Late Mesozoic metamorphic core complexes: new constraints on lithosphere thinning in North China

Metamorphic core complexes (mcc’s) are among the most prominent structural styles of lithosphere extension and thinning during late Mesozoic in North China. In this paper, the geometrical, kinematic and age characteristics of some of the mcc’s, e.g. Liaonan, Waziyu (Yiwulüshan), Yunmengshan, etc., are discussed. Some common characteristics, such as kinematic polarity, geometric asymmetry, occurrence over a time span, scattered and isolated distribution, and progressive development, can provide direct constraints on the regional lithosphere extension and thinning in North China, which does not favor the prevailing plume model，a general delamination model or extensional collapse of overthickened orogenic crust. We argue that several aspects, such as the kinematic polarity at depths during lithosphere extension, gradual break-up of lithosphere plate, relationship between magmatism and regional extension, and coeval activity of mcc’s and Tan Lu fault, should be taken into consideration when constructing a more reasonable model for lithosphere extension and thinning in North China.     

论两宋时期的历史教育

两宋时期,历史教育受到了统治阶级的高度重视。历史教育形式多样,内容丰富,既有针对统治者而开展的以资政、资治为目的的历史教育,又有系统传授历史知识、以培德育人为目的的学校历史教育,同时还有面向普通民众的社会历史教育,极大地促进了两宋历史教育的大众化和通俗化,推动了历史教育的不断发展。     

19世纪吉尔吉斯北部多民族居住格局的形成及影响

19世纪中期沙俄征服吉尔吉斯人之后,将大批俄罗斯、乌克兰农民迁入吉尔吉斯地区.19世纪70、80年代中国西北陕甘回民起义失败后逃入中亚东干人和一部分被迁入中亚的德意志人最终也大部分在吉尔吉斯北部定居下来.大量移民迁居到吉尔吉斯北部地区改变了吉尔吉斯斯坦民族成分和物质文化的构成,打破了吉尔吉斯旧的社会结构,改变了吉尔吉斯斯坦的民族分布格局.     

云南降水场与太平洋海温场典型相关分析

 利用典型相关理论分析云南省5月份降水场与头年5月至当年4月各月太平洋热带海温距平场之间的关系,得出一些有意义的结果.并通过1994～1995年的预报,效果较理想.     

魏晋南北朝的藏书及其影响

魏晋南北朝有官府、民间(私家)、寺观等多种藏书形式.藏书对目录学、历史撰述和文学产生了深刻的影响.     

Modeling studies on the changes of the Subtropical High over the Western Pacific during the last 100 years

Intensity index series of Subtropical High over the Western Pacific was constructed according to modeling results by using of CCM3.6 atmospheric model with climatologically SST forcing for 30 years, and with observed SST forcing from 1900 to 2000. The index series constructed by modeling closely correlated to the observations for 1951-1999 (c.c. 0.72) and to the statistically reconstructed one for 1900-1950 (c.c. 0.51). The index series for 1900-1999 showed significant 80 a and 40 a periodicity. A minimum of persistence in seasonal variations of the index occurred in Autumn, which was called "Autumn Barrier". It may relate to the "Spring Barrier", found in the seasonal variations of SST over the Eastern Equatorial Pacific. The increasing trend shown in the index series for the 20th century may associate with the global warming caused by enhancement of greenhouse effect.     

南水北调中线工程水量调度仿真系统研究

采用面向对象的建模方法与仿真技术，建立南水北调中线工程系统仿真模型，开发系统仿真试验平台，借助该平台模拟水量调度过程，可合理充分地利用各种水资源，实现水资源的优化配置，为决策部门提供有效可靠的参考方案，通过系统的仿真试验，近期调水方案能够较好地解决华北地区的缺水问题。     

河北省丰宁地区两类碱长花岗质岩石

冀北丰宁地区的小坝子潜流纹岩、黑山咀流纹斑岩、老虎沟门花岗岩和窟窿山花岗岩是空间上紧密共生、生成时间相近和矿物组成相似的碱长花岗质岩石，也是华北地区中生代晚期岩浆作用的代表性产物。本文报导了这些岩石的地质学、岩相学的岩石地球化学资料，比较了它们的异同，探讨了物质来源问题，提出它们可以划分为两种成因类型，即一类来源于较浅部的、以火成表壳岩为主的变质物质、另一类为较深部的火成物质的观点。     

An in situ zircon Hf isotopic,U-Pb age and trace element study of banded granulite xenolith from Hannuoba basalt： Tracking the early evolution of the lower crust in the North China craton

Backscattered electron images, in situ Hf isotopes, U-Pb ages and trace elements of zircons in a banded granulite xenolith from Hannuoba basalt have been studied. The results show that the banded granulite is a sample derived from the early lower crust of the North China craton. It is difficult to explain the petrogenesis of the xenolith with a single process. Abundant information on several processes, however, is contained in the granulite. These processes in-clude the addition of mantle material, crustal remelting, metamorphic differentiation and the delamination of early lower crust. About 80% of zircons studied yield ages of 1842 ±40 Ma, except few ages of 3097-2824 Ma and 2489-2447 Ma. The zircons with ages older than 2447 Ma have high εHf (up to +18.3) and high Hf model age (2.5-2.6 Ga), indicating that the primitive materials of the granulite were derived mainly from a depleted mantle source in late Archean. Most εhf of the zircons with early Proterozoic U-Pb age vary around zero, but two have