That more than 82 percent of proved sandstone-type uranium deposits coexist with proved oil-gas or coalfields in the world reflects the fact of coexistence and accumulation of multi-energy minerals including oil,gas,c...That more than 82 percent of proved sandstone-type uranium deposits coexist with proved oil-gas or coalfields in the world reflects the fact of coexistence and accumulation of multi-energy minerals including oil,gas,coal and uranium in the same basin.Especially,this phenomenon is most typical in the Central-east Asia energy basins.Across China,Mongolia and some central Asian countries,the giant Central-east Asia metallogenetic domain(CEAMD)stretches more than 6,000 km from Songliao Basin of China in the east to the Caspian Sea in the west.The multi-energy minerals distribution characteristics of the domain include:their spatial distribution is complicated and ordered;the ore-bearing horizon relates closely to the geographical region;the accumulation/mineralization and localization time is the same or close;the occurrence setting and accumulation/mineralization have close correlation;and they have rich provenance for all the minerals.All of these imply that they have close relations between each other under a unified geodynamic background.The exogenetic uranium mineralization process in CEAMD can be divided into five phases using time limits of 100 Ma,(50±2)Ma,20±(2―4)Ma,8―5 Ma.The major mineralization periods and their differences in each primary uranium-bearing basin are identical to the oil-gas accumulation and localization periods and phases in the same basin,and are also in response to regional tectonics and controlled in general by the regional geodynamic environment.For industrial application and commercial exploitation,it is suggested that an important period for coexistence,accumulation and localization of oil,gas,coal and uranium and their interaction mainly occur in the late/last and post basin evolution.Through generalized analysis and comparison of accumulation/mineralization environment of the energy basins in CEAMD,the authors propose that the relatively stable regional tectonic background and moderate(weaker)structural deformation probably are necessary for formation,coexistence and preservat展开更多
The purpose of the present study was to survey contents of trace elements of Cu, Mn, Fe, and Zn in the surface layer （0-20 cm） in the soil, pasture and serum of sheep in Huangcheng area of Qilian mountain grassland,...The purpose of the present study was to survey contents of trace elements of Cu, Mn, Fe, and Zn in the surface layer （0-20 cm） in the soil, pasture and serum of sheep in Huangcheng area of Qilian mountain grassland, China. Also the soil-plantanimal continuum was analyzed. Soil （n=300）, pasture （n=60）, and blood serum samples from sheep （n=480） were collected from Huangcheng area of Qilian mountain grassland, China. The contents of trace element in the samples were analyzed by atomic absorption spectrophotometer after digestion. The soil trace elements density distribution shows a ladder-like pattern distribution. Equations developed in the present study for prediction of Fe （R2=0.943） and Zn （R2=0.882） had significant R2 values.展开更多
The Laoshan A-type granite is a highly evolved granite body. The study on accessoryminerals indicates that there exist differentiation and accumulation of fluids during the late stage of evolution of the granite. The ...The Laoshan A-type granite is a highly evolved granite body. The study on accessoryminerals indicates that there exist differentiation and accumulation of fluids during the late stage of evolution of the granite. The released fluids are rich in rare-earth elements (REE), high-field-strength elements (HFSE, such as Nb, Ta, Zr, Hf, Th, U, and Y) and volatiles (F, P, CO2, etc.). Owing to the presence of fluid, accessory mineral assemblages have changed during the evolution of A-type granite, and are especially characterized by large amounts of independent REE-Nb-Y-Th minerals present in the late facies. Late-accumulation of fluids may be of the general feature of A-type granites, at least of highly evolved ones.展开更多
基金Jointly supported by the National Important Basic Research Program of China(Grant No.2003CB214607)Program for Changjiang Scholars and Innovative Research Team in University(Grant No.IRT0559)the National Natural Science Foundation of China(Grant No.40372096)
文摘That more than 82 percent of proved sandstone-type uranium deposits coexist with proved oil-gas or coalfields in the world reflects the fact of coexistence and accumulation of multi-energy minerals including oil,gas,coal and uranium in the same basin.Especially,this phenomenon is most typical in the Central-east Asia energy basins.Across China,Mongolia and some central Asian countries,the giant Central-east Asia metallogenetic domain(CEAMD)stretches more than 6,000 km from Songliao Basin of China in the east to the Caspian Sea in the west.The multi-energy minerals distribution characteristics of the domain include:their spatial distribution is complicated and ordered;the ore-bearing horizon relates closely to the geographical region;the accumulation/mineralization and localization time is the same or close;the occurrence setting and accumulation/mineralization have close correlation;and they have rich provenance for all the minerals.All of these imply that they have close relations between each other under a unified geodynamic background.The exogenetic uranium mineralization process in CEAMD can be divided into five phases using time limits of 100 Ma,(50±2)Ma,20±(2―4)Ma,8―5 Ma.The major mineralization periods and their differences in each primary uranium-bearing basin are identical to the oil-gas accumulation and localization periods and phases in the same basin,and are also in response to regional tectonics and controlled in general by the regional geodynamic environment.For industrial application and commercial exploitation,it is suggested that an important period for coexistence,accumulation and localization of oil,gas,coal and uranium and their interaction mainly occur in the late/last and post basin evolution.Through generalized analysis and comparison of accumulation/mineralization environment of the energy basins in CEAMD,the authors propose that the relatively stable regional tectonic background and moderate(weaker)structural deformation probably are necessary for formation,coexistence and preservat
基金The financial supports are greatly appreciated from the Central Public-interest Scientific Institution Basal Research Fund of China(1610322013003)the Agriculture Achievements Transformation Fund Project of the Ministry of Science and Technology of China(2010GB23260564)
文摘The purpose of the present study was to survey contents of trace elements of Cu, Mn, Fe, and Zn in the surface layer （0-20 cm） in the soil, pasture and serum of sheep in Huangcheng area of Qilian mountain grassland, China. Also the soil-plantanimal continuum was analyzed. Soil （n=300）, pasture （n=60）, and blood serum samples from sheep （n=480） were collected from Huangcheng area of Qilian mountain grassland, China. The contents of trace element in the samples were analyzed by atomic absorption spectrophotometer after digestion. The soil trace elements density distribution shows a ladder-like pattern distribution. Equations developed in the present study for prediction of Fe （R2=0.943） and Zn （R2=0.882） had significant R2 values.
文摘The Laoshan A-type granite is a highly evolved granite body. The study on accessoryminerals indicates that there exist differentiation and accumulation of fluids during the late stage of evolution of the granite. The released fluids are rich in rare-earth elements (REE), high-field-strength elements (HFSE, such as Nb, Ta, Zr, Hf, Th, U, and Y) and volatiles (F, P, CO2, etc.). Owing to the presence of fluid, accessory mineral assemblages have changed during the evolution of A-type granite, and are especially characterized by large amounts of independent REE-Nb-Y-Th minerals present in the late facies. Late-accumulation of fluids may be of the general feature of A-type granites, at least of highly evolved ones.
