Fluidization： An Important Process in the Formation of the Qiyugou Au-bearing Breccia Pipes in Central China

Fluidization processes based on experiments are reviewed to gain some useful insights and comparisons with those that occur in hydrothermal systems. Field and petrographic work, and microscope observation were carried out on samples from the Qiyugou Au-bearing breccia pipes from the East Qinling region, Henan Province. Evidence from macro- and micro-textures suggests that the style of breccias in the Qiyugou area can be grouped into three types： （1） jigsaw fit-stockwork texture, in which the interval between clasts is marked by fractures or filled with calcite or quartz veins; （2） larger breccias that are supported by smaller breccias, rock flour and alteration materials; in this type clasts moved over short distances, creating open spaces; （3） fluidized texture, where the clasts of different lithologies have rounded shapes. These observations are compared with those resulting from experiments on fluidization processes. The results of this comparison suggest that fluidization is an important geological process in the formation of the Qiyugou Au-bearing breccia pipes and gold mineralization. In addition, fluidization processes such as expansion, bubbling, slugging, channeling and spouting must have contributed to the formation of the pipes and were conducive to the development of gold mineralization. In the Qiyugou breccia pipes, gold mineralization occurs as disseminations, in stockwork veins, and open space infills. The ore zones form subparallel sheets that are nearly perpendicular to the walls of the pipes.     

一种特殊的地貌现象——碟形洼地群及其成因的探索

使用1926年出版的五万分之一顺直地形图作历史地貌分析，在河北平原西部白洋淀流域地区发现有数量众多、形态奇特的地貌——碟形洼地。用计算机数字地形模拟(DTM)方法对该洼地的个体形态和总体分布特征进行研究，并与国内外其他地区已报道的陨石雨冲击坑对照，判断白洋淀流域的碟形洼地群可能是分布在第四纪松散沉积物上的陨石冲击坑的遗迹。推测冲击可能发生在全新世中—晚期，洼地群是一次规模巨大的陨石雨冲击所形成的。     

新疆塔里木盆地艾协克—桑塔木南地区油气地球化学指标的多重分形性分析

用分形与多重分形的方法研究地球化学场中地球化学指标的分布规律具有重要的意义。本文运用多重分形矩方法研究了新疆塔里木盆地艾协克一桑塔木南地区2000km^2内采集的2085个土壤样中20项油气化探指标的多重分形谱函数形态特征。结果表明，主要成油气指示指标的多重分形谱基本上呈单一“钩状”，显示较弱的多重分形或单一分形；而其他指标多显示较强的多重分形特征。这些性质在研究区广泛存在，将对区域含油性研究有重要的指示意义。     

渤海湾盆地南堡凹陷新近系馆陶组沉积特征

南堡凹陷位于渤海湾盆地黄骅坳陷北部，新近系馆陶组是该凹陷的重要勘探层段。馆陶组以辫状河沉积为主，中段发育曲流河沉积。其油气勘探的首要问题是优质储集砂体的精确对比及有利盖层分布预测。根据高分辨率层序地层学理论以及录井和测井资料，对馆陶组的层序地层样式、沉积特征和储盖组合进行了分析。研究结果表明，该地层具有两种短期旋回和四个中期旋回。在两种短期旋回中，一种是低可容纳空间的非对称旋回，另一种是高可容纳空间的对称旋回。四个中期旋回中，两个以上升半旋回为主体(MSC1、MSC2)，一个是对称旋回(MSC3)，一个以下降半旋回为主体(MSC4)。短、中期旋回均以非对称旋回为主。该地层的长期基准面具有缓慢上升而后快速下降的特点。从MSC1到MSC4旋回，沉积相呈现出冲积扇-辫状河→辫状河-曲流河→曲流河-辫状河相组合的演化过程。自北向南，各中期旋回的可容纳空间增大，沉积主体由砾质河道渐变为砂质河道。由于受基准面中期旋回格架控制，南堡凹陷馆陶组发育上、中、下三套储盖组合。上部储盖组合，因其储、盖层条件最好，应是馆陶组最重要的油气勘探层系。     

大鼠肝炎性假瘤模型的建立与影像学表现

本研究的目的是建立一种可供于影像学研究的大鼠肝炎性假瘤（ＩＰＬ）模型,并研究其影像学的特征。所用的材料和方法是将弗氏佐剂０１ｍｌ／只作大鼠深部注射,１０天后观察大鼠病灶的影像学特征;并取标本做病理检查。结果发现了ＩＰＬ发生率为９０％,大小分别是０３２±０１８ｃｍ。ＩＰＬ的影像学特征表现为强回声结节;ＣＴ平扫为低度圆形影,无强化或仅轻微强化;Ｔ１ＷＩ则呈等或高信号,Ｔ２ＷＩ为略高信号。病理学证实局部肝组织片状坏死并有纤维组织增生及炎细胞浸润。结论是本文研究的大鼠肝炎性假瘤模型具有易建立、容易复制、成功率高、制备周期短和影像学的表现较典型等特点,对今后探讨大鼠肝炎性假瘤的形成机制及影像学特征将发挥积极作用     

A Peculiar Broad Line Radio Galaxy 1938-155： VLA Observation at 90 cm

We observed 1938-155, a broad line radio galaxy (BLRG), with the Very Large Array (VLA) at 90cm with an angular resolution of 6.8" × 4.0". The source consists of two components separated by 4 arcsec (- 20kpc, for H0 = 65km s-1 Mpc-1, q0 = 0.5) along the SE-NW direction. Both components show steep-spectra with a similar spectral index α - 0.83 ± 0.07 (Sv ∝ v-α). The bright double components are surrounded by a low-brightness cocoon. The radio properties of the two bright components are consistent with the hot spots produced by twin jets. An upper limit of - 0.0008 for the core dominance parameter (R) is inferred, suggesting there is no prominent radio core in the source. Assuming a modest viewing angle 30f77, a jet velocity is estimated - 0.07 c, based on the jet to counter-jet brightness ratio (J). The lower limit in jet speed inferred is consistent with no Doppler beaming effect on the jet. The radio galaxy 1938-155 could be an exceptional BLRG with no prominent radio core or jet.     

Design Method of Armour Grate Plates for Sloping Breakwaters

- Laboratory tests have been conducted on the basis of theoretical analysis of stability of armour Grate Plates with reference to 20 structures. Some empirical formulas of statility thickness of Grate Plates have been obtained in consideration of the effects of water depth in front of the structures and critical wave period. The test results have been compared with field data.