«上一篇/Previous Article|本期目录/Table of Contents|下一篇/Next Article»

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

卷:

第45卷

期数:

2023年第01期

页码:

27-41

栏目:

基础地质与矿床地质

出版日期:

2023-01-15

文章信息/Info

Title:

Structural Ore-controlling Model and Metallogenic Target of Longhuo Gold Deposit in Longlin Area, the Western Guangxi, China

文章编号:

1672-6561(2023)01-0027-15

作者:

安 鹏¹; 陈懋弘^2*; 孔志岗¹; 陈 港²; 陈忠斌³; 乐兴文³

(1. 昆明理工大学 国土资源工程学院,云南 昆明 650093; 2. 中国地质科学院矿产资源研究所 自然资源部成矿作用和资源评价重点实验室,北京 100037; 3. 广西壮族自治区第四地质队,广西 南宁 530033)

Author(s):

AN Peng¹;  CHEN Mao-hong^2*;  KONG Zhi-gang¹;  CHEN Gang²;  CHEN Zhong-bin³;  LE Xing-wen³

(1. Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming 650093, Yunnan, China; 2. MNR Key Laboratory of Metallogeny and Mineral Assesment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; 3. No.4 Geology Team of Guangxi Zhuang Autonomous Region, Nanning 530033, Guangxi, China)

关键词:

金矿床;  孤立碳酸盐岩台地;  层状矿体;  卡林型;  构造控矿;  成矿预测;  广西

Keywords:

gold deposit;  isolated carbonate platform;  bedded ore body;  Carlin-type;  structural ore-controlling;  metallogenic prediction;  Guangxi

分类号:

P618.51; P612

DOI:

10.19814/j.jese.2022.06017

文献标志码:

A

摘要:

滇黔桂“金三角”是世界著名的卡林型金矿矿集区之一。该区现有成矿研究多集中在孤立碳酸盐岩台地边缘,很少涉及孤立碳酸盐岩台地内部,导致台地内部的矿体就位因素与控矿模型还不清楚。详细研究了桂西隆林地区隆或金矿这一典型的台地内部金矿床,深入解析矿体控矿构造,构建控矿模型。结果表明隆或金矿区构造运动主要分为3期:第一期为海西期,形成NE向F₀同生断层,并形成台沟相隔的古地理格局,其中在台沟相区沉积了薄层硅质岩-泥岩-粉砂岩组合,为矿床的形成提供了地层条件; 第二期为印支期,形成了隆或穹隆及其NW向的磨毫次级背斜,为成矿提供了构造准备; 第三期为燕山期,表现为F₀断层的重新活动,成为矿区主要的热液流体通道(导矿构造),其西侧发育大量的平行次级正断层及伴生的牵引褶皱,并逐渐向西减弱为节理带和劈理带,这些次级断层-节理-劈理带共同组成了矿区的配矿构造系统,引导成矿流体在磨毫次级背斜核部的下石炭统英塘组硅质岩-碳质泥岩-凝灰岩中交代、充填形成层状矿体。因此,隆或金矿主要受岩性和构造联合控制。根据控矿模型并结合地球物理-地球化学-遥感资料,可以预测:NE向F₀断层西侧附近,隆或金矿深部的次级背斜核部是有利的深部找矿靶区,含矿层位为下石炭统英塘组; F₀断层与隆或穹隆核部的交汇部位是外围有利找矿靶区,含矿层位为下泥盆统郁江组,特别是与寒武系接触的不整合面附近。

Abstract:

