Integration of remote sensing and geographic information systems for geological fault detection on the island of Crete, Greece

Mohamed Elhag,Dalal Alshamsi

doi:10.5194/gi-8-45-2019

Abstract

Abstract. Fracture systems are of great importance in the field of structural geology. Faults commonly afford easy passage to groundwater and fluids such as hydrothermal fluids and magmas or even contribute to earthquake hazard monitoring. For a geologist, it is not always easy to discern such morphotectonic structures at close range. Both remote sensing techniques and spatial modeling permit the recognition and better understanding of the brittle tectonics in an area. This study was an effort to delineate the tectonic structures on Crete by combining Sentinel-2 satellite data and spatial data. For the enhancement and better discrimination of photolineaments primarily recognized on satellite imagery, a variety of enhancement techniques has been applied. The evaluation of a photolineament as a potential fracture zone was based on several factors: the DEM of the study area, the shaded relief, the slopes and corresponding aspects, the drainage network, the geology and general observations on vegetative coverage appearance. The application of these methods revealed several fracture zones, which we recommend be certified by field investigations. Fault-mapping results may be used for a variety of geological and hydrogeological studies. Indicative places of a large concentration of groundwater are of vital importance for subsequent exploitation by areas of need. The present work may provide useful information for further analysis by geophysicists and seismologists.

Highlights

O’ Leary et al (1976) and Colwell (1983) gave an informative definition of the term lineament. It refers to a mappable, single or composite linear feature of a surface, whose parts are aligned in a rectilinear or slightly curvilinear relationship and which differs distinctly from the pattern of adjacent features and presumably reflects a subsurface phenomenon
An extensive literature review on the consideration of linear features and lineaments is well presented by Siegal and Gillespie (1980)
Faults indicate failure of the crust along a surface, accompanied by the relative movement of the geological units from both sides of that surface (Caumon et al, 2009). Such a zone of structural weakness is a major component in structural geology and may be related to a series of other phenomena

Summary

Introduction

O’ Leary et al (1976) and Colwell (1983) gave an informative definition of the term lineament It refers to a mappable, single or composite linear feature of a surface, whose parts are aligned in a rectilinear or slightly curvilinear relationship and which differs distinctly from the pattern of adjacent features and presumably reflects a subsurface phenomenon. Faults indicate failure of the crust along a surface, accompanied by the relative movement of the geological units from both sides of that surface (Caumon et al, 2009). Such a zone of structural weakness is a major component in structural geology and may be related to a series of other phenomena. Locating and identifying the movement is of dual importance to a geologist as the impacts of seismic hazards may endanger lives and involve economic losses (Colwell, 1983)

Methods

Results

Conclusion