|Table of Contents|

Geological Feature and Prospecting of Iron Deposit in Pingshun Area,Southern Taihang Mountain(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2010年第03期
Page:
234-238
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Geological Feature and Prospecting of Iron Deposit in Pingshun Area,Southern Taihang Mountain
Author(s):
ZHANG Hai-dong1;  LIU Jian-chao1;  JIANG Ai-guo2;  LIU Shu-wen1;  GE Xiao-hong1
(1.School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 2.Mining Branch Company, Changzhi Iron and Steel Company Limited, Changzhi 046000, Shanxi, China)
Keywords:
metallogenetic characteristic;  mineralization forecast;  emplacement mechanics;  iron deposit in Pingshun Area;  Southern Taihang Mountain
PACS:
P612;P618.31
DOI:
-
Abstract:
Tentonic characteristics of iron deposit in Pingshun Area of Southern Taihang Mountain and kinetics characteristics of magmatic rocks were discussed. The first magmatic belt belongs to passive emplacement mechanism, forming ore bodies potentially; the second belt belongs to initiative emplacement mechanics, forming ore bodies potentially in anticlinal nucleus and the contact zone of rock and wall. According to the characteristic of rare earth element, trace element and Pb isotope in rock and ore and the relationship between ore and rock bodies, the later diorite is main metallogenic mother rock, and early basic-ultrabasic rock indirectly provides support for forming iron deposit; distribution of ore, which is irregular plate, lenticular shapes, branch and pinnate, is controlled by the contact zone and structural form. Based on the forecasting methods of metallogenic pattern, magnetic anomaly and abnormal electrical, the districts of Shuangjing, Dongjiao and southern fringe of Longjianggou are considered as the prospecting zone.

References:

[1] 刘建朝,张海东,刘淑文,等.太行山南段杂岩体成因研究[J].地质论评,2009,55(3):318-327.
[2] 郑建民,陈懋弘,徐林刚,等.邯邢地区矽卡岩型铁矿构造控矿特征及找矿勘探方向[J].矿床地质 2006,25(增刊):115-118.
[3] 罗照华,邓晋福,韩秀卿.太行山造山带岩浆活动及其造山过程反演[M].北京:地质出版社,1999.
[4] 张海东,刘建朝,刘淑文,等.太行山南段平顺地区矽卡岩铁矿地质特征及成矿模式探讨[J].矿物岩石,2009,29(3):53-59.
[5] 张海东.晋南平顺地区矽卡岩型铁矿成矿作用特征及成矿预测[D].西安:长安大学,2009.
[6] 张 涛.青海那陵郭勒河东晚三叠世侵入岩形成环境及年代学研究[J].西北地质,2009,42(1):62-67.
[7] 赵一鸣,吴良士,白 鸽,等.中国主要金属矿床成矿规律[M].北京:地质出版社,2004.
[8] 朱广彬,刘国范,姚新年,等.东秦岭铅锌银金钼多金属成矿带成矿规律及找矿标志[J].地球科学与环境学报,2005,27(1):44-52.
[9] 张照伟,赵东宏,李文渊,等.陕西省洛南县莲花沟钼矿地质特征及找矿标志[J].西北地质,2008,41(1):74-80.
[10] 刘玉成,杨艺华,王永基.大冶铁矿控矿构造研究及深部隐伏矿体定位预测[J].地质与勘探,2006,42(6):10-16.
[11] 王永基.褶皱构造与隐伏矿床预测[J].地质与勘探,1990,26(7):10-15.
[12] 王 瑜,李朗田,苏绍明.鄂东铁矿成矿地质特征与找矿预测[J].地质与勘探,2007,43(1):17-25.

Memo

Memo:
-
Last Update: 2010-09-20