Geothermal data on bolgarii. The Mizijsky plate

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The Mizijsky plate has tested in the past geosinklinalnoe development and osadkonakoplenie. Its consolidation in paleozoe has not come to the end. Values of the calculated thermal stream on the Mizijsky plate (without northern part of the Bulgarian raising) do not fall outside the limits the normal. Similar results have been received for areas kaledonskih and gertsinskih folded systems.

Tectonic data prove to be true the temperature measurements executed on profile I-I of a northwest direction. Studying of character of isolines shows, that they are influenced by strongly pronounced angular disagreement between triasom and juroj. The Structurally-geological border in a sedimentary layer of a platform has been supported by thermometry data.