The adjacent area of Yunnan, Guizhou, and Guangxi provinces, termed the “Golden Triangle”, is one of the world-famous Carlin-type gold ore concentration areas. Previous metallogenic research in this area mainly focuses on the mineralization at the edge of the carbonate platform. However, it rarely involves the interior of the carbonate platform, so the ore body emplacement factors and ore-controlling models are still unclear within the platform. The Longhuo gold deposit, a typical gold deposit located at the platform's interior in the western Guangxi, was analyzed in detail; the ore-controlling structure and model were fundamentally constructed. The results show that the structures of Longhuo gold deposit can be divided into three periods. ①The first period is Hercynian sedimentary, which forms the NE-trending F₀ syngenetic fault and the platform-trench paleogeographic pattern with the thin-layer siliceous rock-mudstone-siltstone components; the lithology provides the stratigraphic conditions for the formation of the deposit. ②The second period is Indosinian orogenic, which forms the Longhuo dome and NW-trending Mohao secondary anticline; the anticline provides favorable tectonic conditions for the mineralization. ③The third period is Yanshan metallogenic characterized by the reactivation of fault F₀, which is the main hydrothermal fluid migration channel in the mine area. A large number of parallel secondary normal faults and associated traction folds develop on its western side, and gradually weaken into joints and cleavage zones to the west. These secondary fault-joint-cleavage zones together form the ore-allocating tectonic system of the mine area, guiding the ore-forming fluids to replace and filling the siliciclastic-carbonaceous mudstones and tuffs of Lower Carboniferous Yingtang Formation in Mohao secondary anticline core to form bedded ore bodies. Therefore, the Longhuo gold ore body is jointly controlled by lithology and tectonics. According to the metallogenic model, combined with geophysics-geochemistry-remote sensing data, it is predicted that near the western side of the NE-trending fault F₀, the secondary anticline core of the deep part of Longhuo gold deposit is the favorable prospecting target. The ore-bearing stratum is Lower Carboniferous Yingtang Formation. The intersection of fault F₀ and the core of Longhuo dome is the favorable prospecting target for mineralization in the periphery of Lower Devonian Yujiang Formation, especially near the unconformity in contact with Cambrian.

参考文献/References:

