Rare earth element(REE) is widely used in various fields of geology.Study of the existing forms of REE in geological objects is a necessity for us to solve geological problems related with REE.This paper tried to make...Rare earth element(REE) is widely used in various fields of geology.Study of the existing forms of REE in geological objects is a necessity for us to solve geological problems related with REE.This paper tried to make it clear the existing forms of REE in gold-bearing pyrite in Jinshan gold deposit by stepwise dissolution test with ICP-MS analysis.Results showed that content of REE in fluid-inclusions of gold-bearing pyrite was very low,which only took about 0.07%–0.70% of the ΣREE,and that of pyrite phase ...展开更多
Jinshan gold deposit is located in northeastern Jiangxi,South China,which is related to the ductile shear zone.It has a gold reserve of more than 200 tons,with 80%of gold occurring in pyrite. The LREE of gold-bearing ...Jinshan gold deposit is located in northeastern Jiangxi,South China,which is related to the ductile shear zone.It has a gold reserve of more than 200 tons,with 80%of gold occurring in pyrite. The LREE of gold-bearing pyrite is as higher as 171.664 ppm on average,with relatively higher light rare earth elements(LREE;159.556 ppm) and lower HREE(12.108 ppm).TheΣLREE/ΣHREE ratio is 12.612 and(La/Yb)_N is 11.765.These indicate that pyrite is rich in LREE.The(La/Sm)_N ratio is 3.758 and that of(Gd/Yb)_N is 1.695.These are obvious LREE fractionations.The rare earth element(REE) distribution patterns show obvious Eu anomaly with averageδEu values of 0.664,andδCe anomalies of 1.044.REE characteristics are similar to those of wall rocks(regional metamorphic rocks),but different from those of the Dexing granodiorite porphyry and Damaoshan biotite granite.These features indicate that the ore-forming materials in the Jinshan gold deposit derived from the wall rocks, and the ore-forming fluids derived from metamorphic water.The Co/Ni ratio(average value 0.38) of pyrite suggests that the Jinshan gold deposit formed under a medium-low temperature.It is inferred from the values of high-field strength elements,LREE,Hf/Sm,Nb/La,and Th/La of the pyrite that the ore-forming fluids of the Jinshan gold deposit derived from metamorphic water with Cl〉F.展开更多
In order to study the accumulation mechanism of"barkinite",eight Late Permian channel benches(approximately 15-cm across and 10-cm deep) were taken from the Jinshan Mine,Anhui Province,China.The samples were analy...In order to study the accumulation mechanism of"barkinite",eight Late Permian channel benches(approximately 15-cm across and 10-cm deep) were taken from the Jinshan Mine,Anhui Province,China.The samples were analyzed by microscopical and geochemical methods.The microscopical observations indicate that the occurrence modes of"barkinite"in this area are different from those in other areas of China.The ratios of structureless"barkinite"are much higher in the Jinshan Mine,probably due to the flow-water and marine influenced environments.Furthermore, vitrinite macerals also show a strong fluorescence.The vitrinite fluorescence characteristics have not been observed in the Permian"barkinite"coals from northern China.The composition and variation of minerals in the column section also showed that the swamps in the study area were seriously influenced by seawater in the early and late stage during the peat accumulation.展开更多
The Jinshan gold deposit is located in the Northeast Jiangxi province,South China,which related to the ductile shear zone.It contains two ore types,i.e.the alteration-type ore and the goldbearing quartz vein ore.Rb-Sr...The Jinshan gold deposit is located in the Northeast Jiangxi province,South China,which related to the ductile shear zone.It contains two ore types,i.e.the alteration-type ore and the goldbearing quartz vein ore.Rb-Sr age dating is applied to both gold-bearing pyrite in the alteration-type ore and fluid inclusion in the gold-bearing quartz vein to make clear the time of the gold mineralization of the Jinshan deposit.Analytical results of this study yielded that the age of the alteration-type ore bodies is about 838±110Ma,with an initial 87Sr/86Sr value of 0.7045±0.0020.However,the age of the gold-bearing quartz vein-type ore is about 379±49Ma,and the initial 87Sr/86Sr is 0.7138±0.0011.Based on the age data from this work and many previous studies,the authors consider that the Jinshan gold deposit is a product of multi-staged mineralization,which may include the Jinninian,Caledonian,Hercynian,and Yanshanian Periods.Among them,the Jinninian Period and the Hercynian Period might be the two most important ore-forming periods for Jinshan deposit.The Jinninian Period is the main stage for the formation of alteration-type ore bodies,while the Hercynian Period is the major time for ore bodies of gold-bearing quartz vein type.The initial values of the 87Sr/86Sr from this study,as well as the previous isotope and trace element studies,indicate that the ore-forming materials mainly derived from the metamorphic wall rocks,and the ore-forming fluids mainly originated from the deep metamorphic water.展开更多
