浙西大明山区陆地卫星计算机兼容磁带数据的分类研究
文献类型:期刊论文
作者 | 程康 ; 张福祥 |
刊名 | 山地研究
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出版日期 | 1984 |
卷号 | 2期号:4页码:265-271 |
关键词 | 计算机兼容磁带 大明山 陆地卫星 研究区 象元 彩色分类 类目 花岗岩山地 光谱亮度分类研究 |
其他题名 | AN AUTOMATIC CLASSIFIED RESEARCH OF THE COMPUTER COMPATIBLE TAPE(CCT) DATA OF LANDSAT BY ISONMIX METHOD IN DAMING MOUNTAINS OF WEST ZHEJIANG |
通讯作者 | 程康 |
中文摘要 | 研究区位于浙江省临安县境内,属浙江西部大明山区。本区南部为北东东向的昱岭,出露震旦系角岩,海拔1200—1400米,构成昌化江水系与新安江水系的分水岭;中部为大明山主体,属花岗岩穹窿体,呈花岗岩山地;北部系白果—夏林昌化江谷地,由角岩和石灰岩构成,呈低山丘陵形态,海拔不足300米。 |
英文摘要 | ISONMIX DISTANCE METHOD is one of the non-supervised classification method, needing less computer time and having higher accuracy.Using the data of Hangzhou CCT (the Computer Compatible Tape) , which was scanned by Landsat-2 on November 27th, 1976, authors have gained a linear grey - degree map of Darning Mountains of the West Zhejiang with 32-levels, and calculated their statistical features of pixel spectral brightness of 4 MSS bands, resp. by a SIENMENS common computer.Then, some ISONMIX classified maps with a threshold value of 1.5 have been printed for the region. Having corrected an eight-sort digital classification map among them in geometry, we have charted a coloured classification map at a scale of 1:50000,On the coloured map, Daming Mountain region is divided into eight main surface features, i. e. tea-evergreen short shrub, evergreen broad leaf tree,deciduous broad leaf tree, shadow, cogongrass. coniferous tree (pine or fir), dry rice field and evergreen shrub forest.On the basis of, at last, the observation in situ and comprehensive analyses, authors have reinterpreted the gained classification map and obtained some important informations about geology and geomorphology in the region. |
语种 | 中文 |
公开日期 | 2014-08-07 |
源URL | [http://ir.imde.ac.cn/handle/131551/7083] ![]() |
专题 | 成都山地灾害与环境研究所_成都山地所知识仓储(2009年以前) |
推荐引用方式 GB/T 7714 | 程康,张福祥. 浙西大明山区陆地卫星计算机兼容磁带数据的分类研究[J]. 山地研究,1984,2(4):265-271. |
APA | 程康,&张福祥.(1984).浙西大明山区陆地卫星计算机兼容磁带数据的分类研究.山地研究,2(4),265-271. |
MLA | 程康,et al."浙西大明山区陆地卫星计算机兼容磁带数据的分类研究".山地研究 2.4(1984):265-271. |
入库方式: OAI收割
来源:成都山地灾害与环境研究所
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