1968
DOI: 10.1007/bf00207523
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The Broken Hill ore body, Australia

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Cited by 21 publications
(7 citation statements)
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“…Each sample contains some elements of the three main high‐grade schistosity surfaces previously recognized in the Broken Hill Domain (Hobbs, 1966; Hobbs et al. , 1968; Laing et al.…”
Section: Sample Locations and Descriptionsmentioning
confidence: 99%
See 1 more Smart Citation
“…Each sample contains some elements of the three main high‐grade schistosity surfaces previously recognized in the Broken Hill Domain (Hobbs, 1966; Hobbs et al. , 1968; Laing et al.…”
Section: Sample Locations and Descriptionsmentioning
confidence: 99%
“…Each sample contains some elements of the three main high-grade schistosity surfaces previously recognized in the Broken Hill Domain (Hobbs, 1966;Hobbs et al, 1968;Laing et al, 1978;Marjoribanks et al, Skirrow et al, 1999), showing the distribution of the Upper and Lower Willyama Supergroup metasediments. Metamorphic isograds are after Webb & Crooks (2005). 1980; Webb & Crooks, 2005).…”
Section: Sample Locations and Descriptionsmentioning
confidence: 99%
“…Some zones do show faulting and brecciation, but many of the fractures cut and displace the foliation of the retrograde schists, and the minerals of these zones are of very low grade, namely chlorite, clay minerals, * Other retrograde rocks not discussed here are the products of patchy, pseudomorphous retrograde metamorphisms outside the schist zones (see Vernon, 1969;Hobbs et al, 1968).…”
Section: General Structure Of the Retrograde Schist-zonesmentioning
confidence: 97%
“…However, descriptions of brecciation and slickensides suggest that Richards has not distinguished between true retrograde schist-zones (containing sulphide schists) and fault-zones (containing sulphide breccias) in which later fracturing has been operative. The sulphide schists are important in relating metamorphism and emplacement of sulphide rocks at Broken Hill, as discussed by Hobbs et al (1968).…”
Section: Calcareous Rocksmentioning
confidence: 99%
“…In the Broken Hill district of western New South Wales almandine-bearing metapelites are common and widespread throughout the Willyama Complex, which contains metamorphic materials produced by at least two metamorphic episodes (Browne, 1922;Binns, 1962;Hobbs et al, 1968;Vernon & Ransom, 1971). Petrographic and chemical studies have been carried out on the almandine-bearing metapelites produced by the first recognizable (prograde) metamorphic event within the Complex, the Willyama Metamorphism (Binns, 1964).…”
Section: Introductionmentioning
confidence: 98%