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- W1991281736 abstract "Special processing of seismic migrated CDP time section of reference profile 2-DV-A Pevek –<br>settlement of Valunistoye has resulted in quantitative dynamic and geometrical characteristics of a<br>geological section: a seismoacoustic section, density and an average reflector dip, total energy, dispersion<br>and a coefficient of excess of reflectivity factors, and attenuation of local wavetrains. It is established that the<br>behavior of the Moho bottom is quite accurately observed on characteristic “reflectors density of a seismic<br>acoustic section”. The total energy section has appeared to be useful for identifying blocks of the earth’s<br>crust. The analysis of reflector dips on the 2-DV-A profile has shown that in its northwestern part (0–200<br>km) in the crystalline crust the inclination of reflections prevails obviously to the southeast. In the range of<br>200-205 km in the crystalline crust and lower in the mantle, the vertical column of reflections with the<br>northwestern inclination serving as a sharp boundary between large blocks (paleoterrains) of Chukchi<br>microcontinent has shown itself clearly. From 390 to 520 km the northwestern reflector inclinations are<br>dominant in the crystalline crust, which corresponds to the movement of microblocks of the Koryak<br>accretionary belts." @default.
- W1991281736 created "2016-06-24" @default.
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- W1991281736 date "2009-01-01" @default.
- W1991281736 modified "2023-09-24" @default.
- W1991281736 title "Применение динамических и геометрических атрибутов сейсмического разреза для создания модели глубинного строения земной коры Чаун-Чукотки" @default.
- W1991281736 doi "https://doi.org/10.3997/2214-4609.201405319" @default.
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