Load more. The rare-earth elements dysprosiumerbiumterbium and ytterbiumas well as metal elements such as thorium and uranium all replacing yttrium are the expressive secondary components of xenotime. From the selection of dozen hand-specimens, four rock. However, while long-term erosion and rock weathering rates in many parts of Australia are low by world standards, they are not low enough to allow pre-Tertiary regolith and landforms to survive without burial and exhumation. Recognition and influence on reservoir properties and paleoenvironmental analysis.
Deals with the ways in which REE behave during weathering and transport, and in the oceans.
Radiometric dating of sedimentary rocks: The application of diagenetic xenotime geochronology
Precambrian provenance and Silurian metamorphism of the Tsubonosawa Paragneiss in the South Kitakami Terrane, Northeast Japan, revealed by the chemical Th-U-total Pb isochron ages of monazite, zircon and xenotime. Based on 26 SIMS analyses. The stabil. Wang et al. Sign up.
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