[1] HU R Z,SU W C,BI X W,et al.Geology and Geochemistry of Carlin-type Gold Deposits in China[J].Mineralium Deposita,2002,37(3/4):378-392.
[2] HU R Z,FU S L,HUANG Y,et al.The Giant South China Mesozoic Low-temperature Metallogenic Domain:Reviews and a New Geodynamic Model[J].Journal of Asian Earth Sciences,2017,137:9-34.
[3] PETERS S G,HUANG J Z,LI Z P,et al.Sedimentary Rock-hosted Au Deposits of the Dian-Qian-Gui Area,Guizhou,and Yunnan Provinces,and Guangxi District,China[J].Ore Geology Reviews,2007,31(1/2/3/4):170-204.
[4] CLINE J S,MUNTEAN J L,GU X X,et al.A Comparison of Carlin-type Gold Deposits:Guizhou Pro-vince,Golden Triangle,Southwest China,and Northern Nevada,USA[J].Earth Science Frontiers,2013,20(1):1-18.
[5] SU W C,DONG W D,ZHANG X C,et al.Carlin-type Gold Deposits in the Dian-Qian-Gui “Golden Triangle” of Southwest China[M]∥MUNTEAN L L.Diversity in Carlin-style Gold Deposits.Washington DC:Society of Economic Geologists,2018:157-185.
[6] XIE Z J,XIA Y,CLINE J S,et al.Are There Carlin-type Gold Deposits in China?A Comparison of the Guizhou,China,Deposits with Nevada,USA,Deposits[M]∥MUNTEAN L L.Diversity in Carlin-style Gold Deposits.Washington DC:Society of Economic Geologists,2018:187-233.
[7] 王砚耕,索书田,张明发.黔西南构造与卡林型金矿[M].北京:地质出版社,1994.
WANG Yan-geng,SUO Shu-tian,ZHANG Ming-fa.Structure and Carlin-type Gold Deposits in Southwest Guizhou Province[M].Beijing:Geological Publishing House,1994.
[8] 王砚耕,王立亭,张明发,等.南盘江地区浅层地壳结构与金矿分布模式[J].贵州地质,1995,12(2):91-183.
WANG Yan-geng,WANG Li-ting,ZHANG Ming-fa,et al.Texture of the Upper Crust and Pattern of the Disseminated Gold Deposits Distributed in Nanpanjiang Area[J].Guizhou Geology,1995,12(2):91-183.
[9] 胡煜昭,王津津,韩润生,等.印支晚期冲断-褶皱活动在黔西南中部卡林型金矿成矿中的作用:以地震勘探资料为例[J].矿床地质,2011,30(5):815-827.
HU Yu-zhao,WANG Jin-jin,HAN Run-sheng,et al.Role of Late Indosinian Thrust-folding in Ore-forming Process of Carlin-type Gold Deposits,Central Southwestern Guizhou:Seismic Evidence[J].Mineral Deposits,2011,30(5):815-827.
[10] 陈懋弘,毛景文,UTTLEY P J,等.贵州锦丰(烂泥沟)超大型金矿床构造解析及构造成矿作用[J].矿床地质,2007,26(4):380-396.
CHEN Mao-hong,MAO Jing-wen,UTTLEY P J,et al.Structure Analysis and Structural Metallogenesis of Jinfeng(Lannigou)Gold Deposit in Guizhou Province [J].Mineral Deposits,2007,26(4):380-396.
[11] 陈懋弘,黄庆文,李继贤,等.广西乐业林旺金矿床构造解析及构造成矿作用[J].大地构造与成矿学,2010,34(3):349-361.
CHEN Mao-hong,HUANG Qing-wen,LI Ji-xian,et al.Structure Analysis and Structural Metallogenesis of the Linwang Gold Deposit,Leye,Guangxi,China [J].Geotectonica et Metallogenia,2010,34(3):349-361.
[12] CHEN M H,MAO J W,BIERLEIN F P,et al.Structural Features and Metallogenesis of the Carlin-type Jinfeng(Lannigou)Gold Deposit,Guizhou Province,China[J].Ore Geology Reviews,2011,43(1):217-234.
[13] 陈懋弘,谢贤洋,马克忠.贵州泥堡卡林型金矿断控型矿体的地层和岩性条件研究[J].黄金科学技术,2018,26(2):131-142.
