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作 者:MIAO Peisen JIN Ruoshi LI Jianguo ZHAO Hualei CHEN Lulu CHEN Yin SI Qinghong
机构地区:[1]Tianjin Center,China Geological Survey,Tianjin 300170,China
出 处:《Acta Geologica Sinica(English Edition)》2020年第2期583-584,共2页地质学报(英文版)
基 金:the National Key Research and Development Project(grant No.2018YFC0604200);the Ministry of Science and Technology of China(Grant 20I5CB453000).
摘 要:The exploration depth of sandstone-type uranium deposits worldwide is mostly less than 700 m,and most of them occur in strata of fluvial facies(Adams et al.,1981;Jin et al.,2016;Hou et al.,2017).Only a few small uranium deposits have been reported in aeolian depositional environments(Isachsen et al.,1955;Li et al.,2001).In the Pcngyang Jingchuan region of the southwestern Ordos Basin,uranium ore bodies with large thickness and high grade in the aeolian sandstone of the Luohe Formation were newly found at depths from 700 to 1500 m,which have laid the foundation for increasing the uranium resources significantly in the Ordos Basin.
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