Overeducation is widespread across the countries in the world.However,not much is known about the patterns of overeducation in China.This paper examines levels,trends and patterns of overeducation in China over the la...Overeducation is widespread across the countries in the world.However,not much is known about the patterns of overeducation in China.This paper examines levels,trends and patterns of overeducation in China over the last 20 years.Overeducation rate in China increased from 7.24%in 1990to 12.26%in 2000,and further to28.16%in 2010.The pace was much more rapid in the second decade than in the first decade.Overeducation is substantial across all the population subgroups.with widening differentials.Overeducation rates in the big cities like Beijing and Shanghai are much higher than elsewhere in China.China’s rapidly increasing overeducation is largely a result of the implementation of college expansion policy started in the late 1990s.展开更多
The Qilishan gold deposit is located in the southern Zhaolai gold ore belt in the northwestern Jiaodong region.A total of seven gold ore bodies have been found in the mining area.Linglong gneissic biotite granite and ...The Qilishan gold deposit is located in the southern Zhaolai gold ore belt in the northwestern Jiaodong region.A total of seven gold ore bodies have been found in the mining area.Linglong gneissic biotite granite and the NE trending Lingbei fracture control the output and distribution of the gold deposit.The ore bodies with veined or irregular shape occur in the structural alteration zone.The ore bodies of different sizes are NE trending and SE dipping.The constituent minerals of the ores mainly include pyrite,chalcopyrite,native gold,electrum,argentite,matildite,hematite,quartz and calcite.The ores are characterized by metasomatic dissolution structure,as well as veined and brecciated structures.The ore-forming process is divided into four stages,namely quartz-,pyrite-,polymetallic-and carbonate stages.Study on fluid inclusion shows that the deposit is composed of gas-liquid two-phase inclusions （Ⅰ） and three-phase inclusions containing CO2 （Ⅱ）,and that the former dominates.The homogenization temperature is 259.6℃-373.7℃ ; the salinity of three-phase inclusions containing CO2is 5.77%-9.84% （NaCl） ; the salinity of gas-liquid two-phase inclusions is 6.58%-8.54% （NaCl） ; and the estimated ore-forming pressure is 55.2-82.2 MPa.According to the nonlinear relationship between the depth and pressure of the fluid in the fracture zone,the ore-forming depth of the Qilishan gold deposit is calculated as 5.95-7.14 km.It is preliminarily determined that the deposit is a mesophilic and hypothermal gold deposit.展开更多
文摘Overeducation is widespread across the countries in the world.However,not much is known about the patterns of overeducation in China.This paper examines levels,trends and patterns of overeducation in China over the last 20 years.Overeducation rate in China increased from 7.24%in 1990to 12.26%in 2000,and further to28.16%in 2010.The pace was much more rapid in the second decade than in the first decade.Overeducation is substantial across all the population subgroups.with widening differentials.Overeducation rates in the big cities like Beijing and Shanghai are much higher than elsewhere in China.China’s rapidly increasing overeducation is largely a result of the implementation of college expansion policy started in the late 1990s.
基金Supported by Project of Alternative Resources Prospecting in Crisis Mines(No.200623018)
文摘The Qilishan gold deposit is located in the southern Zhaolai gold ore belt in the northwestern Jiaodong region.A total of seven gold ore bodies have been found in the mining area.Linglong gneissic biotite granite and the NE trending Lingbei fracture control the output and distribution of the gold deposit.The ore bodies with veined or irregular shape occur in the structural alteration zone.The ore bodies of different sizes are NE trending and SE dipping.The constituent minerals of the ores mainly include pyrite,chalcopyrite,native gold,electrum,argentite,matildite,hematite,quartz and calcite.The ores are characterized by metasomatic dissolution structure,as well as veined and brecciated structures.The ore-forming process is divided into four stages,namely quartz-,pyrite-,polymetallic-and carbonate stages.Study on fluid inclusion shows that the deposit is composed of gas-liquid two-phase inclusions （Ⅰ） and three-phase inclusions containing CO2 （Ⅱ）,and that the former dominates.The homogenization temperature is 259.6℃-373.7℃ ; the salinity of three-phase inclusions containing CO2is 5.77%-9.84% （NaCl） ; the salinity of gas-liquid two-phase inclusions is 6.58%-8.54% （NaCl） ; and the estimated ore-forming pressure is 55.2-82.2 MPa.According to the nonlinear relationship between the depth and pressure of the fluid in the fracture zone,the ore-forming depth of the Qilishan gold deposit is calculated as 5.95-7.14 km.It is preliminarily determined that the deposit is a mesophilic and hypothermal gold deposit.
