全文获取类型
收费全文 | 1339篇 |
免费 | 300篇 |
国内免费 | 204篇 |
专业分类
测绘学 | 147篇 |
大气科学 | 23篇 |
地球物理 | 549篇 |
地质学 | 709篇 |
海洋学 | 85篇 |
天文学 | 177篇 |
综合类 | 35篇 |
自然地理 | 118篇 |
出版年
2024年 | 7篇 |
2023年 | 19篇 |
2022年 | 28篇 |
2021年 | 38篇 |
2020年 | 52篇 |
2019年 | 72篇 |
2018年 | 38篇 |
2017年 | 57篇 |
2016年 | 62篇 |
2015年 | 70篇 |
2014年 | 55篇 |
2013年 | 74篇 |
2012年 | 94篇 |
2011年 | 62篇 |
2010年 | 70篇 |
2009年 | 72篇 |
2008年 | 76篇 |
2007年 | 122篇 |
2006年 | 142篇 |
2005年 | 90篇 |
2004年 | 89篇 |
2003年 | 60篇 |
2002年 | 68篇 |
2001年 | 51篇 |
2000年 | 38篇 |
1999年 | 53篇 |
1998年 | 28篇 |
1997年 | 25篇 |
1996年 | 25篇 |
1995年 | 20篇 |
1994年 | 18篇 |
1993年 | 9篇 |
1992年 | 7篇 |
1991年 | 13篇 |
1990年 | 5篇 |
1989年 | 13篇 |
1988年 | 3篇 |
1987年 | 7篇 |
1986年 | 1篇 |
1985年 | 2篇 |
1984年 | 1篇 |
1979年 | 2篇 |
1954年 | 5篇 |
排序方式: 共有1843条查询结果,搜索用时 580 毫秒
41.
42.
43.
Abstract The mantle-derived xenoliths entrained in the Pliocene basanite from Baengnyeong Island, South Korea, are spinel lherzolites and spinel harzburgites. The overall compositional range of the Baengnyeong xenoliths matches that of the post-Archean xenoliths of lithospheric mantle origin from eastern China, but without any compositional evidence for a refractory Archean mantle root. Mineral compositions of the xenoliths have been used to estimate the equilibrium temperatures and pressures, and to construct a paleogeothermal gradient of the source region. The xenolith-derived paleogeotherm is constrained from about 820°C at 7.3 kbar to 1000°C at 20.6 kbar. Like those from the post-Archean Chinese xenoliths of lithospheric mantle origin, the Baengnyeong geotherm is considerably elevated relative to the conductive models at the depth of the crust–mantle boundary, reflecting a thermal perturbation probably related to lithospheric thinning. There is no significant P / T difference between harzburgite and lherzolite, which suggests that the harzburgites are interlayered with lherzolites within the depth interval beneath Baengnyeong Island. 相似文献
44.
45.
46.
Abstract. Scanning electron microscopy-cathodoluminescence (SEM-CL) imaging of vein quartz in the Cu-mineralised, Shuteen Complex (South Gobi, Mongolia) has revealed a complex history of crystal growth, dissolution and microfracture healing, associated with several hydrothermal events that could not be detected using other observational techniques (e.g. transmitted/reflected light microscopy, back-scattered electron imaging, or secondary electron imaging).
The quartz initially grew as CL-bright/grey crystals in a 345±30C liquid reservoir, as inferred by the analysis of primary liquid fluid inclusions (average Th of 343C; 6.6∼7.7 wt% NaCleq ). Quartz precipitation occurred at the edge of the crystals as reservoir fluids cooled to 260±25C, as indicated by micron-scale CL-dark/CL-bright quartz growth bands containing abundant fluid inclusions (with an average Th values of 261C). Pressure fluctuations were the likely cause of dissolution, as SEM-CL imaging reveals the quartz have corroded or rounded crystal edges, and precipitation of later quartz into open space. SEM-CL imaging shows the quartz contains healed microfractures that trapped low salinity fluids (3.9 wt% NaC1eq ) with Th values of 173±15C.
