Trans-Baltic Palaeoproterozoic correlations towards the reconstruction of supercontinent Columbia/Nuna

Bogdanova, Svetlana; Gorbatschev, Roland; Skridlaitė, Gražina; Соэсоо, Алвар; Taran, Ludmila; Kurlovich, Dzmitry

doi:10.1016/j.precamres.2014.11.023

Cited by 114 publications

(76 citation statements)

References 98 publications

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“…The East European Craton is the coherent Precambrian, mainly Archaean and Paleoproterozoic, part of the continental plate and occupies the north-eastern portion of Europe (Bogdanova et al , 2015. Three independent crustal segments: Fennoscandia, Sarmatia and Volgo-Uralia, collided to form the EEC (Bogdanova et al 1996).…”

Section: Geological Contextmentioning

confidence: 99%

“…The central station A0 is located about 50 km from the TESZ. The crystalline basement of the EEC is buried beneath a 5-9 km thick cover of sediments, and is interpreted to be the prolongation of the 1.81-1.76 Ga Trans-Scandinavian Igneous Belt (Bogdanova et al 2015 and references therein). The Polish Basin adjoining the part of EEC discussed in this study is filled with Upper Palaeozoic, Meso-and Cenozoic sedimentary 10-12 km sequences, underlain by a sedimentary "pre-Variscan consolidated crust" reaching the depth of 20 km; Moho is located at ca.…”

Section: Geological Contextmentioning

confidence: 99%

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The geophysical characteristic of the lower lithosphere and asthenosphere in the marginal zone of the East European Craton

Grad

Puziewicz

Majorowicz³

et al. 2018

Int J Earth Sci (Geol Rundsch)

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Seismic P-and S-wave velocities of the lower lithosphere and underlying asthenosphere at the SW margin of the East European Craton in northern Poland were obtained with different seismic techniques: seismic refraction, P-residuals of the first arrivals from teleseismic earthquakes, P-wave receiver function, and inversion of the Rayleigh surface wave dispersion curves, the last two using data collected in the passive seismic experiment "13 BB star". The uniform array consisted of 13 stations deployed in a 120 km in diameter area. Below the depth of 180-220 km a decrease of about 6% of the S-wave velocity is interpreted as a thermal gradient zone corresponding to a lithosphere-asthenosphere transition. The average mantle velocities down to a depth of 300 km beneath the array are relatively high, exceeding values for other Precambrian cratons by 0.1-0.2 km/s, and cannot be modeled by reasonable mantle peridotite compositions in the lithospheric part of the profile. We suggest that significant peridotite anisotropy could explain the misfit between measured and calculated seismic velocities in the lithosphere.

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Section: Geological Contextmentioning

confidence: 99%

Section: Geological Contextmentioning

confidence: 99%

The geophysical characteristic of the lower lithosphere and asthenosphere in the marginal zone of the East European Craton

Grad

Puziewicz

Majorowicz³

et al. 2018

Int J Earth Sci (Geol Rundsch)

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“…The area of Po land is di vided into two ma jor mag netic provinces by the NW-SE trending line. The north east ern prov ince, cor re spond ing to the EEC, is char ac ter ized by the pres ence of Narkiewicz et al, 2015), FSB -Fennoscandia-Sarmatia bound ary (af ter Bogdanova et al, 2015); Fennoscandia: MLSZ -Mid-Lith u a nian Su ture Zone, AMCG -An or thosite-Mangerite-Charnockite-Gran ite as so ci a tion, Pa leo zoic mas sifs: 1 -Olsztynek, 2 -M³awa, 3 -Pisz, 4 -E³k, 5 -Tajno; Sarmatia: BPGB -Belarus-Podlasie Granulite Belt, OHB -Okolovo-Holeszów Belt, IBZ -Ivano-Borisov Zone, OMIB -Osnitsk-Mikashevichi Ig ne ous Belt (af ter Krzemiñska et al, in press); Mesoproterozoic mas sifs of Fennoscandia: 6 -Kêtrzyn, 7 -Suwa³ki (af ter Kubicki and Ryka, 1982); other ex pla na tions as in Fig ure 4 in tense mag netic anom a lies. The south west ern prov ince is part of the youn ger Phanerozoic West Eu ro pean Plat form, where the over all in ten sity of ex ist ing mag netic anom a lies is def i nitely lower, ex cept for a few par tic u lar re gions.…”