CHEN Mao-hong,XIE Xian-yang,MA Ke-zhong.Research on Lithology and Stratigraphy Conditions of Fault-controlled Orebody in Nibao Carlin-type Gold Deposit,Guizhou Province[J].Gold Science and Technology,2018,26(2):131-142.
[14] 陈懋弘,乐兴文,李忠阳,等.桂西隆林孤立台地卡林型金矿的“梯式”结构模型及找矿前景[J].大地构造与成矿学,2018,42(5):832-845.
CHEN Mao-hong,LE Xing-wen,LI Zhong-yang,et al.A “Ladder” Model for Carlin-type Gold Deposits in Longlin Isolated Carbonate Rock Platform,Western Guangxi and Its Prospecting Potential [J].Geotecto-nica et Metallogenia,2018,42(5):832-845.
[15] 刘建中,邓一明,刘川勤,等.贵州省贞丰县水银洞层控特大型金矿成矿条件与成矿模式[J].中国地质,2006,33(1):169-177.
LIU Jian-zhong,DENG Yi-ming,LIU Chuan-qin,et al.Metallogenic Conditions and Model of the Superlarge Shuiyindong Stratabound Gold Deposit in Zhenfeng County,Guizhou Province[J].Geology in China,2006,33(1):169-177.
[16] 刘建中,陈景河,邓一明,等.贵州水银洞超大型金矿勘查实践及灰家堡矿集区勘查新进展[J].地质调查与研究,2009,32(2):138-143.
LIU Jian-zhong,CHEN Jing-he,DENG Yi-ming,et al.Exploration of the Shuiyindong Super-scale Gold Deposit and the Evolution of Exploration for Metallogenic Belt of the Huijiabao Anticline in Guizhou Pro-vince[J].Geological Survey and Research,2009,32(2):138-143.
[17] 夏 勇,张 瑜,苏文超,等.黔西南水银洞层控超大型卡林型金矿床成矿模式及成矿预测研究[J].地质学报,2009,83(10):1473-1482.
XIA Yong,ZHANG Yu,SU Wen-chao,et al.Metallogenic Model and Prognosis of the Shuiyindong Super-Large Stratabound Carlin-type Gold Deposit,Southwestern Guizhou Province,China [J].Acta Geologica Sinica,2009,83(10):1473-1482.
[18] 戢兴忠,陈懋弘,刘 旭,等.黔西南泥堡金矿床构造解析及构造控矿作用[J].矿床地质,2018,37(6):1296-1318.
JI Xing-zhong,CHEN Mao-hong,LIU Xu,et al.Struc-ture Analysis and Structural Ore-controlling Role of Nibao Gold Deposit in Southwestern Guizhou Pro-vince[J].Mineral Deposits,2018,37(6):1296-1318.
[19] 国家辉.桂西北超微粒型金矿及其成矿和找矿模式[M].北京:地震出版社,1992.
GUO Jia-hui.Ultramicro Grain-type Gold Deposits in Northwest Guangxi and Their Metallogenic and Pro-specting Models[M].Beijing:Seismological Press,1992.
[20] 陈开礼,郜兆典,杭长松.广西金矿地质[M].南宁:广西科学技术出版社,2002.
CHEN Kai-li,GAO Zhao-dian,HANG Chang-song.Gold Geology in Guangxi [M].Nanning:Guangxi Science & Technology Publishing House,2002.
[21] LI X H,BAI L G,YU Y,et al.Origin and Significance of Pre-mineralization Pyrite in the Jinya Gold Depo-sit,Northwestern Guangxi Province,China:In-situ Trace Element and Sulfur Isotope Constraints[J].Arabian Journal of Geosciences,2021,14(22):2395.
[22] 庞保成,肖 海,付 伟,等.桂西北明山卡林型金矿床热液矿物的显微组构与化学成分特征及其对成矿作用的指示[J].吉林大学学报(地球科学版),2014,44(1):105-119.
PANG Bao-cheng,XIAO Hai,FU Wei,et al.Microfabric and Composition of Hydrothermal Minerals from the Mingshan Carlin Gold Deposit in Northwestern Guangxi and Their Implication for Ore-forming Process [J].Journal of Jilin University(Earth Science Edition),2014,44(1):105-119.
[23] 张长青,王登红,王永磊,等.广西田林县高龙金矿成矿模式探讨[J].岩石学报,2012,28(1):213-224.
ZHANG Chang-qing,WANG Deng-hong,WANG Yong-lei,et al.Discuss on the Metallogenic Model for Gao-long Gold Deposit in Tianlin County,Guangxi,China[J].Acta Petrologica Sinica,2012,28(1):213-224.
