Structural, metamorphic, and geochronological constraints on alternating compression and extension in the Early Paleozoic Gondwanan Pacific margin, northeastern Australia

• Published in: Tectonics (Washington, D.C.) D.C.), 2007-06, Vol.26 (3), p.np-n/a
• Main Authors: Fergusson, C. L., Henderson, R. A., Withnall, I. W., Fanning, C. M., Phillips, D., Lewthwaite, K. J.
• Format: Article
• Language: English
• Subjects: back arc; extension; geochronology; Tasman Orogenic Zone; tectonics
• ISSN: 0278-7407; 1944-9194
• DOI: 10.1029/2006TC001979

The Ross‐Delamerian orogenic belt formed along the early Paleozoic active Pacific margin of the newly merged Gondwana supercontinent. In its northernmost segment in the Townsville region of northeastern Australia, we have identified a short contractional phase of the Delamerian orogeny in the Argentine Metamorphics postdating formation of a mafic breccia with a U‐Pb zircon age of 500 ± 4 Ma. Contraction was followed by widespread inferred extensional deformation with formation of flat‐lying foliation, domal features, and amphibolite grade and greenschist retrograde metamorphism all synchronous with latest Cambrian to Early Ordovician extensional back‐arc volcanism, sedimentation, and intrusions. One of these intrusions gives a U‐Pb zircon age of 480 ± 4 Ma. Foliation related to the extensional deformation is crosscut by a late granodiorite dike with a U‐Pb zircon age of 461 ± 4 Ma. Late east‐west contractional deformation affected the higher‐grade part of the assemblage. In contrast to the Ross‐Delamerian orogenic belt in the Transantarctic Mountains and southeastern Australia, the orogenic belt in northeastern Australia was affected by a short episode of contraction at ∼495 Ma followed by long‐lived back‐arc extension from ∼490 Ma to 460 Ma with subsequent contractional deformation.