TARA > School of Natural Science > Geology >
Chemical abrasion applied to SHRIMP zircon geochronology: An example from the Variscan Karkonosze Granite (Sudetes, SW Poland)
Changes in the hydrological cycle in tropical East Africa during the Paleocene- Eocene Thermal Maximum
Evaluating the utility of 15N and 18O isotope abundance analyses to identify nitrate sources: A soil zone study
Arctic Bay Formation, Borden Basin, Nunavut (Canada): basin evolution, black shale, and dissolved metal systematics in the Mesoproterozoic ocean
Acid Treatment effects on the stable isotopic signature of fossils
