Evidence for early Proterozoic plate tectonics from seismic reflection profiles in the Baltic shield

T. Dahl-Jensen; R. W. Hobbs; S. L. Klemperer; D. H. Matthews; D. B. Snyder; R. Long; T. Matthews; D. J. Blundell; C. E. Lund; H. Palm; L. B. Pedersen; R. G. Roberts; S. A. Elming; P. Heikkinen; H. Korhonen; U. Luosto; S. E. Hjelt; K. Komminaho; J. Yliniemi; R. Meissner; P. Sadowiak; Th Wever; T. Dickmann; E. R. Flueh; A. Berthelsen; H. Thybo; N. Balling; E. Nørmark

doi:10.1038/348034a0

Evidence for early Proterozoic plate tectonics from seismic reflection profiles in the Baltic shield

T. Dahl-Jensen
, R. W. Hobbs
, S. L. Klemperer^*
, D. H. Matthews
, D. B. Snyder
, R. Long
, T. Matthews
, D. J. Blundell
, C. E. Lund
, H. Palm
, L. B. Pedersen
, R. G. Roberts
, S. A. Elming
, P. Heikkinen
, H. Korhonen
, U. Luosto
, S. E. Hjelt
, K. Komminaho
, J. Yliniemi
, R. Meissner

P. Sadowiak, Th Wever, T. Dickmann, E. R. Flueh, A. Berthelsen, H. Thybo, N. Balling, E. Nørmark

^*Bu çalışma için yazışmadan sorumlu yazar

Araştırma sonucu: Dergiye katkı › Makale › bilirkişi

294 Atıf (Scopus)

Özet

Plate tectonics provides the linking framework for all tectonic and magmatic activity seen today, but it is not known when plate tectonics first developed on Earth. New deep seismic reflection and coincident refraction profiles across an exposed, 1.89-Gyr-old volcanic arc complex show a 10-km-thick offset in the Moho and bivergent reflectors in the crust, which were most probably created by plate convergence, subduction and accretion during the Early Proterozoic. Hence, plate tectonic models seem to be applicable for at least the second half of Earth's history.

Orijinal dil	İngilizce
Sayfa (başlangıç-bitiş)	34-38
Sayfa sayısı	5
Dergi	Nature
Hacim	348
Basın numarası	6296
DOI'lar	https://doi.org/10.1038/348034a0
Yayın durumu	Yayınlandı - 1990
Harici olarak yayınlandı	Evet

Belgeye Erişim

10.1038/348034a0

Diğer Dosyalar ve Linkler

Link to publication in Scopus

Alıntı Yap

Dahl-Jensen, T., Hobbs, R. W., Klemperer, S. L., Matthews, D. H., Snyder, D. B., Long, R., Matthews, T., Blundell, D. J., Lund, C. E., Palm, H., Pedersen, L. B., Roberts, R. G., Elming, S. A., Heikkinen, P., Korhonen, H., Luosto, U., Hjelt, S. E., Komminaho, K., Yliniemi, J., ... Nørmark, E. (1990). Evidence for early Proterozoic plate tectonics from seismic reflection profiles in the Baltic shield. Nature, 348(6296), 34-38. https://doi.org/10.1038/348034a0

@article{fb4ca5694c3d4b919e8ef9254f23562b,

title = "Evidence for early Proterozoic plate tectonics from seismic reflection profiles in the Baltic shield",

abstract = "Plate tectonics provides the linking framework for all tectonic and magmatic activity seen today, but it is not known when plate tectonics first developed on Earth. New deep seismic reflection and coincident refraction profiles across an exposed, 1.89-Gyr-old volcanic arc complex show a 10-km-thick offset in the Moho and bivergent reflectors in the crust, which were most probably created by plate convergence, subduction and accretion during the Early Proterozoic. Hence, plate tectonic models seem to be applicable for at least the second half of Earth's history.",

