The Leichhardt River Fault Trough of the Mount Isa terrane developed a complex extensional architecture between approximately 1800 and 1600 Ma, forming the underlying template upon which compressional structures were superimposed during the 1590 to 1500 Ma Isan Orogeny. Basin-fill material accumulated during at least five multiphase periods of rifting and associated postrift subsidence forming a stacked succession of unconformity-bounded sequences. Initial E-W extension was associated with a massive magmatic event. Half graben greater than 50 km in width and of alternating asymmetry localized the extrusion of up to 4 km of continental tholeiites. Thereafter a period of N-S extension resulted in southward tapering north tilted half graben in which synrift basaltic and siliciclastic strata accumulated. N-S extension was followed by regional postrift subsidence and the deposition of a laterally continuous quartzite-carbonate package. A multiphase period of E-W to NW-SE extension ensued during which time two unconformity-bounded sequences accumulated. The stratal architectures of these sequences are strongly asymmetric in cross section, exhibiting a pronounced rotational thickening toward the east, consistent with their deposition in the hanging walls of east dipping tilt blocks between 15 and 40 km in width. Finally, a period of N-S extension resulted in the development of E-W trending F1 drag synclines in the highest level cover rocks. The association of angular unconformities and block-bounding faults, E-W trending synclines and E-W striking faults, and the unique internal fold geometries of fault blocks suggest that many fault-bounded blocks originated as coherent structural entities during rifting and continued to act as such during subsequent shortening.¿ 1997 American Geophysical Union