Stable-isotope geochronology of the Australian regolith
References (126)
A warm equable Cretaceous: the nature of the problem
Earth Sci. Rev.
(1983)- et al.
Application of stable-isotope geochronology to the Australian regolith, and palaeoclimatic implications
(1990) The stable-isotope composition of modern soil carbonate and its relationship to climate
Earth Planet. Sci. Lett.
(1984)The climatic conditions during regolith formation: oxygen- and hydrogen-isotope evidence
Copley—1:250,000 Geological Sheet (SH/54-9) Explanatory notes
(1973)- et al.
Alluvial sandstone composition and paleoclimate. II. Authigenic mineralogy
J. Sediment. Petrol.
(1986) Soil Chemical Analysis—Advanced Course
(1956)- et al.
Clay and shale deposits of Victoria
Mem. Geol. Surv. Vict.
(1952) - et al.
Upper Pleistocene Amazon deep-sea fan muds reflect intense weathering of their mountainous source lands
Chem. Geol.
(1986) - et al.
Stable-isotope investigations of an active geothermal system in the Valles Caldera, Jemez Mountains, New Mexico
J. Volcanol. Geotherm. Res.
(1980)
Cementation of a Pennsylvanian deltaic sandstone: isotopic data
J. Sediment. Petrol.
Hydrogen and oxygen isotope systematics in weathering profiles
Geochim. Cosmochim. Acta
The Australian Climatic Environment
Iron oxide removal from soils and clays by a dithionite-citrate system buffered by sodium bicarbonate
Clays Clay Mineral.
Bauxite in Australia
Australian Bur. Mineral Resources Bull.
Oxygen and hydrogen isotope geochemistry of ocean sediments and shales
Geochim. Cosmochim. Acta
Sub-basaltic weathering, damsites, palaeomagnetism and the age of lateritization
J. Geol. Soc. Australia
A proposed method of defining deeply weathered rock units in regional geological mapping in southwest Queensland
J. Geol. Soc. Australia
Analysis of the anomalous and D/H isotope ratios in tropical rainfall over the western Pacific Ocean
Eos
Isotope studies of insular phosphates explain atoll phosphatization
Nature
Groundwater regimes and isotopic studies, Ranger mine area, Northern Territory
Australian J. Earth Sci.
Aspects of the isotope geochemistry of the Great Artesian Basin, Australia
Aspects of the isotope hydrology of two sandstone aquifers in arid Australia
Effect of climate and vegetation on oxygen-18 and deuterium profiles in soils
Billa Kalina 1:250,000 Geological Sheet: Explanatory notes (SH/53-7)
Commodity review—Clay
N.S.W. Mining Explor. Quart.
Kaolin in New South Wales
Geol. Surv. N.S. W. Min. Res.
Notes on the bauxite deposits of the Mirboo North district of South Gippsland
Mining Geol. J.
An isotopic study of the Australian regolith
Oxygen-isotope dating of the Australian regolith
Nature
Oxygen-isotope dating of the Australian regolith
Nature
Stable-isotope evidence for low-temperature weathering and post-formational hydrogen-isotope exchange in Permian kaolinites
Chem. Geol.
An isotopic study of surficial alunite in Australia.2: Potassium-argon geochronology
Chem. Geol.
Geomorphic evolution of the Fleurieu Peninsula, South Australia
Investigations of ferricretes and related surficial ferruginous materials in parts of southern and eastern Australia
Z. Geomorph.
The isotope hydrology of the Mereenie Sandstone aquifer, Alice Springs, Northern Territory
J. Hydrol.
Tertiary megafossil flora of Maslin Bay, South Australia: A preliminary report
Alcheringa
Intercalation method using formamide for differentiating halloysite from kaolinite
Clays Clay Mineral.
