全文获取类型
收费全文 | 2891篇 |
免费 | 525篇 |
国内免费 | 742篇 |
专业分类
测绘学 | 207篇 |
大气科学 | 505篇 |
地球物理 | 690篇 |
地质学 | 1622篇 |
海洋学 | 382篇 |
天文学 | 161篇 |
综合类 | 219篇 |
自然地理 | 372篇 |
出版年
2024年 | 16篇 |
2023年 | 52篇 |
2022年 | 158篇 |
2021年 | 150篇 |
2020年 | 142篇 |
2019年 | 204篇 |
2018年 | 169篇 |
2017年 | 155篇 |
2016年 | 156篇 |
2015年 | 159篇 |
2014年 | 165篇 |
2013年 | 236篇 |
2012年 | 193篇 |
2011年 | 177篇 |
2010年 | 165篇 |
2009年 | 169篇 |
2008年 | 136篇 |
2007年 | 141篇 |
2006年 | 124篇 |
2005年 | 88篇 |
2004年 | 67篇 |
2003年 | 69篇 |
2002年 | 82篇 |
2001年 | 87篇 |
2000年 | 90篇 |
1999年 | 103篇 |
1998年 | 102篇 |
1997年 | 82篇 |
1996年 | 83篇 |
1995年 | 68篇 |
1994年 | 54篇 |
1993年 | 57篇 |
1992年 | 56篇 |
1991年 | 36篇 |
1990年 | 36篇 |
1989年 | 26篇 |
1988年 | 19篇 |
1987年 | 14篇 |
1986年 | 11篇 |
1985年 | 7篇 |
1984年 | 9篇 |
1983年 | 13篇 |
1982年 | 4篇 |
1981年 | 5篇 |
1979年 | 4篇 |
1978年 | 4篇 |
1977年 | 8篇 |
1976年 | 2篇 |
1969年 | 1篇 |
1968年 | 1篇 |
排序方式: 共有4158条查询结果,搜索用时 31 毫秒
61.
WangShicheng YeShuisheng ZhouDongdai 《中国地质大学学报(英文版)》2003,14(3):207-214
Metallogenic prognosis of synthetic information uses the geological body and the miaeral resource body as a statistical unit to interpret synthetically the information of geology, geophysics, geo-chemistry and remote sensing from the evolution of geology and puts all the information into one entire system by drawing up digitalized interpretation maps of the synthetic information. On such basis, differ-ent grades and types of mineral resource prospecting models and predictive models of synthetic informa-tion can be established. Hence, a new integrated prediction system will be formed of metallogenic prog-nosis (qualitative prediction), mineral resources statistic prediction (determining targets) and mlaeral resources prediction (determining resources amount). 相似文献
62.
During the whole 20th century in China, especially the latest 50 years, we have gotten much geological information about geological mapping, geophysics, geochemistry, mineral exploration,remote sensing, environmental geology, hydrogeology, engineering geology and oceanic geology etc. by our geologists and explorers. All the information has been accmnulated and can be used as a dcision-making foundation for the future plan of geological survey. The spatial database of geological survey ex-tents has been established by using computer technology. The database contained all kinds of exploration sections and collected about 160 000 records in this database. This paper introduces the data construc-tion ,contents and applying systemof this database, and trys to let people know what kinds of geological survey were finished, when the exploration were carried out, and how and where you can get this infor-mation. 相似文献
63.
统计1965年以来影响韶关的热带气旋发现,韶关出现暴雨不仅与热带气旋的路径、强度有关,而且与大气层结稳定度或冷空气的相互作用密切相关。由此结合实况、应用数值预报产品来制作热带气旋暴雨24小时预报。 相似文献
64.
65.
通过对1975~1998年北京动物园动物发病率的统计分析,揭示了不同动物发病率的年变化特征和长期变化趋势,并分季节进行了发病率与气象因子的相关分析,发现冬季兽类发病率、秋季禽类发病率与同期气象因子相关较好,总体看春、夏季动物发病率与气象因子的关系不明显。 相似文献
66.
