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基于资源一号02D卫星高光谱数据的甘肃头吊泉-南大滩地区蚀变矿物填图及金矿化带识别
引用本文:孙雨,刘家军,翟德高,柳振江,张方方,赵英俊,刘鹏飞,王子涛.基于资源一号02D卫星高光谱数据的甘肃头吊泉-南大滩地区蚀变矿物填图及金矿化带识别[J].地质与勘探,2022,58(2):399-409.
作者姓名:孙雨  刘家军  翟德高  柳振江  张方方  赵英俊  刘鹏飞  王子涛
作者单位:中国地质大学(北京)地球科学与资源学院,北京 100083;核工业北京地质研究院,北京 100029;遥感信息与图像分析技术国家级重点实验室,北京 100029,中国地质大学(北京)地球科学与资源学院,北京 100083;中国地质大学(北京)地质过程与矿产资源国家重点实验 室,北京 100083,核工业北京地质研究院,北京 100029;遥感信息与图像分析技术国家级重点实验室,北京 100029
基金项目:国家重点研发计划项目(编号:2017YFC0602100)、中国核工业地质局地勘费项目(编号: 2014170)联合资助
摘    要:高光谱遥感能够根据光谱指纹特征提取蚀变矿物,在地质领域应用成效十分显著。针对最新的资源一号02D卫星高光谱数据特点,首先进行了高光谱数据预处理,选取蚀变矿物光谱特征显著波段进行数据降维,并应用三次样条插值函数对短波红外数据进行光谱波段增值,将光谱采样间隔提高到了2 nm。在优选出矿物填图端元光谱后,应用改进的SAM填图算法提取头吊泉-南大滩地区的褐铁矿、绿泥石、方解石、白云石、短波云母、中短波云母、中长波云母共7种蚀变矿物,详细分析高光谱蚀变矿物的分布特征并开展蚀变矿物的野外地质验证。研究区蚀变矿物与地质体岩性关系密切,多集中在特定地质体的局部地段。方解石和白云石蚀变矿物的定向展布指示了碳酸盐类沉积/变质地层的走向。根据资源一号02D高光谱数据提取的褐铁矿和中短波云母的分布情况,在南大滩-西红滩地段新发现1条长约15 km的金矿化蚀变带,东部的西红滩地段经综合查证存在地表金矿化异常。资源一号02D高光谱数据可以提取褐铁矿等多种蚀变矿物,从而为矿产资源勘查和基础地质调查提供重要的遥感信息。

关 键 词:高光谱矿物填图  金矿化  热液蚀变矿物  资源一号02D卫星  头吊泉-南大滩地区  甘肃省
收稿时间:2021/11/4 0:00:00
修稿时间:2022/3/6 0:00:00

Alteration minerals mapping and identification of gold mineralization belt based on ZY1-02D hyperspectral data in Fangshankounanshan area, Gansu Province[
SUN Yu,LIU Jiajun,ZHAI Degao,LIU Zhenjiang,ZHANG Fangfang,ZHAO Yingjun,LIU Pengfei,WANG Zitao.Alteration minerals mapping and identification of gold mineralization belt based on ZY1-02D hyperspectral data in Fangshankounanshan area, Gansu Province[[J].Geology and Prospecting,2022,58(2):399-409.
Authors:SUN Yu  LIU Jiajun  ZHAI Degao  LIU Zhenjiang  ZHANG Fangfang  ZHAO Yingjun  LIU Pengfei  WANG Zitao
Institution:School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing; Beijing Research Institute of Uranium Geology, Beijing; National Key Laboratory of Remote Sensing Information and Image Analysis Technology, Beijing; State Key Laboratory of Geological Processes and Mineral Resources , China University of Geosciences, Beijing
Abstract:Hyperspectral remote sensing can extract alteration minerals according to spectral fingerprint characteristics, and has achieved the most remarkable effect in the geology field. According to the characteristics of the newest ZY-1 02D satellite hyperspectral data, the hyperspectral data were preprocessed firstly, and then bands with significant spectral characteristics of alteration minerals were selected for dimensionality reduction. The cubic spline interpolation function was applied to increase the spectral bands of the SWIR data, and the spectral sampling interval was increased to 2nm. After optimizing the endmember spectra for mineral mapping, seven alteration minerals including limonite, chlorite, calcite, dolomite, short wave sericite, medium-short wave sericite and medium-long wave sericite were extracted in Fangshankounanshan area by using the improved Sam mapping algorithm. The distribution characteristics of hyperspectral alteration minerals were analyzed in detail, and the field geological verification was also carried out. It was found that alteration minerals in the study area were closely related to the lithology, and the alteration minerals mostly concentrated in the local section of the specific geological body. The directional distribution of calcite and dolomite indicated the trend of carbonates sedimentary or metamorphic strata. According to the distribution of both limonite and medium-short wave sericite extracted from the ZY1-02D hyperspectral data, a new alteration belt of gold mineralization was found, which length was about 15km. In the east of the alteration belt, a surface gold mineralization anomaly in the Xihongtan section had been confirmed after the comprehensive investigation. ZY-1 02D hyperspectral data can extract limonite and other alteration minerals, and thus provide important remote sensing information for mineral resources exploration and basic geological survey.
Keywords:hyperspectral mineral mapping  gold mineralization  hydrothermal alteration mineral  ZY1-02D satellite  Fangshankounanshan area  Gansu Province
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