img

QQ群聊

img

官方微信

高级检索

J4 ›› 2009, Vol. 17 ›› Issue (5): 30-35.

• 矿产勘查 • 上一篇    下一篇

山东省山后金矿区构造控矿分析

庄光军1 ,刘金友2 ,高梦江2 ,刘淑亮2   

  1. 1. 武警黄金第六支队,河南  三门峡 472000;
    2. 武警黄金第七支队,山东  烟台 264004
  • 收稿日期:2009-04-16 修回日期:2009-05-20 出版日期:2009-10-30 发布日期:2011-09-29
  • 作者简介:庄光军(1969-),男,山东日照人,工程师,主要从事金矿地质找矿的组织管理工作. E-mail:hnsmxzgj@163.com.

Analysis on Structural Ore-controlling of Shanhou Gold Deposit in Shandong Province

ZHUANG Guangjun1,LIU J inyou2, GAO Mengjiang2,LIU Shuliang2   

  1. 1. No.6 Gold Geological Party of the CAPF, Sanmenxia 472000, Henan, China;
    2. No.7 Gold Geological Party of the CAPF, Yantai 472000, Shandong, China
  • Received:2009-04-16 Revised:2009-05-20 Online:2009-10-30 Published:2011-09-29

摘要:

胶东地区是我国著名的金矿集中区,金矿主要受胶西北3条“S”形断裂带控制,自西向东分别为三山岛、焦家、招平断裂。其中,招平断裂带为胶东地区重要的金成矿带之一,目前该成矿带内已探明金储量800 t,成矿潜力巨大。莱西市山后金矿区位于夏甸大型金矿床以南,旧店金矿田的北部,招平断裂带的中南段,由山后、北泊、萌山3个矿段组成。随着招平成矿带研究和控制程度的不断增高,显示该区成矿潜力较大。但是,对其成矿规律的研究仅局限于夏甸金矿床以北,对以南地区金成矿规律的研究力度不够。我们从构造应力场方面分析了该区段金成矿地质条件,并对该区成矿远景进行了评价。

关键词: 山后金矿, 物化探特征, 招平断裂带, 构造控矿, 胶东

Abstract:

Jiaodong is the famous gold2concentrated area, gold mainly is controlled by three“S”-type fault belt, from west to east, respectively Sanshandao, Jiaojia and Zhaop ing faults. Zhaoping fault zone is one of the most important gold faults, it has already been proven gold reserves of 800 tons, and the ore-forming potential is great. Shanhou gold deposit is located in Laixi, south of Xiadian gold deposit, north of Jiudian gold deposit,middle-south of Zhaoping fault belt, it is composed of three mining sections, respectively Shanhou, Beibo and Mengshan. With increasing of study and control degree of Zhaoping metallogenic belt, indicating the mineralization potential of this area is great. However, research of metallogenic regularity in this area is limited in north of Xiadian gold deposit, the research extent of southern parts is very low. We analyse the geological conditions of gold mineralization by tectonic stress field, and evaluate the ore prospecting of this area.

Key words: Shanhou gold deposit, Geophysical and geochemical characteristics, Zhaoping fault belt, Structural ore-controlling, Jiaodong

中图分类号: 

  • P618.51


[1] 李示先,刘长春,安郁宏,等. 胶东金矿地质
[M]. 北京:地质出版社, 2007: 59-101.

[2] 苗来成,罗镇宽,关康,等. 胶东招掖金矿带控矿断裂演化规律
[J]. 地质找矿论丛, 1997, 12 (1): 26-35.

[3] 刘晓煌,张效智,哈本海,等. 招平断裂带地质特征及成矿预测浅析
[J]. 黄金, 2003, 24 (12): 10-13.

[4] 邓军. 山东招掖金矿带断裂构造分带与蚀变矿化分带关系研究
[J]. 矿床地质, 1994, 13: 17-18.

[5] 马树江,张华全,刘金友,等. 山东省莱西市山后矿区金矿普查报告
[R]. 烟台:武警黄金第七支队, 2006: 23.

[6] 邓军,徐守礼,吕古贤,等. 胶东西北部断裂构造与成矿作用研究
[J]. 现代地质, 1996, 10 (4): 502-511.

[7] 吕古贤. 山东省玲珑金矿田成矿深度的研究与测算
[J].科学通报, 1995, 40 (15): 1399-1402.

[1] 王杏村,牛树银,燕建设,孙卫志,孙爱群,冯建之,陈超,徐建昌,王社全,崔燮祥,王铮,李斌. 小秦岭中矿带金矿田成矿构造分析[J]. J4, 2012, 20(4): 96-103.
[2] 李军峰,武际春,刘维民,蒋善波,彭洪迎,朱随洲,生显军,赵红浩,王兵. 山东玲珑金矿田51号脉成矿规律研究及远景预测[J]. J4, 2012, 20(4): 113-116.
[3] 孔令芝,朱随洲,韩云松,张龙,储照波,李新年,吴海庆,杨桂彬,叶官威,信太岭,李军峰. 山东玲珑断裂带地球物理特征综合分析及找矿预测[J]. J4, 2012, 20(4): 117-122.
[4] 王营田,王山章,李波,韩宇. 山东大庄子金矿床1号脉成矿规律及深部探矿预测[J]. J4, 2012, 20(4): 123-127.
[5] 刘新会,陈彩华,赵天心,张科利,陈力子,刘爽. 西秦岭寨上金矿原生晕地球化学特征及成矿预测[J]. J4, 2012, 20(4): 7-15.
[6] 刘金友,刘淑亮,高池兴,顿美霞. 山东西涝口金矿地球化学特征研究[J]. J4, 2012, 20(4): 16-20.
[7] 姜维明,齐婓,孟伟,许建波,刘秋杰,吕军恩,原少波,孙健. 山东玲珑矿田东风矿区成矿规律及远景预测[J]. J4, 2012, 20(4): 21-25.
[8] 金念宪,王君亭,孙之夫,李文,廖昌溪,所建成,刘祥朋. 韧性剪切带控制的“焦家式”金矿及其找矿方向[J]. J4, 2012, 20(4): 26-32.
[9] 黄广环. 内蒙古中东部重要成矿带地质特征及找矿潜力分析[J]. J4, 2012, 20(4): 33-38.
[10] 孙杰,李瑞军,邵周伟,徐芬. 山东谢家沟矿区金矿体地质特征及其深部资源详查评价[J]. J4, 2012, 20(4): 39-42.
[11] 郑卫军,刘新会,陈彩华. 甘肃寨上金矿床1∶5万水系沉积物测量综合评价[J]. J4, 2012, 20(4): 43-48.
[12] 马凤山,赵海军,郭捷,王杰,魏爱华. 山东望儿山矿区浅部复采对井筒稳定性影响的数值模拟[J]. J4, 2012, 20(4): 49-53.
[13] 王义春,李波,张永林,韩宇,任晓明,王召敏,王京聪,周奇明. 电吸附化探新方法在麻湾金矿区寻找深部矿体的研究[J]. J4, 2012, 20(4): 62-66.
[14] 刘桂阁,李艳秋,常春郊,丛润祥,张慧玉,陈勇敢,王美娟,朝银银. 区域化探数据处理的综合异常法研究[J]. J4, 2012, 20(4): 67-70.
[15] 王恩敬,郭广军,赵荣欣,王彦伟,于晓杰,吕广耀,王伟涛. 山东寺庄金矿床构造—矿化网络结构研究及应用[J]. J4, 2012, 20(4): 76-80.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!