EUROBRIDGE: New insight into the geodynamic evolution of the East European Craton

Svetlana Bogdanova; R. Gorbatschev; M. Grad; T. Janik; A. Guterch; Elena Kozlovskaya; G. Motuza; G. Skridlaite; V. Starostenko; L. Taran; V. N. Astapenko; A. A. Belinsky; R. G. Garetsky; G. I. Karatayev; V. V. Terletsky; G. Zlotski; S. L. Jensen; M. E. Knudsen; H. Thybo; R. Sand; K. Komminaho; U. Luosto; T. Tiira; J. Yliniemi; R. Giese; J. Makris; A. Čečys; J. Jacyna; L. Korabliova; V. Nasedkin; A. Rimsa; R. Sečkus; W. Czuba; E. Gaczyński; P. Środa; M. Wilde-Piórko; E. Bibikova; Stefan Claesson; S. A. Elming; C. E. Lund; J. Mansfeld; L. Page; K. Sundblad; J. J. Doody; H. Downes; V. B. Buryanov; T. P. Egorova; T. V. Il'chenko; O. M. Kharitonov; D. V. Lysynchuk; O. V. Legostayeva; I. B. Makarenko; V. D. Omel'chenko; M. I. Orlyuk; I. K. Pashkevich; V. M. Skobelev; L. M. Stepanyuk; G. R. Keller; K. C. Miller

doi:10.1144/GSL.MEM.2006.032.01.36

EUROBRIDGE: New insight into the geodynamic evolution of the East European Craton

Svetlana Bogdanova^*, R. Gorbatschev, M. Grad, T. Janik, A. Guterch, Elena Kozlovskaya, G. Motuza, G. Skridlaite, V. Starostenko, L. Taran, V. N. Astapenko, A. A. Belinsky, R. G. Garetsky, G. I. Karatayev, V. V. Terletsky, G. Zlotski, S. L. Jensen, M. E. Knudsen, H. Thybo, R. SandK. Komminaho, U. Luosto, T. Tiira, J. Yliniemi, R. Giese, J. Makris, A. Čečys, J. Jacyna, L. Korabliova, V. Nasedkin, A. Rimsa, R. Sečkus, W. Czuba, E. Gaczyński, P. Środa, M. Wilde-Piórko, E. Bibikova, Stefan Claesson, S. A. Elming, C. E. Lund, J. Mansfeld, L. Page, K. Sundblad, J. J. Doody, H. Downes, V. B. Buryanov, T. P. Egorova, T. V. Il'chenko, O. M. Kharitonov, D. V. Lysynchuk, O. V. Legostayeva, I. B. Makarenko, V. D. Omel'chenko, M. I. Orlyuk, I. K. Pashkevich, V. M. Skobelev, L. M. Stepanyuk, G. R. Keller, K. C. Miller

^*Corresponding author for this work

Eurasia Institute of Earth Sciences

Research output: Chapter in Book/Report/Conference proceeding › Chapter › peer-review

155 Citations (Scopus)

Abstract

The Palaeoproterozoic crust and upper mantle in the region between the Ukrainian and Baltic shields of the East European Craton were built up finally during collision of the previously independent Fennoscandian and Sarmatian crustal segments at c. 1.8-1.7 Ga. EUROBRIDGE seismic profiling and geophysical modelling across the southwestern part of the Craton suggest that the Central Belarus Suture Zone is the junction between the two colliding segments. This junction is marked by strong deformation of the crust and the presence of a metamorphic core complex. At 1.80-1.74 Ga, major late to post-collisional extension and magmatism affected the part of Sarmatia adjoining the Central Belarus Zone and generated a high-velocity layer at the base of the crust. Other sutures separating terranes of different ages are found within Sarmatia and in the Polish-Lithuanian part of Fennoscandia. While Fennoscandia and Sarmatia were still a long distance apart, orogeny was dominantly accretionary. The accreted Palaeoproterozoic terranes in the Baltic-Belarus region of Fennoscandia are all younger than 2.0 Ga (2.0-1.9, 1.90-1.85 and 1.84-1.82 Ga), whereas those in Sarmatia have ages of c. 2.2-2.1 and 2.0-1.95 Ga. Lithospheric deformation and magmatism at c. 1.50-1.45 Ga, and Devonian rifting, are also defined by the EUROBRIDGE seismic and gravity models.

