亚洲货币一体化的前景分析

从国际货币体系改革的大趋势——区域性货币一体化入手，分析亚洲货币一体化的现状，认为创造亚洲的共同货币——亚元是亚洲货币一体化的理想选择。并阐述亚洲货币一体化仍然要大致经历欧洲货币一体化所走过的几个阶段。分析中国在东亚货币一体化进程中的地位和作用。     

影响银行卡追透的相关法律问题及其对策

我国银行卡立法相对滞后，致使实务中的一些问题无法解决，将影响银行卡产业的健康发展。本文分析了影响银行卡追透的七个法律问题，并提出了五个对策建议，以期对促进银行卡产业健康发展能有所裨益。     

China＇s Regional Disparity and Its Policy Responses

The fruits of China＇s rapid economic development over the 3 decades have not been distributed fairly across different regions. Using data from a sample of 815 Chinese listed firrns during 1998-2004, our error-correction investment model showes evidence of different financial constraints on firms＇ investment in different regions. We argue that China＇s regional development policies have contributed greatly to the regional inequalities. To control the rising inequality, China has shifted its focus from the coast to the interior regions. However, it is becoming increasingly difficult for the government to direct the economy, as market mechanisms now have afar greater influence on the economy than the government does. The people-centered approach of the current leadership has meant that substantial attention has been placed on regional development disparities in an attempt to build a ＂harmonious society. ＂ China needs further extensive reforms if all the measures for reducing regional disparity are to be effective.     

对《形状和位置公差》新标准的理解和应用

通过对《形状和位置公差》新、旧国际的对比，综述了新、旧标准间的不同之处、便于迅速了解和应用新标准。     

Are Expected Inflation Rates and Expected Real Rates Negatively Correlated? A Long‐Run Test of the Mundell‐Tobin Hypothesis

Some empirical evidence suggests that the expected real interest and expected inflation rates are negatively correlated. This hypothesis of negative correlation is sometimes known as the Mundell‐Tobin hypothesis. In this article we reinvestigate this negative relation from a long‐term point of view using cointegration analysis. The data on the historical interest rate on T‐bills and the inflation rate indicate that the Mundell‐Tobin hypothesis does not hold in the long run for the United States, the United Kingdom, and Canada. We also obtain similar results using the real interest rate on index‐linked gilt traded in the United Kingdom.     

From T-Bills to Stocks: Seasonal Anomalies Revisited

This paper employed eleven data series which consist of stocks, bonds, bills, equity premiums, term premiums, and various default premiums to investigate whether January seasonality reported in existing literature is robust across different states of the economy as this has important trading implications. For the periods 1926–1990, small stocks, small stock premiums, low grade bonds, and default premiums (spread between high grade, low grade and government bonds) reveal January seasonality and that the seasonality is robust across different states of the economy except for low grade bond returns and default premiums. January seasonality for low grade bond returns and low grade bond default premiums are primarily driven by results found during periods of economic expansion. Overall, January seasonality is more evident during the economic expansion periods although the magnitude of default premiums is larger during periods of economic contraction. Furthermore, prior findings of strong summer equity returns are primarily driven by the results found during the periods of economic contraction. It is also found that equity returns are generally higher during periods of economic expansion.     

井陉西部地区白云岩矿特征及其成因

河北省井陉西部地区白云岩分布广泛，约占此区面积三分之一，主要为三山子白云岩，其中一段赋存有工业价值的白云岩矿体，目前尚未充分开发利用。本文对白云岩矿的地质特征、成因和形成环境等进行了探讨，以引起有关部门和人士的关注，而得以充分开发利用。     

窄岭金矿剪切带基本特征与发展演化模式

河北丰宁窄岭金矿,可以区分3幕Ⅰ级韧性剪切带,1幕Ⅱ级脆韧性剪切带和1幕Ⅲ级脆性剪切带。伴随不同的剪切变形变质作用,分别有花岗岩(红旗菅子群花岗片麻岩)→闪长岩(变闪长岩)→正长斑岩→含金石英脉的侵位。而金矿则是这种多期多阶段构造—岩浆复杂演化使金逐步富集的最终产物。     

福建商专心理健康问题的现状与对策思考

本文通过实证分析福建商专学生存在的心理问题,提出对策,深化了心理咨询工作重要性的认识,并体现了福建商专近年来心理健康教育工作的特色.     

汉诺坝玄武岩中麻粒岩捕虏体的发现

近十余年来,中外地质学家对我国河北西北部的汉诺坝玄武岩及其深源包体进行了广泛深入的研究,发现了种类繁多的上地幔岩石捕虏体,发表了不少专著和论文,但有关麻粒岩捕虏体的报导,迄今为止尚未见到。本文作者经过三年的努力,在汉诺坝玄武岩中发现了五类八种麻粒岩捕虏体,其中包括石榴辉石麻粒岩、斜长石榴辉石麻粒岩、斜长单辉麻粒岩、斜长二辉麻粒岩、石榴钾长石英麻粒岩、石榴斜长石英麻粒岩、辉石二长麻粒岩、辉石钾长麻粒岩。初步研究表明这些麻粒岩大部分是在下地壳环境下形成的,它们具有麻粒岩矿物组合和结构构造特征,但又不完全类同于古老高级变质地体中的麻粒岩。