TY - JOUR
T1 - Retrograde schists of the amphibolite facies at broken hill, New South Wales
AU - Vernon, R. H.
AU - Ransom, D. M.
PY - 1971
Y1 - 1971
N2 - Aluminous, mafic, felsic, calcareous, and sulphide-rich rocks have been involved in localized deformation and retrograde metamorphism at Broken Hill, western New South Wales, where retrograde schist-zones intersect high-grade, regional metamorphic rocks of the lower granulite facies (or the amphibolite-granulite facies transition). Although technically retrograde, the schists contain mineral assemblages indicative of the lower amphibolite facies. The schist-zones were formed by local folding, apparently as part of the third stage of deformation in the Broken Hill area. Copyright.
AB - Aluminous, mafic, felsic, calcareous, and sulphide-rich rocks have been involved in localized deformation and retrograde metamorphism at Broken Hill, western New South Wales, where retrograde schist-zones intersect high-grade, regional metamorphic rocks of the lower granulite facies (or the amphibolite-granulite facies transition). Although technically retrograde, the schists contain mineral assemblages indicative of the lower amphibolite facies. The schist-zones were formed by local folding, apparently as part of the third stage of deformation in the Broken Hill area. Copyright.
UR - http://www.scopus.com/inward/record.url?scp=84954944404&partnerID=8YFLogxK
U2 - 10.1080/00167617108728766
DO - 10.1080/00167617108728766
M3 - Article
AN - SCOPUS:84954944404
SN - 0016-7614
VL - 18
SP - 267
EP - 278
JO - Journal of the Geological Society of Australia
JF - Journal of the Geological Society of Australia
IS - 3
ER -