The DOI matches its Crossref record; 33 of the 33 references it cites were found in a registry or an index.
Temperatures of serpentinization of ultramafic rocks based on O18/O16 fractionation between coexisting serpentine and magnetite
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In the citing paper
“These temperatures are lower than typical serpentinization temperatures in continental settings (85-115 ° C in chrysotile-lizardite mineralogies; Wenner and Taylor, 1971), in agreement with the observation that magnesite vein mineralization postdates serpentinization in the host peridotite rock.”
From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Wenner and Taylor, 1971
Citations
Cites
Empirical Correction Factors for the Electron Microanalysis of Silicates and Oxides
Bence, A. E., & Albee, A. L. (1968) · The Journal of Geology · doi:10.1086/627339 · Cited by 2,133
Geochemistry of hydrothermal ore deposits
Christ, C. L. (1968) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(68)90069-0 · Cited by 2,040
Fyfe, W. S. (1968) · Tectonophysics · doi:10.1016/0040-1951(68)90059-0 · Cited by 904
The oxygen isotope geochemistry of igneous rocks
Taylor, H. P. (1968) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00371729 · Cited by 830
Self-citationAlbee, A. L., & Ray, L. (1970) · Analytical Chemistry · doi:10.1021/ac60294a030 · Cited by 717
Craig, H., Miller, S., Wasserburg, G. J., & Urey, H. C. (1964) · CaltechAUTHORS (California Institute of Technology) · Cited by 592
Craig, H., Miller, S. L., & Wasserburg, G. J. (1964) · CaltechAUTHORS (California Institute of Technology) · Cited by 589
(1967) · CaltechAUTHORS (California Institute of Technology) · Cited by 586
Self-citationBARNES, I., & O'NEIL, J. R. (1969) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1969)80[1947:trbfis]2.0.co;2 · Cited by 392
Relationship Between O18/O16 Ratios in Coexisting Minerals of Igneous and Metamorphic Rocks
TAYLOR, H. P., & EPSTEIN, S. (1962) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1962)73[461:rboric]2.0.co;2 · Cited by 370
Self-citation
Research works printed but not linked: 5
- Fyfe, W. S.: Metamorphism in mobile belts-the glaucophane schist problem. Trans. Leicester Let. and Phil. Soc.61, 36–54 (1967).
- Hostetler, P. B., Coleman, R. G., Mumpton, F. A., Evans, B. W.: Brucite in alpine serpentines. Am. Mineralogist51, 75–98 (1966).
- Page, N. J.: Serpentinization in a sheared serpentinite lens, Tiburon Peninsula, California. Geological survey research. 1968. U. S. Geol. Surv. Profess. Papers600 B, B 21-B 28 (1968).
- Scarfe, C. M., Wyllie, P. J.: Experimental redetermination of the upper stability limit of serpentine up to 3 kbar pressure. Trans. Am. Geophys. Union48, 225 (1967).
- —, Noble, J. A.: Origin of magnetite in the zoned ultramafic complexes of southeastern Alaska. Symposium on Magmatic Ore Deposits. Econ. Geol. Monogr.4, 209–230 (1969).
Cited by
Calculation of oxygen isotope fractionation in hydroxyl-bearing silicates
Zheng, Y.-F. (1993) · Earth and Planetary Science Letters · doi:10.1016/0012-821x(93)90243-3 · Cited by 721
The Serpentinite Multisystem Revisited: Chrysotile Is Metastable
Evans, B. W. (2004) · International Geology Review · doi:10.2747/0020-6814.46.6.479 · Cited by 613
Boron isotope exchange between seawater and the oceanic crust
Spivack, A. J., & Edmond, J. M. (1987) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(87)90198-0 · Cited by 563
Serpentinization as a source of energy at the origin of life
RUSSELL, M. J., HALL, A. J., & MARTIN, W. (2010) · Geobiology · doi:10.1111/j.1472-4669.2010.00249.x · Cited by 527
Serpentinization of abyssal peridotites at mid-ocean ridges
Mével, C. (2003) · Comptes Rendus Géoscience · doi:10.1016/j.crte.2003.08.006 · Cited by 524
Metadata
- Authors
- Wenner, D. B., & Taylor, H. P.
- Affiliations
- California Institute of Technology (US)
- Venue
- Contributions to Mineralogy and Petrology
- Published
- 1971-09
- Volume
- 32
- Issue
- 3
- Pages
- 165-185
- ISSN
- 0010-7999 (ISSN-L)
- 1432-0967
- OpenAlex
- W1988978036
- Cited by
- 405
- References
- 33
- Citations by year
- 2026: 9 · 2025: 8 · 2024: 8 · 2023: 11 · 2022: 7 · 2021: 7 · 2020: 7 · 2019: 13 · 2018: 9 · 2017: 8 · 2016: 7 · 2015: 13 · 2014: 16 · 2013: 9 · 2012: 9
- FWCI
- 4.12
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Contributions to Mineralogy and Petrology (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- serpentinization, ultramafic rocks, oxygen isotope fractionation, antigorite, lizardite, chrysotile, chlorite, Mid-Atlantic Ridge
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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: Temperatures of serpentinization of ultramafic rocks based on O18/O16 fractionation between coexisting serpentine and magnetite. https://app.cochat.ai/papers/10.1007/bf00643332
- The paper
- Wenner, D. B., & Taylor, H. P. (1971). Temperatures of serpentinization of ultramafic rocks based on O18/O16 fractionation between coexisting serpentine and magnetite. Contributions to Mineralogy and Petrology. https://doi.org/10.1007/bf00643332
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.
