王成善,李亚林,刘志飞,等.雅鲁藏布江蛇绿岩再研究:从地质调查到矿物记录[J].地质学报,2005,79(3):323-330. Wang C S, Li Y L,Liu Z F,et al.Yarlung-Zangbo ophiolites revisited:From geological survey to mineral records[J].Acta Geologica Sinica,2005,79(3):323-330.
[2]
Clark R N.Spectroscopy of rocks and minerals and principles of spectroscopy[M]//Rencz A N.Manual of remote sensing,volume 3,remote sensing for the earth sciences.New York:John Wiley and Sons,1999:3-58.
[3]
Rowan L C,Mars J C.Lithologic mapping in the mountain pass,California area using advanced spaceborne thermal emission and reflection radiometer(ASTER)data[J].Remote Sensing of Environment,2003,84(3):350-366.
[4]
Hewson R D,Cudahy T J,Mizuhiko S,et al.Seam less geological map generation using ASTER in the BrokenHil-l Curnamona province of Australia[J].Remote Sensing of Environment,2005,99(1/2):159-172.
[5]
Tommaso I D,Rubinstein N.Hydrothermal alteration mapping using ASTER data in the Infiernillo porphyry deposit,Argentina[J].Ore Geol Rev,2007,32(1/2):275-290.
[6]
李智峰,朱谷昌,张建国,等.基于SPOT数据的铁化蚀变信息提取及找矿应用研究——以陇南金矿区为例[J].国土资源遥感,2011,23(2):91-97. Li Z F,Zhu G C, Zhang J G,et al.The extraction and analysis of iron alteration information based on SPOT data for mineral prediction:A case study of the Longnan gold ore district[J].Remote Sensing for Land and Resources,2011,23(2):91-97.
[7]
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 alternation anomalies from ASTER in the Duobuza porphyry copper deposit[J].Remote Sensing for Land and Resources,2012,24(1):150-154.
[8]
张志军,甘甫平,李贤庆,等.基于ASTER数据的蚀变矿物信息提取——以哈密黄山铜镍矿区为例[J].国土资源遥感,2012,24(2):85-91. Zhang Z J,Gan F P,Li X Q,et al.The extraction of altered mineral information based on ASTER data:A case study of the Huangshan copper-nickel ore district in Hami[J].Remote Sensing for Land and Resources,2012,24(2):85-91.
[9]
李培军,龙玄耀,刘立.基于ASTER数据的蛇绿岩组分识别——以德尔尼矿区为例[J].岩石学报,2007,23(5):1175-1180. Li P J,Long X Y,Liu L.Ophiolite mapping using ASTER data:A case study of Derni ophiolite complex[J].Acta Petrologica Sinica,2007,23(5):1175-1180.
[10]
黄照强,张显峰.基于ASTER的雅鲁藏布江缝合带泽当—罗布莎蛇绿岩套分析和组分识别[J].岩石学报,2010,26(12):3589-3596. Huang Z Q,Zhang X F.Lithological mapping of ophiolite composition in Zedan-Luobusha,Yarlung Zangbo suture zone using advanced spaceborne thermal emission and reflection radiometer(ASTER)data[J].Acta Petrologica Sinica,2010,26(12):3589-3596.
[11]
王国庆,夏斌.西藏罗布莎蛇绿岩及其构造意义[J].大地构造与成矿学,1987,11(4):349-362. Wang G Q,Xia B.The Luobusa ophiolite of Xizang Tibet and its tectonic significance[J].Geotectonica et Meallogenia,1987,11(4):349-362.
[12]
白文吉,方青松,张仲明,等.西藏雅鲁藏布江蛇绿岩带罗布莎地幔橄榄岩的成因[J].岩石矿物学杂志,1999,18(3):193-216. Bai W J,Fang Q S,Zhang Z M,et al.The genesis of Luobusa mantle peridotites in the Yarlung Zangbo river ophiolite zone,Tibet[J].Acta Petrologica et Mineralogica,1999,18(3):193-216.
[13]
王希斌,鲍佩声.豆荚状铬铁矿床的成因——以西藏自治区罗布莎铬铁矿床为例[J].地质学报,1987(2):166-181. Wang X B,Bao P S.The genesis of podiform chromite deposits:A case study of the Luobusha chromite deposit,Tibet[J].Acta Geologica Sinica,1987(2):166-181.
[14]
叶培盛,江万,吴珍汉,等.西藏泽当—罗布莎蛇绿岩的地球化学特征及其构造意义[J].现代地质,2006,20(3):370-377. Ye P S.Jiang W.Wu Z H.Geochemical characteristics of ophiolites in Zedang-Luobusha,Tibet and their tectonic significance[J].Geoscience,2006,20(3):370-377.
[15]
程学展,夏斌,李建峰,等.罗布莎蛇绿岩地幔橄榄岩同位素特征及其成因[J].大地构造与成矿学,2011,35(1):85-94. Cheng X Z,Xia B,Li J F,et al.Sr-Nd-Pb isotopic characteristics and origin of the mantle peridotites from the Luobusha ophiolite[J].Geotectonica et Metallogenia,2011,35(1):85-94.
[16]
Kruse F A,Lefkoff A B,Dietz J B.Expert system-based mineral mapping in northern Death Valley,California/Nevada using the airborne visible/infrared imaging spectrometer(AVIRIS)[J].Remote Sensing of Environment,1993,44(2/3),309-336.
