A structural metamorphic study of the Broken Hill Block, NSW, Australia

The prograde pressure–temperature (P–T) path for the complexly polydeformed Proterozoic Broken Hill Block (Australia) has been reconstructed through detailed structural analysis in conjunction with calculation of compositionally specific P–T pseudosections of pelitic rock units within a high‐tempera...

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Veröffentlicht in:	Journal of metamorphic geology 2005-10, Vol.23 (8), p.745-770
Hauptverfasser:	FORBES, C. J., BETTS, P. G., WEINBERG, R., BUICK, I. S.
Format:	Artikel
Sprache:	eng
Schlagworte:	Broken Hill Block Geology geothermal gradients high-temperature shear zones metamorphism prograde P-T path Rocks
Online-Zugang:	Volltext
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