东北老工业基地核心城市物流体系规划研究——以哈尔滨市为例

振兴东北老工业基地是我国重大区域发展战略之一,其关键环节在于促使核心城市快速发展,发挥其对区域的带动作用。文章以哈尔滨市为例,分析了核心城市物流发展对推动东北老工业基地振兴的基础作用。在运用城市物流规划理论与方法、借鉴国内外经验的基础上,结合城市发展需要和现存问题,对哈尔滨市城市物流体系规划进行了探讨,为其他城市的物流规划提供了一定的思路和模式借鉴。     

输导通道类型对天然气聚集效率的影响

通过对中国大中型气田天然气输导通道类型及影响因素研究,得到中国大中型气田主要有断裂、断裂与不整合组合、砂体、断裂与砂体组合、不整合与砂体组合和不整合6种输导通道类型。其中以断裂为主,其次是断裂与不整合组合,再次是砂体和断裂与砂体组合,最少为不整合和不整合与砂体组合。它们主要受盆地类型、盆地内构造带类型和源储空间位置关系的影响。由中国大中型气田储量、含气面积和聚集时问,通过求取其天然气聚集效率,把中国大中型气田划分为高效、中效和低效3类气田。通过中国大中型气田天然气聚集效率与输导通道类型之间关系分析,得到聚集时间相对较晚的断裂、砂体和断裂与不整合组合形成的输导通道天然气聚集效率相对较高,有利于快速形成大中型气田。     

青藏高原东北缘共和盆地第四纪磁性地层学研究

共和盆地第四纪剖面磁性地层学研究表明,该剖面包含了四个正极性段,三个负极性段,剖面底部地层年龄约为2.11Ma B.P.。结合剖面的沉积特征和已有的孢粉组合特征分析,可以确定该剖面记录了共和盆地2.11Ma B.P.以来的气候变化,且气候发生转型的主要时期依次为1.92 Ma B.P、1.75Ma B.P.、1.40Ma B.P.、1.02 Ma B.P.和0.87Ma B.P.。其主要原因可能是青藏高原强烈隆升远程效应的结果。共和盆地气候变化时间序列的建立为研究青藏高原隆升及环境效应提供有力证据。      

黄河上游地区崩塌滑坡泥石流地质灾害风险评价

本文在对黄河上游地区崩塌、滑坡、泥石流进行野外地质调查和资料收集的基础上,确定了灾害风险评价的主要影响要素和指标体系,进行了以县(市、旗)为单元的风险评价。评价单元共116个。研究区地质灾害风险共分为5级,高风险单元3个,较高风险单元8个,中等风险单元24个,较低风险单元54个,低风险单元27个。风险评价结果表明,评价区内不同地区崩滑流灾害风险程度相对差异较大,总体分布特点是中部地区较高,北部和南部较低。从风险指数的结果来看,有些风评价单元的风险指数非常接近临界值,一旦危险性条件和易损性条件发生改变,将会引起地质灾害的风险级别发生变化。因此,在西部大开发的进程中,无论是在开发资源还是进行各种工程活动,都应注意保护环境,避免地质灾害向着严重的方向发展。      

Typical Geochemical Elements in Loess Deposit in the Northeastern Tibetan Plateau and Its Paleoclimatic Implication

Widespread and thick loess deposit in the northeastern Tibetan Plateau records paleoclimatic changes over the Quaternary period. In this study, we investigate a loess section located in a high terrace of the Huangshui River in the Xining Basin, and collect samples at 20-cm intervals by digging a well of 16-m depth （including paleosol S1 and SO and several loess interlayers over the last glacial-interglacial cycle and the Holocene）. Concentration of some active elements （Sr and Ca） and inert elements （Rb, Zr, Ti） in these loess samples are measured. The results show that ratios of those elements （oxide）, such as Rb/Sr, Ti/Sr, and Zr/CaO ratios, would indicate sensitively paleoclimatic changes, especially the history of precipitation over the last glacial-interglacial and the Holocene. Moreover, the curves of Rb/Sr, Ti/Sr, and Zr/CaO ratios had almost the same variable trends from the bottom to the top and also closely correlated with values of magnetic susceptibility and the global marine δ^18O record. But compared with the curves of magnetic susceptibility, the changes of ratios of these elements （oxide） are clearer and easy to understand. Therefore, the ratios of these typical chemical elements in the loess deposit may be used as an excellent index to investigate the history of paleoclimate, particularly precipitation changes in the northeastern Tibetan Plateau.     