[24] 姚 野,刘希军,时 毓,等.桂西北马雄金矿地质特征及其成因探讨[J].矿物学报,2015,35(增1):256.
YAO Ye,LIU Xi-jun,SHI Yu,et al.Geological Cha-racteristics and Genesis of Maxiong Gold Deposit in Northwestern Guangxi [J].Acta Mineralogica Sinica,2015,35(S1):256.
[25] 彭志永,张人人.广西那坡县果提金矿床地质特征[J].广西地质,1999(2):3-5,40.
PENG Zhi-yong,ZHANG Ren-ren.Geological Cha-racteristics of Guoti Gold Deposit of Guangxi Nabo[J].Guangxi Geology,1999(2):3-5,40.
[26] 庞保成.广西隆或金矿床地质特征与成因探讨[J].南方国土资源,2004(11):74-75.
PANG Bao-cheng.Geological Characteristics and Ge-nesis of Longhuo Gold Deposit in Guangxi [J].Land and Resources of Southern China,2004(11):74-75.
[27] 刘显凡,杨科佑,张兴春.从桂西北隆或金矿的地质地球化学特征看微细粒浸染型金矿的可能成因[J].地质地球化学,1998,26(4):1-8.
LIU Xian-fan,YANG Ke-you,ZHANG Xing-chun.Preliminary Discussion on the Possible Genesis of the Carlin-type Gold Deposits in Terms of the Geology and Geochemistry of the Longhuo Gold Deposit,Northwest Guangxi[J].Geology-geochemistry,1998,26(4):1-8.
[28] 陈懋弘,马克忠,陈 港,等.桂西孤立台地寒武系白云岩中的卡林型金矿床:以隆林德峨金矿为例[J].矿床地质,2021,40(5):891-914.
CHEN Mao-hong,MA Ke-zhong,CHEN Gang,et al.Carlin-type Gold Deposits Hosted in Cambrian Dolostone on Isolated Carbonate Platform in Western Guangxi,China:A Case Study from De'e Gold Depo-sit,Longlin[J].Mineral Deposits,2021,40(5):891-914.
[29] 陈开礼.桂西古侵蚀沉积间断面型金矿床[J].广西地质,2000(4):19-22.
CHEN Kai-li.Palaeoerosion Sedimentary Discontinuity-type Gold Deposit of Western Guangxi[J].Guangxi Geology,2000(4):19-22.
[30] 黄宏伟.广西右江盆地微粒型金矿成因探讨[J].华南地质与矿产,2002,18(1):1-9.
HUANG Hong-wei.Discussion on Origin of Microgranular Gold Deposit in the Youjiang Basin[J].Geo-logy and Mineral Resources of South China,2002,18(1):1-9.
[31] 罗允义.桂西古岩溶型金矿地质特征[J].中国地质,2003,30(2):179-185.
LUO Yun-yi.Geological Characteristics of Paleokarst-type Gold Deposits in Western Guangxi[J].Geology in China,2003,30(2):179-185.
[32] 刘 寅,胡 凯,韩善楚,等.右江盆地构造和演化及对卡林型金矿床的控制作用[J].高校地质学报,2015,21(1):1-14.
LIU Yin,HU Kai,HAN Shan-chu,et al.Structural Evolution of the Youjiang Basin and Its Controlling Effects on the Formation of Carlin-type Gold Deposits[J].Geological Journal of China Universities,2015,21(1):1-14.
[33] 蔡明海,肖俊杰,彭振安,等.黔西南泥堡金矿床构造特征及其控矿作用[J].大地构造与成矿学,2022,46(1):48-62.
CAI Ming-hai,XIAO Jun-jie,PENG Zhen-an,et al.Characteristics and Ore-controlling Significance of Structures in the Nibao Gold Deposit,Southwestern Guizhou[J].Geotectonica et Metallogenia,2022,46(1):48-62.
[34] LI Z X,LI X H.Formation of the 1 300-km-wide Intracontinental Orogen and Postorogenic Magmatic Province in Mesozoic South China:A Flat-slab Subduction Model[J].Geology,2007,35(2):179-182.
[35] 黄汲清.中国大地构造及其演化[M].北京:科学出版社,1980.
HUANG Ji-qing.The Geotectonic Evolution of China[M].Beijing:Science Press,1980.
[36] 广西壮族自治区地质矿产局.广西壮族自治区区域地质志[M].北京:地质出版社,1985.
Bureau of Geology and Mineral Resources of Guangxi Zhuang Autonomous Region.Regional Geology of Guangxi Zhuang Autonomous Region [M].Beijing:Geological Publishing House,1985.
