承德市中关饮用天然矿泉水评价

承德市中关饮用天然矿泉水赋存于侏罗系张家口组地层中，在导水断层作用下，上升补给浅层地下水。该泉水资源丰富，水质良好。经省、部级鉴定，属低钠、低矿化度锶矿泉水。     

芮城大禹神泉天然矿泉水水质评价

矿泉出露于黄河二级阶地冲沟中，属侵蚀悬挂泉。含水层为第四系下更新统胶结砂岩，地下水主要受北部中条山基岩裂隙水补给。１９９２年１２月经地矿部鉴定，符合《饮用天然矿泉水》国家标准（ＧＢ８５３７－８７），属含锶重碳酸－钠镁型矿泉水。     

湘乡东山天然饮用含锌矿泉的地质特征及形成机理

湘乡市东山天然饮用矿泉水,是我省首次发现的大型含锌矿泉。它发育在北东向东台山含水断层带上,该断层长60km以上,倾向北西,斜贯湘乡境内,向西南通过歇马花岗岩体。在泉区,沿断层带发育一条硅化破碎带,最厚处达150m。断层上盘为白垩—第三系红层,下盘为板溪群,均为不透水层,对矿泉起遮挡保护作用。本矿泉水量丰富,每昼夜可取水2000t。泉水中锌和偏硅酸含量,已达到国家天然饮用矿泉水标准,另含10种人体必需的微量元素,属少见的优质矿泉。     

沁县七星泉天然矿泉水水质特征

沁县七星泉（后泉）饮用天然矿泉水是山西发现最早的天然矿泉水之一。１９８７年１１月经国家级鉴定为低钠、低矿化度、锶重碳酸－钙镁型饮用天然矿泉水。可作为瓶装天然矿泉水及矿泉饮料用水予以开发。     

沁水柿庄饮用天然矿泉水水质特征

沁水柿庄饮用天然矿泉水出露于柿在村北端氏小河的一级阶地上。二叠系上石盒子组砂页岩是其主要含水段。经系统监测及理化检验，水位、水量、水质动态稳定，属低钠、低矿化度锶矿泉水。泉区自然环境良好，无工业污染，有利于环境保护及矿泉水开发利用。     

大同市云岗镇竹林寺饮用天然矿泉水

大同市云岗镇竹林寺泉产出于太古界桑干群变质岩地层中，动态稳定，流量９８ｍ￣３／ｄ。经水质检测及勘察评价，该泉水属低钠、锶硫酸重碳酸钙·镁型饮用天然矿泉水。     

武乡南沟锂—锶优质饮用天然矿泉水

南沟矿泉水自沁水盆地三叠系二马营组砂页岩中溢出，自流量４Ｌ／ｓ，水中含锂０．４２３ｍｇ／Ｌ，锶０．４５０ｍｇ／Ｌ。１９９２年２月经山西省矿产储量委员会鉴定属锂—锶重碳酸—钙型优质饮用天然矿泉水。泉区自然环境好，无工业污染，是优良的矿泉水生产基地。     

运城关帝锶—偏硅酸饮用天然矿泉水

山西关帝饮用天然矿泉水产出于关公故里运城市解州关帝庙。经１９９２年１０月、１９９３年４月对两处矿泉水井检测分析，并经地质矿产部、轻工业部及卫生部等职能部门联合鉴定，属锶偏硅酸—重碳酸钙—镁型饮用天然矿泉水。该矿泉地理位置优越，名胜古迹诱人，有良好的开发前景。     

玉田东吉庄饮用天然矿泉水成因分析及水质评价

东吉庄矿泉水是１９８９年由地质矿产部环境管理司会同卫生部、轻工业部等有关单位的国家饮用天然矿泉水技术评审组鉴定通过，符合ＧＢ８５３７－８７的国家标准要求，属含锶重碳酸镁·钙·钠型低矿化度中性饮用天然矿泉水，已于同年建立了奥玉饮料厂，生产瓶装矿泉水及奥玉饮料。为了保护矿泉水资源免遭环境污染，对该矿泉水水源地进行了水源地保护规划。     

浑源鸽子峪天然矿泉水水质评价

浑源鸽子峪矿泉水出露于寒武系上统灰岩中。经历时２年的全面检测，完全符合我国及世界卫生组织所制定的饮用天然矿泉水标准，属低钠、含锶型饮用天然矿泉水。水质优良，清凉、甘甜、爽口，自然流量充沛，且距恒山风景区较近，有良好的开发前景。     

The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures,South Wales,UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia)

Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.     

Définition d'une limite multicritère ; stratigraphie du passage Campanien–Maastrichtien du site géologique de Tercis (Landes,SW France)Definition of a multi-criteria boundary; stratigraphy of the Campanian–Maastrichtian interval of the geological site at Tercis (Landes,SW France)

Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.     

The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts

The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H₂O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H₂O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.     

Late Wuchiapingian (Late Dzhulfian,early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon,central–eastern Peloponnesus,Greece)

Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions. To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.     

PALEONTOLOGY

正20141596 Liu Yunhuan(School of Earth Sciences and Resources,Chang’an University,Xi’an 710054,China);Shao Tiequan Early Cambrian Quadrapyrgites Fossils of Xixiang Boita in Southern Shaanxi Province(Journal of Earth Sciences and Environment,ISSN1672-6561,CN61-1423/P,35(3),2013,p.39-43,3 illus.,20 refs.)     

GEOCHEMICAL EXPLORATION

正20141719 Chen Zhijun(State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China);Chen Jianguo Automated Batch Mapping Solution for Serial Maps:A Case Study of Exploration Geochemistry Maps(Journal of Geology,ISSN1674-3636,CN32-1796/P,37(3),2013,p.456-464,2 illus.,2 tables,10 refs.)     

MICROPALAEONTOLOGY

正20140962 Chen Fenning(Xi’an Institute of Geology and Mineral Resources,Xi’an710054,China);Chen Ruiming Late Miocene-Early Pleistocene Ostracoda Fauna of Gyirong Basin,Southern Tibet(Acta Geologica Sinica,ISSN0001-5717,CN11-1951/P,87(6),2013,p.872-886,6illus.,56refs.)     

PETROLOGY

正1.IGNEOUS PETROLOGY20142008Cai Jinhui(Wuhan Center,China Geological Survey,Wuhan 430205,China);Liu Wei Zircon U-Pb Geochronology and Mineralization Significance of Granodiorites from Fuzichong Pb-Zn Deposit,Guangxi,South China(Geology and Mineral Resources of South China,ISSN1007-3701,CN42-1417/P,29(4),2013,p.271-281,7illus.,     

ENVIRONMENTAL GEOLOGY

正20141205Cheng Weiming(State Key Laboratory of Resources and Environmental Information System,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China);Xia Yao Regional Hazard Assessment of Disaster Environment for Debris Flows:Taking Jundu Mountain,Beijing as an     

PROSPECTING EXPLORATION

正20141266Fan Chaoyan(Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes,Guangzhou 510275,China);Wang Zhenghai On Error Analysis and Correction Method of Measured Strata Section with Wire Projection Method(Journal of