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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Angola (1)
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North Africa
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Egypt (1)
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Southern Africa
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West Africa
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Asia
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North America
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commodities
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geologic age
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Cenozoic
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upper Miocene
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Mesozoic
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Jurassic
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Paleozoic
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lower Paleozoic (1)
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upper Paleozoic (2)
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upper Precambrian
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igneous rocks
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plutonic rocks
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volcanic rocks
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metamorphic rocks
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sulfides (1)
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Primary terms
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Africa
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North Africa
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Southern Africa
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South Africa
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West Africa
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Antarctica
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deep seismic sounding
Passive imaging of collisional orogens: a review of a decade of geophysical studies in the Pyrénées
Fluid Saturation in the Lithosphere of the Altai-Sayan Folded Region according to Magnetotelluric Data
Forward modelling of Bouguer anomalies along a transect of the Southern Apennines and the Southern Tyrrhenian Sea (Italy)
Introduction to this special section: Remote sensing
Recent developments in imaging the earth’s crust by deep seismic data beneath the eastern parts of the Pannonian Basin
Deep seismic reflection data interpretation using balanced filtering method
Deep seismic structure of the boundary zone between the Eurasian and Okhotsk plates in eastern Russia ( along the 3DV deep seismic sounding profile )
Simultaneous Determination of Crustal Thickness and P Wavespeed by Virtual Deep Seismic Sounding (VDSS)
Deformable plate tectonics and regional geodynamic model of the Arctic region and Northeastern Asia
Retro-wedge foreland basin evolution along the ECORS line, eastern Pyrenees, France
Structure of the Earth’s crust in the northern part of the Barents–Kara region along the 4-AR DSS profile
Crustal stretching in the Scandinavian Caledonides as revealed by deep seismic data
Crustal structure in the Polar sector of the Urals folded system ( from DSS data )
Structure and evolution of the Earth’s crust in the region of junction of the Central Asian Fold Belt and the Siberian Platform: Skovorodino–Tommot profile
What drove continued continent-continent convergence after ocean closure? Insights from high-resolution seismic-reflection profiling across the Daba Shan in central China
Geodynamics and stress–strain patterns in different tectonic settings
Ground Truth Determinations of Detonation Sites of Peaceful Nuclear Explosions in the Sakha Republic (Yakutia), Russia
Variations in rift symmetry: cautionary examples from the Southern Rift System (Australia–Antarctica)
Abstract We present a synthesis based on the interpretation of two pairs of deep seismic reflection crustal sections within the Southern Rift System (SRS) separating Australia and Antarctica. One pair of sections is from the conjugate margins between the Great Australian Bight (GAB) and Wilkes Land, in the central sector of the SRS, which broke up in the Campanian. The second pair of conjugate sections is located approximately 400 km further east, between the Otway Basin and Terre Adélie, which probably broke up in Maastrichtian time. Interpretations are based on an integrated synthesis of deep multi-channel seismic, gravity and magnetic data, together with sparse sonobuoy and dredging information, and the conjugate sections are presented with the oceanic crust removed beyond the continent–ocean boundary (COB). At first order, both conjugate pairs show a transition from thinned continental crust, through a wide and internally complex continent–ocean transition zone (COTZ), which shows features in common with magma-poor rifted margins worldwide, such as basement ridges interpreted as exhumed subcontinental mantle. In the central GAB sector, the COTZ is symmetric around the point of break-up and displays a pair of mantle ridges, one on each margin, outboard of which lies a deep-water rift basin. Break-up has occurred in the centre of this basin in this sector of the SRS. In contrast, the Terre Adélie margin is nearly 600 km wide and shows an abandoned crustal megaboudin, the Adélie Rift Block. This block is underlain by interpreted middle crust, and appears to have a mantle ridge structure inboard, as well as an outboard exhumed mantle complex from which mylonitized harzburgite has been dredged. The conjugate margin of the Beachport Sub-basin is relatively narrow ( c. 100 km wide) and does not appear to contain an exhumed mantle ridge, as observed along strike in the GAB. These observations from a single rift spreading compartment show that radically different break-up symmetries and margin architectures can result from an essentially symmetric rifting process involving multiple, paired detachment systems. This indicates the need for caution in interpreting causative mechanisms of rifting from limited conjugate sections in other rifts. We speculate that the underlying crustal composition, rheology and structural preconditioning play a significant role in partitioning strain during the transition to break-up.