Differentiation of the continental crust by relamination
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The formation and continued growth of continents is a more stochastic process than oceanic crust change and is incompletely understood even on modern Earth.
“However, unlike the oceanic crust, which experienced a simple and predictable change in thickness and bulk composition due to secular mantle cooling, the formation and continued growth of the continents is a more stochastic process that is incompletely understood even on the modern-day Earth (Arndt and Goldstein, 1987;Bohlen and Mezger, 1989;Hacker et al., 2011;Spencer et al., 2017).”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Hacker et al., 2011
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- Authors
- Hacker, B. R., Kelemen, P. B., & Behn, M. D.
- Affiliations
- University of California, Santa Barbara (US)
- Lamont-Doherty Earth Observatory (US)
- Woods Hole Oceanographic Institution (US)
- Corresponding author
- Hacker, Bradley R.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2011-07
- Volume
- 307
- Issue
- 3-4
- Pages
- 501-516
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2064536888
- Semantic Scholar
- c79c44a570b1edbe85e6fbb1a1eacb450192b03e
- Cited by
- 536
- References
- 151
- Citations by year
- 2026: 27 · 2025: 37 · 2024: 42 · 2023: 33 · 2022: 42 · 2021: 37 · 2020: 51 · 2019: 37 · 2018: 37 · 2017: 46 · 2016: 27 · 2015: 28 · 2014: 26 · 2013: 33 · 2012: 26
- FWCI
- 26.27
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Funders
- National Science Foundation
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- subduction zone, subduction erosion, eclogitization, felsic gneiss, lower crust, decompression melting, melt extraction, crustal buoyancy, mantle-derived crust
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