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Articles by Christopher R. Fielding
Misleading Basin Margins-Analysis of the Upper Permian Succession in the Retroarc Foreland Bowen Basin of Northeast Australia
Conflicts of Interest The authors declare no conflicts of interest. Supporting Information Filename Description bre70033-sup-0001-TableS1.docxWord 2007 document , 25.9 KB Table S1. Summary of palaeocurrent data used in this study, giving locations, mean direction, standard deviation, vector length, number of data, and explanatory notes. References 1985. “ Geology of the Fort Cooper Coal Measures Interval.” In Proceeding of the Bowen Basin Coal Symposium, vol. 17, 87–92.
The impact of high discharge variability on sedimentology and architecture of bar deposits in the meandering Powder River (Montana, USA)
INTRODUCTION Point bars are perhaps one of the most representative examples of fluvial bars. During the second half of the past century extensive research has led to the development of facies models to recognize these bars in ancient fluvial successions (Bernard et al., 1962; Allen, 1963a, 1964; Collinson, 1978; Jackson, 1978; Smith, 1987; Miall, 2006).
Towards a new generation of fluvial facies models for the interpretation of ancient deposits, based on inter‐annual peak discharge variance of modern rivers
INTRODUCTION Historically, the basis for fluvial facies models, which are used to summarize the one-dimensional, two-dimensional and three-dimensional arrangement of sedimentary deposits in rivers, has been river planform (e.g. Miall, 2010). Many researchers have nonetheless pointed out that there are multiple weaknesses in this approach (Bridge, 1985, 1993a,b; Brierley, 1996; Bristow, 1996; Ethridge, 2011).
Age and pattern of the southern high-latitude continental end-Permian extinction constrained by multiproxy analysis
Abstract Past studies of the end-Permian extinction (EPE), the largest biotic crisis of the Phanerozoic, have not resolved the timing of events in southern high-latitudes. Here we use palynology coupled with high-precision CA-ID-TIMS dating of euhedral zircons from continental sequences of the Sydney Basin, Australia, to show that the collapse of the austral Permian Glossopteris flora occurred prior to 252.3 Ma (~370 kyrs before the main marine extinction).
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