Gold Science and Technology
img

Wechat

Adv. Search
Online Submission Peer Review Office Work

J4 ›› 2008, Vol. 16 ›› Issue (6): 6-10.

• article • Previous Articles     Next Articles

The Geolog ica l Character istics and Prospecting Potentia l in Dazhuangz i Gold Deposit, Shandong Prov ince

ZHOU Guofa1 , LV Guxian2 , SHEN Yuke2 , GUO Tao2 , WANGWei3 ,WE I Genyuan4   

  1. 1. S tate Key Laboratory of Geological Processes and M ineral Resources, China University of Geosciences, Beijing   100083, China;
    2. Institute of Geom echanics, CAGS, Beijing   100081, China;
    3. Industria l Designing Institute of Guangxi, Nanning    530022, Guangxi, China;
    4. Guangxi Geology and M ineral Resources Exploration and Developm ent Co. , L td. , Nanning   530023, Guangxi, China
  • Received:2008-07-01 Revised:2008-08-19 Online:2008-12-23 Published:2011-07-06

PDF (PC)

1141

Abstract:

Dazhuangzi gold deposit, which mainly includes gold2bearing altered rock type and gold2bearing quartz vein type, is located in the edge between J iaolai basin and J iaobei terrane. With the p rogress of research in J iaodong and resource ofDazhuangzi gold deposit reducing, it requests analyzing on ore2forming potentiality and p rospecting target. We can find thatmuch resource can be found in surrounding and deepness of Dazhuangzi gold deposit by comp rehensive analysis on its geological characteristics, ore2grade trend and ore2body trend. According to the resource potentiality it can be divided into three p rospecting targets in Dazhuangzi gold deposit, they are lying on the north superficiality and deepness part of known ore2bodywhich is the most importance one, the deepness part and the south deepness part of known ore2bodywhich is the second importance one, meanwhile the superficiality part of known ore2body also need some farther exp loration work.

Key words: Dazhuangzi gold deposit, Gold, Prospecting potential, Geological characteristics, Shandong

CLC Number: 

  • P618. 51　　

[ 1 ] 朱大岗,张振江. 胶东大庄子金矿地质特征[ J ]. 矿物岩石地球化学通报, 1998, 17 (1) : 9—12.
[ 2 ] 朱大岗,吕古贤,邓军,等. 胶东大庄子金矿地质特征与成因探讨[ J ]. 贵金属地质, 1999, 8 (2) : 81—86.
[ 3 ] 邹为雷,沈远超,张连昌,等. 平度市大庄子金矿床控矿构造特征及金矿赋存规律初步探讨[ J ]. 地质与勘探, 2001,37 (1) : 44—48.
[ 4 ] 郭百创,赵冬冬. 平度市大庄子矿区金矿床成因类型探讨[ J ]. 地质与勘探, 2002, 38 (4) : 36—40.
[ 5 ] 邹为雷,沈远超,张连昌,等. 山东平度大庄子金矿床地质特征及成因[ J ]. 大地构造与成矿学, 2002, 26 ( 4) : 410—415.
[ 6 ] 连国建,胡文` ,张文兰,等. 胶东大庄子金矿地质特征与成因探讨[ J ]. 矿床地质, 2004, 23 (1) : 67—76.
[ 7 ] 张连昌,沈远超,邹为雷,等. 大庄子金矿成矿作用地质地球化学特征及成因[ J ]. 地质与资源, 2002, 11 (1) : 16—22.
[ 8 ] 连国建. 大庄子金矿床稳定同位素地球化学研究[ J ]. 地质找矿论丛, 2003, 18 (1) : 126—131.
[ 9 ] 连国建,史维全,门树宁,等. 山东省平度市大庄子金矿流体包裹体研究[ J ]. 地质与勘探, 2005, 41 (1) : 28—32.
[ 10 ] 邓军,翟裕生,杨立强,等. 构造演化与成矿系统动力学——以胶东金矿集中区为例[ J ]. 地学前缘, 1999, 6(2) : 315—323.
[ 11 ] 邓军,徐守礼,方云,等. 胶东西北部构造体系及金成矿动力学[M ]. 北京:地质出版社, 1996: 61—74.
[ 12 ] 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.
[ 15 ] 邓军,王庆飞,杨立强,等. 胶西北金矿集区成矿作用发生的地质背景[ J ]. 地学前缘, 2004, 11 (4) : 527—533.
[ 16 ] 吕古贤,邓军,郭涛,等. 玲珑—焦家式金矿构造变形岩相形迹大比例尺填图与构造成矿研究[ J ]. 地球学报,1998, 19 (2) : 177—186.
[ 17 ] 丁式江,翟裕生,邓军. 胶东焦家金矿蚀变岩中元素的质量迁移[ J ]. 地质与勘探, 2000, 36 (4) : 28—31.
[ 18 ] 刘金友,段留安. 胶莱盆地北缘金矿特征及找矿前景分析[ J ]. 黄金科学技术, 2006, 14 (2) : 30—35.
[ 19 ] 朱洪岭,张华全. 胶莱盆地西谭格庄地区金成矿前景分析[ J ]. 黄金科学技术, 2006, 14 (2) : 47—51.
[ 20 ] 申玉科. 胶西北金矿集中区构造—蚀变网络研究[D ].北京:中国地质大学(北京) , 2006: 92—101.
[1] N IU Shuyin, CHEN Chao , SUN Aiqun,WANGBaode,MA Baojun, J IANG Xiaoping. Metallogenic Geological Character istics of Shihu Gold Deposit in theWestern Hebei Province [J]. J4, 2008, 16(6): 1-5.
[2] QI Yuanjiang ,L I Fengge ,WANG Cuijuan. THE GEOLOGICAL CHARACTERISITICS AND PROSPECTING EXPERIENCE OF SANDAOCHA GOLD DEPOSIT IN JILIN PROVINCE [J]. J4, 2002, 10(3): 18-25.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!

©2018 Gold Science and Technology　

Telephone：0931-8277791　

E-mail: hjkx@lzb.ac.cn Postcode：730000　

Powered by Beijing Magtech Co. Ltd

陇ICP备17001318号-1