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国土资源遥感  2017, Vol. 29 Issue (1): 199-207    DOI: 10.6046/gtzyyg.2017.01.30
  技术应用 本期目录 | 过刊浏览 | 高级检索 |
北巴颜喀拉山地区岩性遥感解译标志建立
张志军1, 潘思远1, 李明1, 王雁鹤1, 徐延峰2
1. 武警黄金第六支队, 西宁 810000;
2. 北京信威通信技术股份有限公司, 北京 100193
Establishment of lithological remote sensing interpretation keys in north Bayan Hara mountain
ZHANG Zhijun1, PAN Siyuan1, LI Ming1, WANG Yanhe1, XU Yanfeng2
1. No. 6 Glod Geological Party of CAPF, Xining 810000, China;
2. Beijing Xinwei Telecom Technology Co., Ltd, Beijing 100193, China
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摘要 

岩性解译是遥感地质解译中十分重要的内容,解译前首先要根据待解译区地质体的岩性及其组合类型建立遥感解译标志。北巴颜喀拉山群复理石建造因岩性单一、地层厚度巨大、难见顶底且化石稀少,长期以来对该套地层的划分相对困难且争议颇多,形成了众多划分方案。针对这种情况,采用遥感方法,以SPOT5和ETM卫星遥感数据为基础影像,从岩性解译入手进行了最大程度的地质信息挖掘。从4个方面详细阐述了岩性解译和岩性组合划分的依据,系统地介绍了研究区基于遥感影像的岩性可视化解译标志的建立过程。并利用所建立的解译标志重新厘定了地层的影像特征,细分了各地层岩段或岩性组合,取得了对研究区地层岩性的新认识,为北巴颜喀拉山群地层对比及区域地质调查提供了新资料。

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李晓民
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张兴
庄永成
关键词 资源一号02C卫星(ZY-1 02C)水文地质找水线索遥感解译    
Abstract

Lithological interpretation is a very important part in remote sensing geological interpretation. First, interpretation keys must be established according to the lithology and its combination types of the geological body in the area to be interpreted. The stratigraphic division in Bayan Hara Mountain Group is relatively difficult and controversial, resulting in the existence of a large number of division schemes. That is because of single lithology, multilayer formation thickness, single top-bottom and rare fossils of flysch formation in Bayan Har Mountains Group. Aimed at tackling this situation, using remote sensing method, and starting with the lithological interpretation based on the SPOT5 and ETM data, the authors obtained information to the greatest degree. The lithologic interpretation and classification was based on detailed elaboration from four aspects in this study. A systematical description was made on the process of establishment of interpretation keys based on visual image. And then the stratigraphic image was redelimited through the established interpretation keys. The rock section and lithological association were subdivided for each stratum. Some new understanding of formation lithology was obtained in the study area. This would provide new data for stratigraphic correlation as well as regional geological survey in Bayan Har mountains.

Key wordsZY-1 02C satellite (ZY-1 02C)    hydrogeology    clue to water prospecting    remote sensing interpretation
收稿日期: 2015-09-17      出版日期: 2017-01-23
:  TP79  
基金资助:

中国地质调查局地质调查项目“西昆仑与青东基础地质调查”(编号:12120114009001)资助。

作者简介: 张志军(1986-),男,硕士,工程师,主要从事遥感地质方面的研究。Email:zhangzhijun-0001@163.com。
引用本文:   
张志军, 潘思远, 李明, 王雁鹤, 徐延峰. 北巴颜喀拉山地区岩性遥感解译标志建立[J]. 国土资源遥感, 2017, 29(1): 199-207.
ZHANG Zhijun, PAN Siyuan, LI Ming, WANG Yanhe, XU Yanfeng. Establishment of lithological remote sensing interpretation keys in north Bayan Hara mountain. REMOTE SENSING FOR LAND & RESOURCES, 2017, 29(1): 199-207.
链接本文:  
https://www.gtzyyg.com/CN/10.6046/gtzyyg.2017.01.30      或      https://www.gtzyyg.com/CN/Y2017/V29/I1/199

