The DOI matches its Crossref record; 40 of the 40 references it cites were found in a registry or an index.
Subduction and eduction of continental crust: major mechanisms during continent‐continent collision and orogenic extensional collapse, a model based on the south Norwegian Caledonides
Abstract
During continental collision in the middle Silurian, the thickness of the lithosphere under the Caledonides of S. Norway was doubled by subduction of the western margin of Baltica, including the Western Gneiss Region, under Laurentia. Crustal rocks of the Baltic plate reached sub‐Moho depths of near 100 km or more as inferred from the presence of coesite in eclogites. Isostatic calculations indicate an average elevation of the mountain chain of about 3 km at this stage. The subducted lithosphere experienced vertical constrictional strains as a result of slab‐pull by its heavy and cold root. Eduction of the deeply buried crustal material was initiated by decoupling of the Thermal Boundary Layer in the subducted lithosphere. Isostatic rebound resulted in very rapid uplift (1–2 mm yr‐1), and the deep crust was exhumed, mainly by tectonic extensional stripping over a period of 30–40 Myr. The eduction was probably related to a rolling hinge, footwall uplift mechanism, and the early high‐pressure coaxial fabrics were overprinted by extensional simple shear as the deep crust reached middle and upper crustal levels. The model explains the present‐day normal crustal thickness under the exhumed deep rocks without necessarily invoking large‐scale lateral flow of material in the lower crust or igneous underplating.
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Citations
Cites
Extensional collapse of orogens
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Self-citationChopin, C. (1984) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00381838 · Cited by 1,350
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The tectonic evolution of the Tibetan Plateau
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Self-citationCoesite in clinopyroxene in the Caledonides and its implications for geodynamics
Smith, D. C. (1984) · Nature · doi:10.1038/310641a0 · Cited by 773
flexural rotation of normal faults
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Eclogitization of lower crustal granulites by fluid migration through shear zones
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Flexural rotation of normal faults
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The mechanics of the Tibetan Plateau
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Cited by
Li, S., Xiao, Y., Liou, D., Chen, Y., Ge, N., Zhang, Z., Sun, S.-S., Cong, B., Zhang, R., Hart, S. R., et al. (1993) · Chemical Geology · doi:10.1016/0009-2541(93)90063-o · Cited by 1,048
TORSVIK, T., SMETHURST, M., MEERT, J., VANDERVOO, R., MCKERROW, W., BRASIER, M., STURT, B., & WALDERHAUG, H. (1996) · Earth-Science Reviews · doi:10.1016/0012-8252(96)00008-6 · Cited by 799
Differentiation of the continental crust by relamination
Hacker, B. R., Kelemen, P. B., & Behn, M. D. (2011) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2011.05.024 · Cited by 536
Exhumation of high‐pressure rocks: a review of concepts and processes
Platt, J. P. (1993) · Terra Nova · doi:10.1111/j.1365-3121.1993.tb00237.x · Cited by 517
Microdiamond in high-grade metamorphic rocks of the Western Gneiss region, Norway
Dobrzhinetskaya, L. F., Eide, E. A., Larsen, R. B., Sturt, B. A., Trønnes, R. G., Smith, D. C., Taylor, W. R., & Posukhova, T. V. (1995) · Geology · doi:10.1130/0091-7613(1995)023<0597:mihgmr>2.3.co;2 · Cited by 332
Metadata
- Authors
- Andersen, T. B., Jamtveit, B., Dewey, J. F., & Swensson, E.
- Venue
- Terra Nova
- Publisher
- Wiley
- Published
- 1991-05
- Volume
- 3
- Issue
- 3
- Pages
- 303-310
- ISSN
- 0954-4879 (ISSN-L)
- 1365-3121
- OpenAlex
- W2018763910
- Cited by
- 403
- References
- 40
- FWCI
- 10.33
- Type
- journal article
- Language
- en
- Open access
- closed
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- CoChat. (2026). Citation check: Subduction and eduction of continental crust: major mechanisms during continent‐continent collision and orogenic extensional collapse, a model based on the south Norwegian Caledonides. https://app.cochat.ai/papers/10.1111/j.1365-3121.1991.tb00148.x
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- Andersen, T. B., Jamtveit, B., Dewey, J. F., & Swensson, E. (1991). Subduction and eduction of continental crust: major mechanisms during continent‐continent collision and orogenic extensional collapse, a model based on the south Norwegian Caledonides. Terra Nova. https://doi.org/10.1111/j.1365-3121.1991.tb00148.x
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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