last update

07/10/2017

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SpyLOG

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Yakovlev Fedor L. (nglish vers.)

. .-.

(304)

. ..

: 8-499-254-99-50.

e-mail : yak@ifz.ru

 

 

:

 

:

Structural geology, tectonophysics, folds, folding, linear folding, mechanism of folding formation ,hinterland, balanced sections, shortening value, mechanisms of deforming, modeling, mountain building formation, mechanisms of mountain building formation, basin inversion, seismotectonics, seismic risk

Structural geology, tectonophysics, folds, folding, linear folding, mechanism of folding formation ,hinterland, balanced sections, shortening value, mechanisms of deforming, modeling, mountain building formation, mechanisms of mountain building formation, basin inversion, seismotectonics, seismic risk , , , , , , , , , , ,

 

(links)_

(..) ,

-08- -Rus

-09- -Rus

CV (engl.)


Under Construction

( 28 2015, )

Un. Const.
Un. Const.

TPH_2012 (tectonophysics, hold)

GEOMOD_2012 (modeling in tectonics, hold)

Youth TPH_2009 (tectonophysics, hold)

TPH_2008 (tectonophysics, hold)

 

- , , yak@ifz.ru (.)

( A D ):

A.

, - , , ,

  ()
(.., , 1978 2012 , )
: (I VII ):
, (HINTERLAND)
!
!.

; ;
(Folders 1-19)
:

I

1. Foreland vs. Hinterland ():

2. (7 ) (en)

3. (en)

II ()

4. ( 1) (en)

5. , (en)

6. ( 2) (en)

7. ( 2) (en)

III

8. ( 2, 3) (en)

9. ( 3) (en)

10. ( 2, 3)

image003

(Folders 7 and 10)


image004image005 image006

IV

11. ( 3, 4, 5) Und Con

12. ( 3, 5) Und Con

V ,

13. : ( 3, 5)

14. ( 3, 4, 5) Und Con

15. foreland-hinterland ( 3, 4, 5) Und Con

16. 3D ( 3, 4, 5, 6)

VI

17. -3D ( 4, 5, 6) Und Con

VII

18. ( 5, 6) Und Con

19. ,
, ( 5, 6) Und Con

  (
- : ) Und Con

( ,
. ). Und Con

  ( .
.) Und Con

 

 

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, ( 18)

B. Und Con

,

The approaches to study of two main types of mountain building processes and structures are described.
These types are: 1) post-platform mountains and 2) post-folded mountains.

C. Und Con

There are materials of three topics. The kind of regularity in seismic periodicity in North Caucasus is described.
There are results of geological observations in Racha earthquake (1991, Georgia) and Shikotan earthquake (1994, Kuril island, Russia).

D. Und Con

,

There is explanation of new approach in study of fracture formation (It was started in cooperation with the
deceased leader D.Osokina and now it is continuing with V.Voitenko). The complex tectonophysical description of single
fracture formation as joint of stress-field, strain-field, displacements and secondary fracturing is offering.

 

 

Russian and other Links: 

 

to first page *: yak@ifz.ru

 

2015, ,