J. Stephen Daly

Emeritus Professor of Petrology

Dublin City University

Ireland

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J. Stephen Daly is an Emeritus Professor of Petrology at University College Dublin, Ireland. His research encompasses various areas including geophysical and petrological modeling, sedimentary processes, and isotopic analyses across diverse geological settings. His recent publications explore topics such as subsurface temperature modeling in Ireland, Proterozoic granite recrystallization, and sedimentary provenance in the context of ancient geological formations.

J. Stephen Daly

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Articles (18)

A new subsurface temperature model for Ireland from joint geophysical–petrological inversion of seismic, surface heat flow and petrophysical data

Trade, recycling and mixing in local metal management strategies of the later Bronze Age south Carpathian Basin: Lead isotope and chemical analyses of hoarded metalwork

Excess <sup>40</sup>Ar in Alkali Feldspar and <sup>206,207</sup>Pb in Apatite Caused by Fluid-Induced Recrystallisation in a Semi-Closed Environment in Proterozoic (Meta)Granites of the Mt Isa Inlier, NE Australia

Paleoproterozoic (late ‘Laxfordian’) reworking of juvenile Neoarchean Lewisian orthogneisses, Iona, Inner Hebrides, Scotland

Continental-scale sediment mixing and dispersal across northern Gondwana: detrital zircon U-Pb-O-Hf isotopic evidence from the Cambro-Ordovician sandstones overlying the Arabian Shield

Dynamic collapse and regrowth of the Antarctic Ice Sheet in the Weddell Sea sector during the middle Miocene: A novel multi-proxy sedimentary provenance approach using in-situ <sup>87</sup>Rb/<sup>87</sup>Sr dating of detrital K-feldspar

Detrital garnet geochronology by in‐situ U‐Pb and Lu‐Hf analysis: A case study from the European Alps

Late Oligocene Formation of the Pearl River Triggered by the Opening of the South China Sea

Sedimentary recycling in Jianchuan Basin, SE Tibetan Plateau: A solution to the debate on the formation age of the First Bend (Yangtze River)

Cenozoic reorganization of fluvial systems in eastern China: Sedimentary provenance of detrital K-feldspar in Taiwan

Sedimentary provenance perspectives on the evolution of the major rivers draining the eastern Tibetan Plateau

Beyond zircon: Incorporating detrital feldspar pb isotope analysis into the multiproxy toolbox for sedimentary provenance analysis—an example from a long-lived eastern laurentian clastic system

Meter-Scale Chemical and Isotopic Heterogeneities in the Oceanic Mantle, Leka Ophiolite Complex, Norway

No connection between the Yangtze and Red rivers since the late Eocene

Southeastern Tibetan Plateau serves as the dominant sand contributor to the Yangtze River: Evidence from Pb isotopic compositions of detrital K‐feldspar

Constraining the links between the Himalayan belt and the Central Myanmar Basins during the Cenozoic: An integrated multi-proxy detrital geochronology and trace-element geochemistry study

Correction to: Ultrapotassic magmatism in the heyday of the Variscan Orogeny: the story of the Třebíč Pluton, the largest durbachitic body in the Bohemian Massif (International Journal of Earth Sciences, (2020), 109, 5, (1767-1810), 10.1007/s00531-020-01872-2)

Formation of the Three Gorges (Yangtze River) no earlier than 10 Ma

Collaborators (7)

Richard Spikings

Stijn Glorie

SERGIO ANDO'

Christopher Bean

Richard Walker

Joshua Davies

Barry Molloy

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