Original language	English
Title of host publication	European Lithosphere Dynamics
Editors	D.G. Gee, R.A. Stephenson
Pages	599-625
Number of pages	27
DOIs	https://doi.org/10.1144/GSL.MEM.2006.032.01.36
Publication status	Published - 2006

Publication series

Name	Geological Society Memoir
Volume	32
ISSN (Print)	0435-4052

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10.1144/GSL.MEM.2006.032.01.36

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Bogdanova, S., Gorbatschev, R., Grad, M., Janik, T., Guterch, A., Kozlovskaya, E., Motuza, G., Skridlaite, G., Starostenko, V., Taran, L., Astapenko, V. N., Belinsky, A. A., Garetsky, R. G., Karatayev, G. I., Terletsky, V. V., Zlotski, G., Jensen, S. L., Knudsen, M. E., Thybo, H., ... Miller, K. C. (2006). EUROBRIDGE: New insight into the geodynamic evolution of the East European Craton. In D. G. Gee, & R. A. Stephenson (Eds.), European Lithosphere Dynamics (pp. 599-625). (Geological Society Memoir; Vol. 32). https://doi.org/10.1144/GSL.MEM.2006.032.01.36

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title = "EUROBRIDGE: New insight into the geodynamic evolution of the East European Craton",

abstract = "The Palaeoproterozoic crust and upper mantle in the region between the Ukrainian and Baltic shields of the East European Craton were built up finally during collision of the previously independent Fennoscandian and Sarmatian crustal segments at c. 1.8-1.7 Ga. EUROBRIDGE seismic profiling and geophysical modelling across the southwestern part of the Craton suggest that the Central Belarus Suture Zone is the junction between the two colliding segments. This junction is marked by strong deformation of the crust and the presence of a metamorphic core complex. At 1.80-1.74 Ga, major late to post-collisional extension and magmatism affected the part of Sarmatia adjoining the Central Belarus Zone and generated a high-velocity layer at the base of the crust. Other sutures separating terranes of different ages are found within Sarmatia and in the Polish-Lithuanian part of Fennoscandia. While Fennoscandia and Sarmatia were still a long distance apart, orogeny was dominantly accretionary. The accreted Palaeoproterozoic terranes in the Baltic-Belarus region of Fennoscandia are all younger than 2.0 Ga (2.0-1.9, 1.90-1.85 and 1.84-1.82 Ga), whereas those in Sarmatia have ages of c. 2.2-2.1 and 2.0-1.95 Ga. Lithospheric deformation and magmatism at c. 1.50-1.45 Ga, and Devonian rifting, are also defined by the EUROBRIDGE seismic and gravity models.",

author = "Svetlana Bogdanova and R. Gorbatschev and M. Grad and T. Janik and A. Guterch and Elena Kozlovskaya and G. Motuza and G. Skridlaite and V. Starostenko and L. Taran and Astapenko, {V. N.} and Belinsky, {A. A.} and Garetsky, {R. G.} and Karatayev, {G. I.} and Terletsky, {V. V.} and G. Zlotski and Jensen, {S. L.} and Knudsen, {M. E.} and H. Thybo and R. Sand and K. Komminaho and U. Luosto and T. Tiira and J. Yliniemi and R. Giese and J. Makris and A. {\v C}e{\v c}ys and J. Jacyna and L. Korabliova and V. Nasedkin and A. Rimsa and R. Se{\v c}kus and W. Czuba and E. Gaczy{\'n}ski and P. {\'S}roda and M. Wilde-Pi{\'o}rko and E. Bibikova and Stefan Claesson and Elming, {S. A.} and Lund, {C. E.} and J. Mansfeld and L. Page and K. Sundblad and Doody, {J. J.} and H. Downes and Buryanov, {V. B.} and Egorova, {T. P.} and Il'chenko, {T. V.} and Kharitonov, {O. M.} and Lysynchuk, {D. V.} and Legostayeva, {O. V.} and Makarenko, {I. B.} and Omel'chenko, {V. D.} and Orlyuk, {M. I.} and Pashkevich, {I. K.} and Skobelev, {V. M.} and Stepanyuk, {L. M.} and Keller, {G. R.} and Miller, {K. C.}",

