Figure 5* Anninghe fault zone on the Landsat image. 
CONCLUSIONS 
Lineaments are well displayed on Landsat imagery. 
Considerable differences occur between lineament 
rose diagrams from Landsat and the geological map. 
The peak directions are present although they show 
differences in their distribution. Using Landsat 
image as complementary to existing data, a general 
limeament analysis can be made. Geological features 
such as faults/fractures are visible as full linea 
ments on the Landsat images. Several major linea 
ments systems are identified. To derive to a well- 
founded analysis, however, a very good knowledge 
of the geological structure of the area is required. 
ACKNOWLEDGEMENTS 
First and formost, to Dr. Bas N Koopmans for help 
with correction of the test; to N.H.W.Donker for 
digital processing of the lineaments; to some staffs 
of ITC for drawing of the figures and the typing. 
REFERENCES 
1. Cong Bailin, Zhao Dashang, Zhang Wenhua, Zhang 
Zhaozong and Yanmeie, 1973* Geol.Sec. IGA3, no.3 
(in Chinese), 
2. Yan Xianfu,1981»Geol,Journal, no.l(in Chinese), 
3. Huang Zuzhi, 1979» ¿compilation seismic geologi 
cal survey of the strongly seismic area in 
Sichuan-Yinnan region, p.144-161,(in Chinese) 
Seismic Press, Beijing, 
588 
Figure 6. Jinhe-Qinghe fault zone on Landsat image.