The genesis and environmental significance of red and black sedimentary interlayers in coral reef of well Nanyong 2

The results of paleogeomagnetics and geochemistry of the coral reef in well Nanyong 2 of Nansha Islands showed that the bottom of the black sedimentary interlayer corresponds to the conversion boundary line between Brunhes Postive Polarity and Matuyama Reversed Polarity (B/M) and the cold/warm (19/20) climatic conversion bounds on δ¹⁸O curve, 0.78 Ma ago; and the red sedimentary interlayer corresponds to the ReunionⅠpolarity excursion (reversion) of the geomagnetic field, 2.01—2.04 Ma ago. Comparing with the normal light-coloured coral reef rock, the magnetic susceptibility (c), residual magnetization intensity (Mr) and the content of MnO and Fe₂O₃ of the black sedimentary layer appeared obviously positive abnormity. The magnetic susceptibility (c), residual magnetization intensity (Mr) and the content of Fe₂O₃ of the red sedimentary layer also appeared positive abnormity. Combining with the analyzing results of paleontology, we hold that this pair of special and typical sedimentary interlayers was relative to the sudden change of paleoclimate, i.e. the global climatic change and its incidental polarity reversal of the geomagnetic field directly affected the living environment of the paleontological species as well as the dispersion and enrichment of some chemical elements, especially the elements sensitive to redox such as Fe and Mn. For example, the elements Fe and Mn concentrated in the glacial period would be largely oxidized and diluted when the climate warmed up suddenly, and the originally oxidized high valence Fe would be condensed again when the climate cooled suddenly. This is possibly one of the important reasons of appearing and disappearing of the red and black sedimentary events of coral reef in well Nanyong 2.     

精细地质研究在大庆萨中南一区丙块挖潜中的应用

根据现代细分沉积相理论 ,对南一区丙块萨 +葡 II油层进行细分单元砂体沉积相带图研究 ,第一次确立了该区块油层各单砂体三角洲沉积模式 ,并对各沉积单元的沉积特征及平面非均质性进行了描述和分析 ,进而预测和确定了该地区各类砂体中不同类型剩余油富集区 ,对二次加密调整井布井及射孔方案的编制具有指导作用 .     

天宝山铅锌矿床成因分析

天宝山铅锌矿床的铅同位素组成变化大,硫同位素组成变化范围小,成矿温度低于150～250℃,成矿深度为1km。它是我国产于碳酸盐岩层中的MVT铅锌矿床之一,受有利的岩性、岩相和构造的共同控制。该文通过铅、硫、碳同位素组成、稀土元素组成、微量元素和流体包裹体资料,对成矿物质的来源及其搬运、沉淀机理作了探讨。     

陕北长6油层组短期基准面旋回与储层非均质性的关系

鄂尔多斯盆地上三叠统延长组长６油层组为一套砂、泥薄互层的组合类型,储层非均质性很强,尤以层间的非均质性最为严重,明显受基准面升、降,和可容纳空间及沉积物供给量的变化影响。通过高分辨率层序地层的短期基准面升、降旋回过程与储集物性关系的分析,建立了６种不同沉积微相的非均质性模式,探讨了向上变深、向上变浅的非对称型和向上变深后复变浅的对称型短期基准面旋回层序对储层非均质性特征的控制作用     

纤维素纤维及薄膜动态粘弹性及其不连续非常态行为

详细考察了三种再生纤维素样品在宽广温度范围内（－１５０￣３５０℃）的粘弹性能。实验结果表明,在该温度范围内,三种再生纤维素均出现了ａ１、ａ２、ａｓｈ、ａ３、β和γ松弛等多转变。从这些转变的特征值分析,三种样品在结构上存在较大差异。样品ＲＡＹ有较低的结晶度,在晶区内和无定形区域内存在较高的结构不均匀性;样品ＮＥＷ的结晶度较高,在晶区和无定区内存在较高的结构均匀性,而样品ＢＥＮ的超分子结构介于这两者之     

A CORBA-Based Multidatabase System——Panorama Project

0　ＩｎｔｒｏｄｕｃｔｉｏｎＴｈｅｎｅｅｄｆｏｒｉｎｔｅｇｒａｔｉｏｎｏｆｄｉｆｆｅｒｅｎｔｄａｔａｂａｓｅｍａｎａｇｅｍｅｎｔｓｙｓｔｅｍｓ (ＤＢＭＳｓ) ,ｍａｋｉｎｇｄｉｆｆｅｒｅｎｃｅｓｂｅｔｗｅｅｎｔｈｅｓｅｓｙｓｔｅｍｓｉｎｖｉｓｉｂｌｅａｎｄｐｒｏｖｉｄｉｎｇｕｓｅｒｓｗｉｔｈａｕｎｉｆｏｒｍａｃｃｅｓｓｔｏａｌｌｔｈｅｄａｔａｂａｓｅｓｈａｓｇｒｏｗｎｒａｐｉｄｌｙｄｕｒｉｎｇｔｈｅｌａｓｔｄｅｃａｄｅ .Ｈｏｗｅｖｅｒ,ｄａｔａｂａｓｅａｕｔｏｎｏｍｙａｎｄｈｅｔｅｒｏｇｅｎｅｉｔｙ…     

