alteration characteristics of Paishanlou gold deposit，West Liaoning ［J］.Liaoning Geology，（1）：45-52.
	Sun Shouke，Liu Hongtao，Chu Shaoxiong，2012.Origin of the Paishanlou monzogranite in Liaoning Province and its genetic connection with gold mineralization［J］.Acta Petrologica Sinica，28（2）：607-618.
	Wang Ronghu，Jin Chengzhu，Li Jingchun，2008.⁴⁰Ar-³⁹Ar isotopic dating for Paishanlou gold deposit and its geological implication［J］.Journal of Northeastern University（Natural Science），（10）：1482-1485.
	Wang Zuoman，Wang Ende，Li Da，al et，2016.Deep metallogenic geological characteristics and prospecting indicators of Paishanlou gold deposit in western Liaoning［J］.Modern Mining，32（1）：123-125.
	Wu Changsheng，Shi Zhiqiang，Liu Yanbing，2019.Metallogenic prediction in the deep part of Paishanlou gold district in Liaoning and verification effect in target areas［J］.Gold，40（12）：3-7.
	Xu Dabo，2017.Study of metallogenic model of Paishanlou gold deposit in Fuxin City of Liaoning Province［J］.Mining Engineering，15（3）：5-7.
	Yang Yibiao，Jia Sanshi，Wang Ende，al et，2010.Structural superimposed halo study and deep prediction of Liaoning Paishanlou gold deposit［J］.Metal Mine，（4）：100-105.
	Ye Tianzhu，Zhicheng Lü，Pang Zhenshan，al et，2014.Metallogenic Prognosis Theories and Methods in Exploration Areas［M］.Beijing：Geological Publishing House.
	Zhang Qinghai，Liu Yanbing，2020.Geological characteristics and prospecting criteria of Paishanlou gold deposit in Liaoning Province［J］.World Nonferrous Metals，（22）：65-66.
	Zhang X H，Liu Q，MA Y J，al et，2005.Geology，fluid inclusions，isotope geochemistry，and geochronology of the Paishanlou shear zone-hosted gold deposit，North China Craton［J］.Ore Geology Reviews，26（3/4）：325-348.
	Zhang Yanmin，Song Qiang，Tian Lihuan，al et，2012.The mineralization element characteristics of Paishanlou gold deposit and the metallogenic prognosis in the area，Liaoning［J］.Mineral Exploration，3（3）：363-373.
	蔡新明，2018.阜蒙县排山楼金矿成矿演化模式［J］.吉林地质，37（1）：35-37.
	陈冲，魏俊浩，付乐兵，2013.韧性剪切带型金矿床地质特征研究：以辽宁排山楼金矿床与广东河台金矿床为例［J］.黄金，34（10）：12-16.
	董军，2015.辽宁排山楼韧性剪切带型金矿床成矿地质特征及成矿条件分析［J］.现代工业经济和信息化，5（5）：46-48.
	付乐兵，2012.华北克拉通北缘赤峰—朝阳地区中生代构造岩浆演化与金成矿［D］.武汉：中国地质大学.
	贾三石，付建飞，宋建潮，等，2010.辽宁阜新排山楼金矿床微量元素地球化学特征及矿床深部评价［J］.矿床地质，29（增1）：947-948.
	贾三石，王恩德，付建飞，等，2011.辽西排山楼金矿床微量元素地球化学特征及深部找矿预测研究［J］.地球化学，40（3）：266-279.
	李友权，宋雨春，2015.辽宁省阜新蒙古族自治县排山楼矿区金矿资源储量核实报告［R］.阜新：辽宁排山楼黄金矿业有限责任公司.
	罗镇宽，苗来成，关康，等，2001.辽宁阜新排山楼金矿区岩浆岩锆石SHRIMP定年及其意义［J］.地球化学，30（5）：483-490.
	骆辉，赵运起，1997.辽宁阜新排山楼金矿地质和成矿作用［J］.前寒武纪研究进展，20（4）：13-24.
	马丙乾，2020.辽宁阜新金矿床成矿机制及成矿规律研究［J］.世界有色金属，（22）：89-90.
	孟宪刚，2003.辽西医巫闾山北段中生代构造格架及其对金矿形成富集与分布的控制作用［D］.北京：中国地质大学（北京）.
	孟宪刚，冯向阳，邵兆刚，等，2002.辽西医巫闾山变质核杂岩构造系统及其对金矿的控制［J］.地质通报，（12）：841-847.
	倪金龙，刘俊来，唐小玲，等，2014.排山楼金矿韧性剪切带演化过程［J］.中国科学（地球科学），44（7）：1374-1387.
	曲亚军，高殿生，1990.排山楼金矿床地质特征及金质来源［J］.辽宁地质，（4）：304-313.
	曲亚军，高殿生，贾云伟，等，1992.排山楼金矿床的蚀变特征［J］.辽宁地质，（1）：45-52.
	孙守恪，刘红涛，褚少雄，2012.辽宁省排山楼矿区二长花岗岩成因及其与金矿化的关系［J］.岩石学报，28（2）：607-618.
	王荣湖，金成洙，李景春，2008.排山楼金矿床⁴⁰Ar-³⁹Ar年龄及其地质意义［J］.东北大学学报（自然科学版），（10）：1482-1485.
	王佐满，王恩德，李达，等，2016.辽西排山楼金矿深部成矿地质特征与找矿标志［J］.现代矿业，32（1）：123-125.
	武昌胜，史志强，刘彦兵，2019.辽宁排山楼金矿区深部成矿预测及靶区验证效果［J］.黄金，40（12）：3-7.
	徐大波，2017.辽宁省阜新市排山楼金矿成矿模式研究［J］.矿业工程，15（3）：5-7.
	杨义彪，贾三石，王恩德，等，2010.辽宁排山楼金矿构造叠加晕研究及深部预测［J］.金属矿山，（4）：100-105.
	叶天竺，吕志成，庞振山，等，2014.勘查区找矿预测理论与方法［M］.北京：地质出版社.
	张庆海，刘彦兵，2020.辽宁排山楼金矿地质特征及找矿标志分析［J］.世界有色金属，（22）：65-66.
	张彦民，宋强，田立环，等，2012.辽宁排山楼金矿矿化元素特征及成矿预测［J］.矿产勘查，3（3）：363-373.

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