1998
DOI: 10.1080/08120099808728398
|View full text |Cite
|
Sign up to set email alerts
|

Structural development of the Soldiers Cap Group in the Eastern Fold Belt of the Mt Isa Inlier: A succession of horizontal and vertical deformation events and large‐scale shearing

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

1
8
0

Year Published

2000
2000
2023
2023

Publication Types

Select...
8

Relationship

0
8

Authors

Journals

citations
Cited by 26 publications
(9 citation statements)
references
References 42 publications
1
8
0
Order By: Relevance
“…A subhorizontal cleavage can also result from vertical shortening and horizontal extension during diapiric emplacement (Soula 1982), or gravity‐driven orogenic collapse. The latter has been proposed for the Eastern Fold Belt by Mares (1998). Our favoured interpretation for this late flat fabric is that it formed during localised vertical shortening throughout the central part of the Eastern Fold Belt (Figure 8e) during late orogenic emplacement of the Williams Batholith.…”
Section: Discussionmentioning
confidence: 53%
“…A subhorizontal cleavage can also result from vertical shortening and horizontal extension during diapiric emplacement (Soula 1982), or gravity‐driven orogenic collapse. The latter has been proposed for the Eastern Fold Belt by Mares (1998). Our favoured interpretation for this late flat fabric is that it formed during localised vertical shortening throughout the central part of the Eastern Fold Belt (Figure 8e) during late orogenic emplacement of the Williams Batholith.…”
Section: Discussionmentioning
confidence: 53%
“…locally rotated S 2 to shallower orientations. Differences in the tectonothermal history of the Eastern Fold Belt compared with the Western Fold Belt have been suggested by many workers (Holmes 1992;New 1993;Lally 1997;Adshead-Bell 1998;Mares 1998;Rubenach & Barker 1998;Rubenach & Lewthwaite 2002). Until recently, most workers correlated the metamorphic peak with D 2 , which they argued occurred ca 1550 -1530 Ma (Green 1975;Page 1983;Page & Bell 1986;Connors & Page 1995;Pollard & Perkins 1997;Oliver et al 1991Oliver et al , 1999Perkins et al 1999;Reinhardt 1992a, b;Rubenach 1992;Mark et al 1998;Rubenach & Barker 1998;Foster & Rubenach 2001).…”
Section: Mt Isa Inlier Metamorphism 169mentioning
confidence: 91%
“…Cordierite schists accompany albitites in the centre of the anticline, and locally albitisation is accompanied by gedrite + biotite + garnet + staurolite + aluminosilicate. There is abundant evidence, both in the Snake Creek Anticline and elsewhere in the Eastern Fold Belt, for further andalusite and staurolite growth subsequent to the metamorphic peak (Lally 1997;AdsheadBell 1998;Mares 1998;Lewthwaite 2000;Rubenach & Lewthwaite 2002). Much of this late porphyroblast growth could be related to the intrusion of the Williams Batholith.…”
Section: Reaction Rock Typementioning
confidence: 97%
See 1 more Smart Citation
“…Firstly, there are a number of well-documented, natural examples of simple shear fracture patterns that support the theoretical models of, for example, Coulomb (1773), Anderson (1951), Moody & Hill (1956) and Sibson (2000), and the experimental results of Riedel (1929), Cloos (1955) and Tchalenko (1970). The resulting Coulomb–Sibson model has been successfully applied to Au-bearing quartz lode and vein deposits (Mueller, Harris & Lungan, 1988; Vearncombe, 1998; Mares, 1998; Neumayr, Hagemann & Couture, 2000; Kolb & Hagemann, 2009; Dietrich et al . 2011), but is hampered in many cases by the lack of quantitative structural data, and the past tendency of mine geologists to record the strike but not the dip of planar surfaces.…”
Section: Discussionmentioning
confidence: 99%