FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2999402583> ?p ?o ?g. }

• W2999402583 endingPage "1679" @default.
• W2999402583 startingPage "1653" @default.
• W2999402583 abstract "Abstract. Australian terranes concealed beneath Mesozoic cover record complex Precambrian tectonic histories involving a successive development of several Proterozoic to Palaeozoic orogenic systems. This study presents an integrated approach combining K–Ar, 40Ar–39Ar, and Rb–Sr geochronologies of Precambrian authigenic illites from the recently discovered Millungera Basin in north-central Australia. Brittle deformation and repeated fault activity are evident from the sampled cores and their microstructures, probably associated with the large-scale faults inferred from interpretations of seismic surveys. Rb–Sr isochron, 40Ar–39Ar total gas, and K–Ar ages are largely consistent in indicating late Mesoproterozoic and early Proterozoic episodes (∼1115±26, ∼ 1070±25, ∼1040±24, ∼1000±23, and ∼905±21 Ma) of active tectonics in north-central Australia. K–Ar results show that illites from fault gouges and authigenic matrix illites in undeformed adjacent sandstones precipitated contemporaneously, indicating that advection of tectonically mobilized fluids extended into the undeformed wall rocks above or below the fracture and shear (fault gouge) zones. Isotopic age data clearly indicate a Mesoproterozoic minimum age for the Millungera Basin and thus previously unrecorded late Mesoproterozoic–early Neoproterozoic tectonic events in north-central Australia. This study provides insight into the enigmatic time–space distribution of Precambrian tectonic zones in central Australia, which are responsible for the formation of a number of sedimentary basins with significant energy and mineral resources." @default.
• W2999402583 created "2020-01-23" @default.
• W2999402583 creator A5002568647 @default.
• W2999402583 creator A5027381312 @default.
• W2999402583 creator A5047310345 @default.
• W2999402583 creator A5063218145 @default.
• W2999402583 date "2020-09-04" @default.
• W2999402583 modified "2023-10-06" @default.
• W2999402583 title "Precambrian faulting episodes and insights into the tectonothermal history of north Australia: microstructural evidence and K–Ar, &lt;sup&gt;40&lt;/sup&gt;Ar–&lt;sup&gt;39&lt;/sup&gt;Ar, and Rb–Sr dating of syntectonic illite from the intracratonic Millungera Basin" @default.
• W2999402583 cites W1494654048 @default.
• W2999402583 cites W1495755285 @default.
• W2999402583 cites W1496646338 @default.
• W2999402583 cites W1512437395 @default.
• W2999402583 cites W1534009691 @default.
• W2999402583 cites W1539963764 @default.
• W2999402583 cites W1584732846 @default.
• W2999402583 cites W1595855307 @default.
• W2999402583 cites W1624627435 @default.
• W2999402583 cites W1965784458 @default.
• W2999402583 cites W1969095502 @default.
• W2999402583 cites W1970114125 @default.
• W2999402583 cites W1970565634 @default.
• W2999402583 cites W1974334364 @default.
• W2999402583 cites W1977367465 @default.
• W2999402583 cites W1980484856 @default.
• W2999402583 cites W1984401256 @default.
• W2999402583 cites W1985620741 @default.
• W2999402583 cites W1987744675 @default.
• W2999402583 cites W1989818713 @default.
• W2999402583 cites W1990296166 @default.
• W2999402583 cites W1999089294 @default.
• W2999402583 cites W2000629745 @default.
• W2999402583 cites W2002829985 @default.
• W2999402583 cites W2008171079 @default.
• W2999402583 cites W2008174066 @default.
• W2999402583 cites W2010857373 @default.
• W2999402583 cites W2011360218 @default.
• W2999402583 cites W2015056562 @default.
• W2999402583 cites W2016223358 @default.
• W2999402583 cites W2017965015 @default.
• W2999402583 cites W2021014922 @default.
• W2999402583 cites W2024466404 @default.
• W2999402583 cites W2027301078 @default.
• W2999402583 cites W2028163551 @default.
• W2999402583 cites W2028573058 @default.
• W2999402583 cites W2034876293 @default.
• W2999402583 cites W2035742753 @default.
• W2999402583 cites W2039106537 @default.
• W2999402583 cites W2041149139 @default.
• W2999402583 cites W2048240400 @default.
• W2999402583 cites W2048673457 @default.
• W2999402583 cites W2054561136 @default.
• W2999402583 cites W2059345481 @default.
• W2999402583 cites W2060467277 @default.
• W2999402583 cites W2061941219 @default.
• W2999402583 cites W2065633597 @default.
• W2999402583 cites W2067793536 @default.
• W2999402583 cites W2070010147 @default.
• W2999402583 cites W2081423026 @default.
• W2999402583 cites W2082297586 @default.
• W2999402583 cites W2085091769 @default.
• W2999402583 cites W2089786921 @default.
• W2999402583 cites W2093804092 @default.
• W2999402583 cites W2095519999 @default.
• W2999402583 cites W2096229147 @default.
• W2999402583 cites W2096347223 @default.
• W2999402583 cites W2101003439 @default.
• W2999402583 cites W2102866306 @default.
• W2999402583 cites W2103294084 @default.
• W2999402583 cites W2104139642 @default.
• W2999402583 cites W2104903026 @default.
• W2999402583 cites W2106590442 @default.
• W2999402583 cites W2109205858 @default.
• W2999402583 cites W2110481460 @default.
• W2999402583 cites W2111830933 @default.
• W2999402583 cites W2114034587 @default.
• W2999402583 cites W2115177642 @default.
• W2999402583 cites W2116276816 @default.
• W2999402583 cites W2119846469 @default.
• W2999402583 cites W2122711411 @default.
• W2999402583 cites W2124610955 @default.
• W2999402583 cites W2125958318 @default.
• W2999402583 cites W2142440353 @default.
• W2999402583 cites W2142644533 @default.
• W2999402583 cites W2145604970 @default.
• W2999402583 cites W2148460861 @default.
• W2999402583 cites W2151103298 @default.
• W2999402583 cites W2153263119 @default.
• W2999402583 cites W2155128667 @default.
• W2999402583 cites W2159795365 @default.
• W2999402583 cites W2161555731 @default.
• W2999402583 cites W2162868035 @default.
• W2999402583 cites W2168948293 @default.
• W2999402583 cites W2169991175 @default.
• W2999402583 cites W2267465575 @default.
• W2999402583 cites W2319597386 @default.
• W2999402583 cites W2327399076 @default.
• W2999402583 cites W244679186 @default.

• next