The DOI matches its Crossref record; 77 of the 77 references it cites were found in a registry or an index.
Oceanic crustal thickness versus spreading rate
Abstract
A compilation of oceanic crustal thickness from seismic observations collected over the past two decades shows that the average crustal thickness, away from plateaus, is 6 km; no systematic increase of crustal thickness with spreading rate is observed. Instead, the data show large variations in crustal thickness at slow spreading ridges (3 – 8 km for half rates < 20 mm/yr) and small variations in thickness at fast rates (5 – 7 km for half rates > 30 mm/yr). The large variations at slow ridges and small variations at fast ridges are consistent with the results inferred from recent gravity studies of mid‐ocean ridges. Both data sets support the speculation of a transition from a 3‐D structure of crustal accretion at slow ridges to a 2‐D accretion pattern at fast ridges.
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“Specifically, very slow (< 2 cm/yr) and slow (< 5.5 cm/yr) spreading ridges have deep median rift valleys and thin oceanic crust at the spreading axis (Michael et al., 2003), whereas intermediate (> 5.5 cm/yr) and fast (> 10 cm/yr) spreading ridges have more subdued topography at the ridge axis and generate relatively thicker crust (Chen, 1992).”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Chen, 1992
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Self-citation
Metadata
- Authors
- Chen, Y. J.
- Affiliations
- Oregon State University (US)
- Corresponding author
- Chen, Yongshun John
- ORCID
- Chen, Yongshun John
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 1992-04-24
- Volume
- 19
- Issue
- 8
- Pages
- 753-756
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2092103829
- Cited by
- 213
- References
- 77
- Citations by year
- 2025: 3 · 2024: 9 · 2023: 5 · 2022: 6 · 2021: 14 · 2020: 10 · 2019: 8 · 2018: 6 · 2016: 12 · 2015: 8 · 2014: 7 · 2013: 5 · 2012: 5
- FWCI
- 16.06
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geophysical Research Letters (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Physical Sciences › Earth and Planetary Sciences › Geophysics › earthquake and tectonic studies
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Keywords
- oceanic crustal thickness, spreading rate, mid-ocean ridge, slow-spreading ridge, fast-spreading ridges, crustal accretion, gravity anomalies
About these checks
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.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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