Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling
Gespeichert in:
| Datum: | 2010 |
|---|---|
| Hauptverfasser: | , , , , |
| Format: | Artikel |
| Sprache: | English |
| Veröffentlicht: |
Інститут геофізики ім. С.I. Субботіна НАН України
2010
|
| Schriftenreihe: | Геофизический журнал |
| Online Zugang: | http://dspace.nbuv.gov.ua/handle/123456789/103084 |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| Назва журналу: | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| Zitieren: | Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling / V. Starostenko, P. Kuprienko, I. Makarenko, O. Legostaeva, A. Savchenko // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 170-173. — Бібліогр.: 6 назв. — англ. |
Institution
Digital Library of Periodicals of National Academy of Sciences of Ukraine| id |
irk-123456789-103084 |
|---|---|
| record_format |
dspace |
| spelling |
irk-123456789-1030842016-06-14T03:03:32Z Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling Starostenko, V. Kuprienko, P. Makarenko, I. Legostaeva, O. Savchenko, A. 2010 Article Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling / V. Starostenko, P. Kuprienko, I. Makarenko, O. Legostaeva, A. Savchenko // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 170-173. — Бібліогр.: 6 назв. — англ. 0203-3100 http://dspace.nbuv.gov.ua/handle/123456789/103084 en Геофизический журнал Інститут геофізики ім. С.I. Субботіна НАН України |
| institution |
Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| collection |
DSpace DC |
| language |
English |
| format |
Article |
| author |
Starostenko, V. Kuprienko, P. Makarenko, I. Legostaeva, O. Savchenko, A. |
| spellingShingle |
Starostenko, V. Kuprienko, P. Makarenko, I. Legostaeva, O. Savchenko, A. Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling Геофизический журнал |
| author_facet |
Starostenko, V. Kuprienko, P. Makarenko, I. Legostaeva, O. Savchenko, A. |
| author_sort |
Starostenko, V. |
| title |
Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling |
| title_short |
Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling |
| title_full |
Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling |
| title_fullStr |
Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling |
| title_full_unstemmed |
Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling |
| title_sort |
variations in the crustal types of the dnieper-donets basin and surrounding areas from 3d gravity modelling |
| publisher |
Інститут геофізики ім. С.I. Субботіна НАН України |
| publishDate |
2010 |
| url |
http://dspace.nbuv.gov.ua/handle/123456789/103084 |
| citation_txt |
Variations in the crustal types of the Dnieper-Donets Basin and surrounding areas from 3D gravity modelling / V. Starostenko, P. Kuprienko, I. Makarenko, O. Legostaeva, A. Savchenko // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 170-173. — Бібліогр.: 6 назв. — англ. |
| series |
Геофизический журнал |
| work_keys_str_mv |
AT starostenkov variationsinthecrustaltypesofthednieperdonetsbasinandsurroundingareasfrom3dgravitymodelling AT kuprienkop variationsinthecrustaltypesofthednieperdonetsbasinandsurroundingareasfrom3dgravitymodelling AT makarenkoi variationsinthecrustaltypesofthednieperdonetsbasinandsurroundingareasfrom3dgravitymodelling AT legostaevao variationsinthecrustaltypesofthednieperdonetsbasinandsurroundingareasfrom3dgravitymodelling AT savchenkoa variationsinthecrustaltypesofthednieperdonetsbasinandsurroundingareasfrom3dgravitymodelling |
| first_indexed |
2025-07-07T13:16:10Z |
| last_indexed |
2025-07-07T13:16:10Z |
| _version_ |
1836994183219380224 |
| fulltext |
�������
���
����� ����
�3* �������������
�� !"#
$
%&
'(
)�&
�*�*
Variations in the crustal types of the Dnieper-Donets Basin
and surrounding areas from 3D gravity modelling
V. Starostenko, P. Kuprienko, I. Makarenko, O. Legostaeva, A. Savchenko, 2010
Institute of Geophysics, National Academy of Sciences of Ukraine, Kiev, Ukraine
irinam@igph.kiev.ua
There are two reasons for constructing a new
three-dimensional density model of the Dnieper-
Donets Basin (DDB) and surrounding areas. 1) A
lack of reliable data on the structure of the deep
horizons in the sedimentary cover and crystalline
crust. 2) Recently fresh geological and geophysical
data have been obtained for the upper sedimentary
layers (up to depths of 5—6 km) from seismic data
(DSS and MCSP) along the DOBRE1 and DO-
BRE2 profiles [Grad et al., 2003, Maystrenko et
al., 2003].
