Origin of the Griffiths phase and correlation with the magnetic phase transition in the nanocrystalline manganite <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:msub><mml:mi>La</mml:mi><mml:mrow><mml:mn>0.4</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mi>Ca</mml:mi><mml:mrow><mml:mn>0.5</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mi>Sr</mml:mi><mml:mrow><mml:mn>0.5</mml:mn></mml:mrow></mml:msub><mml:mo>)</mml:mo></mml:mrow><mml:mrow><mml:mn>0.6</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mi>MnO</mml:mi><mml:mn>3</mml:mn></mml:msub></mml:mrow></mml:math>-Reference-Cited by-同舟云学术

Origin of the Griffiths phase and correlation with the magnetic phase transition in the nanocrystalline manganite La0.4(Ca0.5Sr0.5)0.6MnO3

Author:

Saha Suvayan^ORCID,Dutta Apurba,Gupta Shuvankar,Bandyopadhyay Sudipta^ORCID,Das I.

Funder

Department of Atomic Energy, Government of India

Department of Science and Technology, Ministry of Science and Technology

Publisher

American Physical Society (APS)

Link

Reference101 articles.

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