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• W2793289314 endingPage "333" @default.
• W2793289314 startingPage "303" @default.
• W2793289314 abstract "Ordovician rocks of the Lachlan Orogen consist of two major associations, mafic to intermediate volcanic and volcaniclastic rocks (Macquarie Arc), which aerially comprise several north–south-trending belts, and the quartz-rich turbidite succession. Relationships between these associations are integral to resolving their tectonic settings and opinions range between contacts being major thrusts, combinations of various types of faults, and stratigraphic contacts with structural complications. Stratigraphic contacts between these associations are found with volcaniclastic-dominant units overlying quartz-turbidite units along the eastern boundary of the eastern volcanic belt and along the southern boundary of the central volcanic belt. Mixing between these major associations is limited and reflects waning quartzose turbidite deposition along a gently sloping sea floor not penetrating steeper volcaniclastic aprons that were developing around the growing volcanic centres formed during late Middle Ordovician to early Silurian Macquarie Arc igneous activity. An island arc setting has been most widely supported for the Macquarie Arc, but the identification and polarity of the associated subduction zone remain a contentious issue particularly for the Early Ordovician phase of igneous activity. The Macquarie Arc initiated within a Cambrian backarc formed by sea-floor spreading behind a boninitic island arc and presumably reflects a renewed response to regional convergence as subduction ceased along the Ross–Delamerian convergent boundary at the East Gondwana continental margin. An extensional episode accompanied initiation of the late Middle Ordovician expansion in island arc development. A SSE-dipping subduction zone is considered to have formed the Macquarie Arc and underwent anticlockwise rotation about an Euler pole at the western termination of the island arc. This resulted in widespread deformation west of the Macquarie Arc in the Benambran Orogeny and development of subduction along the eastern margin of the orogenic belt." @default.
• W2793289314 created "2018-03-29" @default.
• W2793289314 creator A5056310369 @default.
• W2793289314 creator A5085526990 @default.
• W2793289314 date "2018-02-11" @default.
• W2793289314 modified "2023-10-01" @default.
• W2793289314 title "Ordovician Macquarie Arc and turbidite fan relationships, Lachlan Orogen, southeastern Australia: stratigraphic and tectonic problems" @default.
• W2793289314 cites W1211775810 @default.
• W2793289314 cites W1484496509 @default.
• W2793289314 cites W1519544234 @default.
• W2793289314 cites W1676343945 @default.
• W2793289314 cites W1847880314 @default.
• W2793289314 cites W1967034853 @default.
• W2793289314 cites W1967145581 @default.
• W2793289314 cites W1971566844 @default.
• W2793289314 cites W1977326478 @default.
• W2793289314 cites W1978260174 @default.
• W2793289314 cites W1981354663 @default.
• W2793289314 cites W1981511174 @default.
• W2793289314 cites W1985192544 @default.
• W2793289314 cites W1986183163 @default.
• W2793289314 cites W1987197182 @default.
• W2793289314 cites W1988010306 @default.
• W2793289314 cites W1991946360 @default.
• W2793289314 cites W1992161258 @default.
• W2793289314 cites W1995126881 @default.
• W2793289314 cites W1995997068 @default.
• W2793289314 cites W1996085836 @default.
• W2793289314 cites W1996146493 @default.
• W2793289314 cites W2002819080 @default.
• W2793289314 cites W2004974805 @default.
• W2793289314 cites W2010525280 @default.
• W2793289314 cites W2010754180 @default.
• W2793289314 cites W2016103953 @default.
• W2793289314 cites W2017125487 @default.
• W2793289314 cites W2017512729 @default.
• W2793289314 cites W2017899354 @default.
• W2793289314 cites W2018035731 @default.
• W2793289314 cites W2018469218 @default.
• W2793289314 cites W2021357231 @default.
• W2793289314 cites W2025630980 @default.
• W2793289314 cites W2026665741 @default.
• W2793289314 cites W2027239119 @default.
• W2793289314 cites W2028904790 @default.
• W2793289314 cites W2030313209 @default.
• W2793289314 cites W2034335513 @default.
• W2793289314 cites W2034388633 @default.
• W2793289314 cites W2035552411 @default.
• W2793289314 cites W2035847196 @default.
• W2793289314 cites W2037254380 @default.
• W2793289314 cites W2045149304 @default.
• W2793289314 cites W2045351761 @default.
• W2793289314 cites W2047152024 @default.
• W2793289314 cites W2047519592 @default.
• W2793289314 cites W2050925751 @default.
• W2793289314 cites W2052639207 @default.
• W2793289314 cites W2053240935 @default.
• W2793289314 cites W2054084580 @default.
• W2793289314 cites W2059100058 @default.
• W2793289314 cites W2060216964 @default.
• W2793289314 cites W2061401188 @default.
• W2793289314 cites W2061950389 @default.
• W2793289314 cites W2065636104 @default.
• W2793289314 cites W2068365898 @default.
• W2793289314 cites W2069641153 @default.
• W2793289314 cites W2073005616 @default.
• W2793289314 cites W2073379307 @default.
• W2793289314 cites W2074041376 @default.
• W2793289314 cites W2075056148 @default.
• W2793289314 cites W2075261279 @default.
• W2793289314 cites W2077345865 @default.
• W2793289314 cites W2077567954 @default.
• W2793289314 cites W2079273023 @default.
• W2793289314 cites W2080991291 @default.
• W2793289314 cites W2081366650 @default.
• W2793289314 cites W2082717368 @default.
• W2793289314 cites W2087132989 @default.
• W2793289314 cites W2093394213 @default.
• W2793289314 cites W2093688302 @default.
• W2793289314 cites W2094297079 @default.
• W2793289314 cites W2095616085 @default.
• W2793289314 cites W2096858978 @default.
• W2793289314 cites W2111084982 @default.
• W2793289314 cites W2111094916 @default.
• W2793289314 cites W2112921184 @default.
• W2793289314 cites W2128683650 @default.
• W2793289314 cites W2129347742 @default.
• W2793289314 cites W2132255538 @default.
• W2793289314 cites W2132328282 @default.
• W2793289314 cites W2133751738 @default.
• W2793289314 cites W2135004896 @default.
• W2793289314 cites W2138008961 @default.
• W2793289314 cites W2141969284 @default.
• W2793289314 cites W2143316012 @default.
• W2793289314 cites W2157629521 @default.
• W2793289314 cites W2161188118 @default.
• W2793289314 cites W2163182510 @default.
• W2793289314 cites W2171933155 @default.

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