In this study modern software has been applied
[Starostenko et al., 1997; 2004]. It has a principal
advantage over standard approaches because den-
sity maps of individual layers are automatically in-
put into a PC, enabling geological environments to
be approximated very accurately. A technique of con-
structing a 3D model and converting it into a sche-
matic map of layers types are described in detail
elsewhere [Kuprienko et al., 2007].
3D modelling has resulted in a new pattern of
the density for the whole crust of the DDB and sur-
rounding areas. It has been used to compile sche-
matic maps for a thickness of the "granitic, "diorit-
ic" and "basaltic" layers (the upper, middle and lo-
wer crust). Earlier based on the generalization of
relationships of velocity vs. depth and density vs.
velocity for different types of the crust, it has been
put forward a conditional subdivision of the whole
crust into three stages without sharp boundaries be-
tween them. They have been defined as the upper,
middle and lower crust. Due to traditions they have
been named as "granitic, "dioritic" and "basaltic" lay-
ers. Their parameters are as follows: 1) <2.75 gcm 3,
VP<6.30 kms 1; 2) =2.75 2.90 gcm 3, VP=6,30
6,80 kms 1; 3) >2.90 gcm 3, VP>6.80 kms 1 re-
spectively. Petrologically the first range of the pa-
rameters is a mixture of acid and intermediate rocks.
The second series is composed of a mixture of in-
termediate and basic rocks (granodiorites, diorites,
charnokites, many gneisses, shists, metabasic
rocks, and gabbroids). The third row consists of in-
trusive rocks of basic and ultrabasic composition
and metamorphic rocks (granulites, amphibolites)
[Lithospheric …, 1993].
A relationship of a thickness of each layer to a
total thickness of the crust demonstrates the con-
tribution of each layer into a total thickness of the
crust. The name of the crustal type corresponds to
prevailing portion of any layer.
The portion of "granitic" layer (Fig. 1, a) within
the DDB iz characterized by a ratio of 0—0.4. The
highest values correspond to the southern flank of
Poltavskii megabloc (0.4), the northern side and the
southern preflank zone of the Lokhvitskii and Pol-
tavskii megablocs, as well as most of the northern
flank, where the percent ratio is 0,3. The smallest
proportion of the layer belongs to the central zone
of megablocs (0.0—0.1). On the rest of the areas
layer portion is 0.0—0.2.
The portion of "dioritic" layer (Fig. 1, b) is the
largest in the south of the DDB, in south-east of the
northern flank, in the central zone and southern pre-
flank zone of the Chernigovskii, and Poltavskii and
Lokhvitskii megablocs (0.4—0.5). A small portion of
this layer occurres in the southeastern part of the
central zone of the Iziumskii megabloc and in the
north-western Donbass (0.0—0.1). The rest of the
area is characterized by the values of 0.2—0.3.
The maximum portion of the "basalt" layer (Fig. 1,
c) is associated with the north-western Chernigovskii
megablock and the north-western part of the central
zone in the Lokhvitskii megabloc, the south-eastern
Iziumskii megablock and the whole Donbass (0.5—
�������������
�� !"#
$
%&
'(
)�&
�*�* �3�
+,�
�-.�,/�0
��.
���
�1��,
��0.
0�
0���,�
���
�����
��
Fig. 1. Contribution of the "granitic" (a), "dioritic" (b) and "basaltic" (c) layers to a whole thicness of the crust in the Dnieper-
Donets Basin and Donbass: 1 — the boundary of the DDB; 2 — the boundary of the northern flank of the DDB; 3 — the
longitudinal division of the DDB (after Arsiriy et al., 1984) zones: A — northern flank, B — sothern flank, C — Central; 4 — the
transversal division of the DDB (after Dolenko and Varich, 1989) megablocks: Ch — Chernigovskii, L — Lokhitskii, P —
Poltavskii, Iz — Iziumskii, D — Donbass.
0.7). The smallest ratio of the layer (0.2) is related to
the southern preflank zone of the Poltavskii megabloc
and the northern edge of the Iziumskii megablock. In
the rest of area the ratio is 0.3—0.4.
�������
���
����� ����
�3� �������������
�� !"#
$
%&
'(
)�&
�*�*
Fig. 2. Schemetic map of prognostic composition of the Earth’s crust in the DDB and Donbass from 3D gravity modelling.
