连长云,章革,元春华.短波红外光谱矿物测量技术在普朗斑岩铜矿区热液蚀变矿物填图中的应用[J].矿床地质,2005,24(6):621-636. Lian C Y,Zhang G,Yuan C H.Application of SWIR reflectance spectroscopy to Pulang porphyry copper ore district,Yunnan province[J].Mineral Deposits,2005,24(6):621-636.
[2]
章革,连长云,元春华.PIMA在云南普朗斑岩铜矿矿物识别中的应用[J].地学前缘,2004,11(4):460. Zhang G,Lian C Y,Yuan C H.Application of PIMA to Pulang porphyry copper ore district,Yunnan province[J].Earth Science Frontiers,2004,11(4):460.
[3]
章革,连长云,王润生.便携式短波红外矿物分析仪(PIMA)在西藏墨竹工卡县驱龙铜矿区矿物填图中的应用[J].地质通报,2005,24(5):480-484. Zhang G,Lian C Y,Wang R S.Application of the portable infrared mineral analyser(PIMA)in mineral mapping in Qulong copper prospect,Mozhugongka county,Tibet[J].Geological Bulletin of China,2005,24(5):480-484.
[4]
连长云,章革,元春华.短波红外光谱矿物测量技术在热液蚀变矿物填图中的应用——以土屋斑岩铜矿床为例[J].中国地质,2005,32(3):483-493. Lian C Y,Zhang G,Yuan C H.Application of SWIR reflectance spectroscopy in mapping of hydrothermal alteration minerals:A case study of the Tuwu porphyry copper prospect,Xinjiang[J].Geology in China,2005,32(3):483-493.
[5]
张篷,武振凯.PIMA在斑岩型矿床蚀变带划分中的应用综述[J].吉林地质,2011,30(1):129-132. Zhang P,Wu Z K.Application of PIMA in alteration zone division of the porphyry deposit[J].Jilin Geology,2011,30(1):129-132.
[6]
张篷,许虹,孙雨沁.PIMA在金矿床热液蚀变矿物分带中的应用[J].中国矿业,2011(4):155-158. Zhang P,Xu H,Sun Y Q.The application of PIMA on hydrothermal alteration mineral zoning,gold deposit[J].China Mining Magazine,2011(4):155-158.
[7]
徐庆生,郭健,刘阳,等.近红外光谱矿物分析技术在帕南铜-钼-钨矿区蚀变矿物填图中的应用[J].地质与勘探,2011,47(1):107-112. Xu Q S,Guo J,Liu Y,et al.Application of short wave infrared spectrum mineral analyzer(BJKF-1)to alteration mineral mapping at Panan,Tibet[J].Geology and Exploration,2011,47(1):107-112.
[8]
曹烨,李胜荣,申俊峰,等.便携式短波红外光谱矿物测量仪(PIMA)在河南前河金矿热液蚀变研究中的应用[J].地质与勘探,2008,44(2):82-86. Cao Y,Li S R,Shen J F,et al.Application of portable infrared mineral analyzer(PIMA)in the Qianhe gold mine,Henan province[J].Geology and Prospecting,2008,44(2):82-86.
[9]
朱炳玉,马华东,Hewson R.便携式短波红外矿物分析仪(PIMA)在新疆金山金矿勘探中的实验研究[J].新疆有色金属,2010,33(S2):9-11. Zhu B Y,Ma H D,Hewson R.Application of portable infrared mineral analyzer(PIMA)in the Jinshan gold deposit,Xinjiang[J].Xinjiang Nonferrous Metals,2010,33(S2): 9-11.
[10]
赵利青,邓军,原海涛,等.台上金矿床蚀变带短波红外光谱研究[J].地质与勘探,2008,44(5):58-63. Zhao L Q,Deng J,Yuan H T,et al.Short wavelength infrared spectral analysis of alteration zone in the Taishang gold deposit[J].Geology and Prospecting,2008,44(5):58-63.
[11]
Sun Y Y,Philip K S,Yang K.Application of short-wave infrared spectroscopy to define alteration zones assocoated with the Elura Zinc-lead-silver deposit,NSW,Australia[J].Journal of Geochemical Exploration,2001,73(1):11-26.
[12]
Yang K,Browneb P R L,Huntington J F,et al.Characterising the hydrothermal alteration of the Broadlands-Ohaaki geothermal system,New Zealand,using short-wave infrared spectroscopy[J].Journal of Volcanology and Geothermal Research,2001,106(1-2):53-65.
