140OΜα前的后生动物实体化石?

本文首次报道了在我国豫西晚前寒武系白草坪组中发现的一种可能的蠕虫状后生动物实体化石:Ruyangia Cylindrica Hu et Meng,1989。化石产于砂岩表面浪成波痕之波谷中,圆筒状,已压扁,中空,可见长度4.5～9.5cm,直径4mm左右,虫体外壁具体环,环背间距1.5～2mm,虫体一端较大,具平行纵向边缘的纵纹,可能为头部;另一端渐尖,可能为尾部。与该实体化石伴生的有大量遗迹化石。已知白草坪组的时代超过1400Ma,因此,该实体化石的发现对研究地球上后生动物起源与早期演化等具重要意义。     

Describing neutron stars by the relativistic mean field theory

Neutron stars are studied in the framework of the relativistic mean field theory of interacting nucleons, hyperons, and mesons. Within the hadronic freedom, the cores of neutron stars are found to be dominated by hyperons when the density is sufficiently high. The influence of hyperon coupling constants on the transition from a neutron star to a hyperon-dominated strange neutron star is also investigated. It is found that the transition density gets its minimum value when the ratio of hyperon coupling constant to nucleon's takes the value of 0.65, and the calculated maximum mass of the neutron star is 1.4 M which lies within the range of the observational results.     

关于因特网3S服务平台的搭建

3S集成 ,特别是广域网的 3S动态集成 ,是地理信息产业的发展趋势和方向 ,其归宿应该是数字地球。 3S集成系统用户应用服务平台搭建技术在概念层面与因特网 (万维网 )技术融合。开放的面向用户动态跟踪和导航用途的 3S集成系统 ,与因特网通信接口技术和用户界面技术相关。因特网 3S集成系统的功能及其运行效率是其具有实用价值的基础。     

不同约束对GPS观测网平差结果的影响

对卫星轨道和测站坐标的约束程度设计了 4种方案 ,对中国地壳运动观测网络10 18GPS周的基准站观测数据进行了试验研究。结果显示 :松驰轨道和紧约束 IGS站方案的结果与紧约束轨道和 IGS站方案的结果基本一致 ,认为这与先验坐标的精确度较高有关。其他方案之间存在较大的差别。最后讨论了大尺度 GPS监测网数据处理时参考基准的选择问题 ,认为一般情况下 ,应该使用全球解 H文件 ,把平差结果归算到全球参考框架中     

北京大灰厂试验场重力变化特征及其解释

介绍了北京大灰厂试验场（简称京西试验场）的概况，对１９９３年３月以来重力重复观测资料进行了处理。计算了各期重力观测精度，结果显示１９９３年３月～１９９５年５月京西试验场存在一定重力变化。采用给定的模型反演了八宝山断层介质的密度变化，认为断层破碎带介质密度的变化可能是引起地表重力变化的主要因素     

A THEORETICAL DISCUSSION ON TYPES AND MEASUREMENT OF SUSTAINABLE DEVELOPMENT

１ＩＮＴＲＯＤＵＣＴＩＯＮＴｈｅｃｏｒｅｏｆｇｅｏｇｒａｐｈｉｃａｌｓｔｕｄｉｅｓｔｈｅａｒｅａｌｓｙｓｔｅｍｏｆｍａｎｌａｎｄｒｅｌａｔｉｏｎｓｈｉｐＷＵ１９９１ｉｓｔｈｅｓｔａｒｔｉｎｇｐｏｉｎｔｏｆｓｔｕｄｙｉｎｇｒｅｇｉｏｎａｌｓｕｓｔａｉｎａｂｌｅｄｅｖｅｌｏｐｍｅｎｔ．Ｆｒｏｍｔｈｅｐｏｉｎｔｏｆｓｕｓｔａｉｎａｂｌｅｄｅｖｅｌｏｐｍｅｎｔｔｈｅｃｏｏｒｄｉ-ｎａｔｉｏｎｏｆｍａｎｌａｎｄｒｅｌａｔｉｏｎｓｈｉｐｉｓｄｅｖｅｌｏｐｍｅｎｔｓｕｓｔａｉｎ-ａｂｉｌｉｔｙ．…     