See Fig. 1 for conventions.
Based on this information, six types of the crust
are determined for the DDB and Donbass (Fig. 2).
The granitic-dioritic crustal type has the smal-
lest distribution which mainly occurs on the sou-
thern flank of VCM (the Svatovo-Troitskii, Rossos-
hanskyii blocks). Its small massif occurs on the
northern flank of the Ush (the southern flank of the
Poltavskii megablock).
The dioritic type of the crust is distributed in the
northwest and central parts of the southern slope of
VCM, in the southeast of the northern flank zone of
the Chernigovskii and Poltavaskii megablocs, in the
northern flank zone of the Lokhvitskii block, in al-
most whole southern flank zone, on the southern
edge, as well as in northern and southern Donbass.
Leykobazaltic type of the crust is characteristic
of the north-western Chernigovskii and Lokhvitskii
megablocs, north-western parts of the northern flank
zone in the Chernigovskii, Poltavskii, Iziumskii
megablocs, as well as the north-western portion of
the southern flank zone of the Iziumskii megabloc.
Dioritic-basaltic type dominates in the central
region of Poltavskii and the south-east of the cen-
tral zone of the Lokhvitskii megablocs.
Basaltic type of the crust is spread in the south-
east of the northern and southern flank zones of the
Iziumskii megabloc, the most part of Donbass, in
the central zone and in the north-western part of the
southern preflank in the Chernigovskii megabloc. An
isometric area is present in the southern part of the
central zone in the Iziumskii megabloc.
Basaltic-dioritic type of the crust occurs only in
the central zone of the Iziumskiy megabloc. Its pa-
rameters are intermediate between basaltic type,
which is distributed in the central part of the Don-
bass, and diorititic — basaltic, typical for the cen-
tral zone of DDB. A question arises whether the
belt of the basalt-diorite type of the crust is the
transitional zone between the DDB and Donbass?
We should like to give a positive answer to this ques-
tion.
In conclusion, the granitic-dioritic type of the crust
dominates in the flank zones while the basaltic and
basaltic-dioritic types are spread in the central belt
of the DDB and Donbass. It demonstrates the in-
crease in basicity of the rocks from the flanks to
the centre of the depression that proves an axial
compaction.
Grad Y., Gryn’ D., Guterch A., Janik T., Veller R.,
Lang R., Lyngsie S. B., Omelchenko V. D., Staros-
tenko V. I., Stephenson R. A., Stovba S. N., Thy-
bo H., Tolkunov A. DPBRE-fraction’99—velocity
model of the crust and upper mantle beneath the
Donbas Foldbelt (East Ukraine) // Tectonophysics.
— 2003. — 371, �51—4. — P. 81—110.
References
Maystrenko Y., Stovba S., Stephenson R., Bayer U.,
Menyoli E., Gajewski D., Huebscher C., Rabbel W.,
Saintot A., Starostenko V., Thybo H., Tolkunov A.
Crustal-scale pop-up structure in cratonic litho-
sphere: DOBRE deep seismic reflection study of
the Donbas fold belt, Ukraine // Geology. — 2003.
— 31, � 8. — P. 733—736.
�������������
�� !"#
$
%&
'(
)�&
�*�* �3)
+,�
�-.�,/�0
��.
���
�1��,
��0.
0�
0���,�
���
�����
��
Starostenko V. I., Legostaeva O. V., Makarenko I. B.,
Pavlyuk E. V., Sharypanov V. M. On automated com-
putering geologic-geophysical maps images with
the first type ruptures and interactive regime visu-
alization of three-dimensional geophysical models
and their fields // Geophys. J. — 2004. — 26, �51.
— P. 3—13 (in Russian).
Starostenko V. I., Matsello V. V., Aksak I. N., Ku-
lesh V. A., Legostaeva O. V., Yegorova T. P. Automa-
tion of the computer input of images of geophysi-
cal maps and their digital modeling // Geophys. J.
— 1997. — 19, �51. — P. 3—13 (in Russian).
Kuprienko P. Ya., Makarenko I. B., Starostenko V. I.,
Legostaeva O. V. 3-D density model of the Earth’s
crust and upper mantle of the Ukrainian Shield //
Geophys. J. — 2007. — 29, �55. — P. 3—27 (in
Russian).
Lithospheric of the Central and East Europe . Generali-
zation of the researches results / Ed. A. V. Chekunov.
— Kiev: Nauk. dumka, 1993. — 258 p��(in Russian).
|