[13]
Yang K,Huntington J F,Gemmell J B,et al.Variations in composition and abundance of white mica in the hydrothermal alteration system at Hellyer,Tasmania,as revealed by infrared reflectance spectroscopy[J].Journal of Geochemical Exploration,2011,108(2):143-156.
[14]
王艳丽,许虹,韩剑.PIMA在地质中的应用研究[J].地质找矿论丛,2009,24(1):77-82. Wang Y L,Xu H,Han J.Study on application of PIMA to geology[J].Contribution to Geology and Mineral Resources Research,2009,24(1):77-82.
[15]
Biel C,Subías I,Acevedo R D,et al.Mineralogical,IR-spectral and geochemical monitoring of hydrothermal alteration in a deformed and metamorphosed Jurassic VMS deposit at Arroyo Rojo,Tierra delFuego,Argentina[J].Journal of South American Earth Sciences,2012,35:62-73.
[16]
Yitagesu F A,Meer F,Werff H,et al.Spectral characteristics of clay minerals in the 2.5-14 μm wavelength region[J].Applied Clay Science,2011,53(4):581-591.
[17]
Madani A A.Spectral properties of carbonatized ultramafic mantle xenoliths and their host olivine basalts,Jabal Al Maqtal basin,south eastern desert,Egypt,Using ASD FieldSpec spectroradiometer[J].The Egyptian Journal of Remote Sensing and Space Sciences,2011,14(1):41-48.
[18]
李光明,李金祥,秦克章,等.西藏班公湖带多不杂超大型富金斑岩铜矿的高温高盐高氧化成矿流体:流体包裹体证据[J].岩石学报,2007,23(5):935-951. Li G M,Li J X,Qin K Z,et al.High temperature,salinity and strong oxidation ore-forming fluid at Duobuza gold-rich porphyry copper deposit in the Bangonghu tectonic belt,Tibet:Evidence from fluid inclusions[J].Acta Petrologica Sinica,2007,23(5):935-951.
[19]
李金祥,李光明,秦克章,等.班公湖带多不杂富金斑岩铜矿床斑岩—火山岩的地球化学特征与时代对成矿构造背景的制约[J].岩石学报,2008,24(3):531-542. Li J X,Li G M,Qin K Z,et al.Geochemistry of porphyries and volcanic rocks and ore-forming geochronology of Duobuza gold-rich porphyry copper deposit in Bangonghu belt,Tibet:Constraints on metaliogenic tectonic settings[J].Acta Petrologica Sinica,2008,24(3):531-542.
[20]
佘宏全,李进文,丰成友,等.西藏多不杂斑岩铜矿床高温高盐度流体包裹体及其成因意义[J].地质学报,2006,80(9):1434-1446. She H Q,Li J W,Feng C Y,et al.The high-temperature and hypersaline fluid inclusions and its implications to the metallogenesis in Duobuza porphyry copper deposit,Tibet[J].Acta Geologica Sinica,2006,80(9):1434-1446.
[21]
祝向平,陈华安,马东方,等.西藏多不杂斑岩铜金矿床地质与蚀变[J].地质与勘探,2012,48(2):199-206. Zhu X P,Chen H A,Ma D F,et al.Geology and alteration of the Duobuza porphyry copper-gold deposit in Tibet[J].Geology and Exploration,2012,48(2):199-206.
[22]
代晶晶,曲晓明,辛洪波.基于ASTER遥感数据的西藏多龙矿集区示矿信息的提取[J].地质通报,2010,29(5):752-759. Dai J J,Qu X M,Xin H B.The extraction of alteration mineral information using ASTER remote sensing data in Duolong area of Tibet[J].Geological Bulletin of China,2010,29(5):752-759.
[23]
胡紫豪,唐菊兴,张廷斌,等.西藏多不杂斑岩铜矿ASTER遥感蚀变异常特征[J].国土资源遥感,2012,24(1):150-154. Hu Z H,Tang J X,Zhang T B,et al.Characteristics of remote sensing alteration anomalies from ASTER in the Duobuza prophyry copper deposit[J].Remote Sensing for Land and Resources,2012,24(1):150-154.
[24]
西藏地质调查院.1:5万西藏自治区改则县多龙地区地质调查报告[R].拉萨:西藏地质调查院,2008. Institute of Geology Survey in Tibet.Reports on regional geological surveys at 1:50000 scale in Duolong area,Gaize country of Tibet[R].Lasa:Institute of Geology Survey in Tibet,2008.
