全文获取类型
收费全文 | 3404篇 |
免费 | 656篇 |
国内免费 | 2335篇 |
专业分类
大气科学 | 35篇 |
地球物理 | 465篇 |
地质学 | 5234篇 |
海洋学 | 317篇 |
天文学 | 3篇 |
综合类 | 118篇 |
自然地理 | 223篇 |
出版年
2024年 | 48篇 |
2023年 | 138篇 |
2022年 | 202篇 |
2021年 | 220篇 |
2020年 | 209篇 |
2019年 | 231篇 |
2018年 | 218篇 |
2017年 | 263篇 |
2016年 | 245篇 |
2015年 | 261篇 |
2014年 | 304篇 |
2013年 | 261篇 |
2012年 | 323篇 |
2011年 | 287篇 |
2010年 | 239篇 |
2009年 | 255篇 |
2008年 | 252篇 |
2007年 | 268篇 |
2006年 | 301篇 |
2005年 | 277篇 |
2004年 | 229篇 |
2003年 | 180篇 |
2002年 | 141篇 |
2001年 | 148篇 |
2000年 | 137篇 |
1999年 | 100篇 |
1998年 | 122篇 |
1997年 | 150篇 |
1996年 | 95篇 |
1995年 | 72篇 |
1994年 | 68篇 |
1993年 | 35篇 |
1992年 | 36篇 |
1991年 | 22篇 |
1990年 | 21篇 |
1989年 | 13篇 |
1988年 | 12篇 |
1987年 | 4篇 |
1986年 | 4篇 |
1985年 | 2篇 |
1983年 | 1篇 |
1981年 | 1篇 |
排序方式: 共有6395条查询结果,搜索用时 0 毫秒
61.
LA-ICP-MS测定锡石U-Pb同位素年龄时两种普通铅扣除方法的原理及适用性比较 总被引:1,自引:0,他引:1
根据近年来激光烧蚀电感耦合等离子体质谱仪锡石微区原位U-Pb同位素定年的实验结果,结合相关资料,对实验过程中普通铅扣除的2种主要方法,即谐和图法和等时线法的原理、效果、优点和局限性进行了深入的比较。研究成果表明,2种主要方法各有不同的优点及局限性。在实际工作中,要想获得比较准确的测试结果,需要根据具体矿物样品的年龄范围、总的U和Pb含量、普通铅相对含量、测年精度要求等因素,灵活地选择普通铅扣除的方法。 相似文献
62.
T.V. Donskaya D.P. Gladkochub A.M. Mazukabzov S. Denyszyn S.A. Pisarevsky Z.L. Motova E.I. Demonterova 《Russian Geology and Geophysics》2018,59(12):1548-1559
Geological, geochronological, and isotope-geochemical studies of the metadolerites of the Angaul complex, widespread in the Urik-Iya graben of the southern Siberian craton, were carried out. The metadolerites forming separate conformal bodies (sills) among the metasandstones of the Ingash Formation were studied in detail. U-Pb zircon (SHRIMP) dating of metadolerites yielded an age of 1913 ± 24 Ma, and U-Pb baddeleyite (ID-TIMS) dating of these rocks yielded an age of 1914.0 ± 1.7 Ma. Thus, the date of 1914 ± 2 Ma can be taken as the most precise age estimate for the studied rocks. The metadolerites of the Angaul complex correspond in chemical composition to the normal-alkaline tholeiitic basalts. Metadolerites are differentiated rocks with mg# of 36 to 58. They show fractionated REE patterns: (La/Yb)n = 1.2-3.5. All metadolerites, independently of their mg# value, have low contents of Nb (1.6-10.2 ppm) and show well-pronounced negative Nb-Ta anomalies in multielement patterns (Nb/Nb* = 0.19-0.54). The metadolerites are characterized by positive εNd(T) values ranging from 0.4 to 5.2, which correlate well with their SiO2 content and mg# value. The isotope-geochemical parameters of the metadolerites of the Angaul complex indicate that fractional crystallization, along with the assimilation of the host rocks (AFC), might have been the main process during the formation of the most differentiated metadolerites. The geochemical characteristics of metadolerites with the maximum mg# values of 57-58 and εNd(T) = 5.2 suggest that the parental mantle source of the metadolerites resulted from mixing of predominant depleted mantle material with the subcontinental-lithosphere material. Intrusion of the dolerites of the Angaul complex, as well as the deposition of the sedimentary strata of the Ingash Group, took place at the Paleoproterozoic stage of intracontinental extension caused by the collapse of the orogen resulted from the collision of the Biryusa block with the Tunguska superterrane in the southern Siberian craton. 相似文献
63.
O. Mülayim I.O. Yilmaz B. Sari B. Ferré 《Proceedings of the Geologists' Association. Geologists' Association》2021,132(2):188-198
A ‘filament’ event bed/level corresponds to the occurrence of thin elongate calcitic, shells, or plates of pelagic, bivalve or crinoidal, origin, within pelagic, laminated and organic-matter rich limestones. These organic-rich limestones had been generally deposited under hypoxic/anoxic conditions in an outer-ramp environment. These thin elongate, bivalve shells, or crinoidal plates, are found broken in small pieces, disintegrated, or simply preserved parallel to bedding as almost complete specimens. Such ‘filament’ beds were spotted in SE Turkey in deposits, namely the Karababa-A Member, around the Cenomanian-Turonian boundary (C/TB) and above. On a global scale, these filament event beds illustrate sea-level rise related to eustacy and/or climatic change. The abundance of filaments close to the C/TB is a biological marker of high organic productivity resulting from a climatic change to warmer conditions. The prevailing higher sea-level conditions were then favourable to the accumulation and preservation of organic-rich facies, characteristic of the Oceanic Anoxic Event 2 (OAE2). Using both biostratigraphic and carbon isotopic data, those deposits were dated from the latest Cenomanian-Turonian age. ‘Filament’ event beds were recorded in the same order, except for some small differences. A good number of these bio-events are global. Consequently, on a global scale, they are susceptible to constrain the C/TB, especially the base of the Turonian stage, with a significant degree of confidence. 相似文献
64.
