新“港口——腹地”文化模型：广西南流江流域文明史的再发现

受群山限制,局促在一种＂马刺型＂（冂）地理区间的南流江水域,历经＂腹地（桂东南）——港口（北部湾）＂间的长期互动,在岭南旧有的＂腹地（西江）——港口（广州）＂文化发展模式之外,营造了独具一格的南流江本土文化。特别是,在南方稻作文化、佛教来华、妈祖入桂、移民实边与民族融合等多方面,南流江流域文明发展史并没有做成＂西江文明史＂的一个附属分支;相反,南流江流域文明史恰好就是＂中华文明多元一体格局＂在岭南地区的深度演绎。目前,它又是构建＂北部湾文化＂必不可缺的有机部件,更是推进广西现代化进程赖以探寻的＂区域文化力＂。     

Sedimentation processes and sedimentary characteristics of tidal bores along the north bank of the Qiantang Estuary

A tidal bore is a unique Earth surface process, characterized by its highly destructive energy, predictable periodicities and magni-tudes, and the production of characteristic sedimentary features. Tidal bores and associated rapid flood flows are highly turbulent flows of the upper-flow regime with a velocity over several meters per second. Reynolds (Re) and Froude (Fr) numbers, respectively, are larger than 104 and 1.0, making them significantly different from regular tidal flows but analogous to turbidity currents. Until now, understanding of tidal-bore depositional processes and products has been limited because of the difficulty and hazards involved with gauging tidal bores directly. The Qiantang bore is known as the largest breaking bore in the world. Field surveys were carried out in May 2010, along the north bank of the Qiantang Estuary to observe the occurrence of peak bores, including regular observations of current, water level and turbidity at the main channel. Several short cores were sampled on the intertidal flats to study the characteristic sedimentary features of tidal bores. Hydrodynamic and sedimentological studies show that the processes of sediment resuspension, transport and deposition are controlled primarily by the tidal bores, and the subsequent abruptly accelerated and decelerated flood flows, which only account for one tenth of each semidiurnal tidal cycle in the estuary. Tidal-bore deposits are generally poorly sorted because of rapid sedimentation after highly mixed suspension by intense turbulence. This behavior is characteristic of the absence of tractive-current depositional components in a C-M diagram. It also goes along with well-developed massive bedding, graded bedding, basal erosion structures, convolute bedding and dewatering structures. Together, these sedimentary features can constitute fingerprinting of turbidites, widely distributed in the deep-water environment. However, a tidal bore is triggered by intensely deformed tidal waves propagating into a shallow-water environment, which returns to regular tidal flows rapidly after the passage of the bore head. The tidal-bore deposits are usually bounded by the intertidal-flat deposits with typical tidal beddings at the top and on both flanks. The difference between tidal-bore deposits (TBD) and tidal sandy/muddy deposits (TSD/TMD) is evident not only in sedimentary structures, but also in the grain-size composition. They can be clearly distinguished in grain-size bivariate plots, typically the plot of mean grain size vs. standard deviation (or sorting). Some trend variations generally exist in mean grain size with TBD>TSD>TMD, sorting with TMD>TBD>TSD (larger value indicating poorer sorting), and both skewness and kurtosis with TSD>TBD>TMD. These findings will undoubtedly shed new light on our understanding of tidal-bore sedimentology, ancient tidal-bore sedimentary facies and environments, and related oil-and-gas field prospecting.     

汾河下游防洪工程施工措施

通过对堤防、控导工程施工中各阶段要点的分析,提出了施工质量过程控制的措施。     

扬子地台北缘中段中上元古界中金、银矿床稳定同位素地球化学研究

本文系统地研究了扬子地台北缘中段中上元古界中金银矿床的硫、铅、碳、氢、氧同位素组成。研究表明:银洞沟Au-Ag-Pb-Zn矿床、许家坡Au-Ag-Te矿床和白岩沟Au矿床的成矿物质具深源特征,成矿流体为混有少量大气水和岩浆水的变质流体;东沟坝Au-Ag-Pb-Zn重晶石型矿床成矿物质及成矿流体皆具多来源的特征。     

嘉陵江鲿科鱼类骨学研究（Ⅲ）─—头骨的比较

对从嘉陵江合川至北碚段收集的４属１１种科鱼类脊头骨作了系统的比较研究。结果表明，属、黄颡鱼属、拟属和属在下颞骨的有无，嗅神经孔和舌颌骨与颅骨关节面的构成，泪骨的形态，上枕骨嵴的长短及其与背鳍第一辐鳍骨的关系，颅骨的比例性状等方面具有一分明显的属间差异，头骨形态亦可作为种间分类的重要依据之一。     

盘锦地区苇塘及河口鱼类调查

盘锦地区位于辽东半岛东南部,水源丰富,池塘泡沼、水库星罗棋布,适于渔业发展,特别是我省重要河流——辽河在此入海,所以河口及洄游鱼类尤多,我们在野外工作中收集了55种标本,隶属11目24科,观察了生境分布,对盘锦地区水利资源的综合利用有一定意义。     

浙江瓯江口地区平原形成过程

在对瓯江口地区的野外调查的基础上,参阅了有关的考古资料和文献,从沉积学、地貌学、考古学等角度,综合论述了本区包括海湾充填、平原塑造以及岸线变迁的成陆过程。     

长江口悬浮颗粒有机絮凝研究

用带电子探针的扫描电子显微镜分析和测定了长江口悬浮颗粒样品,在不同盐度的试样中,首次发现了大小、形状,组成各不相同的有机絮凝体.作者根据长江口的物理化学环境和悬浮颗粒的性质,探讨了有机絮凝体的形成机理,认为二步桥联模式能比较园满地解释长江口悬浮颗粒有机絮凝体的形成.