Title:
Signature of Griffith phase in (Tb1-xCex)MnO3

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dc.contributor.authorAbhishek Kumar
dc.contributor.authorG.D. Dwivedi
dc.contributor.authorA. Singh
dc.contributor.authorR. Singh
dc.contributor.authorK.K. Shukla
dc.contributor.authorH.D. Yang
dc.contributor.authorA.K. Ghosh
dc.contributor.authorSandip Chatterjee
dc.date.accessioned2026-02-07T08:16:57Z
dc.date.issued2016
dc.description.abstractGriffith phase phenomena is attributed to existence of FM (ferromagnetic) cluster in AFM (antiferromagnetic) ordering which usually occurs in ferromagnetic and antiferromagnetic bilayers or multilayers. In (Tb1-xCex)MnO3 evolution of Griffith phase have been observed. The observed Griffith phase might be due to the exchange interaction between Mn3+/Mn2+ states. © 2016 Author(s).
dc.identifier.doi10.1063/1.4948166
dc.identifier.isbn978-073541378-8
dc.identifier.issn0094243X
dc.identifier.urihttps://doi.org/10.1063/1.4948166
dc.identifier.urihttps://dl.bhu.ac.in/bhuir/handle/123456789/29180
dc.publisherAmerican Institute of Physics Inc.
dc.subjectGriffith Phase
dc.subjectMultiferroics
dc.titleSignature of Griffith phase in (Tb1-xCex)MnO3
dc.typePublication
dspace.entity.typeConference paper

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