Structure-Forming Peculiarities at the Early Stage of Antarctic–Australia Separation Based on Physical Modeling

• Published in: Izvestiya. Physics of the solid earth Vol. 55; no. 2; pp. 256 - 269
• Main Authors: Dubinin, E. P., Leitchenkov, G. L., Grokholsky, A. L., Sergeeva, V. M., Agranov, G. D.
• Format: Journal Article
• Language: English
• Published: Moscow Pleiades Publishing 01.03.2019; Springer Nature B.V
• Subjects: Earth; Earth and Environmental Science; Earth crust; Earth Sciences; Geophysics/Geodesy; Lithosphere; Modelling; Morphology; Ocean floor; Ocean models; Oceanic crust; Profiles; Ridges; Rifting; Seismic analysis; Seismic profiles; Spreading; Spreading centres; Australia; crustal structure; ocean; physical modeling; ultraslow sea-floor spreading; Mawson Sea; passive margin; Antarctic
• DOI: 10.1134/S1069351319020022
• ISSN: 1069-3513

The peculiarities of the formation of the structure of the Earth’s crust in the Australian–Antarctic basin during the early break-up between Australia and Antarctica are considered. The study period encompasses long-lasting rifting (~160–80 Ma), ultraslow spreading (~80–45 Ma) with the formation of the proto-oceanic mainly ultrabasic crust, spreading (~45–40 Ma), and stationary sea-floor spreading with intermediate velocities (after 40 Ma). The various stages of the oceanic opening clearly manifest themselves by the change in the basement morphology (the top of the second oceanic layer) on the seismic profiles. Physical modeling has made it possible to reveal the peculiarities of the surface morphology of the oceanic (magmatic) crust which developed in the conditions of the transition from ultraslow to slow and intermediate spreading. Our experiments established that (1) the presence of a stronger block in the pre-breakup model lithosphere in the pathway of the propagating rift faults can significantly affect the geometry of the spreading axis in its vicinity and lead to the development of transverse structures and a highly rugged relief; (2) under the conditions of ultraslow spreading, numerous ridge jumps occur; (3) the temporary cessation of the sea-floor spreading leads to the development of linear high-amplitude rises which in the natural conditions correspond to amagmatic ridges.