Application Research of Comprehensive Geophysical Prospecting Methods and Geological Characters for Porphyry Molybdenum Multiple Metal Deposits in the North Area of the Northern Dabie Mountains
Received date: 2013-12-29
Revised date: 2014-03-10
Online published: 2014-11-04
On the basis of analyzing geological background of regional metallogenic in north of Dabie Mountains,geologic feature of large porphyry molybdenum polymetallic in the Tangjiaping was systemically described with the methods of stone of rock (ore) physical properties test,controlled source audio-frequency magnetotelluric sounding method (CSAMT) and spectrum IP method(SIP).The results showed that there is phyical differences between porphyry molybdenum ore body and wall rock.Meanwhile,using the two kinds of electrical method can well reflect the ore-forming geological spatial location and morphology,indicating that the method combined with porphyry molybdenum polymetallic deposit was effective,which can provide important technical reference for porphyry deposits in the area in the future.
Key words: CSAMT; SIP; porphyry molybdenum deposit; polymetallic ore; north of Dabie Mountains
LI Bing , SHANG Jiange , ZHANG Zhihui , LIU Qingquan , DING Yunhe , WEI Mingjun , LI Yongfeng . Application Research of Comprehensive Geophysical Prospecting Methods and Geological Characters for Porphyry Molybdenum Multiple Metal Deposits in the North Area of the Northern Dabie Mountains[J]. Gold Science and Technology, 2014 , 22(3) : 36 -42 . DOI: 10.11872/j.issn.1005-2518.2014.03.036
[1] 杨永飞,李诺,倪智勇.陕西省华县金堆城斑岩型钼矿床流体包裹体研究[J].岩石学报,2009,25(11):2983-2993.
[2] 赵瑞锋,穆新华.狮子庙金钼矿田成因机制探讨[J].黄金科学技术,2009,17(6):39-41.
[3] 李洪英,毛景文,王晓霞,等.陕西金堆城钼矿区花岗岩Sr、Nd、Pb同位素特征及其地质意义[J].中国地质,2011,38(6):1536-1550.
[4] 黄典豪,侯增谦,杨吉明,等.东秦岭钼矿带内碳酸岩脉型钼(铅)矿床地质—地球化学特征、成矿机制及成矿构造背景[J].地质学报,2009,83(12):1968-1984.
[5] 何亚清,陈凤群,杨建敏,等.豫西石窑沟金钼矿床地质特征研究[J].黄金科学技术,2013,21(1):28-32.
[6] 徐晓春,岳书仓,潘成荣,等.河南桐柏老湾花岗岩岩浆动力学与成矿[J].岩石学报,2001,17(2):245-253.
[7] 马宏卫.河南桐柏老湾金矿综合找矿标志及找矿模型[J].物探与化探,2007,31(3):211-215.
[8] 王洪恩.桐柏银洞坡金矿床构造形迹研究[J].现代矿业,2006,25(6):6-8.
[9] 陈良,戴立军,王铁军,等.河南省老湾金矿床地球化学特征及矿床成因[J].现代地质,2009,23(2):277-284.
[10] 张宗恒,方国松,侯海燕,等.河南桐柏老湾金矿床地质特征及成因探讨[J].黄金地质,2002,8(3):20-26.
[11] 杨泽强.河南商城县汤家坪钼矿辉钼矿铼—锇同位素年龄及地质意义[J].矿床地质,2007,26(3):289-295.
[12] 李靖辉.大别山(北麓)斑岩型钼矿床成矿系列及成矿规律[J].东华理工大学学报(自然科学版),2008,31(1):25-30.
[13] 李俊平,李永峰,罗正传,等.大别山北麓钼矿重大进展及其矿床地质特征研究[J].大地构造与成矿学,2011,35(4):576-586.
[14] 罗正传,李永峰,王义天,等.大别山北麓河南新县地区大银尖钼矿床辉钼矿Re-Os同位素年龄及其意义[J].地质通报,2010,29(9):1349-1354.
[15] 李毅,李诺,杨永飞,等.大别山北麓钼矿床地质特征和地球动力学背景[J].岩石学报,2013,29(1):95-106.
[16] 李永峰,李俊平,罗正传,等.河南省新县墨斗河钼多金属矿床地质特征及找矿远景[J].地质找矿论丛,2013,28(1):20-26.
[17] 杨泽强,万守全,马宏卫,等. 河南商城县汤家坪钼矿床地球化学特征与成矿模式[J].地质学报,2008,82(6):788-794.
[18] 李悦辉,王季伟.河南商城汤家坪钼矿成矿地质特征与构造解析[J].华南地质与矿产,2009,(4):37-42.
[19] 袁德志,赵瑞强,李吉林.河南省商城县汤家坪钼矿床成因研究[J].现代矿业,2008,24(8):21-24.
[20] 徐公权.河南省商城县汤家坪斑岩型钼矿床成因探讨[J].资源环境与工程,2011,25(2):95-98.
[21] 徐公权,刘合胜.河南省商城县汤家坪钼矿地质特征及勘查方法探讨[J].资源环境与工程,2010,24(3):238-241.
[22] 杨艳,张静,刘家军,等.河南汤家坪钼矿床流体成矿作用研究[J].中国地质, 2008,35(6):1240-1249.
[23] 杨泽强.商城县汤家坪钼矿地球化学特征及找矿远景[J].物探与化探,2008,32(6):590-618.
[24] 徐友灵.汤家坪钼矿床地质特征[J].现代矿业,2005,21(7):27-29.
[25] 杨泽强.河南省商城县汤家坪钼矿围岩蚀变与成矿[J].地质与勘探,2007, 43(5):17-22.
[26] 杨泽强.北大别山商城汤家坪富钼花岗斑岩体地球化学特征及构造环境[J].地质论评,2009,55(5):745-752.
[27] 刘清泉,柳玉虎,李永峰,等.大别山北麓斑岩型钼矿床成矿地质条件及矿床成因[J].地质找矿论丛,2013,28(1):27-33.
[28] 刘金友,丁宪华,刘淑亮,等.CSAMT法在西涝口金矿勘查中的应用[J].黄金科学技术, 2013,21(3):16-20.
[29] 柳建新,郭振威,郭荣文,等.CSAMT和重力方法在狮子温泉深部地球物理勘查中的应用[J].地球物理学进展,2009,24(5):1868-1873.
[30] 李志杰,杨瑞亭.地球物理勘探方法及其在多金属找矿中的应用[J].黄金科学技术,2009,17(2):38-41.
[31] 汤井田,何继善.可控源音频大地电磁法及其应用[M].长沙:中南大学出版社,2005.
[32] 何继善.可控源音频大地电磁法[M].长沙:中南大学出版社,1990.
[33] 郭衍游,唐菊兴,董树义.偶极幅频激电法在西藏玉龙铜矿床定位预测研究中的应用[J].华南地质与矿产,2002, (4):70-74.
[34] 崔先文,何展翔,刘雪军,等.频谱激电法在大港油田的应用[J].石油地球物理勘探,2004,39(增):101-105.
[35] 李冰, 晁代超, 魏明君, 等.电磁测深技术在深部铁矿探测中的应用研究——以河南舞阳铁矿区为例[J].中国地质,2013,40(5):1644-1654.
[36] 李冰,丁云河,魏明君,等.综合物探法开展深部隐伏岩(矿)体勘查的探索研究——以河南西部多金属成矿带为例[J].黄金科学技术,2012,20(6):21-26.
/
〈 | 〉 |