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ABSTRACT SEVERAL authors have considered the genesis of various ores in terms of plate tectonic theory1–6. Most have discussed various possibilities for the origin of the ore solutions of
massive sulphides and, with the exception of Guild6, have stated or implied a fairly close genetic relationship between ore deposition and the processes of seafloor spreading and subduction.
The nature of this relationship is, however, by no means clear and I suggest here that it may be very tenuous. Access through your institution Buy or subscribe This is a preview of
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ADDITIONAL ACCESS OPTIONS: * Log in * Learn about institutional subscriptions * Read our FAQs * Contact customer support SIMILAR CONTENT BEING VIEWED BY OTHERS THE IMPLICATIONS OF CRUSTAL
ARCHITECTURE AND TRANSCRUSTAL UPFLOW ZONES ON THE METAL ENDOWMENT OF A WORLD-CLASS MINERAL DISTRICT Article Open access 29 August 2022 LINKS BETWEEN LARGE IGNEOUS PROVINCE VOLCANISM AND
SUBDUCTED IRON FORMATIONS Article 25 May 2023 GIANT IMPACTS AND THE ORIGIN AND EVOLUTION OF CONTINENTS Article 10 August 2022 REFERENCES * Sawkins, F. J., _J. Geol._, 80, 377 (1972). Article
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Scholar * Guild, P. W., _Proc. twenty-fourth int. geol. Congr._, 4, 17 (1972). CAS Google Scholar * Sangster, D. F., _Can. geol. Surv._, Paper 72–22 (1972). * Craig, H., in _Hot Brines
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Google Scholar Download references AUTHOR INFORMATION AUTHORS AND AFFILIATIONS * Department of Geology, University of Tasmania, Hobart, Australia, 7005 M. SOLOMON Authors * M. SOLOMON
View author publications You can also search for this author inPubMed Google Scholar RIGHTS AND PERMISSIONS Reprints and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE SOLOMON, M. Massive
sulphides and plate tectonics. _Nature_ 249, 821–822 (1974). https://doi.org/10.1038/249821a0 Download citation * Received: 17 December 1973 * Revised: 09 April 1974 * Issue Date: 28 June
1974 * DOI: https://doi.org/10.1038/249821a0 SHARE THIS ARTICLE Anyone you share the following link with will be able to read this content: Get shareable link Sorry, a shareable link is not
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