Late Devonian time was a period of rapid upheaval in the Earth system, including climate change, sea level changes, widespread ocean anoxia, and Frasnian-Famennian mass extinction; cause(s) these changes remain(s) uncertain. The Lennard Shelf Canning Basin Western Australia contains carbonate reef sections spanning much Epoch has been sampled for paleomagnetic analysis with studies by Hansma co...

Abstract. In Europe, formation of the Palaeozoic Variscan orogenic belt, and Mesozoic–Cenozoic Alpine–Carpathian belt led to a widespread inversion events within forelands both domains. We used legacy 2-D seismic data together with newly acquired 3-D that, for first time, precisely imaged sub-Zechstein (i.e. sub-evaporitic) upper successions in NW Poland order develop quantitative, balanced mod...

Red Hill I forms the northern end of the Northern Simpson Park Range, northwest of Eureka, Nevada. The Red Hill I locality (lowest part of Red Hill section II in Murphy et al. 1976, Red Hill I of Gregory et al. 1977) lies near the exposed bottom of a sequence of reddish, yellow and greenish gray silty lime mudstones, approximately 80 m thick, at the base of the southwest flank of Red Hill (NW ,...