知识产权制度的产业异质性假设

知识产权制度是激励创新的重要手段,知识产权制度绩效评价的要点在于创新激励效应。对知识产权制度激励效应在不同产业中的显著差异性出发,对知识产权制度作用机制的产业特质进行了深入的思考并在历史文献研究的基础上提出了知识产权制度的产业异质性假设。对知识产权领域长期以来忽视中观层面研究进行深刻反思,将产业层面的分析引入知识产权的研究框架。     

Noble gases in corundum megacrysts from the basalts in Changle, Shandong Province, eastern China

This study presents noble gaseous data of the corundum megacrysts from the Cenozoic basalts in Changle, Shandong Province, eastern China. It is known that no noble gaseous data of corundum megacryst have been documented before. The 3He/4He ratios (1.13-7.37 Ra) of the corundums from Changle vary from atmosphere to MORB values; the 20Ne/22Ne (9.67-10.75) and 21Ne/22Ne (0.0280-0.0372) data define two linear trends on Ne three-isotope diagram, respectively, along the MFL and the correlation line between atmosphere and MORB; the 38Ar/36Ar (0.177-0.194) ratios, the 40Ar/36Ar (280.9 -404.2) ratios and the 128-136Xe/132Xe ration with obvious 129Xe excess are generally higher than at-mospheric component, but the 40Ar/36Ar ratios are much closer to atomospheric ratio. The isotopic compositions of noble gases (particularly for He and Ar) of the corundums are similar to those of py-roxene, anorthoclase megacrysts, and mantle-derived xenoliths from this area, and those of man-tle-derived xenoliths from several areas in eastern China. Therefore, the noble gases trapped in the corundums probably are from mantle source, representing a ‘mixed fluid' produced by the interaction between the lithospheric mantle and fluids releasing from the convective plate. Both the noble gas isotopic compositions and the oxygen isotopic compositions of the solid corundums are not the characteristics of crustal source. These suggest that the corundums crystallized from mantle-derived magmas with minimal crustal contamination.     

河北近北庄磁铁矿的矿物学和地球化学组成及其药用意义

通过采用X射线衍射（XRD）、X射线荧光光谱法（XRF）和电感耦合等离子质谱（ICP-MS）等分析方法对河北近北庄磁铁矿的矿物学和化学组成特征进行了分析,分析表明,河北近北庄磁铁矿为沉积变质型磁铁矿;磁铁矿样品中Zn、Se、Mn、Mo等人体必需的微量元素平均含量较高,富集系数分别为2.22、2.11、1.85、1.8,Zn、Mn等微量元素具有安神作用,表明该区磁铁矿有一定的医用价值.     

Vegetation Spatial Heterogeneity of Different Soil Regions in Inner Mongolia, China

The vegetation spatial heterogeneity and ecological characteristics in different soil regions were analyzed by surveying the vegetation in 12 different soil regions of Inner Mongolia, China, including conifer- ous-broadleaf deciduous forests, shrub, grassland, and desert regions with 1122 large 2 cm × 2 cm quad- rats (actual size 30 km × 30 km, referred to as L-quadrat hereafter) in about 1.18 million km2. Each L- quadrat was divided into four small 1 cm × 1 cm quadrats (actual size 15 km × 15 km, S-quadrat). The vegetation was analyzed based on the beta-binomial distribution to describe the frequency of occurrence and spatial heterogeneity for each kind of vegetation. The weighted average of the heterogeneity of all vegeta- tion in the same soil region provides a measure of the soil regional landscape level heterogeneity which de- scribes the spatial complexity of the regional landscape composition of the existing vegetation. Comparison of the vegetation characteristics in the 12 soil regions shows that, the calcic gray soil has the highest average vegetation type per quadrat. The largest soil region is calcic chestnut soil and has the most vegetation types. Every soil region has its own dominant vegetation sequence which dominates in occurrence and dominant vegetation types which dominates in spatial heterogeneity. For the Inner Mongolian vegetation, the weighted average of the heterogeneity is 0.60 and the vegetation diversity index is 4.47.