The main purpose of this paper is to present a fundamental concept of U-Pb isotopic spectrum-system and to apply this idea to the interpretation of the mechanism of uranium ore formation. It is evident from a number o...The main purpose of this paper is to present a fundamental concept of U-Pb isotopic spectrum-system and to apply this idea to the interpretation of the mechanism of uranium ore formation. It is evident from a number of examples of uranium deposits that the uranium deposits formed in various processes are characterized by different types of U-Pb isotopic spectrum-system.展开更多
Based on the evolutionary theory of U-Pb isotopic system, we have studied the genetic model for a uranium deposit occurring in the carbonate-silicolite-pelite. The data show that the U-deposit is characterized by a mu...Based on the evolutionary theory of U-Pb isotopic system, we have studied the genetic model for a uranium deposit occurring in the carbonate-silicolite-pelite. The data show that the U-deposit is characterized by a multi.stage evolution with respect to its U-Pb isotopic system, and the mechanism of its genesis can be expained by later repeated superimposition of mineralization which took place at about 200±10 m.y.; 100±10 m.y., 60 ± 10 m.y.and 11 ± 1 m.y. ago. These mineralization stages are closely related to the regional geological tectonic activity.展开更多
A new boron-silicon gel ion emitter is developed for lead isotope analysis. As a result, a sensitivity of about 10^-7As/μg can be obtained, which permits mass spectrometry to be conducted for lead in the order of 10 ...A new boron-silicon gel ion emitter is developed for lead isotope analysis. As a result, a sensitivity of about 10^-7As/μg can be obtained, which permits mass spectrometry to be conducted for lead in the order of 10 nanogram. The mass spectrometry bltnk weight of lead is about 0o2 nanogram. As compared with zirconium-silicon gel the ion beam from lead is more stable.展开更多
Nd model ages(TDM) of the Pre-Mesozoic crustal rock samples from Southeast China range from 1.2 to 3.5Ga.Two age peaks of 1.4Ga and 1.8 Ga are observed in the histogram of TDM model ages.Available U-Pb zircon inherita...Nd model ages(TDM) of the Pre-Mesozoic crustal rock samples from Southeast China range from 1.2 to 3.5Ga.Two age peaks of 1.4Ga and 1.8 Ga are observed in the histogram of TDM model ages.Available U-Pb zircon inheritance ages are concentrated around 1.2-1.4Ga,1.8Ga and 2.5Ga,respectively.The combined use of Sm-Nd and U-Pb zircon inheritance ages suggests that the formation of the Precambrian curst is of episodic character.The oldest crustal nucleus may have been formed during the Late Archean(2.5Ga or older?).A rapid production of the crust took place 1.8 Ga ago,consistent with the global crust formation event at 1.7-1.9Ga.Another important episode of the addition of juvenile crustal material from the mantle in Southeast China took place 1.2-1.4Ga ago,during which the pre-existing crust was strongly reworked and/or remelted.展开更多
The crystal form,chemical composition and U-Pb isotopic composition of various zircon fractions is a Middle Proterozoic granite pluton from the Baoban area suggest that the zircons are typically magmatogenic in nature...The crystal form,chemical composition and U-Pb isotopic composition of various zircon fractions is a Middle Proterozoic granite pluton from the Baoban area suggest that the zircons are typically magmatogenic in nature,and different from those of sedimentary and epigenetic orgins.The various zircon fractions yielded and age of about 1440.87Ma,which may represent the ge of zircon crystallization.The so-called aoban-group migmatite is,as a matter of fact,a Middle Proterozoic granite pluton.展开更多
文摘The main purpose of this paper is to present a fundamental concept of U-Pb isotopic spectrum-system and to apply this idea to the interpretation of the mechanism of uranium ore formation. It is evident from a number of examples of uranium deposits that the uranium deposits formed in various processes are characterized by different types of U-Pb isotopic spectrum-system.
文摘Based on the evolutionary theory of U-Pb isotopic system, we have studied the genetic model for a uranium deposit occurring in the carbonate-silicolite-pelite. The data show that the U-deposit is characterized by a multi.stage evolution with respect to its U-Pb isotopic system, and the mechanism of its genesis can be expained by later repeated superimposition of mineralization which took place at about 200±10 m.y.; 100±10 m.y., 60 ± 10 m.y.and 11 ± 1 m.y. ago. These mineralization stages are closely related to the regional geological tectonic activity.
文摘A new boron-silicon gel ion emitter is developed for lead isotope analysis. As a result, a sensitivity of about 10^-7As/μg can be obtained, which permits mass spectrometry to be conducted for lead in the order of 10 nanogram. The mass spectrometry bltnk weight of lead is about 0o2 nanogram. As compared with zirconium-silicon gel the ion beam from lead is more stable.
文摘Nd model ages(TDM) of the Pre-Mesozoic crustal rock samples from Southeast China range from 1.2 to 3.5Ga.Two age peaks of 1.4Ga and 1.8 Ga are observed in the histogram of TDM model ages.Available U-Pb zircon inheritance ages are concentrated around 1.2-1.4Ga,1.8Ga and 2.5Ga,respectively.The combined use of Sm-Nd and U-Pb zircon inheritance ages suggests that the formation of the Precambrian curst is of episodic character.The oldest crustal nucleus may have been formed during the Late Archean(2.5Ga or older?).A rapid production of the crust took place 1.8 Ga ago,consistent with the global crust formation event at 1.7-1.9Ga.Another important episode of the addition of juvenile crustal material from the mantle in Southeast China took place 1.2-1.4Ga ago,during which the pre-existing crust was strongly reworked and/or remelted.
基金This project was financially supported by the National Natural Science Foundation of China
文摘The crystal form,chemical composition and U-Pb isotopic composition of various zircon fractions is a Middle Proterozoic granite pluton from the Baoban area suggest that the zircons are typically magmatogenic in nature,and different from those of sedimentary and epigenetic orgins.The various zircon fractions yielded and age of about 1440.87Ma,which may represent the ge of zircon crystallization.The so-called aoban-group migmatite is,as a matter of fact,a Middle Proterozoic granite pluton.
