全文获取类型
收费全文 | 4436篇 |
免费 | 712篇 |
国内免费 | 1185篇 |
专业分类
测绘学 | 570篇 |
大气科学 | 265篇 |
地球物理 | 309篇 |
地质学 | 4340篇 |
海洋学 | 241篇 |
天文学 | 25篇 |
综合类 | 376篇 |
自然地理 | 207篇 |
出版年
2024年 | 10篇 |
2023年 | 45篇 |
2022年 | 136篇 |
2021年 | 169篇 |
2020年 | 157篇 |
2019年 | 216篇 |
2018年 | 150篇 |
2017年 | 162篇 |
2016年 | 218篇 |
2015年 | 194篇 |
2014年 | 341篇 |
2013年 | 254篇 |
2012年 | 345篇 |
2011年 | 307篇 |
2010年 | 277篇 |
2009年 | 235篇 |
2008年 | 261篇 |
2007年 | 311篇 |
2006年 | 304篇 |
2005年 | 312篇 |
2004年 | 298篇 |
2003年 | 244篇 |
2002年 | 202篇 |
2001年 | 172篇 |
2000年 | 168篇 |
1999年 | 143篇 |
1998年 | 138篇 |
1997年 | 135篇 |
1996年 | 101篇 |
1995年 | 68篇 |
1994年 | 54篇 |
1993年 | 53篇 |
1992年 | 54篇 |
1991年 | 20篇 |
1990年 | 20篇 |
1989年 | 11篇 |
1988年 | 17篇 |
1987年 | 8篇 |
1986年 | 11篇 |
1985年 | 1篇 |
1984年 | 2篇 |
1982年 | 1篇 |
1980年 | 5篇 |
1979年 | 1篇 |
1978年 | 1篇 |
1977年 | 1篇 |
排序方式: 共有6333条查询结果,搜索用时 78 毫秒
81.
FLAC数值模拟软件及其在地学中的应用 总被引:15,自引:0,他引:15
FLAC是以拉格朗日差分法为基础的一种数值模拟应用软件,主要用于岩土力学工程。近年地质学家将其应用到地质构造和块体运动学、动力学研究中,以证实或证伪地球学家们提出的相关地球动力学模型。本文初步介绍了FLAC应用软件的基本原理、使用方法以及它在国内外地质学上的几个应用实例。 相似文献
82.
非常规综合物化探方法油气预测研究中存在的主要问题为:缺乏系统与综合的基础性理论研究,异常形成的机理还不十分清楚,在参数的优化组合及异常的求取上尚有诸多不足。针对后一种情况,选择松辽盆地东岭构造作为实验区进行了有益的探索。选取低能吸附烃、放射性测氡及土壤热释光三类参数进行了优化组合,分别计算了综合指标MAE与MAC及组合熵,然后对各值采用泛克里格法求取异常,取得了良好的效果。下一步研究应从异常形成的机理入手,建立三维非常规综合物化探油气预测模式,以提高油气预测成功率。 相似文献
83.
84.
X射线衍射峰五基本要素的物理学意义与应用 总被引:6,自引:0,他引:6
本文根据Bragg衍射方程、Scherrer方程、衍射强度计算原理,研究讨论了X射线衍射5构成要素中的衍射峰位置、衍射峰宽度、衍射峰高度的物理学意义。根据实验研究证明了衍射峰不对称性的几何条件特征,并用地质事实验证了衍射形态变化与晶格应变和粒度大小的内在联系。从而阐明了单个衍射峰5基本构成要素的完整物理学意义,并以实例论证了5要素的实际应用价值。 相似文献
85.
86.
