The fourth dimension

The fourth dimension-GeologyPage
Figure 2 from Francesco Casu1 and Andrea Manconi: (A) Optical image (source Google Earth) of the study area, the Afar rift zone, Ethiopia, with indication of the used ascending (ASC) and descending (DESC) Envisat advanced synthetic aperture radar (ASAR) frames (purple and blue shading, respectively). The areas where pixel offsets have been computed in the ASC and DESC orbits are indicated by the black and white rectangles, respectively. (B) Differential interferogram between 12 June 2006 and 23 September 2009 (ASC orbit, track 300) in radar coordinates, superimposed on a SAR amplitude image of the area. Large displacements caused the high fringe rate as well as the coherence loss in the near field.

Remote sensing techniques facilitate observations and monitoring of ground displacements. In particular, space-borne Differential Synthetic Aperture Radar Interferometry (DInSAR) allows accurate measurements of ground deformation by properly analyzing multi-temporal satellite acquisitions over the region of interest.

However, limitations of DInSAR may arise when large and/or rapid surface deformation occurs, including those caused by active rifting. Understanding the three-dimensional characteristics of the deformation field, as well as its temporal evolution, cannot be accomplished by DInSAR alone.

Accurate spatial and temporal dense information on the displacements is, however, crucial for the correct interpretation of complex geological phenomena. In this paper, Francesco Casu and Andrea Manconi propose an algorithm to retrieve the four-dimensional (i.e., along north, east, up, and time) surface deformation field over zones affected by active rifting.

In the Afar depression system, one of the locations worldwide where active rifting processes can be observed, Casu and Manconi retrieved information in areas where data was not previously recorded. Their method demonstrates its validity in complex situations such as rifting episodes, where the deformation associated to repeated intrusions, faulting, and lithospheric extension might overlap in space and time.

Reference:
Four-dimensional surface evolution of active rifting from spaceborne SAR data
Francesco Casu, 1 IREA (Istituto per il Rilevamento Elettromagnetico dell’Ambiente), National Research Council, Via Diocleziano 328, 80124 Napoli, Italy; and Andrea Manconi and Dept. of Earth Sciences, Swiss Federal Institute of Technology, 8902 Zurich, Switzerland. Themed issue: Anatomy of Rifting: Tectonics and Magmatism in Continental Rifts, Oceanic Spreading Centers, and Transforms.  DOI: 10.1130/GES01225.1

Note: The above post is reprinted from materials provided by Geological Society of America.

SHARE