معرفی
Dr. George Dix is a Professor in the Department of Earth Sciences at Carleton University, affiliated with the Ottawa-Carleton Geoscience Centre. His research focuses on carbonate sedimentology, stratigraphy, and tectonics, with a particular emphasis on understanding depositional processes, diagenetic histories, and tectonic influences on sedimentary systems. His work spans Ordovician to Neoproterozoic intervals, often integrating field observations, geochemical analyses, and geochronological data.
Key research themes include the evolution of carbonate platforms and foreland basins, particularly in the Ottawa Embayment and Arctic Canada. He has contributed significantly to studies of carbonate facies analysis, sequence stratigraphy, and the role of hydrothermal fluid flow in diagenetic processes. His publications frequently address the interplay between tectonic activity and sedimentation, such as the impact of the Taconic orogeny on Ordovician successions.
Dr. Dix’s recent work highlights innovative applications of isotopic stratigraphy (e.g., δ13C) and U-Pb geochronology to refine chronostratigraphic frameworks. His research also explores the hydrochemical signatures of mantle plumes and their influence on bedrock structures in the Ottawa-Bonnechere Graben.
Publications since 2018 reveal a continued focus on Late Ordovician platform dynamics, mixed-sediment systems, and the integration of lithostratigraphy with tectonic interpretations. Earlier work (e.g., 2014) extends to Neoproterozoic carbonate ramps and Patagonian Oligocene-Miocene platforms, underscoring his expertise in diverse temporal and geographical contexts.
Despite the breadth of his research, Dr. Dix’s work consistently emphasizes the application of detailed field data to solve large-scale geological questions, bridging sedimentology, stratigraphy, and tectonics.