为研究贵州北部马鬃岭铝土矿床中富锂铝质粘土岩的物源体系及其锂的来源,对出露于大竹园组顶部的该类岩石进行了锆石U-Pb定年、Lu-Hf同位素及锆石微量元素分析。分析结果表明富锂铝质粘土岩中碎屑锆石普遍发育岩浆振荡环带,为造山作用/弧作用相关的岩浆岩类锆石。碎屑锆石U-Pb年龄从早泥盆世到太古宙(411~3001 Ma)均有分布,具627~879 Ma和925~1018 Ma两个主峰及539~602 Ma一个次峰。εHf(t)值为-27.61~7.03之间,二阶段模式年龄(tDM2)分布在1242~3387 Ma之间。结合碎屑锆石U-Pb-Hf同位素、微量元素特征及区域地质对比,认为富锂铝质粘土岩中碎屑锆石最主要的初始物源区为南岭-云开地体、江南造山带西段新元古代岩浆岩,其锂可能来源于江南造山带西段桂北-黔东地区860~750 Ma的基性岩。 相似文献
65.
66.
Fluctuation of the carbon isotope composition of marine carbonates has recently been developed as a powerful tool for the identification of ocean-wide anoxic conditions and changes in the world budget of carbon and oxygen. A change in δ13 from the normal marine values (0 to + 2%) to values highly enriched in 13C (+3·5 to 4·5%) is recorded at the base of the Zechstein sequence both in central Germany and northeastern England. The change occurred over a relatively short period of time indicating a rapid and pronounced change in the organic carbon/carbonate budget. Evidence from other Permian basins show similar highly enriched δ13C values. This change may correspond to that in carbon balance distinguished by the Garrels and Perry (1975) model and based on the change in sulphur isotopic composition during the Permian. 相似文献
67.
68.
川西成都盐盆平落4井富钾硼溴浓卤水水化学同位素地球化学特征及形成机制 总被引:6,自引:0,他引:6
根据盐盆的演化历史,水化学组分H,O,S,B等同位素组成综合分析,该浓卤水具有海,陆相混合型卤水的特征,一些元素的富集是在成盐成卤晚期由外来卤水和地层水流入盐盆混合并溶解盐层,在蒸发条件下形成的。 相似文献
69.
长江口海域悬浮颗粒有机物的稳定氮同位素分布及其生物地球化学意义 总被引:4,自引:0,他引:4
对2006年2,5,8,11月份长江口海域表层水体中的悬浮颗粒物(SPM)进行稳定氮同位素分析,根据不同季节、不同区域内其1δ5N值的变化研究水体中氮的迁移、转化等生物地球化学过程,揭示其环境行为,从而对该海域的氮循环机制进行探索。研究发现:该海域悬浮颗粒有机物的稳定氮同位素组成(1δ5Np)分布范围较宽,在0.6‰~8.2‰之间,具有明显的时空分布特点,反映了不同程度的陆源输入和氮的生物地球化学过程的影响。口门内,表层水体中1δ5Np的变化主要受长江径流的陆源输入影响,生物地球化学作用影响较弱;最大浑浊带,水体中的悬浮颗粒有机氮受微生物的降解活动影响明显,各季节均存在不同程度的颗粒物分解作用;外海区,陆源输入减弱,悬浮颗粒物的δ15Np值主要受微藻的同化吸收作用以及一定程度的颗粒物分解作用影响。 相似文献
70.
WANG Luyao LIU Kai MA Yan ZHANG Yaoyao TONG Jue JIA Wuhui ZHANG Shouchuan SUN Junliang 《《地质学报》英文版》2024,98(3):801-818
Geothermal resources are increasingly gaining attention as a competitive, clean energy source to address the energy crisis and mitigate climate change. The Wugongshan area, situated in the southeast coast geothermal belt of China, is a typical geothermal anomaly and contains abundant medium- and low-temperature geothermal resources. This study employed hydrogeochemical and isotopic techniques to explore the cyclic evolution of geothermal water in the western Wugongshan region, encompassing the recharge origin, water–rock interaction mechanisms, and residence time. The results show that the geothermal water in the western region of Wugongshan is weakly alkaline, with low enthalpy and mineralization levels. The hydrochemistry of geothermal waters is dominated by Na-HCO3 and Na-SO4, while the hydrochemistry types of cold springs are all Na-HCO3. The hydrochemistry types of surface waters and rain waters are Na-HCO3 or Ca-HCO3. The δD and δ18O values reveal that the geothermal waters are recharged by atmospheric precipitation at an altitude between 550.0 and 1218.6 m. Molar ratios of major solutes and isotopic compositions of 87Sr/86Sr underscore the significant role of silicate weathering, dissolution, and cation exchange in controlling geothermal water chemistry. Additionally, geothermal waters experienced varying degrees of mixing with cold water during their ascent. The δ13C values suggest that the primary sources of carbon in the geothermal waters were biogenic and organic. The δ34S value suggests that the sulfates in geothermal water originate from sulfide minerals in the surrounding rock. Age dating using 3H and 14C isotopes suggests that geothermal waters have a residence time exceeding 1 kaBP and undergo a long-distance cycling process. 相似文献