甘肃陇山地区葫芦河群变质玄武岩及大地构造环境恢复

葫芦河群变质玄武岩以其高不相容元素、稀土元素和低MgO、Cr和Ni含量有别于现代洋中脊玄武岩和岛弧玄武岩,在FeO-MgO-Al_2O_3和Ti/100-Zr-Y×3判别图上,均落在大陆玄武岩区。在剖面上,与变质玄武岩整合接触的巨厚的变砂岩和大量出现的火山角砾岩和集块岩是浅海环境的标志;密集的辉绿岩墙群是拉张性大地构造环境的特征。因此,本文认为葫芦河群变质玄武岩原岩形成于陆内裂陷海盆环境。     

Lamproitic Rocks from a Continental Collision Zone: Evidence for Recycling of Subducted Tethyan Oceanic Sediments in the Mantle Beneath Southern Tibet

Major and trace element, Sr–Nd–Pb isotope and mineralchemical data are presented for newly discovered ultrapotassiclavas in the Tangra Yumco–Xuruco graben in southern Tibet.The ultrapotassic lavas are characterized by high MgO, K₂O andTiO₂, low Al₂O₃ and Na₂O contents, and also have high molarK₂O/Al₂O₃, molar (K₂O + Na₂O)/Al₂O₃ and K₂O/Na₂O ratios. Theirhigh abundances of incompatible trace elements such as largeion lithophile elements (LILE) and light rare earth elements(LREE) reach the extreme levels typical of lamproites. The lamproitesshow highly radiogenic ⁸⁷Sr/⁸⁶Sr (0· 7166–0·7363) and unradiogenic ¹⁴³Nd/¹⁴⁴Nd (0· 511796–0·511962), low ²⁰⁶Pb/²⁰⁴Pb (18· 459–18· 931),and elevated radiogenic ²⁰⁷Pb/²⁰⁴Pb (15· 6732–15·841) and ²⁰⁸Pb/²⁰⁴Pb (39· 557–40· 058) ratios.On the basis of their geochemical and isotopic systematics,the lamproites in south Tibet have a distinct magma source thatcan be differentiated from the sources of potassic lavas inthe east Lhasa and Qiangtang blocks. Their high Nb/Ta ratios(17· 10–19· 84), extremely high Th/U ratios(5· 70–13· 74) and distinctive isotope compositionsare compatible with a veined mantle source consisting of partialmelts of subducted Tethyan oceanic sediments and sub-continentallithospheric depleted mantle. Identification of the lamproitesand the delineation of their mantle source provide new evidencerelevant for models of the uplift and extension of the Tibetanplateau following the Indo-Asia collision. Metasomatism by partialmelts from isotopically evolved, old sediment subducted on theyoung Tethyan slab is an alternative explanation for PrecambrianNd and Pb model ages. In this model, differences in isotopiccomposition along-strike are attributed to differences in thetype of sediment being subducted, thus obviating the need formultiple metasomatic events over hundreds of million years.The distribution of lamproites, restricted within a north–south-trendinggraben, indicates that the initiation of east–west extensionin south Tibet started at 25 Ma. KEY WORDS: lamproites; subducted oceanic sediment; Tibetan active continental collision belt     

Influence of underground space development mode on the groundwater flow field in Xiong’an new area

The degree and scale of underground space development are growing with the continuous advancement of urbanization in China. The lack of research on the change of the groundwater flow field before and after the development of underground space has led to various problems in the process of underground space development and operation. This paper took the key development zone of the Xiong’an New Area as the study area, and used the Groundwater modeling system software (GMS) to analyse the influence on the groundwater flow field under the point, line, and surface development modes. The main results showed that the underground space development would lead to the expansion and deepening of the cone of depression in the aquifer. The groundwater level on the upstream face of the underground structure would rise, while the water level on the downstream face would drop. The “line” concurrent development has the least impact on the groundwater flow field, and the maximum rise of water level on the upstream side of the underground structure is expected to be approximately 3.05 m. The “surface” development has the greatest impact on the groundwater flow field, and the maximum rise of water level is expected to be 7.17 m.