全文获取类型
收费全文 | 450篇 |
免费 | 199篇 |
国内免费 | 119篇 |
专业分类
测绘学 | 28篇 |
大气科学 | 66篇 |
地球物理 | 205篇 |
地质学 | 315篇 |
海洋学 | 32篇 |
天文学 | 37篇 |
综合类 | 5篇 |
自然地理 | 80篇 |
出版年
2023年 | 3篇 |
2022年 | 14篇 |
2021年 | 18篇 |
2020年 | 20篇 |
2019年 | 28篇 |
2018年 | 18篇 |
2017年 | 28篇 |
2016年 | 24篇 |
2015年 | 23篇 |
2014年 | 32篇 |
2013年 | 30篇 |
2012年 | 19篇 |
2011年 | 30篇 |
2010年 | 13篇 |
2009年 | 28篇 |
2008年 | 45篇 |
2007年 | 34篇 |
2006年 | 40篇 |
2005年 | 25篇 |
2004年 | 24篇 |
2003年 | 23篇 |
2002年 | 21篇 |
2001年 | 28篇 |
2000年 | 22篇 |
1999年 | 19篇 |
1998年 | 24篇 |
1997年 | 21篇 |
1996年 | 13篇 |
1995年 | 19篇 |
1994年 | 17篇 |
1993年 | 25篇 |
1992年 | 10篇 |
1991年 | 7篇 |
1990年 | 6篇 |
1989年 | 4篇 |
1988年 | 3篇 |
1986年 | 1篇 |
1985年 | 3篇 |
1984年 | 1篇 |
1983年 | 1篇 |
1980年 | 1篇 |
1978年 | 1篇 |
1976年 | 1篇 |
1975年 | 1篇 |
排序方式: 共有768条查询结果,搜索用时 859 毫秒
51.
研究了三元体系Li~+,Mg~(2+)∥SO_4~(2-)—H_2O在25℃时的相关系和平衡液相的密度、粘度、折光率、电导等物化性质,该体系为简单共饱型,两段溶解度曲线对应于体系的两种原始组份Li_2SO_4·H_2O和MgSO_4·7H_2O的结晶区,无复盐和固溶体形成,亦无脱水作用发生,应用电解质溶液Pitzer模型检测该体系25C的溶解度,并用经验或半经验公式对平衡液相的密度和折光率进行了理论计算,计算值与实验值非常接近。 相似文献
52.
53.
The nature and distribution of fluids during amphibolite facies metamorphism, Naxos (Greece) 总被引:1,自引:0,他引:1
On the basis of fluid inclusion evidence, pervasive influx of deep-seated CO2 -rich fluids has been invoked to account for mid- to upper amphibolite facies (M2B ) metamorphism on the island of Naxos (Cyclades, Greece). In this paper, mineral devolatilization and melt equilibria are used to constrain the composition of both syn- and post-peak-M2B fluids in the deepest exposed levels of the metamorphic complex. The results indicate that peak-M2B fluids were spatially and compositionally heterogeneous throughout the high-grade core of the complex, whereas post-peak-M2B fluids were generally water-rich. The observed heterogeneities in syn-M2B fluid composition are inconsistent with pervasive CO2 -flushing models invoked by previous workers on the basis of fluid inclusion evidence. It is likely that few CO2 -rich fluid inclusions on Naxos preserve fluids trapped under peak metamorphic conditions. It is suggested that many of these inclusions have behaved as chemically open systems during the intense deformation that accompanied the uplift of the metamorphic complex. A similar process may explain the occurrence of some CO2 -rich fluid inclusions in granulite facies rocks. 相似文献
54.
作者再次改进了引潮位展开,潮波振幅给到小数后第六位,共3070个潮波.文中论述了引潮位展开的精度,同时给出为了保证潮汐计算的高精度而所需引入的各项改正及其说明. 相似文献
55.
56.
为了研究东台吉乃尔盐湖卤水蒸发时的相化学,确定钾、镁和锂盐的结晶特性,在实验室内25℃等温蒸发实验基础上和自然条件下进行了冬夏季日晒蒸发试验.东台吉乃尔盐湖卤水是由氯化钠饱和的多组分复杂体系构成的.卤水中存在的离子是Na+、K+、Mg2+、Li+、Ca2+、B3+、SO42-和Cl-.试验数据与Na+、K+、Mg2+Cl-、SO42-KH2O五元体系介稳平衡数据进行了讨论和比较.Autenrieth相图被用来表示各数据间的关系和证明冬夏季蒸发时结晶行为的差别. 相似文献
57.
This paper is concerned with the thermodynamic theory of solution and precipitation processes in wet crustal rocks and with the mechanism of steady pressure-solution slip in contact zones, such as grain-to-grain contacts, fracture surfaces, and permeable gouge layers, that are infiltrated by a mobile aqueous solution phase. A local dissipation jump condition at the phase boundary is fundamental to identifying the thermodynamic force driving the solution and precipitation process and is used here in setting up linear phenomenological relations to model near-equilibrium phase transformation kinetics. The local thermodynamic equilibrium of a stressed pure solid in contact with its melt or solution phase is governed by Gibbs's relation, which is rederived here, in a manner emphasizing its independence of constitutive assumptions for the solid while neglecting surface tension and diffusion in the solid. Fluid-infiltrated contact zones, such as those formed by rough surfaces, cannot generally be in thermodynamic equilibrium, especially during an ongoing process of pressure-solution slip, and the existing equilibrium formulations are incorrect in overlooking dissipative processes tending to eliminate fluctuations in superficial free energies due to stress concentrations near asperities, defects, or impurities. Steady pressure-solution slip is likely to exhibit a nonlinear dependence of slip rate on shear stress and effective normal stress, due to a dependence of the contact-zone state on the latter. Given that this dependence is negligible within some range, linear relations for pressure-solution slip can be derived for the limiting cases of diffusion-controlled and interface-reaction-controlled rates. A criterion for rate control by one of these mechanisms is set by the magnitude of the dimensionless quantityk/2C
pD, wherek is the interfacial transfer coefficient, is the mean diffusion path length,C
p is the solubility at pressurep, andD is the mass diffusivity. 相似文献
58.
矿床中存在着岩浆离熔成因的磁黄铁矿-镍黄铁矿矿石和热液改造成因的黄铁矿-针镍矿-辉镍矿矿石。研究证明现在矿石中存在的硫化物均为较低温度条件下的变质产物,并且矿物组合的更替不仅同温度变化有关,同时还受体系中氧逸度和硫离子活度的控制。矿物组合的地球化学分析表明,现有Fe-Ni-S体系低温(<300℃)相平衡图解之间存在着矛盾的原因可能是忽略了氧化-还原条件的影响。 相似文献
59.
根据浙闽台站记录的台湾琉球近震资料,研究了该区Lg波的组成及各震相的基本特征。研究表明,该区Lg波由多个速度不同的波群组成,在Lg1和Lg2两种波中可以分出Lg′1、Lg″1;和Lg′2、Lg″2四种震相,不同震区各震相的记录特征明显不同,鲜明地反映出地壳结构由大陆型向海洋型过渡的特点。此外,还对波列中的未知震相、影响震相记录特征的其它因素,以及震相标注和Lg波走时表等问题进行了讨论。 相似文献
60.