[37] 陈懋弘,程彦博,章 伟,等.右江褶皱带燕山期岩浆作用与成矿作用初步研究[C]∥陈毓川.第九届全国矿床会议论文集.北京:地质出版社,2008:241-242.
CHEN Mao-hong,CHENG Yan-bo,ZHANG Wei,et al.Preliminary Study on Yanshanian Magmatism and Mineralization in Youjiang Fold Belt [C]∥CHEN Yu-chuan.Proceedings of the 9th National Conference on Mineral Deposits.Beijing:Geological Publishing House,2008:241-242.
[38] 卢卫平,方少仙.桂西北隆或石炭系沉积相:一个孤立的古碳酸盐台地剖析[J].西南石油学院学报,1986,8(2):1-13.
LU Wei-ping,FANG Shao-xian.Carboniferous Sedimentary Facies of Longhuo,North-western Guangxi:A Dissection on an Ancient Isolated Carbonate Platform [J].Journal of Southwest Petroleum Institute,1986,8(2):1-13.
[39] 蒋柏昌,张 喜,蒋征林.广西隆或金矿床地质特征及控矿因素分析[J].南方国土资源,2013(7):30-33.
JIANG Bo-chang,ZHANG Xi,JIANG Zheng-lin.Geological Characteristics and Ore-controlling Factors of Longhuo Gold Deposit in Guangxi [J].Land and Resources of Southern China,2013(7):30-33.
[40] 唐松华,何小强.广西隆或金矿成矿作用与火山活动关系探讨[J].南方国土资源,2006(11):31-33.
TANG Song-hua,HE Xiao-qiang.Discussion on the Relationship Between Mineralization and Volcanic Activity of Longhuo Gold Deposit in Guangxi [J].Guangxi Land and Resources of Southern China,2006(11):31-33.
[41] 张振贤,吴均贵,曾广海.广西隆林县隆或金矿的地质特征和成因分析[J].广西地质,1996(4):15-25.
ZHANG Zhen-xian,WU Jun-gui,ZENG Guang-hai.Geological Characteristics and Genesis Analysis of Gold Deposit at Longhuo in Guangxi[J].Guangxi Geo-logy,1996(4):15-25.
[42] 罗寿文,陈开礼,黄 巧.广西隆林卡林型金矿地质特征及成因探讨[J].地质科技情报,2010,29(4):100-105.
LUO Shou-wen,CHEN Kai-li,HUANG Qiao.Metallogenetic Characteristics and Genesis of Carlin-type Gold Deposits in Longlin Region,Guangxi[J].Geological Science and Technology Information,2010,29(4):100-105.
[43] 张洪瑞,杨天南,侯增谦,等.青海南部东莫扎抓矿区挤压断层带结构及其对铅锌成矿的控制[J].矿床地质,2015,34(2):261-272.
ZHANG Hong-rui,YANG Tian-nan,HOU Zeng-qian,et al.Internal Structure of Fault Zone and Its Control on Mineralization:A Case Study of Dongmozhazhua Pb-Zn Deposit,Southern Qinghai Province[J].Mineral Deposits,2015,34(2):261-272.
[44] 杨成富,刘建中,顾雪祥,等.南盘江—右江盆地构造演化与金锑成矿作用[J].地球学报,2020,41(2):280-292.
YANG Cheng-fu,LIU Jian-zhong,GU Xue-xiang,et al.The Relationship of Tectonic Evolution and Au-Sb Mineralization in Nanpanjiang-Youjiang Basin[J].Acta Geoscientica Sinica,2020,41(2):280-292.
[45] 刘建中,夏 勇,张兴春,等.层控卡林型金矿床矿床模型:贵州水银洞超大型金矿[J].黄金科学技术,2008,16(3):1-5.
LIU Jian-zhong,XIA Yong,ZHANG Xing-chun,et al.Model of Strata Karlin-type Gold Deposit:The Shui-yindong Super-scale Gold Deposit[J].Gold Science and Technology,2008,16(3):1-5.
[46] 黄启勋.广西隐伏花岗岩及其找矿意义[J].物探与化探,1994,18(1):61-70.
HUANG Qi-xun.Concealed Granite Bodies in Guang-xi and Their Ore-prospecting Significance[J].Geophysical and Geochemical Exploration,1994,18(1):61-70.
[47] 广西壮族自治区地球物理探矿队.1:200 000西林幅金锑砷组合异常图[R].柳州:广西壮族自治区地球物理探矿队,1989.
Geophysical Prospecting Team of Guangxi Zhuang Autonomous Region.1:200 000 Xilin Au-Sb-As Assemblage Anomaly Map[R].Liuzhou:Geophysical Prospecting Team of Guangxi Zhuang Autonomous Region,1989.

