全文获取类型
收费全文 | 7269篇 |
免费 | 1374篇 |
国内免费 | 4571篇 |
专业分类
测绘学 | 4篇 |
大气科学 | 35篇 |
地球物理 | 757篇 |
地质学 | 11241篇 |
海洋学 | 567篇 |
天文学 | 12篇 |
综合类 | 274篇 |
自然地理 | 324篇 |
出版年
2024年 | 85篇 |
2023年 | 247篇 |
2022年 | 400篇 |
2021年 | 469篇 |
2020年 | 419篇 |
2019年 | 506篇 |
2018年 | 452篇 |
2017年 | 518篇 |
2016年 | 530篇 |
2015年 | 544篇 |
2014年 | 648篇 |
2013年 | 558篇 |
2012年 | 661篇 |
2011年 | 597篇 |
2010年 | 486篇 |
2009年 | 510篇 |
2008年 | 481篇 |
2007年 | 540篇 |
2006年 | 597篇 |
2005年 | 539篇 |
2004年 | 463篇 |
2003年 | 387篇 |
2002年 | 297篇 |
2001年 | 333篇 |
2000年 | 292篇 |
1999年 | 238篇 |
1998年 | 298篇 |
1997年 | 300篇 |
1996年 | 179篇 |
1995年 | 138篇 |
1994年 | 118篇 |
1993年 | 79篇 |
1992年 | 81篇 |
1991年 | 53篇 |
1990年 | 41篇 |
1989年 | 30篇 |
1988年 | 25篇 |
1987年 | 15篇 |
1986年 | 9篇 |
1985年 | 11篇 |
1984年 | 6篇 |
1981年 | 3篇 |
1979年 | 2篇 |
1978年 | 3篇 |
1977年 | 2篇 |
1976年 | 7篇 |
1975年 | 4篇 |
1973年 | 4篇 |
1972年 | 2篇 |
1971年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
171.
172.
Sharon S. Crowley Peter D. Warwick Leslie F. Ruppert James Pontolillo 《International Journal of Coal Geology》1997,34(3-4)
The origin and distribution of twelve potentially Hazardous Air Pollutants (HAPs; As, Be, Cd, Cr, Co, Hg, Mn, Ni, Pb, Sb, Se, and U) identified in the 1990 Clean Air Act Amendments were examined in relation to the maceral composition of the A1 bed (Paleocene, Calvert Bluff Formation, Wilcox Group) of the Calvert mine in east-central Texas. The 3.2 m-thick A1 bed was divided into nine incremental channel samples (7 lignite samples and 2 shaley coal samples) on the basis of megascopic characteristics. Results indicate that As, Cd, Cr, Ni, Pb, Sb, and U are strongly correlated with ash yield and are enriched in the shaley coal samples. We infer that these elements are associated with inorganic constituents in the coal bed and may be derived from a penecontemporaneous stream channel located several kilometers southeast of the mining block. Of the HAPs elements studied, Mn and Hg are the most poorly correlated to ash yield. We infer an organic association for Mn; Hg may be associated with pyrite. The rest of the trace elements (Be, Co, and Se) are weakly correlated with ash yield. Further analytical work is necessary to determine the mode of occurrence for these elements. Overall, concentrations of the HAPs elements are generally similar to or less than those reported in previous studies of lignites of the Wilcox Group, east-central region, Texas. Petrographic analysis indicates the following ranges in composition for the seven lignite samples: liptinites (5–8%), huminites (88–95%), and inertinites (trace amounts to 7%). Samples from the middle portion of the A1 bed contain abundant crypto-eugelinite compared to the rest of the samples; this relationship suggests that the degradation of plant material was an important process during the development of the peat mire. With the exception of Hg and Mn, relatively low levels of the HAPs elements studied are found in the samples containing abundant crypto-eugelinite. We infer that the peat-forming environment for this portion of the coal bed was very wet with minimal detrital input. Relatively high concentrations of crypto-humotelinite were found in samples from the top and base of the coal bed. The presence of abundant crypto-humotefinite in this part of the coal bed suggests the accumulation of wood-rich peat under conditions conducive to a high degree of tissue preservation in the peat mire. Although several of the trace elements (Be, Co, Ni, and Sb) exhibit enrichment in these samples, they are not necessarily chemically associated with humotelinite. We infer that these elements, with the exception of Be, are possibly associated with deposition of the roof and floor rock of the coal bed; however, further analytical work would be necessary to confirm this hypothesis. Beryllium may have an organic origin. 相似文献
173.
同位素稀释中子活化分析铼与感耦等离子体质谱法测定锇相结合,应用于辉钼矿及铜_镍硫化物矿物的铼_锇年龄测定,取得了满意的结果,扩大了铼_锇测年法的应用范围。 相似文献
174.
