全文获取类型
收费全文 | 2327篇 |
免费 | 234篇 |
国内免费 | 362篇 |
专业分类
测绘学 | 220篇 |
大气科学 | 165篇 |
地球物理 | 174篇 |
地质学 | 1110篇 |
海洋学 | 132篇 |
天文学 | 920篇 |
综合类 | 83篇 |
自然地理 | 119篇 |
出版年
2024年 | 5篇 |
2023年 | 14篇 |
2022年 | 29篇 |
2021年 | 21篇 |
2020年 | 38篇 |
2019年 | 50篇 |
2018年 | 30篇 |
2017年 | 53篇 |
2016年 | 67篇 |
2015年 | 68篇 |
2014年 | 131篇 |
2013年 | 102篇 |
2012年 | 178篇 |
2011年 | 71篇 |
2010年 | 98篇 |
2009年 | 141篇 |
2008年 | 169篇 |
2007年 | 170篇 |
2006年 | 203篇 |
2005年 | 208篇 |
2004年 | 129篇 |
2003年 | 157篇 |
2002年 | 148篇 |
2001年 | 122篇 |
2000年 | 76篇 |
1999年 | 108篇 |
1998年 | 45篇 |
1997年 | 40篇 |
1996年 | 48篇 |
1995年 | 40篇 |
1994年 | 28篇 |
1993年 | 48篇 |
1992年 | 30篇 |
1991年 | 20篇 |
1990年 | 13篇 |
1989年 | 8篇 |
1988年 | 1篇 |
1987年 | 1篇 |
1986年 | 8篇 |
1985年 | 1篇 |
1984年 | 2篇 |
1983年 | 2篇 |
1977年 | 1篇 |
1975年 | 1篇 |
排序方式: 共有2923条查询结果,搜索用时 578 毫秒
991.
992.
993.
Li-Cai Deng Heidi Jo Newberg Chao Liu Jeffrey L. Carlin Timothy C. Beers Li Chen Hsu-Tai Lee Carl J. Grillmair Puragra Guhathakurta Zhan-Wen Han Jin-Liang Hou Sebastien Lepine Jing Li Xiao-Wei Liu Kai-Ke Pan J. A. Sellwood Bo Wang Hong-Chi Wang Fan Yang Brian Yanny Hao-Tong Zhang Yue-Yang Zhang Zheng Zheng Zi Zhu 《天体物理学报》2012,(7):735-754
994.
995.
Sukran Akkus Tulin Bal Nagihan M. Karaaslan Emre Yaman Ersin Kilinc Mehmet Yaman 《洁净——土壤、空气、水》2013,41(12):1229-1234
Five‐step sequential extractions were employed to fractionation of Ni, Cr and Cu in soil polluted by anthropogenic activities and determine the mobility of the metals. Twelve samples were collected on an agricultural area that was located near an airport and intercity roads in Elazig‐Turkey. Exchangeable, organically bounded, carbonate bounded, adsorbed species on Fe and Mn oxides and residual species (except silicates) of Ni, Cr and Cu were extracted into solution by using CaCl2, Na4P2O7, Na2EDTA, NH2OH–HCl and HNO3–H2O2, respectively. Mobile metal concentrations in fractions and total recoverable in soils were determined by using inductively coupled plasma‐optical emission spectrometry (ICP‐OES). Total recoverable Ni, Cr and Cu concentrations were in the range of 40–119, 45–126 and 23–72 mg kg?1, respectively. It was observed that total concentrations of metals in some of the samples were higher than the permitted values. The sum of the mobile percentages of metals was found to be lower than 50%. The Ni, Cr and Cu percentages for exchangeable species are in the ranges of 0.18–1.64, 0.03–0.59 and 0.42–2.53%, respectively. 相似文献
996.