The use of bromine pentafluoride in the extraction of oxygen in silicates for isotopic analysis
Geochim. Cosmochim. Acta
Petrography, distribution, origin and age of ferricrete and silcrete in the Armidale area, N.S.W
Chronology of landscape evolution and soil development in the upper Flinders River area, Queensland, based on isotopic dating of Cainozoic basalts
Australian J. Earth Sci.
Diagenetic development of kaolinite
Clays Clay Mineral.
The age of the lateritized summit surface on Kangaroo Island and adjacent areas of South Australia
J. Geol. Soc. Australia
Stable isotopes in precipitation
Tellus
Use of environmental isotopes in arid-zone hydrology
Duricrusted residuals on the Barrier and Cobar pediplains of NSW
J. Geol. Soc. Australia
A minimum age for the duricrust
Australian J. Sci.
In search of the origin of cement in siliciclastic sandstones: an isotopic approach
Chem. Geol.
Meteoric burial diagenesis of Pennsylvanian arkosic sandstones, southwestern Anadarko Basin, Texas
Amer. Assoc. Petrol. Geol. Bull.
The age and geomorphic correlations of deep-weathering profiles, silcrete and basalt in the Roma-Amby region
J. Geol. Soc. Australia
Climates throughout Geologic Time
Cited by (94)
Stable isotope proxy records in tropical terrestrial environments
2020, Palaeogeography, Palaeoclimatology, PalaeoecologyAntiquity of the giant inselberg Burringurrah (Mount Augustus), Western Australia, inferred from oxygen isotope dating of kaolinitic weathering
2019, GeomorphologyCitation Excerpt :With decreasing age, these minerals are progressively enriched in 18Ο, and by correlating sample δ18Ο values with independent age constraints, it has been possible to establish a timescale, which allows application of the dating method to profiles of unknown ages. Accordingly, samples from known-age weathering profiles in eastern and central Australia, provide a chronology wherein Permian kaolinites have δ18Ο values of +6 to +10‰, Jurassic-early Cretaceous +10 to +15‰, late Cretaceous-Paleogene +15 to +17.5‰ and Neogene +17.5 to +21.3‰ (Bird and Chivas, 1988a, 1989, 1993). That such a range of δ18Ο values (15‰ variation) is still faithfully preserved at Earth's surface is testament to the lack of later oxygen isotopic exchange, as all profiles have been subject to rain- and groundwaters with progressively changing (increasing) δ18Ο values.
Landscape evolution and geochemical dispersion of the DeGrussa Cu-Au deposit, Western Australia
2019, Ore Geology ReviewsCitation Excerpt :This led to a decrease in erosion rates and allowed deep weathering to occur under a humid sub-tropical to tropical climate (e.g., De Broekert, 2002 and references therein). This long surficial exposure time resulted in a complex history of weathering that dates back to at least the Late Mesozoic (Bird and Chivas, 1989). Residual weathering profiles resulted from the overprinting of several climatic changes, including water table fluctuations, together with variations in salinity and groundwater residence times.
Rare-earth element and stable isotope signatures of kaolin from a Pliocene lateritic weathering profile at mid-latitude region (Andalusia, Spain): Implications for paleoweathering and paleoclimatic reconstructions
2018, CatenaCitation Excerpt :In fact, kaolinite is an abundant clay mineral in paleosol profiles that formed in paleotropical sites (e.g. Sheldon and Tabor, 2009). However, the stable isotope composition of kaolinite reveals that much of the kaolinitic regoliths formed under relatively cold conditions, suggesting that, contrary to classical interpretations, laterization and deep weathering phenomena are not solely the result of weathering in tropical or subtropical climates (Bird and Chivas, 1989). It has been also suggested that development of kaolinitic profiles at extra-tropical latitudes may be the result of a greenhouse warming induced by increased atmospheric CO2 levels (e.g. Dowsett et al., 1992; Barron et al., 1993; Thiry, 2000; Krause et al., 2010).
- ∗
Present address: Department of Geology, University of Western Ontario, London, Ontario, N6A 5B7, Canada.