The DOI matches its Crossref record; 125 of the 125 references it cites were found in a registry or an index.
Contrasting styles of Phanerozoic and Precambrian continental collision
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“numerical modelling (ex.Sizova et al., 2014) generally predicts wide orogenic hinterlands with abundant syn-orogenic magmatism (in some models), lower elevations and enhanced syn-orogenic extension in the Mesoproterozoic.”
From The Grenville Province: revisiting the orogenic framework and integrating recent findings (2025) · cites this paper as Sizova et al., 2014
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Citations
Cites
The volume and composition of melt generated by extension of the lithosphere
McKENZIE, D., & BICKLE, M. J. (1988) · Journal of Petrology · doi:10.1093/petrology/29.3.625 · Cited by 2,951 · cited 1×
“Ambient mantle potential temperatures are inferred to have been significantly higher than the present day, which would have led to the production of a greater volume of primary melts with higher MgO (McKenzie and Bickle, 1988; Nisbet et al., 1993; Herzberg et al., 2007, 2010).”
BackgroundConnolly, J. A. D. (2005) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2005.04.033 · Cited by 2,246
Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation
Schmidt, M. W., & Poli, S. (1998) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(98)00142-3 · Cited by 1,935
Element transport from slab to volcanic front at the Mariana arc
Elliott, T., Plank, T., Zindler, A., White, W., & Bourdon, B. (1997) · Journal of Geophysical Research: Solid Earth · doi:10.1029/97jb00788 · Cited by 1,512
4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zircon
Valley, J. W., Lackey, J. S., Cavosie, A. J., Clechenko, C. C., Spicuzza, M. J., Basei, M. A. S., Bindeman, I. N., Ferreira, V. P., Sial, A. N., King, E. M., et al. (2005) · Contributions to Mineralogy and Petrology · doi:10.1007/s00410-005-0025-8 · Cited by 1,222
Thermal history of the Earth and its petrological expression
Herzberg, C., Condie, K., & Korenaga, J. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.01.022 · Cited by 1,148 · cited 6×
“The temperature of the ambient upper-mantlewhere this transition in geodynamic regimes occurs corresponds broadly to the Neoproterozoic Era.”
BackgroundInfluential(2011) · SpringerReference · doi:10.1007/springerreference_43921 · Cited by 1,030
Thermal Conductivity of Rocks and Minerals
Clauser, C., & Huenges, E. (2013) · AGU Reference Shelf · doi:10.1029/rf003p0105 · Cited by 1,019
U-Th Isotopes in Arc Magmas: Implications for Element Transfer from the Subducted Crust
Hawkesworth, C. J., Turner, S. P., McDermott, F., Peate, D. W., & van Calsteren, P. (1997) · Science · doi:10.1126/science.276.5312.551 · Cited by 983
A change in the geodynamics of continental growth 3 billion years ago
Dhuime, B., Hawkesworth, C. J., Cawood, P. A., & Storey, C. D. (2012) · Science · doi:10.1126/science.1216066 · Cited by 923 · cited 6×
“…high-temperature, low-to-moderate pressuremetamorphic rockswith extensivemagmatism that has contributed significantly to crustal growth (e.g. Brown, 2007; Ahäll andConnelly, 2008;Gapais et al., 2009; Kukkonen and Lauri, 2009; Smithies et al., 2011; Dhuime et al., 2012; Percival et al., 2012).”
BackgroundInfluential
Cited by
Kelsey, D. E., & Hand, M. (2015) · Geoscience Frontiers · doi:10.1016/j.gsf.2014.09.006 · Cited by 441
Precambrian geodynamics: Concepts and models
Gerya, T. (2014) · Gondwana Research · doi:10.1016/j.gr.2012.11.008 · Cited by 352
Self-citationGeneration of felsic crust in the Archean: A geodynamic modeling perspective
Sizova, E., Gerya, T., Stüwe, K., & Brown, M. (2015) · Precambrian Research · doi:10.1016/j.precamres.2015.10.005 · Cited by 332
Self-citationThe zircon archive of continent formation through time
Roberts, N. M. W., & Spencer, C. J. (2015) · Geological Society, London, Special Publications · doi:10.1144/sp389.14 · Cited by 298
The contribution of metamorphic petrology to understanding lithosphere evolution and geodynamics
Brown, M. (2014) · Geoscience Frontiers · doi:10.1016/j.gsf.2014.02.005 · Cited by 279
Self-citation
Metadata
- Authors
- Sizova, E., Gerya, T., & Brown, M.
- Venue
- Gondwana Research
- Publisher
- Elsevier BV
- Published
- 2014-03
- Volume
- 25
- Issue
- 2
- Pages
- 522-545
- ISSN
- 1342-937X (ISSN-L)
- OpenAlex
- W2010259407
- Cited by
- 314
- References
- 125
- FWCI
- 22.56
- Type
- journal article
- Language
- en
- Open access
- closed
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
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How to cite
Cite CoChat for the checks on this page, and the paper for its own findings.
- This page
- CoChat. (2026). Citation check: Contrasting styles of Phanerozoic and Precambrian continental collision. https://app.cochat.ai/papers/10.1016/j.gr.2012.12.011
- The paper
- Sizova, E., Gerya, T., & Brown, M. (2014). Contrasting styles of Phanerozoic and Precambrian continental collision. Gondwana Research. https://doi.org/10.1016/j.gr.2012.12.011
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