Zhang Lifei Sun Min Wu Jiahong Department of Geology Peking University Beijing Department of Earth Sciences University of Hong Kong Hong Kong Shenyang Institute of Geology Mineral Resources CAGS Shenyang Liaoning Liu Xinzhu 《《地质学报》英文版》1997,71(1):15-32
The Kuandian Complex is scarcely preserved Early Proterozoic volcanic suite, formed2.3-2.4 Ga ago. It is located in an Early Proterozoic mobile belt bounded by the ArchaeanRangrim and Ryonggang Blocks of the northeastern Sino-Korean Craton. The Complex ismainly made up of amphibolites, gneisses, leucoleptite, leptite and layered granite. Petrologicaland geochemical studies show that the protoliths of the Complex are mainly assoctations ofbimodal volcanics and anorogenic granites. The Kuandian amphibolites are depleted in Nb, Ta,P and Ti, and enriched in LILE, e.g. K, Rb and Cs, with pronounced depletion of Sr relative toNd and Pb; La/Nb ratios are higher than 1(1.75 to 5.18). The trace element patterns of theamphibolites are similar to continental flood basalts formed by the Gondwana break-up, suchas those in South Karoo and Tasmania, which shows continental contamination. ε_(Nd) valuesranging from 0.70 to 1.94 of the Kuandian amphibolites and the relationships between Nb/Yband La/Yb suggest that contamination of basaltic magma happened in the mantle, rather thanalong the conduit. Isotope ratios of ~(208)Pb/~(204)Pb, ~(207)Pb/ ~(204)Pb, ~(206)Pb/~(204)Pb, ~(143)Nd/~(144)Ndand ~(87)Sr/~(86)Sr indicate that the magma was derived from a contaminated mantle source likeDMM or a mixture of DMM and EM2. The Kuandian Complex has Dupal anomaly, as is thecase with some continental basalts in the south hemisphere, e.g. in South Karoo and Tasmania.Petrochemical modelling proposes that the Kuandian gneiss, granite, and amphibolite camefrom the same parental magma, being products of strong fractional crystallization. Protoliths ofthe Kuandian Complex were formed in extensional tectonic setting during the transition fromcontinental crust to oceanic crust. The formation of the Kuandian Complex indicates that 2.3or 2.4 Ga ago tectonic evolution of the Sino-Korean craton was different from that of otherwell-studied Precambrian cratons, e.g. the North American shield, European platform andAustralian continent in that strong volcanic eruption resulted in its accretion. Besides, the con-taminated magma source with a Dupal anomaly for the Complex indicates that crust-mantleconvection whose scale was similar to that of the present plate tectonics had occurred at leastbefore the formation of the Kuandian Complex (2.3-2.4 Ga B.P). 相似文献
175.
云南老王寨金矿煌斑岩地球化学研究中的某些问题──与宋新宇等同志商榷 总被引:2,自引:0,他引:2
本文对“云南老王寨金矿煌斑岩地球化学研究”一文中的部分结论及其解释,提出一些不同意见与原文作者宋新宇等先生商榷 相似文献
176.
扬子地块西缘灯影组层控铅锌矿床成因的地球化学论证 总被引:5,自引:0,他引:5
扬子地块西缘灯影组层控铅锌矿床成因的地球化学论证邵世才(有色总公司北京矿产地质研究所,北京100012)李朝阳(中国科学院地球化学研究所,贵阳550002)关键词层控铅锌矿床地球化学矿床成因扬子地块西缘1矿床地质特征扬子地块西缘灯影组铅锌矿床呈南北向... 相似文献
177.
粤东北嵩溪银锑矿床地质地球化学初步研究 总被引:5,自引:0,他引:5
粤东北嵩溪银锑矿床地质地球化学初步研究肖振宇郑庆年(广东有色金属地质勘查院,广州510080)陈繁荣张湖(中国科学院广州地球化学研究所,广州510640)关键词地质地球化学银锑矿床嵩溪嵩溪银锑矿床发现于粤东北地区,有嵩溪、黄沙塘等矿床和梅子坑、仙客社... 相似文献
178.
泥炭档案气候变化重建的定量模型 总被引:3,自引:1,他引:3
泥炭档案气候变化重建的定量模型*陶发祥洪业汤(中国科学院地球化学研究所,贵阳550002)李汉鼎冷雪天(东北师范大学地理系,长春130024)关键词泥炭档案纤维素稳定同位素气候变化定量模型用泥炭档案定量重建大气CO2浓度的研究已取得重要进展[1],但... 相似文献
179.
高温高压下水岩界面反应与金的迁移富集 总被引:1,自引:0,他引:1
高温高压下水岩界面反应与金的迁移富集王玉荣阚小凤王志强(中国科学院广州地球化学研究所,广州510640)关键词水岩界面反应自发电池实验地球化学本实验以哈达门沟[1]及东坪金矿[2]为地质背景,研究钾长石岩中金矿化富集的物理化学条件。该区金矿既与早期变... 相似文献
180.
滇黔桂微细浸染型金矿铅同位素组成及应用 总被引:6,自引:1,他引:6
滇黔桂微细浸染型金矿铅同位素组成及应用*刘显凡刘家军朱赖民(中国科学院地球化学研究所,贵阳550002)卢秋霞(成都理工学院,成都610059)关键词微细浸染型金矿铅同位素组成矿质来源上地幔分异混染滇黔桂1矿床地质背景研究区位于扬子地台西南缘与华南加... 相似文献