山东沿海地区自然灾害与对策

分析山东省沿海地区自然灾害现状及其影响，并预测它的发展趋势，提出加强减灾工程建设与海岸带管理等对策。     

山东中生代橄榄安粗岩系火山岩的地质、地球化学特征及岩石成因

山东中生代橄榄安粗岩系火山岩主要分布在沂沭断裂带及其两侧的断陷型陆相火山盆地中，为早白垩世火山活动的产物．Ｒｂ－Ｓｒ全岩等时年龄变化于１１１．４～１１９．６Ｍａ．岩石组合主要为粗面玄武岩－橄榄安粗岩－安粗岩－粗面岩．这套岩石在化学上具有富碱富钾、富铝贫钛、高氧化系数及富轻稀土和大离子亲石元素的特点，并具有较高的ＩＳｒ值和明显偏低εＮｄ值．根据对岩石地质、地球化学特征和产出构造环境的详细分析，表明这套岩石的成因应主要是富集型地幔的部分熔融     

A Study on the Geological—Geochemical Dynamics of Hydrothermal Ore Deposition as Exemplified by the Muping—Rushan Gold Deposit Belt,Eastern Shandong,China

This paper presents a method of establishing a hydrothermal ore-forming reaction system.On the basis of the study of four typical hydrothermal deposits,the following conclusions concerning geochemical dynamic controlling during hydrothermal mineralization have been sions concerning geochemical dynaamic controlling during hydrothermal mineralization have been drawn:(1)The regional tectonic activities control the concentration and dispersion of elements in the ore-forming process in terms of their effects on the thermodynamic nature and conditions of the ore-forming reaction system.(2)During hydrothermal mineralization the activites of ore-bearing faults can be divideb into two stages:the brittle splitting stage and the brittle-tough tensing stage,which would create characteristically different geodynamic conditions for the geochemical thermodynamic ore-forming system.(3)The hydrothermal ore-forming reaaction system is an open dynamic system.At the brittle splitting stage the system was so strongly supersaturated and unequilibrated as to speed up and enhance the crystallization and differentiation of ore-forming fluids.And at the brittle-tough tensing stage,the ore-forming system was in a weak supersaturated state;with decreasing temperature and pressure the crystallization of oreforming material would show down,and it can be regarded as an equilibrated state.(4)In the lates stages of hydrothermal evolution,gold would be concentrated in the residual ore-forming solution.The pulsating fracture activite in this stage led to the crush of pyrite ore and it was then filled with gold-enriched solution,forming high-grage“fissure”gold ore.This ore-forming process could be called the coupling mechanism of ore formation.     

榴辉岩的化学分类

以山东荣成地区的榴辉岩为例,把榴辉岩分为镁一榴辉岩、铁一榴辉岩和钙一榴辉岩三类。三类榴辉岩的岩石化学,主要造岩矿物成分都有明显差别,石榴石分别是镁铝榴石、铁铝榴石和钙铝榴石。绿辉石的硬玉分子也有不同。三类榴辉岩的化学成分限制是Mg-榴辉岩MgO>10%,石榴石以镁铝榴分子占优势,Fe-榴辉岩的MgO<10,石榴石以铁铝榴石分子占优势。Ca-榴辉岩CaO>19%,石榴石以钙铝榴石分子优势。     

ENSO事件与鲁西北夏季降水的关系

应用近百年ENSO事件的研究成果和ENSO事件影响年的资料，统计分析近50年来ENSO事件与鲁西北夏季降水关系，为短期气候预测和汛期气象服务提供参考依据。     

胜利油区孤南洼陷古、新近系充填层序与沉积环境

孤南洼陷是济阳坳陷沾化凹陷的一个新生代次级洼陷。边界断层的活动差异性造成洼陷形态为典型的南超北断的箕状洼陷；多次的构造运动形成了湖盆的多次抬升剥蚀和沉降。充填序列可以划分为4个构造层序；沉积体系可划分出河流、扇三角洲、三角洲及湖泊体系等4种；洼陷的沉积受同沉积构造活动及物源补给状况的控制。     

“天后”妈祖

<正>妈祖,又称天妃、天后、天上圣母、娘妈,封号"辅兜昭孝纯正灵应孚济护国庇民妙灵昭应弘仁普济天妃",是历代船工、海员、旅客、商人和渔民共同信奉的神祇。山东沿海渔民普遍称其为"海神娘娘",山东最东端的部分渔民把渔船归航称为"归山",因此把天后也称作"归山娘娘"。古代在海上航行经常受到风浪的袭击而船沉人亡,为了祈求平