Section: Magnetic Anomaly Patternmentioning

confidence: 99%

“…These belts are re garded as a south ern frag ment of the Fennoscandian part of EEC, bor der ing Sarmatia from the NW (Bogdanova et al, 2006;Krzemiñska et al, in press). How ever, ac cord ing to the new tectonic sub di vi sion of the South Bal tic re gion (Bogdanova et al, 2015), the BPGB and OHB be long to Sarmatia.…”

Section: Podlasie Zonementioning

confidence: 99%

A new magnetic anomaly map of Poland and its contribution to the recognition of crystalline basement rocks

Petecki

Rosowiecka

2017

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A new mag netic anom aly map of Po land and its con tri bu tion to the rec og ni tion of crys talline base ment rocks. Geo log i cal Quar terly, 61 (4): 934-945, doi: 10.7306/gq.1383 Mag netic to tal field mea sure ments ac quired in Po land be tween 1974 and 2011 have been com piled in a new dig i tal da ta base that pro vides a com plete pic ture of mag netic anom a lies of the coun try. The data com pi la tion and fur ther pro cess ing pro cedures used to cre ate the mag netic anom aly da ta base and maps that ac com pany this ar ti cle are briefly sum ma rized. The reduced-to-the-pole and pseudogravity anom aly maps were com puted to ac cu rately lo cate anom a lies above their caus ative bod ies as well as to sim plify anom aly pat terns and em pha size prin ci pal mag netic do mains within the base ment. An in ter preta tion of the mag netic maps re veals a lot of mag netic base ment prov inces and do mains in di cat ing base ment di vi sion into blocks and struc tural el e ments, which are im por tant for un der stand ing the re gional tec tonic set ting of Po land.Key words: mag netom etry, Earth's to tal mag netic field map, pseudogravity, crys tal line base ment, Po land.

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“…The 1.92-1.66 Ga Paleoproterozoic province The 1.92-1.66 Ga Paleoproterozoic province in the southernmost Baltic Shield (Fig. 2) exposes bedrock formed and variably metamorphosed and deformed along a long-lived active continental margin (Mansfeld, 1996;Stephens et al, 2009;Bogdanova et al, 2015;Kleinhanns et al, 2015). It includes Paleoproterozoic rocks reworked and/or formed in a series of accretionary orogenic events at 1.92-1.79 Ga (Svecofennian orogeny ;Lahtinen et al, 2005), and wide-spread alkali-calcic, granitic to quartzmonzodioritic magmatic rocks (Transscandinavian Igneous Belt, stippled in Figs.…”

Section: Orogenic Provinces In the Southernmost Baltic Shieldmentioning

confidence: 99%

Hallandian 1.45Ga high-temperature metamorphism in Baltica: P–T evolution and SIMS U–Pb zircon ages of aluminous gneisses, SW Sweden

Ulmius

Andersson

Möller

2015

Precambrian Research

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Trans-Baltic Palaeoproterozoic correlations towards the reconstruction of supercontinent Columbia/Nuna

Cited by 114 publications

References 98 publications

The geophysical characteristic of the lower lithosphere and asthenosphere in the marginal zone of the East European Craton

The geophysical characteristic of the lower lithosphere and asthenosphere in the marginal zone of the East European Craton

A new magnetic anomaly map of Poland and its contribution to the recognition of crystalline basement rocks

Hallandian 1.45Ga high-temperature metamorphism in Baltica: P–T evolution and SIMS U–Pb zircon ages of aluminous gneisses, SW Sweden

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