Ion-adsorption rare earth elements (iREE) deposits are the globally predominant source of
heavy rare earth elements (HREE), which are mainly discovered and mined in southern …

Regolith-hosted rare earth element (REE) deposits, also called ion-adsorption or weathered
crust elution-deposited REE deposits are distributed over Jiangxi, Guangdong, Fujian …

On the basis of extensive studies of synthetic perovskite-structured compounds it is possible
to derive a hierarchy of hettotype structures which are derivatives of the arisotypic cubic …

Recent increase of the demand for rare earth elements (REEs), especially dysprosium and
terbium used in the permanent magnet industry is modifying a concept of the REE …

Regolith-hosted rare earth element (REE) resources in South China are the dominant global
source of heavy REEs (HREEs), which are critical for high technology and military industries …

In our study we explore the applicability of rutile as a pathfinder for orogenic gold deposits,
which are an important source of this metal worldwide. We analysed rutile associated with …

Abstract The Zhaibei Granite in Jiangxi Province, southern China, hosts an ion-adsorption
light rare earth element (LREE) deposit. Recently, heavy REE (HREE) ores have also been …

Over the past few decades, numerous ion adsorption type rare earth element (REE) deposits
have been discovered in the weathering crusts of granitic and volcanic rocks, and a great …

Since 2011, certain advances have been made through the resource investigation,
metallogenesis research, mining supervision and environmental protection of ion-adsorption …

The geochronology, petrogenesis and tectonic setting of granites associated with tin–
tungsten mineralization in southern Myanmar remain unclear. This work presents whole …