SEM-CL imaging provides a means of deciphering the thermal and chemical evolution of the fossil Shuteen hydrothermal system, and the nature of hydrothermal quartz vein-forming processes, by facilitating the correlation of distinct fluid inclusion populations and their relative chronology, with specific hydrothermal events. 相似文献
The quartz initially grew as CL-bright/grey crystals in a 345±30C liquid reservoir, as inferred by the analysis of primary liquid fluid inclusions (average Th of 343C; 6.6∼7.7 wt% NaCl
SEM-CL imaging provides a means of deciphering the thermal and chemical evolution of the fossil Shuteen hydrothermal system, and the nature of hydrothermal quartz vein-forming processes, by facilitating the correlation of distinct fluid inclusion populations and their relative chronology, with specific hydrothermal events. 相似文献
47.
The Clementine spacecraft orbited the Moon and acquired science data for 10 weeks in the Spring of 1994. During this time
it collected global 11-band multispectral images and near global altimetry. Select areas of the Moon were imaged at 25 m/pixel
in visible light and 60 m/pixel in thermal wavelengths. From these datasets a new paradigm for the evolution of the lunar
crust emerged. The Moon is no longer viewed as a two-terrane planet, the Apollo samples were found not to represent the lunar
crust as a whole, and the complexity of lunar crustal stratigraphy was further revealed. More than ten years later the Clementine
datasets continue to significantly advance lunar science and will continue to do so as new measurements are returned from
planned missions such as Chandrayaan, SELENE, and Lunar Reconnaissance Orbiter. This paper highlights the scientific research
conducted over the last decade using Clementine data and summarizes the influence of Clementine on our understanding of the
Moon. 相似文献
48.
49.
右江盆地晚侏罗世钾玄质高镁安山岩的厘定及其构造意义 总被引:4,自引:4,他引:0
右江盆地在大地构造上处于特提斯和滨太平洋构造域的结合部位。本文报道了该盆地东部杨屯安山岩的岩相学、年代学和地球化学特征。杨屯安山岩具斑状结构和气孔状构造,斑晶主要为辉石,基质以针状斜长石微晶为主,含少量辉石。LA-ICP-MS锆石U-Pb定年结果表明杨屯安山岩的喷发时代为159.3±2.8Ma,即晚侏罗世。样品的Si O2含量为53.13%~55.71%,具高MgO(6.74%~8.85%)、Mg#值(63~72)、Cr(416×10~(-6)~565×10~(-6))和Ni(207×10~(-6)~246×10~(-6)),低Fe OT/MgO(0.83~1.23)等特征,与典型高镁安山岩的特征相似。所有样品具高K2O(3.39%~4.77%)和K2O/Na2O(1.31~2.33),同时也具钾玄质岩石的地球化学特征。样品强烈富集大离子亲石元素和轻稀土元素,而亏损高场强元素,具较高的Rb/Sr(0.20~0.46)和较低的Ba/Rb(7.17~9.30),富集的Sr-Nd同位素组成((87Sr/86Sr)i=0.70738~0.70739,εNd(t)=-3.6~-3.4)。元素和同位素特征表明杨屯钾玄质高镁安山岩是含金云母的富集岩石圈地幔部分熔融的产物,形成于板内伸展环境而不是岛弧环境。晚侏罗世杨屯钾玄质高镁安山岩的厘定,反映了该时期右江地区处于岩石圈伸展-减薄阶段。 相似文献
50.
《Marine Policy》2016
Seeing the ocean through the eyes of seabirds could help meet the challenges of managing common-pool marine resources both in protected and unprotected areas. First, seabirds are top-predators, exposed to all threats affecting the oceans, and this makes them ideal sentinel organisms for monitoring changes within marine ecosystems. Second, seabirds cross both ecological and political boundaries, and following their movements should help making interdependencies within and between marine ecosystems more visible. Third, seabirds are conspicuous and often charismatic animals, which interact differently with different groups of stakeholders and provide the opportunity to acknowledge and discuss each other's values and interests. In this paper, we present these research avenues using a seabirds’ view, for tackling marine conservation and management issues, and we give operational examples of implementation based on our work in the English Channel. 相似文献