Compared to the sandstone-type uranium deposits in the Ordos Basin and the Songliao Basin, the Tamusu uranium deposit in the Bayingobi Basin formed in fault-depression transition region displays distinctive features. First, the uranium-bearing sandstones
Uranium exploration breakthrough was extremely rare in an aeolian depositional sys-tem. In order to know the complicate characteristics of oxidation associated closely with uranium min- eralization in the aeolian depositional system, petrology and mineral
Large quantities of metal sulfides are widely distributed in uranium ores from the Mid-dle Jurassic Zhiluo Formation of the Shuanglong uranium deposit, southern Ordos Basin, providing a convenient condition to study the relationship between metal sulfides
The main central thrust (MCT) is one of the major thrusts in Himalayas. In central Hi-malaya, MCT was defined as a contact between underlying Lesser Himalayan Sequence (LHS) and overlying higher Himalayan crystallines (HHC). However, in the Kashmir Himala
The Zoujiashan uranium deposit in the Xiangshan ore field is the largest volcanic-related uranium deposit in China. Hematite-and fluorite-type ores are the predominant mineralization styles. Hematitization in the Xiangshan ore field is closely associated
In order to determine the provenance and variation characteristics of sandstone-type uranium deposits located in the southwest Ordos Basin, U-Pb geochronology and Hf isotope analyses were conducted on detrital zircons from the Late Mesozoic strata of the
To investigate biostratigraphy of Albian sediments (Kazhdumi Formation) in the Zagros Basin, 280 samples in four sections were prepared which are nominated as Murshan-e-Bala, Fahliyan- e-Pain, Kupon and Tale-e-Afghani. Stratigraphic distribution of identi