Share Email Print

Proceedings Paper

Method for interpreting stereo-simulated ERS and Landsat-TM data: geological application to the Velay area (France)
Author(s): Jean-Paul Deroin; Olivier Rouzeau
Format Member Price Non-Member Price
PDF $17.00 $21.00

Paper Abstract

The aim of this study is to present a method for improving the geological interpretation of remotely sensed data in areas which are never entirely free of cloud cover (temperate or tropical climatic zones). The method is based on the production of ortho-images and pseudo- stereoscopic pairs by means of a digital elevation model (DEM). The interpretation is done under a mirror-stereoscope on geometrically corrected images. The images could be interpreted in terms of geomorphology (volcanoes, drainage patterns, etc.), petrography (volcanic differentiates), and structure (faults, annular anomalies). By using stereoscopy it is possible, on a TM 4 5 2 color-composite to distinguish three-dimensional geological features using their spectral responses. These features are not clearly visible without stereoscopy. ERS 1 radar stereoscopy improves the hierarchization of the lineament pattern. The combination of backscattering and stereoscopic view emphasizes geological structures characterized essentially by their texture.

Paper Details

Date Published: 21 December 1994
PDF: 11 pages
Proc. SPIE 2318, Recent Advances in Remote Sensing and Hyperspectral Remote Sensing, (21 December 1994); doi: 10.1117/12.197226
Show Author Affiliations
Jean-Paul Deroin, Bureau de Recherches Geologiques et Minieres (France)
Olivier Rouzeau, Bureau de Recherches Geologiques et Minieres (France)

Published in SPIE Proceedings Vol. 2318:
Recent Advances in Remote Sensing and Hyperspectral Remote Sensing
Pat S. Chavez Jr.; Carlo M. Marino; Robert A. Schowengerdt, Editor(s)

© SPIE. Terms of Use
Back to Top
Sign in to read the full article
Create a free SPIE account to get access to
premium articles and original research
Forgot your username?