[1] 赵英时.遥感应用分析原理与方法[M].北京:科学出版社,2003:1-502. Zhao Y S.Analysis Principle and Method of Remote Sensing Application[M].Beijing:Science Press,2003:1-502.
[2] 江涛.遥感影像解译标志库的建立和应用[J].地理空间信息,2010,8(5):31-33. Jiang T.Construction and application of the visual interpretation bank of remote sensing images[J].Geospatial Information,2010,8(5):31-33.
[3] 濮静娟.遥感图像目视解译原理与方法[M].北京:中国科学技术出版社,1992:1-226. Pu J J.Principle and Method of Visual Interpretation Based on Remote Sensing Image[M].Beijing:China Science and Technology Press,1992:1-226.
[4] 刘刚,于学政.浅谈遥感技术在1:5万区调中的应用[J].国土资源遥感,1997,9(1):14-19.doi:10.6046/gtzyyg.1997.01.03. Liu G,Yu X Z.The method of 1:50000 geological mapping using remote sensing technology[J].Remote Sensing for Land and Resources,1997,9(1):14-19.doi:10.6046/gtzyyg.1997.01.03.
[5] 赵福岳,方洪宾,张瑞江.遥感在1:25万区域地质编(填)图工作中的应用效果和作用[J].国土资源遥感,1997,9(3):15-18,33.doi:10.6046/gtzyyg.1997.03.03. Zhao F Y,Fang H B,Zhang R J.The application of remote sensing technique to 1:250000 regional geological mapping[J].Remote Sensing for Land and Resources,1997,9(3):15-18,33.doi:10.6046/gtzyyg.1997.03.03.
[6] 宋晚郊,张绪教,高万里,等.东昆仑造山带巴颜喀拉山群ASTER岩性信息提取[J].现代地质,2013,27(1):116-123. Song W J,Zhang X J,Gao W L,et al.Extraction of lithological information from Bayan Har Mountain Group of East Kunlun Orogenic Belt using ASTER image[J].Geoscience,2013,27(1):116-123.
[7] 张焜,李宗仁,马世斌.基于ZY-102C星数据的遥感地质解译——以塔吉克斯坦帕米尔地区为例[J].国土资源遥感,2015,27(3):144-153.doi:10.6046/gtzyyg.2015.03.23. Zhang K,Li Z R,Ma S B.Remote sensing geological interpretation based on ZY-102C satellite images:A case study of Pamir area,Tajikistan[J].Remote Sensing for Land and Resources,2015,27(3):144-153.doi:10.6046/gtzyyg.2015.03.23.
[8] 董丽娜,张微,王雪,等.江西盛源火山盆地遥感地质解译与铀矿找矿前景分析[J].国土资源遥感,2015,27(4):102-108.doi:10.6046/gtzyyg.2015.04.16. Dong L N,Zhang W,Wang X,et al.Remote sensing geological interpretation and uranium prospecting perspective analysis of Shengyuan volcanic basin in Jiangxi Province[J].Remote Sensing for Land and Resources,2015,27(4):102-108.doi:10.6046/gtzyyg.2015.04.16.
[9] 王锋德,赵志芳,毛雨景,等.云南绿春地区遥感地质特征与找矿远景综合分析[J].国土资源遥感,2012,24(2):98-104.doi:10.6046/gtzyyg.2012.02.18. Wang F D,Zhao Z F,Mao Y J,et al.A comprehensive analysis of remote sensing geological characteristics and ore prospecting perspective of Luchun area,Yunnan Province[J].Remote Sensing for Land and Resources,2012,24(2):98-104.doi:10.6046/gtzyyg.2012.02.18.
[10] 张雪亭.青海省大地构造格架研究[D].北京:中国地质大学(北京),2006:1-114. Zhang X T.Study on the Tectonic Framework of Qinghai[D].Beijing:China University of Geosciences(Beijing),2006:1-114.
[11] 崔军文,张晓卫,唐哲民.青藏高原的构造分区及其边界的变形构造特征[J].中国地质,2006,33(2):256-267. Cui J W,Zhang X W,Tang Z M. Tectonic divisions of the Qinghai-Tibet Plateau and structural characteristics of deformation on their boundaries[J].Geology in China,2006,33(2):256-267.