In order to understand the diagenesis and its influence on porosity and permeability of sandstones from Yingcheng Formation in Jinshan field,applying thin sections,casting and scanning electron microscope,the authors ...In order to understand the diagenesis and its influence on porosity and permeability of sandstones from Yingcheng Formation in Jinshan field,applying thin sections,casting and scanning electron microscope,the authors studied petrography,diagenesis,porosity and permeability of Yingcheng Formation sandstone reservoir. The results show that the reservoir of Yingcheng Formation is mainly composed of lithic arkoses. Sandstones experienced compaction,pressolution,cementation,metasomatism and dissolution. The primary pores of the sandstones are undeveloped; most of pores are the secondary pores,which are mainly intragranular dissolution pores in feldspar and debris. The compaction and cementation reduced the primary pores in sandstones,the porosity and permeability decreased; while the dissolution formed the secondary pores,resulting in the porosity and permeability increase. Due to compaction and cementation,the porosity and permeability are reduced with increasing of depth. There exists an abnormal enlargement of porosity and permeability within a depth range 2310--2450 m. In combination with analysis of petrology,the dissolution of feldspar and debris is most developed in the depth range. Therefore,compaction,cementation and dissolution are the important factors which affect the porosity and permeability of sandstones.展开更多
Ceramics in China has thousands of years of history, fragile is the natural properties of ceramics, then the ceramic rcpan technology has become China's ceramic history and crafts history of one of the important cont...Ceramics in China has thousands of years of history, fragile is the natural properties of ceramics, then the ceramic rcpan technology has become China's ceramic history and crafts history of one of the important content. Jinshan is a way to rcpai, porcelain with lacquer art. with a strong decorative. With a near perfect means to lace the imperfect, to create a magnificent art boutique.展开更多
The Jinshan gold deposit consists of gold\|bearing ultramylonite and gold\|bearing quartz vein ores. The Rb\|Sr isochron age of fluid inclusions in quartz from quartz veins is the same as that of the gold\|bearing ult...The Jinshan gold deposit consists of gold\|bearing ultramylonite and gold\|bearing quartz vein ores. The Rb\|Sr isochron age of fluid inclusions in quartz from quartz veins is the same as that of the gold\|bearing ultramylonite, suggesting that both the types of orebodies were formed simultaneously in the Caledonian period, in the range 406-409 Ma. REE patterns and sulfur, lead, carbon, hydrogen and oxygen isotope data, as well as the composition of fluid inclusions, have shown that the ore\|forming fluids were derived from formation water, and the ore\|forming materials came from the gold\|hosted rocks. The Jinshan gold deposit occurring in a Caledonian brittle\|ductile zone in metamorphosed microclastic rocks owes its origin to Caledonian reworking processes.展开更多
The Chinese painting Flood Ouerflows Jinshan Temple draws its subject from a beautiful and well-known legend,The white Snake.In the tale Jinshan was an islet in the Yangtze River of yesteryear.Inorder to aave her husb...The Chinese painting Flood Ouerflows Jinshan Temple draws its subject from a beautiful and well-known legend,The white Snake.In the tale Jinshan was an islet in the Yangtze River of yesteryear.Inorder to aave her husband kept in a temple at the top of the isle.Bai Niangzi.incarnation of the whitesnake.bravely fought Monk Fahat.She borrowed the Yangtze River’s water to overcome Jinshan Templeand force Fahai to release her husband.展开更多
你也许已从本期目录中发现:一个新专栏又诞生了!Denise Noblet,一位来自澳大利亚的作家,现执教于上海金山区。她的文章感情真挚,坦诚热情,行文优美,读Denise的文章,既可学到新鲜活泼的英语,特别是散发澳大利亚“风味”的遣词造句,乃至...你也许已从本期目录中发现:一个新专栏又诞生了!Denise Noblet,一位来自澳大利亚的作家,现执教于上海金山区。她的文章感情真挚,坦诚热情,行文优美,读Denise的文章,既可学到新鲜活泼的英语,特别是散发澳大利亚“风味”的遣词造句,乃至拼写,比如本文的标题中的G’day,Denise称:“G’dayis Australian for“Good day”。We often use it instead of“hello”,同时,读者还可窥见一个外国人是从怎样的视角来认识中国。现在,越来越多莘莘学子远游到澳大利亚去留学。读者朋友,假如你有问题想问,写信或发email给本刊,本刊将择要请Denise作答。】展开更多
Denise Noblet的这篇文章有感而发,真情动人,却让人抱憾!她已经离开了上海市金山区的那所学校。回到澳大利亚。而她现在的“接班者”(另一老外)向她倾诉了内心的痛苦。这些痛苦勾起了她对往事的回忆。一个澳大利亚的教师,不远万里,来到...Denise Noblet的这篇文章有感而发,真情动人,却让人抱憾!她已经离开了上海市金山区的那所学校。回到澳大利亚。而她现在的“接班者”(另一老外)向她倾诉了内心的痛苦。这些痛苦勾起了她对往事的回忆。一个澳大利亚的教师,不远万里,来到中国,向学生传授英语知识,尽心尽力。想方设法。然而,结果并不美好!Denise Noblet在文章中披露了这样一个令人心痛的事实:Once, theywere so naughty that I stormed outside and cried while they laughed at me through the windows. 本文发人深省的一句是:This is not an indictment(本义:控告)on the students, but rather a failing of the Chinese education system.展开更多
