Variations in continental volcanic arc emissions have the potential to control atmospheric
carbon dioxide (CO2) levels and climate change on multimillion-year time scales. Here we …

Understanding the stratigraphic architecture of shelf-margin clinoforms is key to determining
how sediments are transferred to deep-water settings and how the interplay of tectonics …

Full‐plate reconstructions describe the history of past continental motions and how plate
boundaries have evolved to accommodate these motions. Traditionally, tectonic …

Despite many years of study, the processes involved in the post-breakup development of
passive margins remain poorly understood. Integration of apatite fission track analysis …

Passive margin highlands occur on most continents on Earth and play a critical role in the
cycle of weathering, erosion, and atmospheric circulation. Yet, in contrast to the well …

Abstract The Upper Cretaceous sedimentary sequence at International Ocean Discovery
Program Site U1512 in the Ceduna Sub-basin of the Great Australian Bight represents a …

U-Pb geochronology and Lu-Hf isotope analysis of detrital zircon from the mid-Cretaceous
Winton and Mackunda Formations in the Eromanga Basin were employed to investigate …

There is growing recognition that pulses of compressive tectonic structuring punctuate the
post‐breakup subsidence histories of many 'passive'rifted continental margins. To obtain …

Detrital zircon U–Pb geochronology has enabled advances in the understanding of
sediment provenance, transportation pathways, and the depositional age of sedimentary …

This paper exposes the unique set of attributes explaining why precious opal has formed in
such abundance in central Australia, and almost nowhere else on Earth. The Early …