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Manning Orocline

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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 December 2016
Lithosphere (2016) 8 (6): 684–698.
... with recently published structural, paleomagnetic, and geochronological constraints, our data suggest that counterclockwise rotations occurred between 285 and 275 Ma in the course of the formation of the southern segment of the New England oroclines (Manning orocline). The rotation incorporated both continental...
Journal Article
Journal: GSA Bulletin
Published: 01 September 1969
GSA Bulletin (1969) 80 (9): 1797–1800.
... of tectonic transport to the much larger Cordilleran Orocline proposed by Carey (1958). The presence of the folds in central Idaho supports Carey's concept of translational rotation of the northwestern United States in response to deep crustal movements. 8 1 1969 Copyright © 1969, The Geological...
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.238.01.22
EISBN: 9781862394865
.... Geeve et al. (2002) recently argued on stratigraphic and geological grounds for a comparable age, mid-Namurian to latest Carboniferous, for rotation of the Manning Orocline (Fig. 1 ) as concluded by them from their palaeomagnetic data of the southern Tamworth Belt (Terrane). Korsch and coworkers...
FIGURES | View All (11)
Journal Article
Journal: GSA Bulletin
Published: 01 July 2007
GSA Bulletin (2007) 119 (7-8): 882–896.
...Alexander C. Robinson; An Yin; Craig E. Manning; T. Mark Harrison; Shuan-Hong Zhang; Xiao-Feng Wang Abstract Detailed field mapping, geochronologic and thermochronologic analyses, and petrologic investigations conducted along the southern segment of the late Cenozoic Kongur Shan extensional system...
FIGURES | View All (12)
Journal Article
Journal: GSA Bulletin
Published: 01 July 2004
GSA Bulletin (2004) 116 (7-8): 953–973.
...Alexander C. Robinson; An Yin; Craig E. Manning; T. Mark Harrison; Shuan-Hong Zhang; Xiao-Feng Wang Abstract The late Cenozoic Kongur Shan extensional system lies along the northeastern margin of the Pamir at the western end of the Himalayan-Tibetan orogen, accommodating east-west extension...
FIGURES | View All (22)
Journal Article
Journal: GSA Bulletin
Published: 01 July 2015
GSA Bulletin (2015) 127 (7-8): 1052–1063.
... ; Rosenbaum, 2012 ). The oroclinal structure is composed of a Z-shaped northern segment (Texas and Coffs Harbour oroclines; Korsch and Harrington, 1987 ; Lennox and Flood, 1997 ; Li et al., 2012 ; Murray et al., 1987 ; Offler and Foster, 2008 ), and a more controversial S-shaped southern segment (Manning...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2017
GSA Bulletin (2017) 129 (5-6): 547–569.
... continuity and the tectonic nature of this shear zone are still poorly understood, but its development has supposedly made a significant impact on the architecture of the western Central Asian orogenic belt and the formation of the Kazakhstan orocline. Here, we provide new insight into the evolution...
FIGURES | View All (13)
Journal Article
Journal: Geosphere
Published: 09 April 2019
Geosphere (2019) 15 (3): 856–881.
...Peter J. Haproff; Andrew V. Zuza; An Yin; T. Mark Harrison; Craig E. Manning; Chandra S. Dubey; Lin Ding; Chen Wu; Jianlin Chen Abstract The Cenozoic India-Asia collision generated both the east-trending Himalayan orogen and the north-trending Eastern and Western Flanking Belts located along...
FIGURES | View All (20)
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 16 May 2019
Lithosphere (2019) 11 (4): 560–580.
... not primarily accommodated along discrete, large displacement faults (>400 km) faults. Instead, oroclinal bending of the northern Pamir, and dextral shear along the Pamir margins, may be largely responsible for the northward deflection of terranes. 11 06 2018 27 02 2019 02 04 2019...
FIGURES | View All (13)
Journal Article
Journal: Geosphere
Published: 01 April 2011
Geosphere (2011) 7 (2): 582–596.