基金supported by the National Natural Science Foundation of China (40373025)
文摘Rare earth element(REE) is widely used in various fields of geology.Study of the existing forms of REE in geological objects is a necessity for us to solve geological problems related with REE.This paper tried to make it clear the existing forms of REE in gold-bearing pyrite in Jinshan gold deposit by stepwise dissolution test with ICP-MS analysis.Results showed that content of REE in fluid-inclusions of gold-bearing pyrite was very low,which only took about 0.07%–0.70% of the ΣREE,and that of pyrite phase ...
基金supported by the National Natural Science Foundation of China(No. 40373025)
文摘Jinshan gold deposit is located in northeastern Jiangxi,South China,which is related to the ductile shear zone.It has a gold reserve of more than 200 tons,with 80%of gold occurring in pyrite. The LREE of gold-bearing pyrite is as higher as 171.664 ppm on average,with relatively higher light rare earth elements(LREE;159.556 ppm) and lower HREE(12.108 ppm).TheΣLREE/ΣHREE ratio is 12.612 and(La/Yb)_N is 11.765.These indicate that pyrite is rich in LREE.The(La/Sm)_N ratio is 3.758 and that of(Gd/Yb)_N is 1.695.These are obvious LREE fractionations.The rare earth element(REE) distribution patterns show obvious Eu anomaly with averageδEu values of 0.664,andδCe anomalies of 1.044.REE characteristics are similar to those of wall rocks(regional metamorphic rocks),but different from those of the Dexing granodiorite porphyry and Damaoshan biotite granite.These features indicate that the ore-forming materials in the Jinshan gold deposit derived from the wall rocks, and the ore-forming fluids derived from metamorphic water.The Co/Ni ratio(average value 0.38) of pyrite suggests that the Jinshan gold deposit formed under a medium-low temperature.It is inferred from the values of high-field strength elements,LREE,Hf/Sm,Nb/La,and Th/La of the pyrite that the ore-forming fluids of the Jinshan gold deposit derived from metamorphic water with Cl〉F.
基金supported by the National Science Fundamental of China Project(No.40773040)by the project of the Science Foundation of Hebei(Nos. D2009000832 and D2008000727).
文摘In order to study the accumulation mechanism of"barkinite",eight Late Permian channel benches(approximately 15-cm across and 10-cm deep) were taken from the Jinshan Mine,Anhui Province,China.The samples were analyzed by microscopical and geochemical methods.The microscopical observations indicate that the occurrence modes of"barkinite"in this area are different from those in other areas of China.The ratios of structureless"barkinite"are much higher in the Jinshan Mine,probably due to the flow-water and marine influenced environments.Furthermore, vitrinite macerals also show a strong fluorescence.The vitrinite fluorescence characteristics have not been observed in the Permian"barkinite"coals from northern China.The composition and variation of minerals in the column section also showed that the swamps in the study area were seriously influenced by seawater in the early and late stage during the peat accumulation.
基金supported by the National Natural Science Foundation of China (No. 41202083, 40373025)the Research Award Fund for Outstanding Middle-aged and Young Scientist of Shandong Province (BS2013HZ024)
文摘The Jinshan gold deposit is located in the Northeast Jiangxi province,South China,which related to the ductile shear zone.It contains two ore types,i.e.the alteration-type ore and the goldbearing quartz vein ore.Rb-Sr age dating is applied to both gold-bearing pyrite in the alteration-type ore and fluid inclusion in the gold-bearing quartz vein to make clear the time of the gold mineralization of the Jinshan deposit.Analytical results of this study yielded that the age of the alteration-type ore bodies is about 838±110Ma,with an initial 87Sr/86Sr value of 0.7045±0.0020.However,the age of the gold-bearing quartz vein-type ore is about 379±49Ma,and the initial 87Sr/86Sr is 0.7138±0.0011.Based on the age data from this work and many previous studies,the authors consider that the Jinshan gold deposit is a product of multi-staged mineralization,which may include the Jinninian,Caledonian,Hercynian,and Yanshanian Periods.Among them,the Jinninian Period and the Hercynian Period might be the two most important ore-forming periods for Jinshan deposit.The Jinninian Period is the main stage for the formation of alteration-type ore bodies,while the Hercynian Period is the major time for ore bodies of gold-bearing quartz vein type.The initial values of the 87Sr/86Sr from this study,as well as the previous isotope and trace element studies,indicate that the ore-forming materials mainly derived from the metamorphic wall rocks,and the ore-forming fluids mainly originated from the deep metamorphic water.