It has long been debated that the Dabie orogenic belt belongs to the North China or Yangtze craton. In recent years, eastern
China has been suggested, based on the Pb isotopic compositions of Phanerozoic ore and Mesozoic granitoid K-feldspar (revealing
the crust Pb) in combination with Meso-Cenozoic basalts (revealing the mantle Pb), being divided into the North China and
Yangtze Pb isotopic provinces, where the crust and mantle of the Yangtze craton are characterized by more radiogenic Pb. In
this sense, previous researchers suggested that the pro-EW-trending Dabie crogenic belt with less radiogenic Pb in the crust
was part of the North China craton. In this paper, however, the Late Cretaceous basalts in the central and southern parts
of the Dabie orogenic belt are characterized by some more radiogenic Pb (206Pb/204Pb=17.936−18.349,207Pb/204Pb=15.500−15.688,208Pb/204Pb=38.399−38.775) and a unique U-Th-Pb trace element system similar to those of the Yangtze craton, showing that the Mesozoic
mantle is of the Yangtze type. In addition, the decoupled Pb isotopic compositions between crust and mantle were considerably
derived from their rheological inhomogeneity, implying a complicated evolution of the Dabie orogenic belt.
The study was funded by the National Natural Science Foundation of China (No. 49794043) and the Open Laboratory of Constitution,
Interaction and Dynamics of the Crust-Mantle System, China. 相似文献
87.
88.
Jean S. Kane 《Geostandards and Geoanalytical Research》2002,26(1):7-29
As in all fields of sample analysis, reference materials play a large role in supporting measurements in the geosciences. While a rather large number of materials are in distribution (> 380), not all are equally effective or fit-for-purpose in supporting laboratory data quality and thereby assuring the desired comparability of measurements between laboratories. Equally important, reference values that are not fit-for-purpose cannot be used effectively to establish traceability links between laboratory measurements and national and international standards. The needed fitness-for-purpose is not achieved for reference values either when more than one reference value has been proposed and a consensus does not exist among users as to which should be used by all, or when reference value uncertainties are too large in comparison to those of routine laboratory measurements. The focus of this review will be, first to outline the current reality, and second to suggest ways in which certifications of RMs can be improved to provide reference values that are universally accepted and more fit-for-purpose in general laboratory use. The discussion will be illustrated largely by current uses of USGS BCR-1, NIST SRM 610 and IAEA NBS28, as these three materials are those for which the largest body of newly published data exists, according to recent bibliographies of the geoanalytical literature published annually in Geostandards Newsletter: The Journal of Geostandards and Geoanalysis. 相似文献
89.
90.
The garnet-muscovite geothermometer was refined through empirical calibration by using natural rocks metamorphosed under the physical conditions of 238—1306 MPa and 490—700℃. Input temperatures and pressures were determined through simultaneously applying the garnet-biotite geothermometer and the garnet-biotite-plagioclase-quartz barometer, assuming that all FeO in muscovite and garnet be ferrous. Garnet was treated as the asymmetric quaternary solid solution, and muscovite as the symmetric binary solid solution. Input muscovite compositions include Fe atoms between 0.03—0.19 and Mg atoms between 0.04—0.16 on the basis of 11 oxygen atoms, and input garnet compositions include spessartine fractions between 0.01—0.289, grossular fractions between 0.028—0.273, and the Fe/Mg ratio between 3.387-18.986. The resulting garnet-muscovite geothermometer reproduces temperatures within (50℃ compared with the garnet-biotite thermometer. Total random error of ±37℃ of the new thermometer may stem from the pressure uncertainty of ±200 MPa, and uncertainties of ±5% of Fe and Mg components in muscovite, and ±5% of Fe, Mg, Mn and Ca components in garnet, altogether. When there exist 10%, 20%, 30%, 40% and 50% Fe3+ in muscovite, respectively, the computed garnet-muscovite temperatures will be 1—6℃, 2—12℃, 3—16℃, 5—24℃ and 7—29℃, respectively, lower than those obtained when assuming that all FeO be ferrous. The new garnet-muscovite geothermometer can efficiently reflect temperature change of typical prograde sequences and contact aureole rocks, and may be applied to low- to high-grade and low- to high-pressure metamorphic rocks. 相似文献