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Kelsie Dadd

Researcher at Macquarie University

Publications -  30
Citations -  989

Kelsie Dadd is an academic researcher from Macquarie University. The author has contributed to research in topics: Basalt & Volcanic rock. The author has an hindex of 12, co-authored 27 publications receiving 769 citations. Previous affiliations of Kelsie Dadd include Australian Research Council & University of Technology, Sydney.

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Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Expedition 349

TL;DR: In this paper, the authors combined analyses of deep tow magnetic anomalies and International Ocean Discovery Program Expedition 349 cores to show that seafloor spreading started around 33 Ma in the northeastern South China Sea (SCS), but varied slightly by 1-2 Myr along the northern continent-ocean boundary.
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Seismic stratigraphy of the central South China Sea basin and implications for neotectonics

TL;DR: In this paper, the authors used the International Ocean Discovery Program Expedition 349 data to map seismic sequence boundaries and facies of the central basin and neighboring regions of the South China Sea and found that the most active faulting and vertical uplifting now occur in the southern East Subbasin, caused most likely by the active and fastest subduction/obduction of Taiwan and the collision between the northeast Palawan and the Luzon arc.
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Late Silurian bimodal volcanism of southwestern New Brunswick, Canada: Products of continental extension

TL;DR: In this paper, the authors analyzed 115 volcanic rocks for major and trace element concentrations and found that the sequence is subalkalic and bimodal (basalt-rhyolite) with within-plate tectonic affinities.
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Magma composition and viscosity as controls on peperite texture : an example from Passamaquoddy Bay, southeastern Canada

TL;DR: In the Passamaquoddy Bay area, southeastern Canada, silurian mafic lava flows and rhyolite sills interacted with wet sediment to produce peperitic breccia as mentioned in this paper.
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Post-collisional, Late Neoproterozoic, high-Ba-Sr granitic magmatism from the Dom Feliciano Belt and its cratonic foreland, Uruguay: Petrography, geochemistry, geochronology, and tectonic implications

TL;DR: For example, in this paper, the authors used zircon U-Pb LA-ICP-MS data for three plutons to confirm their Late Neoproterozoic age; 634±7.3 (Sierra de los Caracoles), 604±-3.0 (Cortez Blanco) and 597±−3.6 (Guayabo).