同沉积断裂对沉积的控制作用——以乌尔逊凹陷为例

本文主要探讨同沉积断裂对沉积充填、层序结构、砂分散体系、凹陷迁移规律等的控制作用,乌尔逊凹陷作为陆内裂谷盆地内二级凹陷断层十分发育,以其为例探讨同沉积断裂活动控制下的凹陷沉积作用。     

古氧相分析在黄骅拗陷歧南次凹沙河街组沉积环境研究中的应用

把古氧相分析理论与方法应用于黄骅拗陷歧南次凹古近系沙河街组沉积环境研究之中,通过古氧相分析中的微量元素V/Cr和Ni/Co分析,以及岩石与古生物分析表明,歧南次凹沙河街组具有以常氧为主、贫氧为辅的沉积环境;同时,古盐度分析指示为咸水、半咸水环境,地球物理学(地震、布格重力异常)研究结果为深水封闭湖泊环境,对比分析认为歧...     

珠江口盆地白云凹陷珠海组碎屑岩储层特征及成因机制

通过岩石铸体薄片、粒度分析和压汞分析等手段,分析白云凹陷珠海组储层的岩石学特征和物性演化特征,研究沉积环境和成岩演化过程对储层特征的影响机制。研究结果表明:储层主要以长石质石英砂岩和长石岩屑质石英砂岩为主,颗粒支撑并以碳酸盐、自生石英和黏土矿物接触式胶结。储层物性总体具有中低孔中低渗特征,以粒间溶蚀扩大孔为主,其次为珠海组底部黏土膜保护的原生孔隙,分选好的中-粗喉型喉道使孔隙连通性良好;在凹陷西斜坡,珠海组上部和底部分别发育钙质砂岩夹层和铁泥质砂岩夹层。三角洲前缘环境是珠海组储层物性良好的先决条件;酸性流体的溶蚀溶解作用和绿泥石黏土膜保护是储层物性较好的根本原因,压实作用是粒间孔隙损失的主要原因,而部分储层渗透率较低是因为自生石英和黏土矿物充填喉道;钙质砂岩夹层物性差是胶结作用所致,而铁泥质砂岩夹层物性差是压实和胶结共同作用的结果。     

关于保持党的纯洁性的理论思考

保持党的纯洁性是马克思主义政党的本质要求。中国共产党自建党以来始终重视保持党的纯洁性,因为它是党的生命力和战斗力源泉,是党取得新民主主义革命、社会主义建设和改革开放伟大胜利的保证。当前我们要从保障改善民生、改进工作作风和改革党内民主等方面着手,保持党的纯洁性。     

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.     

Origin软件在测稳压管伏安特性实验数据处理中的应用

简要介绍了计算机在实验数据处理中的应用，利用THMR-1型电阻元件伏安特性测量实验仪测稳压管的伏安特性，通过origin软件对该实验数据进行处理，以便更好地将origin软件应用于物理实验数据的处理．     

鸟类起源研究取得重大进展

鸟类起源于兽脚类恐龙的假说得到了广泛承认,但鸟类起源研究方向依然存在许多薄弱环节,主要包括鸟类手指同源问题、兽脚类分异时间框架问题以及羽毛起源和早期演化的一些问题。我们近年来在这些问题上取得了一系列重要进展。化石资料显示,兽脚类恐龙在向鸟类进化当中,其外侧两指退化;而现代发育学证据表明,鸟类手指是两侧退化,保留了中间3指。我们通过研究新疆侏罗系地层中发现的泥潭龙,提出了一种外侧和两侧退化模式结合的新假说。该假说可以解释古生物学与发育学资料之间的矛盾。我们报道的一件产自辽宁中上侏罗统髫髻山组的近鸟龙化石,代表了早于始祖鸟的带羽毛的物种,我们提出了包括鸟类在内的主要兽脚类恐龙类群出现于中侏罗世的一个快速演化事件,解决了有关鸟类兽脚类恐龙起源假说的时间悖论问题。我们报道了在北票龙化石中发现的一种新的原始羽毛类型,给出了发育学解释,推测羽毛起源的时间可能在三叠纪中期,对于羽毛起源和早期演化研究具有重要意义。     

浅谈我国古汉字的绘画艺术美

本文从绘画的角度，阐释了古汉字的起源、演变以及汉字本身所蕴含的绘画艺术美和书法艺术。     

糖类遗传与生命起源

从遗传学角度探讨了糖类与生命起源，讨论了遗传学上的再认识，提出糖类在遗传学上扮演着重要、核心的角色、糖类是生命起源物质，基因是糖类衍生物。生命诞生过程可能是：先有糖类、然后有氨基酸和碱基；磷酸及其盐类既是生命物质的组成部分、也是催化剂，阳光或地热为能源，于是诞生了基因。生命体是分子相互作用、有序组合、自我调控的耗散体系。     

缅甸翡翠砾石中蓝雾和黑皮的成因探讨

 通过对缅甸翡翠砾石产区地质背景、样品观察、矿物学及地球化学等分析，认为蓝雾以及黑皮是在沉积深埋成岩过程中，在有一定温度、压力和流体介质作用下形成的，硬玉的水解溶蚀和绿泥石的沉淀是蓝雾以及黑皮形成的主要原因，形成绿泥石的物质来源有来自硬玉水解溶蚀的组分和来自沉积层中的流体、填隙物中的Fe、Mg等元素的加入，有机质的存在可能促进了Fe、Mg等物质的迁移及沉淀作用。