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
Citations
Cites
DeMets, C., Gordon, R. G., Argus, D. F., & Stein, S. A. (1990) · Geophysical Journal International · doi:10.1111/j.1365-246x.1990.tb06579.x · Cited by 3,815
Multi-channel seismic imaging of a crustal magma chamber along the East Pacific Rise
Detrick, R. S., Buhl, P., Vera, E. E., Mutter, J. C., Orcutt, J. A., Madsen, J., & Brocher, T. M. (1987) · Nature · doi:10.1038/326035a0 · Cited by 756
Evidence from gravity data for focusedmagmatic accretionalong the Mid-Atlantic Ridge
Lin, J., Purdy, G. M., Schouten, H. A., Sempéré, J., & Zervas, C. E. (1990) · Nature · doi:10.1038/344627a0 · Cited by 584
Structure and constitution of the lower oceanic crust
Christensen, N. I., & Salisbury, M. H. (1975) · Reviews of Geophysics · doi:10.1029/rg013i001p00057 · Cited by 503
Kuo, B., & Forsyth, D. W. (1988) · Marine Geophysical Research · doi:10.1007/bf00310065 · Cited by 404
Vera, E. E., Mutter, J. C., Buhl, P., Orcutt, J. A., Harding, A. J., Kappus, M. E., Detrick, R. S., & Brocher, T. M. (1990) · Journal of Geophysical Research Atmospheres · doi:10.1029/jb095ib10p15529 · Cited by 390
Melt-enhanced deformation: A major tectonic process
Hollister, L. S., & Crawford, M. L. (1986) · Geology · doi:10.1130/0091-7613(1986)14 · Cited by 368
Oceanic spreading rate and crustal thickness
Reid, I. D., & Jackson, H. R. (1981) · Marine Geophysical Research · doi:10.1007/bf00163477 · Cited by 323
The spreading rate dependence of three‐dimensional mid‐ocean ridge gravity structure
Lin, J. G., & Morgan, J. P. (1992) · Geophysical Research Letters · doi:10.1029/91gl03041 · Cited by 293
Structure of young oceanic crust at 13°N on the East Pacific Rise from expanding spread profiles
Harding, A. J., Orcutt, J. A., Kappus, M. E., Vera, E. E., Mutter, J. C., Buhl, P., Detrick, R. S., & Brocher, T. M. (1989) · Journal of Geophysical Research Atmospheres · doi:10.1029/jb094ib09p12163 · Cited by 249
Research works printed but not linked: 5
- Detrick R. S., Chapter VI: Crustal structure of oceanic fracture zones, in The Tectonics of Fracture Zones
- Jackson H. R., 1980, Crustal refraction and seismic reflection results from FRAM 1 (abstract), Eos Trans. AGU, 61, 276
- Rowlett H., 1974, An ocean bottom seismometer (OBS) refraction profile on the Mid‐Atlantic Ridge at 13°S (abstract), Eos Trans. AGU., 55, 294
- Abbott D., 1987, Statistics of fracture zones, subduction of ridges, and the composition of Ophiolites (abstract), Eos Trans. AGU., 69, 408
- Blackman D. K., Isostatic compensation of tectonic features of MAR: 25–27°30′S, J. Geophys. Res.
Cited by
Sorted by citations
CRUST 5.1: A global crustal model at 5° × 5°
Mooney, W. D., Laske, G., & Masters, T. G. (1998) · Journal of Geophysical Research Atmospheres · doi:10.1029/97jb02122 · Cited by 1,029
A possible role for garnet pyroxenite in the origin of the "garnet signature" in MORB
Hirschmann, M. M., & Stolper, E. M. (1996) · Contributions to Mineralogy and Petrology · doi:10.1007/s004100050184 · Cited by 830
Mantle Melting and Melt Extraction Processes beneath Ocean Ridges: Evidence from Abyssal Peridotites
Niu, Y. (1997) · Journal of Petrology · doi:10.1093/petroj/38.8.1047 · Cited by 562
Variation with spreading rate of oceanic crustal thickness and geochemistry
Bown, J. W., & White, R. S. (1994) · Earth and Planetary Science Letters · doi:10.1016/0012-821x(94)90082-5 · Cited by 399
Permeability within basaltic oceanic crust
Fisher, A. T. (1998) · Reviews of Geophysics · doi:10.1029/97rg02916 · Cited by 373
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
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