Paleomagnetism of the Carboniferous-Permian Myall blocks, Tamworth Belt, southern New England Orogen: Permian counterclockwise rotations and Triassic clockwise rotation

This paleomagnetic study on the Myall blocks of the southern New England Orogen complements studies on four other Tamworth Belt blocks aiming to unravel evolution of the Tamworth Belt and the Manning Orocline in particular. Focus is on ignimbritic successions that have partly interlinked stratigraphies across the five blocks and can retain primary magnetisations despite prevalent overprinting. This makes the Tamworth Belt prospective to oroclinal testing by comparing poles and pole paths for individual blocks across its curved structure. Paleomagnetic, rock magnetic and magnetic fabric results are detailed from an upper lower Carboniferous to lower Permian succession, sampled across forearc basin and arc sites (64) of the western Myall Block and forearc basin sites (16) of the eastern Myall Block. Predominantly thermal demagnetisations show a widely present low-temperature component, attributed to late Oligocene weathering, intermediate-temperature primary and overprint components confined to the Nerong Volcanics, and high-temperature primary and overprint components. Overprinting proved more prevalent in the Myall blocks than in other Tamworth Belt blocks, with five phases dated from mid-Carboniferous to mid-Triassic. Comparison of primary and overprint poles against Carboniferous, Permian and Triassic reference paths shows counterclockwise rotations ranging from 20-45 degrees for the western Myall Block forearc basin, to 30 degrees to 90 degrees west to east across the southwestern Myall Block arc complex, to 85-110 degrees for the eastern Myall Block forearc basin, occurring from the latest Carboniferous-early Permian Tablelands phase probably to the mid- to late Permian initial pulse of the Hunter-Bowen phase. The southwestern Myall Block also shows a mid-Triassic, or later, clockwise rotation ranging west to east from 50 degrees to 110 degrees.

Automated summary

This study focuses on the paleomagnetic characteristics of the Myall blocks in the southern New England Orogen, revealing different phases of magnetization and prevalent overprinting. The comparison of primary and overprint poles across different blocks suggests counterclockwise rotations in the western Myall Block forearc basin and diverse rotation patterns in other areas. Overall, the findings contribute to understanding the geological evolution of the Tamworth Belt and the Manning Orocline.