Transpression and tectonic exhumation in the Heimefrontfjella, western orogenic front of the East African/Antarctic Orogen, revealed by quartz textures of high strain domains

Abstract

The metamorphic basement of the Heimefrontfjella in western Dronning Maud Land (Antarctica) forms the western margin of the major ca. 500 million year old East African/East Antarctic Orogen that resulted from the collision of East Antarctica and greater India with the African cratons. The boundary between the tectonothermally overprinted part of the orogen and its north-western foreland is marked by the subvertical Heimefront Shear Zone. North-west of the Heimefront Shear Zone, numerous low-angle dipping ductile thrust zones cut through the Mesoproterozoic basement. Petrographic studies, optical quartz c-axis analyses and x-ray texture goniometry of quartz-rich mylonites were used to reveal the conditions that prevailed during the deformation. Mineral assemblages in thrust mylonites show that they were formed under greenschist-facies conditions. Quartz microstructures are characteristic of the subgrain rotation regime and oblique quartz lattice preferred orientations are typical of simple shear-dominated deformation. In contrast, in the Heimefront Shear Zone, quartz textures indicate mainly flattening strain with a minor dextral rotational component. These quartz microstructures and lattice preferred orientations show signs of post-tectonic annealing following the tectonic exhumation. The spatial relation between the sub-vertical Heimefront Shear Zone and the low-angle thrusts can be explained as being the result of strain partitioning during transpressive deformation. The pure-shear component with a weak dextral strike-slip was accommodated by the Heimefront Shear Zone, whereas the north–north-west directed thrusts accommodate the simple shear component with a tectonic transport towards the foreland of the orogen.

• Dronning Maud Land
• quartz microfabrics
• X-ray texture goniometry
• shear zones
• mylonites.

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Acknowledgements

Funding for this study provided by the German Science Foundation within the project Gesteinsbestand und strukturelle Entwicklung der Heimefrontfjella/Antarktika (Sp 235/8) is gratefully acknowledged. The fieldwork was logistically supported by the Alfred Wegener Institute. This manuscript has greatly benefited from the reviews by L.F.G. Morales, H. Stünitz, S. Oriolo and R.J. Thomas. We also would like to thank H. Goldman for the editorial handling. This is a contribution to the IGCP 648 Supercontinent Cycles and Global Geodynamics project.

Notes

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