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1.
赣北庐山伟晶岩形成时代新认识*毕华(中国科学院地球化学研究所,贵阳550002)谭克仁张琴华项新葵朱元松(中国科学院长沙大地构造研究所,长沙410013)(江西地质矿产局916地质大队,九江332100)关键词伟晶岩形成时代早元古代庐山庐山东南麓鄱阳...  相似文献   

2.
温度对稻田甲烷排放的影响   总被引:3,自引:0,他引:3  
温度对稻田甲烷排放的影响于心科,李宁,李春园,邵波(中国科学院兰州地质所气体地球化学国家重点实验室兰州730000)王卫东,谢小立(中国科学院长沙农业现代化研究所长沙410125)关键词稻田,甲烷排放,温度1水稻及其生态和实验实验田位于中国科学院桃源...  相似文献   

3.
为适应国家可持续发展的战略需求和国际海洋地质科学的发展,根据中国科学院知识创新工程的部署,已由中国科学院长沙大地构造研究所与广州地球化学研究所,通过整合共同组建中国科学院南方海洋科学基地。中国科学院院长路再祥院士指出:“两所整合,是为了保持与加强我国这支可贵的南方地球与海洋科学研究队伍,为国家未来发展及世界地球与海洋科学作出应有贡献。”大陆边缘动力学与矿产资源;海-陆相互作用及其环境效应,将是南方海洋科学基地今后主要研究与发展创新的方向。《大地构造与成矿学》,从2003年(二十七卷)起,将作为中…  相似文献   

4.
徐夕生 《地质论评》2007,53(1):125-125
由海内外众多单位发起,南京大学地球科学系、成矿作用国家重点实验室主办,国家自然科学基金委员会地球科学部、教育部科技委资源与环境学部、江苏省国土资源厅、中国地质调查局南京地质矿产研究所、中国科学院地球化学研究所、中国科学院广州地球化学研究所和中国地质大学(北京)协办的“2006年全国岩石学与地球动力学研讨会”成功地在南京举行。[第一段]  相似文献   

5.
微细浸染型金矿成矿动力学模型化研究   总被引:1,自引:0,他引:1  
微细浸染型金矿成矿动力学模型化研究@刘荣高¥中国科学院地球化学研究所成矿动力学,计算机模拟,水—岩作用,金矿微细浸染型金矿成矿动力学模型化研究刘荣高(中国科学院地球化学研究所,贵阳550002)关键词成矿动力学计算机模拟水—岩作用金矿热液矿床的形成同热液与...  相似文献   

6.
油气成因理论研究进展   总被引:1,自引:0,他引:1  
油气成因理论研究进展杜建国,张友联,谢鸿森,姜峰(中国科学院兰州地质研究所,兰州730000)(中国科学院兰州文献情报中心.兰州730000)(中国科学院地球化学研究所.贵阳550002)关键词石油和天然气,深部流体,地幔热,壳幔交代纵观众说纷纷的油...  相似文献   

7.
我国非金属矿物材料发展现状与趋势   总被引:1,自引:0,他引:1  
我国非金属矿物材料发展现状与趋势汪灵,张振禹(中国科学院长沙大地构造研究所,长沙410013)(中国科学院地质研究所,北京100029)关键词非金属矿,矿物材料,矿物材料学矿物材料是指以天然矿物或岩石为主要原料,经不以提纯金属和化工原料为目的加工改造...  相似文献   

8.
2: 1型层状硅酸盐的羟基定位结构及其矿物材料学意义   总被引:1,自引:0,他引:1  
2∶1型层状硅酸盐的羟基定位结构及其矿物材料学意义汪灵张振禹(中国科学院长沙大地构造研究所,长沙410013)(中国科学院地质研究所,北京100029)关键词层状硅酸盐羟基定位结构矿物材料学羟基是层状硅酸盐矿物的重要组成部分,对层状硅酸盐矿物的晶体结...  相似文献   

9.
煤矸石—水相互作用的溶解动力学及其环境地球化学效应研究党志(中国科学院地球化学研究所,贵阳550002)关键词水—岩作用煤矸石地球化学动力学采煤矿区复垦环境效应收稿日期:1997-3-10作者简介:党志男1962年生博士生环境地球化学煤矸石以其量多、...  相似文献   

10.
稳定同位素交换反应动力学储雪蕾(中国科学院地质研究所100029)关键词稳定同位素地球化学,同位素交换反应,化学反应动力学稳定同位素(如氢、碳、氧和硫等)被广泛用于地学研究中,它们或作为示踪剂指示物质来源,或作为温度计用来讨论地质体形成温度或地质作用...  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.
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.  相似文献   

15.
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.)  相似文献   

16.
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.)  相似文献   

17.
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.)  相似文献   

18.
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.,  相似文献   

19.
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  相似文献   

20.
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  相似文献   

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