author = "T. Dahl-Jensen and Hobbs, \{R. W.\} and Klemperer, \{S. L.\} and Matthews, \{D. H.\} and Snyder, \{D. B.\} and R. Long and T. Matthews and Blundell, \{D. J.\} and Lund, \{C. E.\} and H. Palm and Pedersen, \{L. B.\} and Roberts, \{R. G.\} and Elming, \{S. A.\} and P. Heikkinen and H. Korhonen and U. Luosto and Hjelt, \{S. E.\} and K. Komminaho and J. Yliniemi and R. Meissner and P. Sadowiak and Th Wever and T. Dickmann and Flueh, \{E. R.\} and A. Berthelsen and H. Thybo and N. Balling and E. N{\o}rmark",

year = "1990",

doi = "10.1038/348034a0",

language = "English",

volume = "348",

pages = "34--38",

journal = "Nature",

issn = "0028-0836",

publisher = "Nature Research",

number = "6296",

}

Dahl-Jensen, T, Hobbs, RW, Klemperer, SL, Matthews, DH, Snyder, DB, Long, R, Matthews, T, Blundell, DJ, Lund, CE, Palm, H, Pedersen, LB, Roberts, RG, Elming, SA, Heikkinen, P, Korhonen, H, Luosto, U, Hjelt, SE, Komminaho, K, Yliniemi, J, Meissner, R, Sadowiak, P, Wever, T, Dickmann, T, Flueh, ER, Berthelsen, A, Thybo, H, Balling, N & Nørmark, E 1990, 'Evidence for early Proterozoic plate tectonics from seismic reflection profiles in the Baltic shield', Nature, hac. 348, no. 6296, pp. 34-38. https://doi.org/10.1038/348034a0

TY - JOUR

T1 - Evidence for early Proterozoic plate tectonics from seismic reflection profiles in the Baltic shield

AU - Dahl-Jensen, T.

AU - Hobbs, R. W.

AU - Klemperer, S. L.

AU - Matthews, D. H.

AU - Snyder, D. B.

AU - Long, R.

AU - Matthews, T.

AU - Blundell, D. J.

AU - Lund, C. E.

AU - Palm, H.

AU - Pedersen, L. B.

AU - Roberts, R. G.

AU - Elming, S. A.

AU - Heikkinen, P.

AU - Korhonen, H.

AU - Luosto, U.

AU - Hjelt, S. E.

AU - Komminaho, K.

AU - Yliniemi, J.

AU - Meissner, R.

AU - Sadowiak, P.

AU - Wever, Th

AU - Dickmann, T.

AU - Flueh, E. R.

AU - Berthelsen, A.

AU - Thybo, H.

AU - Balling, N.

AU - Nørmark, E.

PY - 1990

Y1 - 1990

N2 - Plate tectonics provides the linking framework for all tectonic and magmatic activity seen today, but it is not known when plate tectonics first developed on Earth. New deep seismic reflection and coincident refraction profiles across an exposed, 1.89-Gyr-old volcanic arc complex show a 10-km-thick offset in the Moho and bivergent reflectors in the crust, which were most probably created by plate convergence, subduction and accretion during the Early Proterozoic. Hence, plate tectonic models seem to be applicable for at least the second half of Earth's history.

AB - Plate tectonics provides the linking framework for all tectonic and magmatic activity seen today, but it is not known when plate tectonics first developed on Earth. New deep seismic reflection and coincident refraction profiles across an exposed, 1.89-Gyr-old volcanic arc complex show a 10-km-thick offset in the Moho and bivergent reflectors in the crust, which were most probably created by plate convergence, subduction and accretion during the Early Proterozoic. Hence, plate tectonic models seem to be applicable for at least the second half of Earth's history.

UR - https://www.scopus.com/pages/publications/0025660039

U2 - 10.1038/348034a0

DO - 10.1038/348034a0

M3 - Article

AN - SCOPUS:0025660039

SN - 0028-0836

VL - 348

SP - 34

EP - 38

JO - Nature

JF - Nature

IS - 6296

ER -

Evidence for early Proterozoic plate tectonics from seismic reflection profiles in the Baltic shield

Özet

Belgeye Erişim

Diğer Dosyalar ve Linkler

Parmak izi

Alıntı Yap