... positioning system geodetic velocities indicates >3 cm yr −1 of arc-parallel extension of the Himalaya. Several models have sought to explain Himalayan arc-parallel extension and strike-slip faulting, including lateral extrusion of Tibet, oroclinal bending of the Himalaya, radial spreading of Tibet...
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Journal Article
Published: 01 March 2003
Journal of the Geological Society (2003) 160 (2): 209–218.
..., the blocks limited by wrench-faults rotated anticlockwise in bookshelf manner. The data presented rule out the existing model of oroclinal bending of the Rhenohercynian zone at the eastern termination of the Variscan belt. Fig. 2.  Location of the sampling sites. Stereographic projections...
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Journal Article
Published: 07 February 2020
Bulletin de la Société Géologique de France (2020) 191 (1): 2.
... in an apparent orocline. Bending was associated with transpressional crustal thickening and high-grade metamorphism ( Pitra et al. , 2010 ) in the southeastern Kénéma-Man domain, while voluminous magmatism and sinistral transpression took place along the northern flank of the bend ( Égal et al. , 2002...
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Image
The Tasmanides of eastern Australia with sample localities referred to in t...
Published: 14 July 2016
; lesz, Louth-Eumarra Shear Zone (north boundary); LLK, Loch Lilly-Kars Belt; M, Manning Orocline; MRV, Mount Read Volcanics; MZ, Melbourne Zone; MWFZ, Mount Wellington Fault Zone; N, Nambucca basin; NSW, New South Wales; op, Olepoloko Fault; PMFS, Peel Manning Fault System Qld, Queensland; SA, South
Image
East Australia and the southern New England orogeny. (A) Tectonic map of ea...
Published: 01 July 2015
oroclinal structure. The locations of the Nambucca block and sampling sites are shown. Abbreviations: Dy—Dyamberin block, HPv—Halls Peak volcanics, Ma—Manning block; QLD—Queensland; NWS—New South Wales.
Image
Schematic cross sections of the New England region: (A) 300 Ma, showing com...
Published: 01 November 2011
Figure 7. Schematic cross sections of the New England region: (A) 300 Ma, showing compressive deformation and crustal thickening of pre-Permian arc-trench system and termination of magmatism along western arc. Arrow symbols along Peel-Manning fault system (PMFS) indicate sinistral strike-slip
Journal Article
Journal: GSA Bulletin
Published: 01 November 2011
GSA Bulletin (2011) 123 (11-12): 2240–2255.
...Figure 7. Schematic cross sections of the New England region: (A) 300 Ma, showing compressive deformation and crustal thickening of pre-Permian arc-trench system and termination of magmatism along western arc. Arrow symbols along Peel-Manning fault system (PMFS) indicate sinistral strike-slip...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2010
GSA Bulletin (2010) 122 (1-2): 145–161.
... the south-dipping Main Pamir Thrust and associated faults to the south (e.g., Burt-man and Molnar, 1993 ), it is not presently clear how deformation is absorbed at the southeastern end of the fault, in the Western Kunlun Shan. Although the fault system appears to link with the north-directed Hotan fold...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.246.01.02
EISBN: 9781862394940
... is not clear-cut everywhere and further work may result in the two cycles being combined. Fig. 13. Map of relations in the New England Orogen: ( a ) deformed state geology (note the triple orocline); (b) undeformed New England Orogen, after Cawood & Leitch (1985) . Late Carboniferous-Early Permian...
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Journal Article
Journal: Geology
Published: 14 June 2021
Geology (2021)
... (ChRMs) are 350 °C to 580 °C, which are characterized by also been recognized in the Man-Leo Shield isolated typically from 535 °C to 580 °C, con- antipodal, north-down and south-up directions in the southern WAC, such as the northeast- sistently showing northwest-up and southeast- (Fig. 2D). One dike...
Journal Article
Published: 04 June 2021
Journal of the Geological Society (2021) jgs2020-121.
... of the study area ( Fig. 2 ), is composed of a mixture of oceanic and continental fragments and has a long history of island-arc volcanism spanning the Cambrian–Silurian ( Degtyarev et al. 2015 ). The other, mostly short-lived arcs (e.g. Selety, Baidaulet–Akbastau arcs) of the Kazakhstan Orocline also formed...
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