Phase equilibrium modelling of Palaeoproterozoic ultrahigh-temperature sapphirine granulite from the Inner Mongolia Suture Zone, North China Craton: implications for counterclockwise P-T path

Shimizu, H.; Tsunogae, T.; Santosh, M.; Liu, S.; Li, J.

doi:10.1002/gj.2504

Phase equilibrium modelling of Palaeoproterozoic ultrahigh-temperature sapphirine granulite from the Inner Mongolia Suture Zone, North China Craton: implications for counterclockwise P-T path

Date

2013

Authors

Shimizu, H.

Tsunogae, T.

Santosh, M.

Liu, S.

Li, J.

Editors

Santosh, M.
Somerville, I.

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Journal article

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Geological Journal, 2013; 48(5):456-466

Statement of Responsibility

Hisako Shimizu, oshiaki Tsunogae, M. Santosh, S. J. Liu, J. H. Li

DOI

10.1002/gj.2504

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Abstract not available

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https://doi.org/10.1002/gj.2504

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http://hdl.handle.net/2440/104346

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Phase equilibrium modelling of Palaeoproterozoic ultrahigh-temperature sapphirine granulite from the Inner Mongolia Suture Zone, North China Craton: implications for counterclockwise P-T path

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