济阳坳陷车西洼陷漫湖洪水—风暴沉积与砂体横向预测

渐新统沙二段是济阳坳陷车西地区的主力油层,为了弄清其油气分布和控制因素,综合利用大量的地质和地球物理资料,首次在该段识别出漫湖洪水—风暴重力流沉积.该沉积具有明显的重力流沉积特征,砂岩的成分和结构成熟度均较低,粒度概率图多由悬浮次总体组成,沉积序列可用Bouma序列来描述.在明确了砂体的沉积层位和沉积边界的基础上,描述了漫湖洪水—风暴的沉积特征并建立了沉积模式,系统分析了这个环境下储集性砂体的分布及其油气聚集特征,为车西洼陷的进一步勘探指明了方向.     

Cryptomelane（KxMn8-xO16）： Natural active octahedral molecular sieve（OMS-2）

The Xiangtan manganese deposit (XTM) used to be considered a supergene oxide manganese ore in South China. We reported a new identification of the naturally outcropping cryptomelane by examining the physical, chemical and structural features of the XTM supergene oxide manganese ore. The MnO2 content was over 90%, K2O more than 3%, and water from 2.2%-3.1% which is similar to one in zeolite. The cell parameters of the cryptomelane were given as a0 = 0.9974 nm, b0 = 0.2863 nm, c0 = 0.9693 nm and β= 91.47°. There was a larger pseduotetragonal tunnel in the natural cryptomelane that was formed by [MnO6] octahedral double chains with aperture of 0.462×0.466 nm2, filled with K cations resulting in some Mn3+ substituting for Mn4+ to balance the negative charges of structure. The finding is important not only for prospecting manganese resources in South China, but also in application of octahedral molecular sieve of natural cryptomelane as that developed in the tetragonal molecular sieve of natural zeolite o     

Loess-soil sequences in southern Anhui Province： Magnetostratigraphy and paleoclimatic significance

Two parallel loess-soil sequences from Xuancheng and Fanchang in southern Anhui Provinces are dated using geomagnetic and luminescence methods.The Brunhes/Matuyama(B/M) reversal boundary is recognized within the lower part of the so-calles Vermiculated Red Soil (VRS) in the Xuancheng section while the entire Fanchang sequence is of Brunhes age.This indicated that the most recent VRS in southern China,a stratigraphic marker and an indication of extremely warm-humid conditions,was formed during the middle Pleistocene,chronologically correlative with the S4 and S5 soil units in northern China.Microscopic and sedimentologic in vestigations reveal that eolian deposition started in this region at about 0.85 MaBp,roughly synchronous with the well-known Mid-Pleistocene climate change of global significance.The strengthening of both summer and winter monsoon circulations and the consequent river hydrological changes at that time would have provided favorable conditions for sustained eolian deposition in the middle-lower reaches of the Yangtze River since 0.85 MaBP.     

沉积物对汽油机碳氢排放物形成的预测与实验研究

建立了汽油机燃烧室沉积物处未燃碳氢生成和氧化模型，测量了有、无燃烧室沉积物时发动机排气中的碳氢摩尔浓度．实验结果表明：沉积物的存在将增加发动机碳氢排放量，在本实验用机及实验条件下，沉积物将使发动机排气中的碳氢摩尔浓度增加２０％～３０％．计算结果表明：本模型能较好地预测出沉积物形成的排气碳氢摩尔浓度     

两种醇沉方式对杜仲水提液中氯原酸含量的影响

对一次醇沉及多次醇沉后杜仲水提液中氯原酸的含量做了对比分析．结果表明，分次醇沉比一次醇沉所得的产品纯度高；当乙醇浓度最终为９０％时，一次醇沉的损失率为１８．９％，而分次醇沉的损失率仅为６．８％．     

利用地表化探详查方法确定断块油藏边界

对我国东部某断块油田进行了地表化探详查研究．采用０．２５ｋｍ×０．２５ｋｍ测网，通过地表土壤介质的地化分析，确定了该油田长期以来悬而未决的油藏边界，建立了断块油气藏可能的异常模式，并从油气化探角度提出了对该油藏进行进一步钻探的合理化建议．该项试验成果表明，利用地表化探详查的方法确定我国东部断块油藏的边界和含油层分布是可行的．     

山西中条山胡—篦型铜矿床成矿地质条件与矿床成因

本文以含矿地层的构造解折为基础，讨论了胡—篦型铜矿的成矿地质条件，认为矿床成因是多种因素控制下的热液矿床。     

河南鲁山黄土岭韧性剪切带型金矿床包裹体研究

包裹体研究表明，河南鲁山黄土岭韧性剪切带型金矿的成矿流体为低盐度、中低温度、高硫、富ＨＣＯ和Ｃｌ－及碱金属离子的热流体。包裹体类型有ＣＯ２，ＣＯ２－Ｈ２Ｏ及Ｈ２Ｏ三种，它们在矿物中共生，并且各自的密度、盐度有区别，表明包裹体捕获时流体发生过沸腾作用，有过相态分离。包裹体水同位素研究结果显示热液以变质水为主，混有一定量的岩浆水与雨水。沸腾作用、相态分离是矿床形成的关键因素。ＣＯ２包裹体大量出现、流体中ＣＯ２的高含量、富硫等是这类矿床的找矿标志。     

广西茶山锑矿床成矿流体研究

本文通过矿床地质、成矿流体、泥盆系合矿性和稀土元素地球化学研究，总结出茶山锑矿床成矿流体具有热卤水特征，并未获得岩浆热液成因的证据。