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Ian Cartwright
Researcher at Monash University, Clayton campus
Publications - 228
Citations - 7699
Ian Cartwright is an academic researcher from Monash University, Clayton campus. The author has contributed to research in topics: Groundwater & Groundwater recharge. The author has an hindex of 45, co-authored 219 publications receiving 6810 citations. Previous affiliations of Ian Cartwright include Flinders University & University of Leeds.
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An extended episode of early Mesoproterozoic metamorphic fluid flow in the Reynolds Range, central Australia*
TL;DR: The products of metamorphic fluid flow are preserved in zones within the marbles and metamorphosed semipelites of the Upper Calcsilicate Unit in the granulite portion of the Late Palaeoproterozoic Reynolds Range Group, northern Arunta Block, central Australia.
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Increasing Australian–Indonesian monsoon rainfall linked to early Holocene sea-level rise
Michael L. Griffiths,Russell N. Drysdale,Michael K. Gagan,Jian-xin Zhao,Linda K. Ayliffe,John Hellstrom,Wahyoe S. Hantoro,Silvia Frisia,Y-X Feng,Ian Cartwright,E. St. Pierre,M. J. Fischer,Bambang W. Suwargadi +12 more
TL;DR: In this article, the authors presented a precisely dated reconstruction of monsoon rainfall over the past 12,000 years, based on oxygen isotope measurements from two stalagmites collected in southeast Indonesia.
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Late Holocene drought responsible for the collapse of Old World civilizations is recorded in an Italian cave flowstone
Russell N. Drysdale,Giovanni Zanchetta,John Hellstrom,Roland Maas,Anthony E. Fallick,Matthew Pickett,Ian Cartwright,Leonardo Piccini +7 more
TL;DR: In this article, stable isotope, trace element, and organic fluorescence data from a calcite flowstone collected from the well-watered Alpi Apuane karst of central-western Italy indicate that the climatic event responsible for this drought was also recorded in mid-latitude Europe.
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Controls on elevated fluoride and arsenic concentrations in groundwater from the Yuncheng Basin, China
TL;DR: In this paper, chemical analysis of groundwater and sediments was carried out to investigate causes of elevated F(-) (1.5-6.6 mg/L) and As concentrations (10-27 mu g/L), in groundwater from the Yuncheng Basin, northern China.
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Cl/Br ratios and environmental isotopes as indicators of recharge variability and groundwater flow: An example from the southeast Murray Basin, Australia
TL;DR: In groundwater from the shallowest Shepparton Formation, homogenisation of Cl/Br and δ 18 O values and a decline in 14 C activities with depth imply that vertical flow dominates as discussed by the authors.