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基于ASTER数据的断裂构造判读:以甘肃白银地区为例

黄生海, 石火生   

  1. 南京大学 地球科学系, 南京 210093
  • 收稿日期:2005-12-20 修回日期:2005-12-20 出版日期:2005-12-20 发布日期:2005-12-20

Fault Analysis Based on ASTER Imaging Information: Introduced by an Application Test in Baiyin Area, Gansu Province

HUANG Sheng-hai, SHI Huo-sheng   

  1. Department of Earth Sciences, Nanjing University, Nanjing 210093, China
  • Received:2005-12-20 Revised:2005-12-20 Online:2005-12-20 Published:2005-12-20

摘要: ASTER传感器提供了包括可见光-近红外(VNIR)、短波红外(SWIR)、热红外(TIR)共14个波段的地物波谱数据。其中最高分辨率在VNIR波段达到了15m。另外,在获得地物波谱数据的同时,它还能利用在03N波段和03B波段以不同视角获得的图像组成立体像对,从而获得同一地区的高程数据。这些特点为该数据的地质应用提供了很大的方便。由于断裂构造能造成断裂带内及其两侧之间地质环境与地貌特征的差异,这种差异会造成相应地区遥感影像中地物的波谱特征及空间分布即纹理型式上的差别。反之,使用多种图像处理技术,通过增强图像的灰度差并获取纹理图像,可以使这种差异凸现出来分析图像中的这些差异,找出在灰度和纹理上的规律性变化,不但可以推断可能的断裂分布,并可确定它的性质.利用ASTER数据高空间分辨率、多波谱段及同时提供DEM数据的特点,将之用于甘肃白银地区断裂构造的识别和判读。试验表明,利用该数据判读的结果与实地调查结果有相当的一致性。

Abstract: ASTER sensor provides 14 bands of spectral information including visible and near infrared (VNIR), short wave infrared (SWIR) and thermal infrared (TIR) . The highest spatial resolution is 15 meters which lies in VNIR bands. Besides, the stereo imaging of the same area can be obtained simultaneously by the nadir- and aft-looking of 03 N and 03 B bands respectively. Topographic information can then be derived from them by certain algorithm. All these characteristics make it very convenient in geological application. The fault system may cause differences in geology and morphology inside and outside the system. Accordingly, these differences may produce different spectral and textural characteristics in the image. In the reverse, the characteristics can be emphasized by enhancing the difference of intensity and texture by using certain image processing technology. Analysis then can be done on their difference, some tally with certain laws can be regarded as fault system, and its attribute may be concluded. An application of ASTER data in Baiyin area of Gansu province was introduced in this paper. The results show a high consistency with the field survey as shown in the local geology map.