Report on 34 Ga SHRIMP Zircon Age from the Yuntaishan Geopark in Jiaozuo, Henan Province

1 Introduction According to recent researches, the North China Craton consists of three parts: the eastern block, western block and central zone (Zhao, 2001; Wilde et al., 2002). Paleoarchean continental blocks and zircon residuals have only been found in a few regions, such as Anshan, East Liaoning (Liu et al., 1992; Song et al., 1996; Wan et al., 2002, 2005), Caozhuang, East Hebei (Liu et al., 1992) and Xinyang, West Henan (Zheng et al., 2004), which are mainly distributed in the east…     

Synthesis of Pb-Feldspar by Ion Exchange Reaction and Its Implications

Feldspar and Pb（NO3）2 were mixed and reacted at T=380℃ to synthesize Pb-feldspar. In the XRD （X-ray diffraction） pattern of the product, the d values （crystal lattice spacing） of the five peaks are 0.654, 0.342, 0.332, 0.327 and 0.257 nm. The XPS analysis results show that the binding energy of Pb 4f（7/2） in the feldspar was between 137.81-138.03 eV. Pb^2＋ can replace alkali and alkali earth cations in the feldspar structure through ion exchange reaction to form Pb-feldspar.     

The Basic Shape Classification of Space Debris with Light Curves

We study the machine learning method for classifying the basic shape of space debris in both simulated and observed data experiments, where light curves are used as the input features. In the dataset for training and testing, simulated light curves are derived from four types of debris within different shapes and materials. Observed light curves are extracted from Mini-Mega TORTORA (MMT) database which is a publicly accessible source of space object photometric records. The experiments employ the deep convolutional neural network, make comparisons with other machine learning algorithms, and the results show CNN (Convolutional Neural Network) is better. In simulational experiments, both types of cylinder can be distinguished perfectly, and two other types of satellite have around 90% probability to be classified. Rockets and defunct satellites can achieve 99% success rate in binary classification, but in further sub-classes classifications, the rate becomes relatively lower.     

2003～2004年吴忠、灵武地区地震活动性分析

2003年12月至2004年8月,宁夏吴忠、灵武地区出现了一次地震活动增强过程,与已有震例震前的地震活动增强过程非常相似,因此导致了一次地震短临预测,但此次地震预测后来证实为虚报。从经验预报的角度来看此次地震短临预测的依据是充分的。但利用地震活动加速模型进行分析的结果表明,此次地震活动过程能量释放随时间的加速程度不够,不足以导致一次Ms5．0以上地震的发生。因此认为,现阶段地震预报应结合物理预测方法来进行,以克服经验预报的局限性。     

伽师强震群的深部动力学条件

根据天山造山带及其两侧的塔里木盆地和准噶尔盆地的岩石圈二维速度结构、二维密度结构、二维电性结构、壳幔过渡带的详细结构以及大地热流和震源深度的分布,再结合对新疆西北部的蛇绿岩带、高压变质带和岩浆岩分布的综合分析,建立了天山造山带的地球动力学“层间插入消减”模型。该模型认为,塔里木板块的中上地壳在库尔勒断裂附近向天山造山带的中下地壳层间插入;而下地壳连同岩石圈地幔向天山造山带的上地幔俯冲消减。在天山的西段（哈萨克斯坦境内）,费尔干纳地块由北向南插入到南天山之下约180km的深处,在其东段（中国境内）,塔里木盆地由南向北插入南天山之下。这两个具有不同方向的下降板片的接触部位为费尔干纳走滑断裂。我国的伽师、喀什、乌恰地震区均落在这两个具有不同俯冲方向板块的结合部位附近,有着特殊的深部构造背景。南、北两大板块的双向挤压必定产生强大的应力,在地震区附近,这种应力的积累与释放具有4个显著的特点：（1）板片的俯冲消减速度约高达每年22mm左右;（2）应力的积累与释放速率加快;（3）应力释放较容易;（4）应力释放较为集中。这4个特点可能是伽师地区在较短的时间内连续发生数次强震的构造因素。