Wechat
J4 ›› 2012, Vol. 20 ›› Issue (3): 40-45.
• article • Previous Articles Next Articles
XIAO Xiaoqiang,HU Jun,GUAN Bo,SU Shengnian
Received:
Revised:
Online:
Published:
Abstract:
The east section of Eastern Kunlun is as the hot spot of prospecting recent years, more deposits (points) found one by one.Using geological,geophysics and geochemical comprehensive ways,the study results show that the old metamorphic rock(precambrian) is the important ore-bearing horizon,its characteristics is similar with the precambrian around the Qaidam Basin,which is as nappe overlying on the later layer,turning into relic rock sheet, underwent long distance and low angle push.It acted geosyncline foundation recepting sedimentary and basic to neutral magma injecting,showing a rich material source,also undergone multi-structure-heat events,means there is good prospects.We have found two gold deposits,and a few of mineralization points,most of which distribute in precambiran,showing there was a good metallogenic prospecting in precambrian layer.
Key words: Gold ore-belt, Geological characteristics, Prospecting analysis, East section of Eastern Kunlun
CLC Number:
XIAO Xiaoqiang,HU Jun,GUAN Bo,SU Shengnian. Geological Characteristics and Prospecting Analysis of Gold Ore Belt in East Section of Eastern Kunlun[J].J4, 2012, 20(3): 40-45.
0 / / Recommend
Add to citation manager EndNote|Reference Manager|ProCite|BibTeX|RefWorks
URL: http://www.goldsci.ac.cn/EN/
http://www.goldsci.ac.cn/EN/Y2012/V20/I3/40
[1] 孙崇仁.青海省岩石地层[M].武汉:中国地质大学出版社,1997. [2] 中国科学院矿床地球化学开放研究试验室.矿床地球化学[M].北京:地质出版社,1997. [3] 张建新,孟繁聪,万渝生,等.柴达木盆地南缘金水口群的早古生代构造热事件:锆石U-Pb SHRIMP年龄证据[J].地质通报,2003,22(6):397-404. [4] 王灿国,王青海,简平.东昆仑前寒武纪基底变质岩系的锆石SHRIMP年龄及其构造意义[J].地学前缘,2004,11(4):481-490. [5] 祁生胜,宋泰钟,王秉璋.对原“苦海群”的重新认识及其构造演化特征[J].青海地质,2002,(1):22-30. [6] 吴庭祥,张绍宁, 施根红,等.东昆仑东段金矿区地层含矿性分析[J].矿产与地质,2009,23(5):431-441. [7] 石国本.地弯区金的“三位一体”构造成矿及其中国的分布[J].黄金科技动态,1992,1(2):6-11. [8] 肖荣阁,翟裕生,邓军,等.变质岩区金矿成矿系统[J].地学前缘,1999,6(2):243-250. [9] 李智明,薛春纪,王晓虎,等.东昆仑区域成矿特征及有关找矿突破问题分析[J].地质评论,2007,53(5):708-717. [10] 陆露,胡道功,张永清,等.昆中断裂带同构造花岗斑岩锆石U-Pb年龄及其构造意义[J].地质力学学报,2010,16(1):36-43. [11] 陶平,肖旭东,张慧,等.湘黔桂浅变质岩区含金建造及其与金矿的关系[J].地质科技情报,2009,28(2):110-114. [12] 王秉璋,朱迎堂,张智勇,等.昆秦接合部造山带非史密斯地层的一些特点——苦海—赛什塘—羊曲构造混杂带剖析[J].青海地质,2000,(1):9-17. [13] 陈树云,伊有昌,吴小霞,等.青海东昆仑东段区域成矿地质特征及金属矿产找矿方向研究[J].黄金科学技术,2007,15(4):9-17. [14] 孙王勇.东昆仑东段深大断裂的新认识[J].物探与化探,2007,31(5):408-413. [15] 刘世英.东昆仑雪水河地区遥感地质调查与找矿效果[J].黄金科学技术,2011,19(6):44-48. [16] 郭跃进.青海东昆仑东段果洛龙洼金矿床地球化学特征与成矿模式[D].昆明:昆明理工大学,2011.
Cited