The Northward Shift of Climatic Belts in China During the Last 50 Years and the Corresponding Seasonal Responses 总被引:29,自引:0,他引:29
Along the meridian of 105°E, the Chinese region are divided into two parts, east and west. The results show that in the east part of China the temperate extratropical belt, the warm extratropical belt,and the northern subtropical belt shift northward significantly, whereas the middle subtropical belt and the southern subtropical belt have less or no change. As for the northern subtropical belt, the maximal northward shift can reach 3.7 degrees of latitude. As for the warm extratropical belt, along the meridian of 120°-125°E, the maximal northward shift can reach 3-4 degrees. In the west part of China, each climatic belt changes little. Only in the Xinjiang area are the significant northward shifts. Correspondingly, it is found that in the last 50 years the traditional seasons have changed. For Beijing, Hailar, and Lanzhou, in general, summer becomes longer and winter shorter over the last 50 years. Summer begins early and ends late with respect to early 1950s. Contrary to the summer, winter begins la 相似文献
67.
68.
丽江大研镇震灾分布和地脉动测量结果之间的相关性 总被引:4,自引:2,他引:4
丽江7.0级地震后,大研镇被毁建筑物的地理分布呈显4条条带,伤亡人员的地理分布和上述条带重合。91个短周期地脉动测点的观测资料表明,分布在上述条带内的大多数测点,其卓越周期大于0.3S;条带外的测点,其卓越周期一般在0.1S左右。作认为卓越周期和烈度异常之间良好的相关性,是因为地脉动卓越周期和地方震的频谱之间存在良好的相关性。 相似文献
69.
Mesoscale surface turbulent fluxes over a complex terrain surrounded by oceans have been investigated using a 3-D numerical mesoscale model, under conditions with and without synoptic flows. The study indicated that under synoptically calm condition, the allocation and intensity of mesoscale surface turbulent fluxes (MSTFs) were greatly impacted by the thermally forced mesoscale circulation (TFMC) over mesoscale heterogeneous landscape. The max-imum values of sensible (Hs) and latent (LE) heat fluxes were located over the convergent zones and considerably im-pacted by the soil wetness (M), but did not depend strongly on the atmospheric background thermal stability (β0). The simulated results suggested that the sensible heat flux was closely proportional to the square of wind speed in the surface layer. By the action of synoptic flow, the allocation of LE was shifted to downwind, its intensity increased. 相似文献
70.
Liu Jian Ye Zhizheng Han Chunrui Liu Xinbo Qu Gaosheng 《Journal of Asian Earth Sciences》1997,15(6):465
This paper focuses on a borehole, Xichen-1 well, drilled on the Chenhang Island, Xisha Islands in the South China Sea. Mineralogical, petrographic, stable isotopic and minor-element data from the Holocene to Pleistocene interval (0–179 m ) in the Xichen-1 well are discussed in detail. The 400-m-long core is divisible into four mineralogical facies: a high-Mg calcitic aragonite facies (0–16.91 m, Holocene), an aragonitic low- Mg calcite facies (16.91–30.60 m, Late Pleistocene), a low- Mg calcitic facies (30.60–179 m, Middle-Early Pleistocene) and a low- Mg calcitic and dolomitic facies (179–400 m, Early Pleistocene–Late Miocene). The Holocene section has much higher whole-rock δ18O and δ13C values and Mg and Sr content than the non-dolomitized Pleistocene limestones (16.91–179 m). The 16.91–165 m interval is characterized by a relatively invariant oxygen isotopic composition and very heterogeneous carbon isotopic composition. Between 165 and 179 m, there is a positively correlated increase of whole-rock δ18O and δ18C with depth, and Mg content also shows a gradual increase with depth. Petrographic data demonstrate that the Pleistocene reef sequence has been extensively affected by meteoric waters. We conclude that the Late Pleistocene section (16.91–30.60 m) and the Middle-Early Pleistocene section (30.60–165 m) have suffered incomplete and complete meteoric diagenesis, respectively, and that the Early Pleistocene interval (165–179 m) was diagenetically altered in a meteoric–marine mixing environment. 相似文献