[12] 张以茀.可可西里-巴颜喀拉三叠纪沉积盆地的划分及演化[J].青海地质,1996(1):1-17. Zhang Y F.Division and evolution of the Hoh Xil-Bayan Har sedimentary basin[J].Qinghai Geology,1996(1):1-17.
[13] 潘桂棠,丁俊,姚东生,等.青藏高原及邻区地质图(1:1500000)说明书[M].成都:成都地图出版社,2004:1-133. Pan G T,Ding J,Yao D S,et al.Geological Map of the Qinghai-Xizang(Tibet) Plateau and Adjacent Areas(1:1500000)[M].Chengdu:Chengdu Cartographic Publishing House,2004:1-133.
[14] 朱迎堂.可可西里-巴颜喀拉三叠纪沉积盆地的形成及演化[D].成都:成都理工大学,2006:1-166. Zhu Y T.The Formation and Evolution of the Hoh Xil Bayan Har-Triassic Sedimentary Basin[D].Chengdu:Chengdu University of Technology,2006:1-166.
[15] 张以茀.对巴颜喀拉区三叠纪地层系统的认识[J].中国区域地质,1995(1):21-31. Zhang Y F.Some opinions about the Triassic stratigraphy in the Bayan Hara area[J].Regional Geology of China,1995(1):21-31.
[16] 张雪亭,杨生德.青海省板块构造研究——1:100万青海省大地构造图说明书[M].北京:地质出版社,2007:1-213. Zhang X T,Yang S D.Study on Plate Tectonics in Qinghai Province:The Structure of the Land in Qinghai Province(1:1000000)[M].Beijing:Geological Publishing House,2007:1-213.
[17] 青海省地质矿产局.青海省岩石地层[M].武汉:中国地质大学出版社,1997:1-340. Qinghai Bureau of Geology and Mineral Resources. Stratigraphy(Lithostratic) of Qinghai Province[M].Wuhan:China University of Geosciences Press,1997:1-340.
[18] 陈守建,李荣社,计文化,等.巴颜喀拉构造带二叠-三叠纪岩相特征及构造演化[J].地球科学-中国地质大学学报,2011,36(3):393-408. Chen S J,Li R S,Ji W H,et al.Lithostratigraphy character and tectonic-evolvement of Permian-Trias in the Bayankala Tectonic Belt[J].Earth Science-Journal of China University of Geosciences,2011,36(3):393-408.
[19] 杨欣德,鄢犀利.青海达日-久治地区巴颜喀拉盆地研究进展[J].地质力学学报,2011,17(1):79-90. Yang X D,Yan X L.New results and major progresses in regional survey of the Darlag-Jigzhi Sheets[J].Journal of Geomechanics,2011,17(1):79-90.
[20] 蔡雄飞,陈斌,刘德民,等.青海境内三叠系上巴颜喀拉山亚群中部遗迹化石的发现及几点思考[J].地层学杂志,2006,30(3):263-268. Cai X F,Chen B,Liu D M,et al.Discovery of the Triassic ichnofossils in middle part of the Upper Bayanharashan Subgroup in Qinghai and its implications[J].Journal of Stratigraphy,2006,30(3):263-268.
[21] 沙淑清,王宗秀,郭通珍,等.巴颜喀拉山东段花岗岩锆石SHRIMP定年及其地球化学特征[J].地球学报,2007,28(3):261-269. Sha S Q,Wang Z X,Guo T Z,et al.Zircon SHRIMP dating and geochemical characteristics of granites in the eastern part of the Bayan Har mountains[J].Acta Geoscientica Sinica,2007,28(3):261-269.
[22] 朱亮璞,龙云林,徐茂松.用SAR与TM数字复合图像编制1:5万~1:10万解译地质图的优点及精度分析[J].国土资源遥感,1991,3(2):48-52.doi:10.6046/gtzyyg.1991.02.08. Zhu L P,Long Y L,Xu M S.Digital SAR-TM combination image for 1:50,000-1:100,000 interpretation geologic mapping[J].Remote Sensing for Land and Resources,1991,3(2):48-52.doi:10.6046/gtzyyg.1991.02.08.
[23] 钱程,韩建恩,朱大岗,等.基于ASTER-GDEM数据的黄河源地区构造地貌分析[J].中国地质,2012,39(5):1247-1260. Qian C,Han J E,Zhu D G,et al.An analysis of geomorphologic characteristics of the Yellow River source region based on ASTER-GDEM[J].Geology in China,2012,39(5):1247-1260.

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