Matches in SemOpenAlex for { <https://semopenalex.org/work/W2102100058> ?p ?o ?g. }
- W2102100058 endingPage "2799" @default.
- W2102100058 startingPage "2771" @default.
- W2102100058 abstract "A re-evaluation of existing onshore and offshore gravity, magnetic, seismic reflection, and well data from the Australo-Antarctic margins suggests that magmatism and along-strike lithospheric heterogeneities have influenced the localization of initial rifting. The 3D crustal architecture of the Australian and Antarctic margins, which formed during multiple rifting episodes spanning ~80 My, reveal local asymmetries along strike. Rift structures from the broad, late Jurassic (165-145 Ma) rift zone are partially overprinted by a narrower, mid-to-late Cretaceous rift zone ~100 Ma, which evolved in highly extended crust. This late-stage rift zone is located within a region of heterogeneous crust with faults that cut late syn-rift strata, interpreted as a continent ocean transition zone. This late stage transitional rift is populated by seismically identified rift-parallel basement highs and intra-crustal bodies with corresponding positive Bouguer gravity and magnetic anomalies. These undrilled features can be interpreted as exposures of exhumed mantle rocks, lower crustal rocks and/or as discrete magmatic bodies. Our results suggest that strain across an initially broad Australo-Antarctic rift system (165-145 Ma) migrated to a narrow rift zone with some magmatism at 100-83 Ma. Breakup did not occur until ~53 Ma within the eastern Bight-Wilkes and Otway-Adelie margin sectors, suggesting a west to east propagation of seafloor spreading. The prolonged eastwards propagation of seafloor spreading processes and the increased asymmetry of the Australian-Antarctic margins coincides with a change from rift-perpendicular to oblique rifting processes, which in turn coincide with along- strike variations in cratonic to Palaeozoic lithosphere." @default.
- W2102100058 created "2016-06-24" @default.
- W2102100058 creator A5008365801 @default.
- W2102100058 creator A5042658053 @default.
- W2102100058 creator A5074621972 @default.
- W2102100058 creator A5084234210 @default.
- W2102100058 creator A5085722785 @default.
- W2102100058 date "2013-08-01" @default.
- W2102100058 modified "2023-10-09" @default.
- W2102100058 title "The spatial and temporal evolution of strain during the separation of Australia and Antarctica" @default.
- W2102100058 cites W1499747575 @default.
- W2102100058 cites W1519872695 @default.
- W2102100058 cites W1548890681 @default.
- W2102100058 cites W1586206811 @default.
- W2102100058 cites W1586341875 @default.
- W2102100058 cites W1586873887 @default.
- W2102100058 cites W1588980084 @default.
- W2102100058 cites W1608450344 @default.
- W2102100058 cites W1810418208 @default.
- W2102100058 cites W1860912165 @default.
- W2102100058 cites W1862013975 @default.
- W2102100058 cites W1940667170 @default.
- W2102100058 cites W1968534064 @default.
- W2102100058 cites W1969432053 @default.
- W2102100058 cites W1970041780 @default.
- W2102100058 cites W1974349230 @default.
- W2102100058 cites W1974850963 @default.
- W2102100058 cites W1974927257 @default.
- W2102100058 cites W1976449296 @default.
- W2102100058 cites W1976486629 @default.
- W2102100058 cites W1976549999 @default.
- W2102100058 cites W1977728452 @default.
- W2102100058 cites W1977809937 @default.
- W2102100058 cites W1984550449 @default.
- W2102100058 cites W1986609283 @default.
- W2102100058 cites W1989072731 @default.
- W2102100058 cites W1990919062 @default.
- W2102100058 cites W1993952923 @default.
- W2102100058 cites W1996341887 @default.
- W2102100058 cites W1997235146 @default.
- W2102100058 cites W2005846638 @default.
- W2102100058 cites W2007889801 @default.
- W2102100058 cites W2008875140 @default.
- W2102100058 cites W2010272491 @default.
- W2102100058 cites W2010986993 @default.
- W2102100058 cites W2011941260 @default.
- W2102100058 cites W2012306113 @default.
- W2102100058 cites W2012589147 @default.
- W2102100058 cites W2014206039 @default.
- W2102100058 cites W2017893316 @default.
- W2102100058 cites W2021196398 @default.
- W2102100058 cites W2030727148 @default.
- W2102100058 cites W2033996862 @default.
- W2102100058 cites W2034753142 @default.
- W2102100058 cites W2039290573 @default.
- W2102100058 cites W2040274885 @default.
- W2102100058 cites W2042806383 @default.
- W2102100058 cites W2046640225 @default.
- W2102100058 cites W2047172161 @default.
- W2102100058 cites W2053979714 @default.
- W2102100058 cites W2057805069 @default.
- W2102100058 cites W2061967453 @default.
- W2102100058 cites W2064119724 @default.
- W2102100058 cites W2064551732 @default.
- W2102100058 cites W2067550860 @default.
- W2102100058 cites W2072805282 @default.
- W2102100058 cites W2072972330 @default.
- W2102100058 cites W2073705357 @default.
- W2102100058 cites W2074344573 @default.
- W2102100058 cites W2075372263 @default.
- W2102100058 cites W2075772841 @default.
- W2102100058 cites W2076588934 @default.
- W2102100058 cites W2077028606 @default.
- W2102100058 cites W2078992461 @default.
- W2102100058 cites W2081696323 @default.
- W2102100058 cites W2083733990 @default.
- W2102100058 cites W2084208854 @default.
- W2102100058 cites W2084535484 @default.
- W2102100058 cites W2087990387 @default.
- W2102100058 cites W2090466505 @default.
- W2102100058 cites W2092115534 @default.
- W2102100058 cites W2094266796 @default.
- W2102100058 cites W2096967048 @default.
- W2102100058 cites W2099130556 @default.
- W2102100058 cites W2102649721 @default.
- W2102100058 cites W2104252941 @default.
- W2102100058 cites W2104315271 @default.
- W2102100058 cites W2104382116 @default.
- W2102100058 cites W2106157587 @default.
- W2102100058 cites W2114458004 @default.
- W2102100058 cites W2115314373 @default.
- W2102100058 cites W2119666905 @default.
- W2102100058 cites W2122437722 @default.
- W2102100058 cites W2123786602 @default.
- W2102100058 cites W2123844571 @default.
- W2102100058 cites W2127878314 @default.
- W2102100058 cites W2129244095 @default.
- W2102100058 cites W2132706046 @default.