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1.
天然和实验冲击球粒陨石矿物的变形变质比较研究谢先德陈鸣戴诚达(中国科学院广州地球化学研究所,广州510640)A.El.Goresy(Max-PlanckInstitutfurKernphysik,69029Heidelberg,Germany)关键...  相似文献   

2.
PrecambrianMetamorphismofTiya-OlokitMetamorphicBeltinNorthernBalkalRegionanditsMetallogeny¥A.I.Sizykh;A.A.Belogolov(Departmen...  相似文献   

3.
苏锡常平原第Ⅱ承压水超采区划分方法   总被引:1,自引:0,他引:1  
陈锁忠 《江苏地质》1995,19(1):21-25
苏锡常平原第Ⅱ承压水超采区划分方法陈锁忠(江苏省地质环境监测总站,南京,210049)关键词:地下水,含水层,超采区,水文地质,江苏。MethodtoClassifytheOverloadMiningDistrictsofNo.ⅡConfinedWa...  相似文献   

4.
1.IntroductionThesystematictheoryinRockMasEngineeringGeologyistheRockMasEngineeringGeomechanicsestablishedbyGuDezhen(1979).He...  相似文献   

5.
苗升明 《江苏地质》1995,19(3):174-175
不同熔(溶)矿方法对硅酸盐岩石中氧化钛分析结果的影响苗升明江苏省东海县环境监测站,东海,222300关键词:熔(溶)矿法,硅酸盐岩石,氧化钛,化学分析,江苏东海EffectivenessofDifferentMethodsofMeltingorDis...  相似文献   

6.
Jiaodong Granitoids and Gold Mineralization¥ChenGuangyuan;SunDaisheng;ShaoYue(DepartmentofGeologyandMineralResources,ChinaUni...  相似文献   

7.
矿物的定义     
矿物的定义E.H.Nickel(DivisionofExploTation&Mining,CSIRO,WembleyWA6014,Aust,tralia)响应矿物学界提出和要求颁布的、与当代技术发展相适应的矿物新定义的建议,国际矿物协会(IMA)新矿...  相似文献   

8.
A New Mid Early Pleistocene Mammalian FaunaDiscovered in Choukoutien,ChinaandItsApplication in Biostratigraphy¥ChengJie(Depar...  相似文献   

9.
Wecolectedorientedmagnetostratigraphicsamplesatthesamebed(Bed27,limestone)ofAandDsectionsnamedbyShengetal.(1984)ofMeishansect...  相似文献   

10.
黄维平  施倪承 《岩石学报》1996,12(4):619-626
Rietevld方法是采用粉末衍射进行晶体结构修正及解析的一种方法。Rietveld方法的代表软件是R.A.Young程序。该程序给用户使用的主要困难是由于其输入控制文件(ICF),是一个严格格式化的文本文件,其次是在运行时受到常规内存的限制。本文介绍了用MicrosoftC7.0及MicrosoftSDK3.1对R.A.Young程序的改进,(1)用对话框输入各种控制参数,形成初始化文件(INI),然后再将其转换为输入控制文件(ICF);(2)用Windows多文档界面(MDI)实现图形显示,编辑和存储;(3)设计一软件接口,使在Windows下启动R.A.Young计算程序;(4)用FORTRANPowerStation编译器对R.A.Young程序源代码进行重新编译,使其不受常规内存限制。用改进后的R.A.Young程序,对绿辉石的结构进行了修正  相似文献   

11.
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.  相似文献   

12.
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.  相似文献   

13.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
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.  相似文献   

14.
Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ1 roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).  相似文献   

15.
HYDROGEOLOGY     
正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level  相似文献   

16.
正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7),  相似文献   

17.
18.
正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci-  相似文献   

19.
正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli-  相似文献   

20.
正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.)  相似文献   

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