Геоэлектрическая 2D модель вдоль профиля Сарата — Кельменцы
The geoelectrical cross section along the profile Sarata–Kelmensy was obtained for the first time by REBOOC and IGF Polish AS code. The conductive objects with resistivity less than 10 Ohm·m explaining the Carpathian anomaly of conductivity are sited under the Folded Carpathians in an interval of d...
Збережено в:
| Дата: | 2008 |
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| Автори: | , , |
| Формат: | Стаття |
| Мова: | Russian |
| Опубліковано: |
Видавничий дім "Академперіодика" НАН України
2008
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| Теми: | |
| Онлайн доступ: | http://dspace.nbuv.gov.ua/handle/123456789/4127 |
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| Назва журналу: | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| Цитувати: | Геоэлектрическая 2D модель вдоль профиля Сарата — Кельменцы / Б.Т. Ладанивский, И.М. Логвинов, В.Н. Тарасов // Доп. НАН України. — 2008. — № 1. — С. 101-105. — Бібліогр.: 13 назв. — рос. |
Репозитарії
Digital Library of Periodicals of National Academy of Sciences of Ukraine| Резюме: | The geoelectrical cross section along the profile Sarata–Kelmensy was obtained for the first time by REBOOC and IGF Polish AS code. The conductive objects with resistivity less
than 10 Ohm·m explaining the Carpathian anomaly of conductivity are sited under the Folded Carpathians in an interval of depths of 2–18 km. The integrated conductivity of those objects was estimated about (1.8–2.3) · 108S · m. |
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