Abstract

Abstract Abstract. Some fractures in the crust are expressed at the surface as a field of point-like features that have developed in response to usually fluid processes within those fractures. We describe two complementary quantitative methods for analysing such point-like features from remotely-sensed imagery in terms of structural alignment. The two-point azimuth method is probabilistic and tests for the existence of regional and field-wide structural anisotropies. By contrast, the Hough transform method is deterministic and locates specific alignments. These methods have been applied to a Landsat Multispectral Scanner (MSS) image of the Pinacate Volcanic Field in north-west Mexico. The point-like features of interest are cinder cones and maars. The results reveal a northerly structural anisotropy and specific alignments, trending mainly northerly and north-northwesterly, have been mapped. This application was limited by the relatively coarse spatial resolution of the MSS image used. However, although o...

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.