year = "2006",

doi = "10.1144/GSL.MEM.2006.032.01.36",

language = "English",

isbn = "1862392129",

series = "Geological Society Memoir",

pages = "599--625",

editor = "D.G. Gee and R.A. Stephenson",

booktitle = "European Lithosphere Dynamics",

}

Bogdanova, S, Gorbatschev, R, Grad, M, Janik, T, Guterch, A, Kozlovskaya, E, Motuza, G, Skridlaite, G, Starostenko, V, Taran, L, Astapenko, VN, Belinsky, AA, Garetsky, RG, Karatayev, GI, Terletsky, VV, Zlotski, G, Jensen, SL, Knudsen, ME, Thybo, H, Sand, R, Komminaho, K, Luosto, U, Tiira, T, Yliniemi, J, Giese, R, Makris, J, Čečys, A, Jacyna, J, Korabliova, L, Nasedkin, V, Rimsa, A, Sečkus, R, Czuba, W, Gaczyński, E, Środa, P, Wilde-Piórko, M, Bibikova, E, Claesson, S, Elming, SA, Lund, CE, Mansfeld, J, Page, L, Sundblad, K, Doody, JJ, Downes, H, Buryanov, VB, Egorova, TP, Il'chenko, TV, Kharitonov, OM, Lysynchuk, DV, Legostayeva, OV, Makarenko, IB, Omel'chenko, VD, Orlyuk, MI, Pashkevich, IK, Skobelev, VM, Stepanyuk, LM, Keller, GR & Miller, KC 2006, EUROBRIDGE: New insight into the geodynamic evolution of the East European Craton. in DG Gee & RA Stephenson (eds), European Lithosphere Dynamics. Geological Society Memoir, vol. 32, pp. 599-625. https://doi.org/10.1144/GSL.MEM.2006.032.01.36

TY - CHAP

T1 - EUROBRIDGE

T2 - New insight into the geodynamic evolution of the East European Craton

AU - Bogdanova, Svetlana

AU - Gorbatschev, R.

AU - Grad, M.

AU - Janik, T.

AU - Guterch, A.

AU - Kozlovskaya, Elena

AU - Motuza, G.

AU - Skridlaite, G.

AU - Starostenko, V.

AU - Taran, L.

AU - Astapenko, V. N.

AU - Belinsky, A. A.

AU - Garetsky, R. G.

AU - Karatayev, G. I.

AU - Terletsky, V. V.

AU - Zlotski, G.

AU - Jensen, S. L.

AU - Knudsen, M. E.

AU - Thybo, H.

AU - Sand, R.

AU - Komminaho, K.

AU - Luosto, U.

AU - Tiira, T.

AU - Yliniemi, J.

AU - Giese, R.

AU - Makris, J.

AU - Čečys, A.

AU - Jacyna, J.

AU - Korabliova, L.

AU - Nasedkin, V.

AU - Rimsa, A.

AU - Sečkus, R.

AU - Czuba, W.

AU - Gaczyński, E.

AU - Środa, P.

AU - Wilde-Piórko, M.

AU - Bibikova, E.

AU - Claesson, Stefan

AU - Elming, S. A.

AU - Lund, C. E.

