Geochemical and Geochronological Characterization of Metal Deposits in China and Egypt
This community investigates the origin, timing, and chemical evolution of metal deposits, primarily in China and Egypt, using isotopic and mineralogical data to reconstruct the tectonic environments that formed them.
The research focuses heavily on gold, rare earth, and trace element mineralization, with a specific emphasis on orogenic belts and cratonic settings in South and North China. Key methodologies include zircon U-Pb geochronology, sulfur and noble gas isotope fractionation, and fluid inclusion analysis. These techniques are applied to determine the sources of ore-forming fluids and the timing of metal deposition. The work frequently examines the geochemical characteristics of host rocks and the implications of these findings for understanding regional tectonic evolution.
The community represents a significant share of research tracked for Neodymium (20.8%) and Thorium (15.1%). It also contains 2,521 papers related to Thorium and 2,294 papers related to Neodymium.
The community comprises 31,550 papers, published predominantly in Geochimica et Cosmochimica Acta, Ore Geology Reviews, and Minerals.
Recent work continues to apply these methods to specific mineral systems, including studies on lithium-rich granites, rare earth element magmas, and tin mineralization in Southeast Asia.