相似文献/References:

[1]王义天,李霞,王瑞廷,等.陕西凤太矿集区丝毛岭金矿床成矿时代的Ar-Ar年龄证据[J].地球科学与环境学报,2014,36(03):61.
　WANG Yi-tian,LI Xia,WANG Rui-ting,et al.Evidence of Ar-Ar Age for the Metallogenic Epoch of Simaoling Gold Deposit in Fengxian-Taibai Ore Cluster of Shaanxi[J].Journal of Earth Sciences and Environment,2014,36(01):61.
[2]张婷,彭建堂.湘西合仁坪钠长石石英脉型金矿床围岩蚀变及质量平衡[J].地球科学与环境学报,2014,36(04):32.
　ZHANG Ting,PENG Jian-tang.Wall-rock Alteration and Mass Balance of Herenping Albite-quartz Vein-type Gold Deposit in the Western Hunan[J].Journal of Earth Sciences and Environment,2014,36(01):32.
[3]宋慈安,宋玮,丁汝福,等.甘肃北山地区460金矿床植物地球化学异常形成的地学机制[J].地球科学与环境学报,2016,38(06):766.
　SONG Ci-an,SONG Wei,DING Ru-fu,et al.Formation Geo-mechanism of Botanogeochemical Anomaly of 460 Au Deposit in Beishan Area of Gansu[J].Journal of Earth Sciences and Environment,2016,38(01):766.
[4]刘新会,刘爽,李渊,等.丁家山古楼山金矿床成矿流体储运规律[J].地球科学与环境学报,2006,28(01):24.
　LIU Xin-hui,LIU Shuang,LI Yuan,et al.Storage and Moving of Ore-forming Fluid of Dingjiashan-Gulushan Gold Deposit[J].Journal of Earth Sciences and Environment,2006,28(01):24.
[5]舒建生,杨兴科,王磊,等.新疆冰达坂阿拉沟成矿条件及有利区带[J].地球科学与环境学报,2006,28(04):15.
　SHU Jian-sheng,YANG Xing-ke,WANG Lei,et al.Metallogenetic Environment and Prospective Provinces of Bingdaban-Alagou Zone of Enrichment in Tianshan Mountains，Xingjiang[J].Journal of Earth Sciences and Environment,2006,28(01):15.
[6]隗合明,赵国斌,焦建刚.河南夏馆—二郎坪一带叠加 改造型金矿床地质特征及成矿模式[J].地球科学与环境学报,2005,27(01):39.
　WEI He-ming,ZHAO Guo-bin,JIAO Jian-gang.Geological features and metallogenic model of hydrothermal superimposion (regeneration) gold deposits from Xiaguan to Erlangping in Henan[J].Journal of Earth Sciences and Environment,2005,27(01):39.
[7]张高鑫,刘建朝,张海东*,等.陕西勉略宁地块车渡磁铁石英岩型金矿床多期成矿作用[J].地球科学与环境学报,2020,42(03):355.[doi:10.19814/j.jese.2020.03036]
　ZHANG Gao-xin,LIU Jian-chao,ZHANG Hai-dong*,et al.Multistage Mineralization of Chedu Magnetite Quartzite Gold Deposit in Mianluening Block of Shaanxi, China[J].Journal of Earth Sciences and Environment,2020,42(01):355.[doi:10.19814/j.jese.2020.03036]

备注/Memo

备注/Memo:

收稿日期:2022-06-09; 修回日期:2022-08-08投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(42072110); 广西找矿突破战略行动地质矿产勘查项目(桂国土资函[2018]377号)
作者简介:安 鹏(1997-),男,土家族,贵州铜仁人,理学硕士研究生,E-mail:ap483645400@163.com。
*通讯作者:陈懋弘(1971-),男,广西桂林人,研究员,理学博士,E-mail:mhchen666@163.com。

常用功能

更新日期/Last Update: 2023-01-30