文摘In order to understand the diagenesis and its influence on porosity and permeability of sandstones from Yingcheng Formation in Jinshan field,applying thin sections,casting and scanning electron microscope,the authors studied petrography,diagenesis,porosity and permeability of Yingcheng Formation sandstone reservoir. The results show that the reservoir of Yingcheng Formation is mainly composed of lithic arkoses. Sandstones experienced compaction,pressolution,cementation,metasomatism and dissolution. The primary pores of the sandstones are undeveloped; most of pores are the secondary pores,which are mainly intragranular dissolution pores in feldspar and debris. The compaction and cementation reduced the primary pores in sandstones,the porosity and permeability decreased; while the dissolution formed the secondary pores,resulting in the porosity and permeability increase. Due to compaction and cementation,the porosity and permeability are reduced with increasing of depth. There exists an abnormal enlargement of porosity and permeability within a depth range 2310--2450 m. In combination with analysis of petrology,the dissolution of feldspar and debris is most developed in the depth range. Therefore,compaction,cementation and dissolution are the important factors which affect the porosity and permeability of sandstones.
文摘Ceramics in China has thousands of years of history, fragile is the natural properties of ceramics, then the ceramic rcpan technology has become China's ceramic history and crafts history of one of the important content. Jinshan is a way to rcpai, porcelain with lacquer art. with a strong decorative. With a near perfect means to lace the imperfect, to create a magnificent art boutique.
文摘The Jinshan gold deposit consists of gold\|bearing ultramylonite and gold\|bearing quartz vein ores. The Rb\|Sr isochron age of fluid inclusions in quartz from quartz veins is the same as that of the gold\|bearing ultramylonite, suggesting that both the types of orebodies were formed simultaneously in the Caledonian period, in the range 406-409 Ma. REE patterns and sulfur, lead, carbon, hydrogen and oxygen isotope data, as well as the composition of fluid inclusions, have shown that the ore\|forming fluids were derived from formation water, and the ore\|forming materials came from the gold\|hosted rocks. The Jinshan gold deposit occurring in a Caledonian brittle\|ductile zone in metamorphosed microclastic rocks owes its origin to Caledonian reworking processes.
文摘The Chinese painting Flood Ouerflows Jinshan Temple draws its subject from a beautiful and well-known legend,The white Snake.In the tale Jinshan was an islet in the Yangtze River of yesteryear.Inorder to aave her husband kept in a temple at the top of the isle.Bai Niangzi.incarnation of the whitesnake.bravely fought Monk Fahat.She borrowed the Yangtze River’s water to overcome Jinshan Templeand force Fahai to release her husband.
文摘你也许已从本期目录中发现:一个新专栏又诞生了!Denise Noblet,一位来自澳大利亚的作家,现执教于上海金山区。她的文章感情真挚,坦诚热情,行文优美,读Denise的文章,既可学到新鲜活泼的英语,特别是散发澳大利亚“风味”的遣词造句,乃至拼写,比如本文的标题中的G’day,Denise称:“G’dayis Australian for“Good day”。We often use it instead of“hello”,同时,读者还可窥见一个外国人是从怎样的视角来认识中国。现在,越来越多莘莘学子远游到澳大利亚去留学。读者朋友,假如你有问题想问,写信或发email给本刊,本刊将择要请Denise作答。】
文摘Denise Noblet的这篇文章有感而发,真情动人,却让人抱憾!她已经离开了上海市金山区的那所学校。回到澳大利亚。而她现在的“接班者”(另一老外)向她倾诉了内心的痛苦。这些痛苦勾起了她对往事的回忆。一个澳大利亚的教师,不远万里,来到中国,向学生传授英语知识,尽心尽力。想方设法。然而,结果并不美好!Denise Noblet在文章中披露了这样一个令人心痛的事实:Once, theywere so naughty that I stormed outside and cried while they laughed at me through the windows. 本文发人深省的一句是:This is not an indictment(本义:控告)on the students, but rather a failing of the Chinese education system.