利用H/V方法研究琼北火山区的浅表层地质变化特征

海南琼北活火山作为华南沿海重要的第四纪火山, 一直受到国内外学者的广泛关注, 目前对该火山的形成演化已开展了大量深部地质结构的研究, 但对其表层地质结构特征仍然缺乏详细了解。水平-垂直频谱比法(简称H/V方法)已被广泛应用于浅表层地质结构的研究, 本文基于35个便携式微功耗地震仪组成的流动台阵观测数据, 采用经典全波场H/V_(full)和瑞利波椭圆率H/V_(Ray)分析方法, 获得了琼北火山区H/V曲线峰值频率(F₀)和放大倍数(A₀)的空间变化特征。琼北火山区H/V曲线峰值频率变化强烈, 以长流-仙沟断裂为界, 断裂西南侧很难从H/V曲线中获取清晰的F₀和A₀, 而断裂东北侧则存在明显的F₀和A₀。结合已有地质资料, 本文认为长流-仙沟断裂西南侧处于凹陷区, 其浅表层火山岩未发生明显的风化作用, 而东北侧位于隆起区域, 地表火山岩受到了比较严重的风化作用。这一研究结果表明, H/V方法可反映表层火山岩的风化状态, 火山岩出露场地H/V曲线的峰值频率和放大倍数随风化作用程度的增强而表现得更加明显。本研究为琼北火山区浅表火山岩风化状态和地震危险性评估提供了重要的信息支撑。     

对影响招远市黄金矿山地质环境评价的几点认识

招远市黄金资源蕴藏丰富,开采历史悠久,素有“金城天府”之称,建国以来,累计向国家交售黄金近200t,是全国第一产金大市（县）。其矿山地质环境问题不同于一般的县市,通过对其矿山地质环境特点的分析,认为招远市金矿区矿山地质环境影响评价的重点为采空塌陷,地裂缝,渣石流等地质灾害及水环境等。     

The formation of porphyry copper deposits

Copper is a moderately incompatible chalcophile element. Its behavior is strongly controlled by sulfides. The speciation of sulfur is controlled by oxygen fugacity. Therefore, porphyry Cu deposits are usually oxidized (with oxygen fugacities > ΔFMQ +2) (Mungall 2002; Sun et al. 2015). The problem is that while most of the magmas at convergent margins are highly oxidized, porphyry Cu deposits are very rare, suggesting that high oxygen fugacity alone is not sufficient. Partial melting of mantle peridotite even at very high oxygen fugacities forms arc magmas with initial Cu contents too low to form porphyry Cu deposits directly (Lee et al. 2012; Wilkinson 2013). Here we show that partial melting of subducted young oceanic slabs at high oxygen fugacity (>ΔFMQ +2) may form magmas with initial Cu contents up to >500 ppm, favorable for porphyry mineralization. Pre-enrichment of Cu through sulfide saturation and accumulation is not necessarily beneficial to porphyry Cu mineralization. In contrast, re-melting of porphyritic hydrothermal sulfide associated with iron oxides may have major contributions to porphyry deposits. Thick overriding continental crust reduces the “leakage” of hydrothermal fluids, thereby promoting porphyry mineralization. Nevertheless, it is also more difficult for ore forming fluids to penetrate the thick continental crust to reach the depths of 2–4 km where porphyry deposits form.     

Isolation,purification and characterization of the hydrogen evolution promoting factor of hydrogenase ofSpirulina platensis

A component (s-factor) with obvious promoting effect on hydrogen evolution of hydrogenase has been isolated and extracted from a cell-free preparation ofSpirulina platensis. The effect of the s-factor in the reaction system is similar to that of Na₂S₂O₄, but is coupled with light. The s-factor has the maximum absorption peak at 620 nm in the oxidized state, at 590 nm in the reduced state. The partially purified s-factor showed two bands by SDS-PAGE and is distinctly different from phycocyanin, which has no change of oxidized state and reduced state absorption spectra, and also has no promoting effect on hydrogenase ofSpirulina platensis under the light. The research supported by the NSFC.     

山东省产业重心转移与可持续发展研究

 本文利用经济空间结构的重心研究方法,分析了山东省近八年来产业重心的转移,提出了山东省产业可持续发展战略     

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一种抗简单功耗分析攻击的椭圆曲线标量乘快速实现算法

针对添加伪点加法在抵抗简单功耗分析攻击的同时效率损失过大的问题,为更好兼顾效率与安全,提出一种新的标量乘快速实现算法——随机伪操作法,通过以单片机为核心运算控制芯片的功耗分析平台进行实测分析验证,随机伪操作法不但能够很好抵抗简单功耗分析攻击,而且相对于添加伪点加法运算效率提高30%-50%。     

CATASTROPHIC ECO-ENVIRONMENTAL CHANGE IN THE SONGNEN PLAIN, NORTHEASTERN CHINA SINCE 1900S

Although the Songnen Plain in the northeastern China was developed relatively late in the temperate zone of the world, its eco-environment has changed greatly. This paper analyzes the changes of land cover and the rates and trends ofdesertification during the past 100 years in the Songnen Plain. According to the macroscopic analysis, we find that the eco-environment in the plain has reached to the threshold of catastrophic change since the 1950s. The Thorn Needle Catastrophic Model was used to determine and validate this conclusion. Human activities, including large-scale construction projects, such as huge dams and dikes, and excessive grazing were the primary factors contributing to regional eco-environmental catastrophe. And irrational reclamation of the wilderness also affected the eco-environmental change. The results reveal the complex human-land interactions.     

中国近海棱梭群体形态学和耳石形态学研究

为研究棱梭不同地理群体间的形态差异,使用多元统计分析方法对采集自金门、厦门、虎门、湛江、北海和防城港6个地点邻近海域的棱梭群体样本的形态和矢耳石形态两方面进行比较研究。对棱梭样本的形态研究结合传统形态学和地标形态学开展,对矢耳石的形态研究则将传统耳石形态分析法和椭圆傅里叶分析法相结合,形态和耳石形态数据的分析结果相似。主成分分析结果表明从28个棱梭形态量度指标提取的前8个主成分累积贡献率为65. 868%,从85个耳石形态指标提取的前23个主成分的累积贡献率为79. 290%,根据临界值85. 000%可以推断这6个棱梭群体间形态和耳石形态上的差异不能够单独依靠少数指标来判断;聚类分析的结果总体显示出群体间差异与地理距离等因素相关联的分布规律;在判别分析中形态学量度指标的综合判别正确率为75. 9%,而耳石形态学指标的综合判别正确率略低,为69. 3%;对棱梭形态量度指标的单因子方差分析显示湛江棱梭群体与其他群体在形态上存在显著差异的量度指标较少。栖息地环境、饵料组成和海流等可能是导致形态学差异和耳石形态差异形成的主要因素。另一方面,理化因子的相似性和群体间的交流会减弱群体间形态和耳石形态的差异。