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particular, the tail-like shapes of related geological and geophysical fields or
morphological anomalies (including the present-day topography), allows
discriminating impact structures from ring structures of magmatic origin, to a
large degree of confidence.
The use of gravity information is important for some seismological
objectives as well, specifically, for identifying seismic blocks, lineaments, and
other seismic-morphological structures revealed by means of GIS-ENDDB
visualization and mathematical tools during analysis of the spatial patterns of
seismicity.
An obvious advantage of the presented system consists in the possibility
for its continuous updating with the advance in methods and technologies.
The authors are grateful to I.I. Kalinnikov (Institute of Physics of the
Earth RAS, Moscow), K.K. Khazanovich-Wulff (Planetology Department of
the Russian Geographical Society, St Petersburg) for useful discussions and
ideas.
R EFERENCES
[1]
Mikheeva, A.V. (2013). The Complete Catalog of the Earth's Impact
Structures. labmpg.sscc.ru/impact/index1.html .
[2]
Mikheeva, A.V. On studying of natural disasters using the Earth's
remote sensing materials; Proc. Latin American Remote Sensing Week
(LARS 2013), October 23-25; Santiago de Chile, 2013.
[3]
Dyadkov, P.G.; Mikheeva, A.V. The EEDB - Expert Earthquake
Database for Seismic Geodynamic Research. Bull. Novosibirsk
Computing Center. Ser. Math. Model. in Geoph. 2010, vol. 13, pp. 15-
30.
[4]
Mikheeva, A.V.; Djadkov, P.G. Methods of complex analysis used for
learning the seismicity regularities and anomalies; Digital conference
proceedings: 25th International cartographic conference of the ICA
(Paris, 3-8 July 2011); Paris, 2011.
[5]
Mikheeva, A.V. Studying a spatial-temporal distribution of seismicity in
the area around Fukushima Prefecture by GIS-EEDB program tools.
Bull. Novosibirsk Computing Center. Ser. Numer. Anal. 2013, vol.16,
pp. 65-79.
[6]
Mikheeva, A.V. General laws of spatial-temporal distribution of the
Earth's impact structures. Bull. Novosibirsk Computing Center. Ser.
Math. Model. in Geoph. 2010, vol. 13, pp. 127-140.
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