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29.01.2008 .
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. : ( ), - - , . . – ( 1). (. 2).

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(DI) -1 – +1,75 . 87,7% 1 , 5% (-0,5) – (-1). 13% . 39,9% – 1,5. , (DI < 0,5) 20 [1,3].

DI . - . , , : , , , , , , , (. ), , , , 1 .

DI . – ( DI – 0,3-0,5) ( DI – 0,5-0,75). DI – +0,2-(-0,2), – +0.1-(-0.1).

, - , 0.75-1.25 , DI - – 0,2-0,4 [1].

6 - 7 ( -81, -97). 10 , M > 7 100, 200 . , , , Mmax – 6,5-7,5 35-50 [2].

- () , : - , [3].

- . (DI) -1 – +1,75 , DI - - 0,2 - 0,4 . 87.7% 1 , 12% [1,3].

- , . [3]:

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DI . – . , - , - [3].

- . , ( 1:25 000, 1:50 000) - , - - . , - [3,1,5,12].

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1. .. , - - . // ³ . .. . – : , 2001. – . 6. – . 9. - . - . 132-138.

2. .. - ` . // ³ . .. . – : , 2003. - . 8. - . 5. - . - . 171-179.

3. .. - . // ³ . .. . – : , 2004. - . 9. - . 4. - . - . 212-218.

4. .., .., .. - // . – : в, ­­– 2003, – 3, . 39-44.

5. .. - - // . .2. . – : . – 2004. –. 2. – .70-75.

6. . 1:200 000. . L-36-II () / .., ϳ .., Գ .., ϳ .., .., .., .., .., .. / – .: ̳ 㳿 , , , - в. – 2004. - 112 .

7. .., .. - // : . – : . – 1999. - .138-141.

8. .., .. // : . – : . – 1999. - .141-143.

9. .., .., .. ( - ) // - „ . . 㳿 ”. – : „...” - „” . – 2004. - . 61-64.

10. .. // . .. . : . .. , -: „”. – 1998. - . 1. - . – . 70-76.

11. .. - -200 / I- - - . – : . – 2001. – .134-135.

12. - / . . , . . , . . , . . / « / – » // : «». – 2003. – .78-80.

 

.. - . . – . – 04.00.07 ­– . . – , 2005.

- 1:25 000 – 1: 50 000 ( 156 2). , , - 1: 1 000 000 – 1: 2 500 000. 53 , , , , Mmax – 6,5-7,7, 1 35-50, 100 200 .

, (DI < 0,5) 20 . . 88% 1 , 12% .

- . .

: , - , , - .

.. - . . – . – 04.00.07. – . 쳿 . – , 2005.

. - 1:25 000 – 1:50 000 ( 156 2). ϳ , , ϳ- ' 1:1 000 000 – 1:2 500 000. 53 , , , , Mmax – 6,5 – 7,7 – 35-50, 100 200 .

, , , (DI < 0,5) 20 . . 88% 1 , 12% – .

- . .

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Fesenko A.V. Engineering-geologic bases for the purposes of an estimation of seismic danger of Odessa region. - the Manuscript. – The dissertation on competition of a scientific degree of the Candidate of geologic sciences on a speciality 04.00.07 - engineering geology. Institute of geological sciences of the National Academy of sciences of Ukraine. - Kiev, 2005.

On territory of Odessa region the analysis of engineering - geological conditions and an estimation of a degree of local seismic danger in scales 1:25 000 - 1 : 50 000 are conducted. On territory of East and Southern Carpathian mountains, Moldova, Northwest Black Sea Coast are conducted the analysis of regional seismic danger in scales 1 : 1 000 000 - 1 : 2 500 000. On this territory given 53 seismic zones, from them the most dangerous are zones Vrancha, Buzau, Ialomita, Satu Mare with Mmax 6.5 - 7.7 and average repeatability at 35-40, 100 and 200 years.

It is established, that favorable in the seismic relation (DI <0.5) are less than 20 percent of c. Odessa. On 88 % of territory of Odessa the total increment of seismic intensity exceeds 1 point by the international seismic scale MSK-64, and on 12 % of territory the seismic point can be lowered up.

Are created engineering - geological and geomorphological bases of territory of Odessa for the purposes of seismic microdivision into districts.

Key words: seismic danger, engineering - geological conditions, seismic microdivision into districts, engineering - geological division into districts.


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