Study of changes in the lineament structure, caused by earthquakes in South America by applying the lineament analysis to the Aster (Terra) satellite data

Arellano-Baeza, A. A.; Zverev, A. T.; Malinnikov, V. A.

doi:10.1016/j.asr.2005.07.068

Cited by 28 publications

(15 citation statements)

References 22 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…Time series of alignment distributions on the Earth's surface are investigated before and after an earthquake. Significant changes in alignment distributions (density, direction) were recorded before an earthquake [15].…”

Section: Optical Sensorsmentioning

confidence: 99%

Satellite Remote Sensing in Seismology. A Review

Тронин

2009

Remote Sensing

110

View full text Add to dashboard Cite

A wide range of satellite methods is applied now in seismology. The first applications of satellite data for earthquake exploration were initiated in the '70s, when active faults were mapped on satellite images. It was a pure and simple extrapolation of airphoto geological interpretation methods into space. The modern embodiment of this method is alignment analysis. Time series of alignments on the Earth's surface are investigated before and after the earthquake. A further application of satellite data in seismology is related with geophysical methods. Electromagnetic methods have about the same long history of application for seismology. Stable statistical estimations of ionosphere-lithosphere relation were obtained based on satellite ionozonds. The most successful current project "DEMETER" shows impressive results. Satellite thermal infra-red data were applied for earthquake research in the next step. Numerous results have confirmed previous observations of thermal anomalies on the Earth's surface prior to earthquakes. A modern trend is the application of the outgoing long-wave radiation for earthquake research. In '80s a new technology-satellite radar interferometry-opened a new page. Spectacular pictures of co-seismic deformations were presented. Current researches are moving in the direction of pre-earthquake deformation detection. GPS technology is also widely used in seismology both for ionosphere sounding and for ground movement detection. Satellite gravimetry has demonstrated its first very impressive results on the example of the catastrophic Indonesian earthquake in 2004. Relatively new applications of remote sensing for seismology as atmospheric sounding, gas observations, and cloud analysis are considered as possible candidates for applications.

show abstract

Section: Optical Sensorsmentioning

confidence: 99%

Satellite Remote Sensing in Seismology. A Review

Тронин

2009

Remote Sensing

110

View full text Add to dashboard Cite

show abstract

“…However, only a few studies have been made to establish a relationship between the appearance and migration of hypocenters and the volcanic processes of intrusions. In particular Gambino et al, (2004) analyzed the location of microseismicity preceding the 2002-2003 Mt. Etna eruption.…”

Section: Introductionmentioning

confidence: 99%

“…Recently Chastin and Main (2003) have tested the Voigts hypothesis using the seismic data from volcano Kilauea, Hawaii. They have found that acceleration of earthquake rates is not observed systematically before all individual eruptions.…”

Section: Introductionmentioning

confidence: 99%

Use of the ASTER satellite images for evaluation of structural changes in the Popocatépetl volcano related to microseismicity

Arellano-Baeza

Garcia

Trejo-Soto

et al. 2009

Advances in Space Research

Self Cite

View full text Add to dashboard Cite

“…New technologies make it possible not only to track the date of lineaments formation, and, hence, geophysical fields in geological time scales (Loiane et al,2014), but, also to track changes in the structure of lineaments due to the influence of strong earthquakes (Arellano-Baeza et al, 2006). north-eastern and north-west spread (Stativa et al, 2006 B).…”

Section: Introductionmentioning

confidence: 99%

“…Start of theoretical studies of the lineament structures and large-scale irregularities of the earth's crust has been given in works (Hobbs, 1904;Hubbert, 1937), which are being successfully developed at present with the use of new technologies for analyzing digital models, such as geophysical fields and landforms (Anokhin, Odessa, 2001;Arellano-Baeza et al, 2006;Anokhin, Maslow, 2009;Gilmanova et al, 2012;Loiane et al, 2014). New technologies make it possible not only to track the date of lineaments formation, and, hence, geophysical fields in geological time scales (Loiane et al,2014), but, also to track changes in the structure of lineaments due to the influence of strong earthquakes (Arellano-Baeza et al, 2006).…”

Section: Introductionmentioning

confidence: 99%

Systems of Lineaments of Magnetic and Gravity Anomalies in the Zone of Convergent Interaction of the Amur and the Eurasian Tectonic Plates

Trofimenko¹,

Grib²,

Mel'nikov³

et al. 2015

MAS

View full text Add to dashboard Cite

We studied the spatial distribution of anomalies of the gravitational and the magnetic fields at the border between the Amur and the Eurasian plates. Methods of statistical analysis showed that the systems of anomalies of geophysical fields fit into the regular spatial structures and are controlled by lineaments of latitude, longitude and diagonal stretch, as well as zones of plastic-elastic flow of rocks (shear-zone). These facts allowed us to establish time of formation of the orthogonal system of geophysical fields anomalies in the strike azimuths (84-354 0 ). As a result of comparing diagonal system of geophysical fields anomalies with spatial distribution of the fields of contemporary seismicity and epicenters of strong earthquakes, an assumption was made that the diagonal system of lineaments fit into zones of tectonic deformation and has been controlling the epicentral fields of contemporary seismicity since the Mesozoic period of seismotectonic activation. The main result of this study is the synthesis of early scientific works and getting new ideas about the spatial distribution of anomalies of geophysical fields. Establishing the sequence of forming isolated systems of anomalies and relationships between geophysical fields and seismicity is the subject of further research.

show abstract

Study of changes in the lineament structure, caused by earthquakes in South America by applying the lineament analysis to the Aster (Terra) satellite data

Cited by 28 publications

References 22 publications

Satellite Remote Sensing in Seismology. A Review

Satellite Remote Sensing in Seismology. A Review

Use of the ASTER satellite images for evaluation of structural changes in the Popocatépetl volcano related to microseismicity

Systems of Lineaments of Magnetic and Gravity Anomalies in the Zone of Convergent Interaction of the Amur and the Eurasian Tectonic Plates

Contact Info

Product

Resources

About