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Conductivity of the Earth’s crust and upper mantle in Ukraine
| Content Provider | Semantic Scholar |
|---|---|
| Author | Kulik, Stanislav |
| Copyright Year | 2009 |
| Abstract | On the western slope of the Ukrainian Shield (USh) at the depth (H) from 3 to 6 km lies Volynian conductive anomaly (CA) with specific resistance () of the order of 10 Ohm•m. Chernovtsy-Korostenian CA on the USh territory, extending from the surface (the top of the conductor is at the depth of 50 m) to the depth of 1.5 km, manifests itself as two local sections with =10 Ohm•m. They are galvanically connected with submeridianal CA (H=3-15 km, =10 Ohm•m). Chernovtsy-Korostenian CA, outside of USh, was found on the southern part of Volyn-Podolian plate (VPP) (H=6-15 km, =10 Ohm•m). The anomaly gets deeper in the north (H=15-30km). Section of the anomaly with =5 Ohm•m is located within the borders of Rosinian and Podolian megablocks and contains an object with =1000 Ohm•m. Western part of CA (=20 Ohm•m) stretches out of the USh in two directions – south and southwest, along Podolian fracture zones till Golovanian seaming zone (SZ). In the northwestern part of USh, on the border of the Volynian and Rosinian blocks, in the Earth Crust (H=15-30 km) lies Korostenian CA (=30 Ohm•m). |
| File Format | PDF HTM / HTML |
| Alternate Webpage(s) | https://meetingorganizer.copernicus.org/EGU2009/EGU2009-12776.pdf |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |
