FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1161563488> ?p ?o ?g. }

• W1161563488 endingPage "267" @default.
• W1161563488 startingPage "257" @default.
• W1161563488 abstract "Analysis of the distribution patterns of Pb isotope data from mineralised samples using the plumbotectonic model of Carr et al. (1995), which invokes mixing between crustal and mantle reservoirs, indicates systematic spatial patterns that reflect major metallogenic and tectonic boundaries in the Paleozoic Lachlan and Delamerian orogens in New South Wales and Victoria, Australia. This distribution pattern accurately maps the boundary between the Central and Eastern Lachlan subprovinces. The Central Lachlan Subprovince is characterised by Pb isotope characteristics with a strong crustal signature, whereas the Eastern Lachlan Subprovince is characterised by variable crustal and mantle signatures. The Macquarie Volcanic Province is dominated by Pb with a mantle signature: known porphyry Cu–Au and high sulphidation epithermal Au–Cu deposits in the province are associated with a zone characterised by the strongest mantle signatures. In contrast, granite-related Sn deposits in the Central Lachlan Subprovince are characterised by the strongest crustal signatures. The Pb isotope patterns are broadly similar to Nd isotope model age patterns derived from felsic magmatic rocks, although a lower density of Nd isotope data locations makes direct comparison difficult. The two reservoirs identified by Carr et al. (1995) do not appear to be isotopically linked: the crustal source was not formed via extraction from the mantle source. Rather, the two reservoirs formed separately. The mantle reservoir may have been sourced from a subducting proto-Pacific plate, whereas the crustal reservoir is most likely to be extended Australian crust. The data allow the possibility that the proto-Pacific mantle source was isotopically linked to the western Tasmanian crustal source. Comparison of Pb isotope data from the Girilambone district, Central Lachlan Subprovince, (e.g., Tritton and Avoca Tank Cu deposits) with those from the Cobar Cu–Au–Zn–Pb district, Eastern Lachlan Subprovince, in north central New South Wales indicates a less radiogenic signature, and probably older age, for deposits in the Girilambone district. Hence, a syngenetic volcanic-associated massive sulphide origin for these deposits is preferred over a syn-tectonic origin. The data are also consistent with formation of the Girilambone deposits in a back-arc basin inboard from the earliest phase of the Macquarie Volcanic Province." @default.
• W1161563488 created "2016-06-24" @default.
• W1161563488 creator A5006352389 @default.
• W1161563488 creator A5013965255 @default.
• W1161563488 creator A5028793009 @default.
• W1161563488 creator A5031089224 @default.
• W1161563488 creator A5035034660 @default.
• W1161563488 creator A5035457098 @default.
• W1161563488 creator A5057423083 @default.
• W1161563488 creator A5074885593 @default.
• W1161563488 date "2016-07-01" @default.
• W1161563488 modified "2023-10-06" @default.
• W1161563488 title "Metallogenesis and geodynamics of the Lachlan Orogen: New (and old) insights from spatial and temporal variations in lead isotopes" @default.
• W1161563488 cites W1420785588 @default.
• W1161563488 cites W1484496509 @default.
• W1161563488 cites W1758925611 @default.
• W1161563488 cites W1993737629 @default.
• W1161563488 cites W2004352894 @default.
• W1161563488 cites W2014002279 @default.
• W1161563488 cites W2015648139 @default.
• W1161563488 cites W2030313209 @default.
• W1161563488 cites W2037866865 @default.
• W1161563488 cites W2044297606 @default.
• W1161563488 cites W2054361306 @default.
• W1161563488 cites W2058203412 @default.
• W1161563488 cites W2058915769 @default.
• W1161563488 cites W2059100058 @default.
• W1161563488 cites W2061401188 @default.
• W1161563488 cites W2073671350 @default.
• W1161563488 cites W2079273023 @default.
• W1161563488 cites W2109946900 @default.
• W1161563488 cites W2111094916 @default.
• W1161563488 cites W2112921184 @default.
• W1161563488 cites W2114276383 @default.
• W1161563488 cites W2135588124 @default.
• W1161563488 cites W2146357803 @default.
• W1161563488 cites W2148847797 @default.
• W1161563488 cites W2152843609 @default.
• W1161563488 cites W2171933155 @default.
• W1161563488 cites W2334542214 @default.
• W1161563488 cites W4214634076 @default.
• W1161563488 doi "https://doi.org/10.1016/j.oregeorev.2015.07.005" @default.
• W1161563488 hasPublicationYear "2016" @default.
• W1161563488 type Work @default.
• W1161563488 sameAs 1161563488 @default.
• W1161563488 citedByCount "17" @default.
• W1161563488 countsByYear W11615634882015 @default.
• W1161563488 countsByYear W11615634882016 @default.
• W1161563488 countsByYear W11615634882017 @default.
• W1161563488 countsByYear W11615634882021 @default.
• W1161563488 countsByYear W11615634882022 @default.
• W1161563488 countsByYear W11615634882023 @default.
• W1161563488 crossrefType "journal-article" @default.
• W1161563488 hasAuthorship W1161563488A5006352389 @default.
• W1161563488 hasAuthorship W1161563488A5013965255 @default.
• W1161563488 hasAuthorship W1161563488A5028793009 @default.
• W1161563488 hasAuthorship W1161563488A5031089224 @default.
• W1161563488 hasAuthorship W1161563488A5035034660 @default.
• W1161563488 hasAuthorship W1161563488A5035457098 @default.
• W1161563488 hasAuthorship W1161563488A5057423083 @default.
• W1161563488 hasAuthorship W1161563488A5074885593 @default.
• W1161563488 hasConcept C121332964 @default.
• W1161563488 hasConcept C127313418 @default.
• W1161563488 hasConcept C127413603 @default.
• W1161563488 hasConcept C136752280 @default.
• W1161563488 hasConcept C141646446 @default.
• W1161563488 hasConcept C146458902 @default.
• W1161563488 hasConcept C151730666 @default.
• W1161563488 hasConcept C154912208 @default.
• W1161563488 hasConcept C164304813 @default.
• W1161563488 hasConcept C17409809 @default.
• W1161563488 hasConcept C2776698055 @default.
• W1161563488 hasConcept C53942344 @default.
• W1161563488 hasConcept C62520636 @default.
• W1161563488 hasConcept C67236022 @default.
• W1161563488 hasConcept C77928131 @default.
• W1161563488 hasConcept C78519656 @default.
• W1161563488 hasConceptScore W1161563488C121332964 @default.
• W1161563488 hasConceptScore W1161563488C127313418 @default.
• W1161563488 hasConceptScore W1161563488C127413603 @default.
• W1161563488 hasConceptScore W1161563488C136752280 @default.
• W1161563488 hasConceptScore W1161563488C141646446 @default.
• W1161563488 hasConceptScore W1161563488C146458902 @default.
• W1161563488 hasConceptScore W1161563488C151730666 @default.
• W1161563488 hasConceptScore W1161563488C154912208 @default.
• W1161563488 hasConceptScore W1161563488C164304813 @default.
• W1161563488 hasConceptScore W1161563488C17409809 @default.
• W1161563488 hasConceptScore W1161563488C2776698055 @default.
• W1161563488 hasConceptScore W1161563488C53942344 @default.
• W1161563488 hasConceptScore W1161563488C62520636 @default.
• W1161563488 hasConceptScore W1161563488C67236022 @default.
• W1161563488 hasConceptScore W1161563488C77928131 @default.
• W1161563488 hasConceptScore W1161563488C78519656 @default.
• W1161563488 hasLocation W11615634881 @default.
• W1161563488 hasOpenAccess W1161563488 @default.
• W1161563488 hasPrimaryLocation W11615634881 @default.
• W1161563488 hasRelatedWork W1979938218 @default.
• W1161563488 hasRelatedWork W1984408471 @default.

• next