Nguo Sylvestre KANOUO Khin ZAW Rose Fouateu YONGUE Frederick Lin SUTHERLAND Sebastien MEFFRE Emmanuel NJONFANG Changqian MA Milan Stafford TCHOUATCHA 《Resource Geology》2012,62(3):316-324
Zircons and other heavy minerals (corundum, rutile, ilmenite, magnetite, sillimanite) are identified in the Nsanaragati gem corundum placer deposit, in the western part of the Mamfe sedimentary basin, SW Cameroon. These alluvial minerals have different morphological characteristics and zircons, in particular, vary mostly in colour and shape. They are reddish, brownish, yellowish, pink or colourless. These minerals form rounded and sub‐rounded alluvial grains, prismatic, pyramidal or dipyramidal crystals. Reddish zircons retain their original crystallographic shape. Trace element and U–Pb isotopic geochemical analyses of these reddish zircons, using the LA‐ICP‐MS method give significant Hf (4576–6334 ppm), Th (46–1565 ppm) and U (66–687 ppm) contents, with Th/U ratio ranging from 0.6 to 3.0. The 206Pb/238U corrected mean age gave 12.39 ± 0.55 Ma, which characterizes an Upper Cenozoic (Serravallian) magmatic event. The zircons are probably sourced from a magmatic field in the South eastern boundary of the Cross River Formation. The Cameroon Volcanic Line of basaltic and alkaline lavas and intrusions which lie east of the Mamfe Basin mostly range in age from 37 Ma to <1 Ma. The zircons may also relate to the Mount Bambouto plateau lavas which lie northeast of the Mamfe sedimentary basin and have an eruptive age range of 21–14 Ma. The oldest Nsanaragati reddish zircon ages overlap within error with the end stages of the Bambouto eruptions. This eruptive or a related episode provides a potential source for megacrystic reddish zircons within the Nsanagarati placer deposit. 相似文献
997.
Patrick H. Donohue Antonio Simonetti Clive R. Neal 《Geostandards and Geoanalytical Research》2012,36(1):61-73
Seven ilmenite (FeTiO3) megacrysts derived from alnöite pipes (Island of Malaita, Solomon Islands) were characterised for their major and trace element compositions in relation to their potential use as secondary reference materials for in situ microanalysis. Abundances of thirteen trace elements obtained by laser ablation ICP‐MS analyses (using the NIST SRM 610 glass reference material) were compared with those determined by solution‐mode ICP‐MS measurements, and these indicated good agreement for most elements. The accuracy of the LA‐ICP‐MS protocol employed here was also assessed by repeated analysis of MPI‐DING international glass reference materials ML3B‐G and KL2‐G. Several of the Malaitan ilmenite megacrysts exhibited discrepancies between laser ablation and solution‐mode ICP‐MS analyses, primarily attributed to the presence of a titano‐magnetite exsolution phase (at the grain boundaries), which were incorporated solely in the solution‐mode runs. Element abundances obtained by LA‐ICP‐MS for three of the ilmenite megacrysts (CRN63E, CRN63H and CRN63K) investigated here had RSD (2s) values of < 20% and therefore can be considered as working values for reference purposes during routine LA‐ICP‐MS analyses of ilmenite. 相似文献
998.
999.
1000.
贵州务正道地区铝土矿床稀土元素组成及地质意义 总被引:2,自引:0,他引:2
稀土元素(REE)是一组具有相同地球化学性质和特殊地球化学属性的指示性元素。务正道地区主要矿床稀土元素组成显示出,矿层和下伏志留系韩家店组地层稀土元素总量、配分模式基本一致,相关性较好,揭示铝土矿成矿物源与下伏志留系韩家店组有成因联系;矿层和韩家店组LREE/HREE均大于1,轻稀土富集较强烈,而重稀土不同程度亏损;(La/Ce)N平均0.87,总体较低;δCe平均1.22,为弱-中等比值,表明铝土矿物源主要来自陆源,沉积环境主要为陆相沉积,局部为海相沉积;主要层位(La/Sm)N>(Gd/Yb)N,说明轻重稀土元素分异较好;稀土元素富集对岩性有选择性,在矿层及富含绿泥岩、粉砂质页岩的志留系韩家店组地层中强烈富集,在石炭系黄龙组白云质灰岩及二叠系栖霞组灰岩中贫化。 相似文献