序言 世界研究机构实际上在所有科学研究领域内均大量地利用从美国宇航局实验地球资源卫星获得的照片(Freden和Mevcanti,1973;Freden等,1974)。所得的照片在地质学方面有各种不同用途,可是重点多半放在构造方面。根据这些研究,判读并确定了许多地壳变动带。但是,根据现代研究进一步表明,这些卫星照片在圈定现代活动带时 Preamble World research institutes actually make extensive use of photographs obtained from NASA’s Experimental Earth Resources satellite in all areas of scientific research (Freden and Mevcanti, 1973; Freden et al., 1974). The resulting photographs have various uses in geology, but the emphasis is mostly on the structure. Based on these studies, many crustal movement bands have been interpreted and identified. However, according to modern research, it has been further shown that when these satellite photos delineate modern activity bands