AU - Mansfeld, J.

AU - Page, L.

AU - Sundblad, K.

AU - Doody, J. J.

AU - Downes, H.

AU - Buryanov, V. B.

AU - Egorova, T. P.

AU - Il'chenko, T. V.

AU - Kharitonov, O. M.

AU - Lysynchuk, D. V.

AU - Legostayeva, O. V.

AU - Makarenko, I. B.

AU - Omel'chenko, V. D.

AU - Orlyuk, M. I.

AU - Pashkevich, I. K.

AU - Skobelev, V. M.

AU - Stepanyuk, L. M.

AU - Keller, G. R.

AU - Miller, K. C.

PY - 2006

Y1 - 2006

N2 - The Palaeoproterozoic crust and upper mantle in the region between the Ukrainian and Baltic shields of the East European Craton were built up finally during collision of the previously independent Fennoscandian and Sarmatian crustal segments at c. 1.8-1.7 Ga. EUROBRIDGE seismic profiling and geophysical modelling across the southwestern part of the Craton suggest that the Central Belarus Suture Zone is the junction between the two colliding segments. This junction is marked by strong deformation of the crust and the presence of a metamorphic core complex. At 1.80-1.74 Ga, major late to post-collisional extension and magmatism affected the part of Sarmatia adjoining the Central Belarus Zone and generated a high-velocity layer at the base of the crust. Other sutures separating terranes of different ages are found within Sarmatia and in the Polish-Lithuanian part of Fennoscandia. While Fennoscandia and Sarmatia were still a long distance apart, orogeny was dominantly accretionary. The accreted Palaeoproterozoic terranes in the Baltic-Belarus region of Fennoscandia are all younger than 2.0 Ga (2.0-1.9, 1.90-1.85 and 1.84-1.82 Ga), whereas those in Sarmatia have ages of c. 2.2-2.1 and 2.0-1.95 Ga. Lithospheric deformation and magmatism at c. 1.50-1.45 Ga, and Devonian rifting, are also defined by the EUROBRIDGE seismic and gravity models.

AB - The Palaeoproterozoic crust and upper mantle in the region between the Ukrainian and Baltic shields of the East European Craton were built up finally during collision of the previously independent Fennoscandian and Sarmatian crustal segments at c. 1.8-1.7 Ga. EUROBRIDGE seismic profiling and geophysical modelling across the southwestern part of the Craton suggest that the Central Belarus Suture Zone is the junction between the two colliding segments. This junction is marked by strong deformation of the crust and the presence of a metamorphic core complex. At 1.80-1.74 Ga, major late to post-collisional extension and magmatism affected the part of Sarmatia adjoining the Central Belarus Zone and generated a high-velocity layer at the base of the crust. Other sutures separating terranes of different ages are found within Sarmatia and in the Polish-Lithuanian part of Fennoscandia. While Fennoscandia and Sarmatia were still a long distance apart, orogeny was dominantly accretionary. The accreted Palaeoproterozoic terranes in the Baltic-Belarus region of Fennoscandia are all younger than 2.0 Ga (2.0-1.9, 1.90-1.85 and 1.84-1.82 Ga), whereas those in Sarmatia have ages of c. 2.2-2.1 and 2.0-1.95 Ga. Lithospheric deformation and magmatism at c. 1.50-1.45 Ga, and Devonian rifting, are also defined by the EUROBRIDGE seismic and gravity models.

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U2 - 10.1144/GSL.MEM.2006.032.01.36

DO - 10.1144/GSL.MEM.2006.032.01.36

M3 - Chapter

AN - SCOPUS:33846115674

SN - 1862392129

SN - 9781862392120

T3 - Geological Society Memoir

SP - 599

EP - 625

BT - European Lithosphere Dynamics

A2 - Gee, D.G.

A2 - Stephenson, R.A.

ER -

EUROBRIDGE: New insight into the geodynamic evolution of the East European Craton

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