全文获取类型
收费全文 | 7984篇 |
免费 | 1386篇 |
国内免费 | 2124篇 |
专业分类
测绘学 | 756篇 |
大气科学 | 1498篇 |
地球物理 | 1958篇 |
地质学 | 4085篇 |
海洋学 | 1131篇 |
天文学 | 240篇 |
综合类 | 735篇 |
自然地理 | 1091篇 |
出版年
2024年 | 29篇 |
2023年 | 108篇 |
2022年 | 278篇 |
2021年 | 356篇 |
2020年 | 264篇 |
2019年 | 360篇 |
2018年 | 408篇 |
2017年 | 361篇 |
2016年 | 425篇 |
2015年 | 395篇 |
2014年 | 472篇 |
2013年 | 525篇 |
2012年 | 539篇 |
2011年 | 550篇 |
2010年 | 541篇 |
2009年 | 538篇 |
2008年 | 468篇 |
2007年 | 535篇 |
2006年 | 401篇 |
2005年 | 397篇 |
2004年 | 388篇 |
2003年 | 309篇 |
2002年 | 443篇 |
2001年 | 382篇 |
2000年 | 352篇 |
1999年 | 306篇 |
1998年 | 189篇 |
1997年 | 189篇 |
1996年 | 173篇 |
1995年 | 158篇 |
1994年 | 143篇 |
1993年 | 93篇 |
1992年 | 78篇 |
1991年 | 63篇 |
1990年 | 58篇 |
1989年 | 41篇 |
1988年 | 40篇 |
1987年 | 35篇 |
1986年 | 18篇 |
1985年 | 15篇 |
1984年 | 16篇 |
1983年 | 6篇 |
1982年 | 13篇 |
1981年 | 9篇 |
1980年 | 8篇 |
1979年 | 2篇 |
1976年 | 3篇 |
1975年 | 2篇 |
1972年 | 2篇 |
1971年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
881.
882.
新疆乌苏市农七师红山煤矿2号矿区钻探施工技术 总被引:1,自引:0,他引:1
本文从施工设备及技术处理等方面阐述了红山煤矿2号矿区钻探施工工艺,为进一步开展煤田勘查施工工作提供了借鉴。 相似文献
883.
INTRODUCTIONThe distribution of remaining oil is often de-scribed qualitatively .The remaining oil distributedinthe whole reservoir is calculated according to thecharacteristics of the space distribution of the satura-tion of remaining oil . Logging data are required toaccomplish this . However , many such projects can-not be completed.This method of studyingremainingoil distribution cannot be quantified efficiently and isunable to provide an effective quantitative forecast ofthe distribu… 相似文献
884.
885.
通过对2006年5月3日和7月17日库尔勒地区两次强对流天气的形势和物理量对比分析,以及库尔勒新一代天气雷达(CINRAD-CC)产品中的组合反射率(CR)、风暴相对平均径向速度(V)等产品的分析,得出库尔勒地区夏季强对流天气过程发生时的有利天气形势、物理量场分布及多谱勒天气雷达产品特征。 相似文献
886.
在灰色聚类方法原理的基础上,探讨了如何通过白化函数生成灰色聚类矩阵,并以常州市第Ⅱ承压地下水为例进行了水质评价,评价结果表明,常州市大部分第Ⅱ承压地下水水质优良,达到了Ⅰ类水,未遭受外来物质的污染,评价结果符合实际情况。 相似文献
887.
鄂尔多斯盆地西峰油田白马南特低渗岩性油藏储层地质建模 总被引:2,自引:0,他引:2
以鄂尔多斯盆地西峰油田白马南长81砂岩油藏为例,应用随机序贯高斯模拟法(SUS)和序贯指示模拟法(SIS)建立研究目标的储层地质模型,进而探讨了在特低渗岩性油藏中相对高渗透储层形成的控制因素。认为长81油藏储层的形成主要受控于沉积作用;成岩作用对改善储层物性及油气的运聚起了重要的作用。砂体的三维模拟结果显示主砂体位于研究区西部,呈西南-东北向展布。储层物性参数的三维模拟也表明优质储层主要分布在主砂体带上长石溶蚀相和绿泥石薄膜胶结成岩相区。 相似文献
888.
An 8.1Ma calcite record of Asian summer monsoon evolution on the Chinese central Loess Plateau 总被引:5,自引:0,他引:5
Chen XiuLing Fang XiaoMin An ZhiSheng Han WenXia Wang Xin Bai Yan Hong Ye 《中国科学D辑(英文版)》2007,50(3):392-403
Carbonates in loess-red clay sequences consist mainly of calcite and dolomite. The EDTA analysis of carbonates in different size fractions and magnetic susceptibility reveal that calcite is a sensitive index of summer monsoon. The chemical analysis of carbonates and calcite from an 8.1 Ma loess-red clay sequence at Chaona on the Chinese central Loess Plateau shows that the evolution of the Asian summer monsoon experienced four stages, namely 8.1―5.5 Ma, 5.5―2.8 Ma, 2.8―1.5 Ma and 1.5―0 Ma, with increasing intensification and fluctuation, suggesting a possible combining impacts of uplift of the Tibetan Plateau and global changes on the Asian summer monsoon. 相似文献
889.
Fossil oyster reefs are indicators of past sea levels, and their formation is usually dated by means of radiocarbon. However, radiocarbon dating of the shells from coastal areas may be complicated by the varying sources of carbon. Here we applied optical dating methods to date the samples from above and below a fossil oyster bed in a section on the coast of Bohai Bay, China. The optical ages of the sediments were used to constrain the oyster bed. Single-aliquot regenerative-dose procedures using the OSL signal from fine grain quartz, the IRSL and post-IR OSL signals from polymineral fine grains were employed to determine equivalent dose (De). The behaviors of the different luminescence signals from quartz and polymineral grains during De measurements were examined. The results showed that the quartz OSL signal is more reliable than the polymineral IRSL and post-IR OSL signals with respect to dating for these coastal samples. The optical ages indicated that the oyster reef formed between ca. 6.2 and 5.0 ka. 相似文献
890.
Wang XiaoYuan Zeng ZhiGang Liu ChangHua Yin XueBo Yu ShaoXiong Yuan ChunWei Zhang GuoLiang Wang XiaoMei 《中国科学D辑(英文版)》2007,50(9):1433-1440
During the DY105-12, 14cruise (R/V DAYANG YIHAO, November 2003) on East Pacific Rise (EPR) 12- 13°N, the submarine hydrothermal activity was investigated and the CTD hydrocast was carried out at EPR12°39′N-12°54′N. From the temperature anomalies and the concentrations of magnesium, chlorine, bromine in seawater samples, we discover that magnesium depletes 9.3%-22.4%, chlorine and bro- mine enrich 10.3%-28.7% and 10.7%-29.0% respectively relative to normal seawater at the stations which have chemistry anomalies, moreover temperature and chemistry anomalies are at the same layer. The depletion of magnesium in the plume may be caused by a fluid lacking of magnesium which rises after the hydrothermal fluid reaches the equilibrium with ambient seawater, the enrichment of chlorine and bromine might be the result of inputting later brine which is generated by phase separation due to hydrothermal activity. In addition, the Br/Cl ratio in the abnormal layers at the survey area is identical to that in seawater, which implies that halite dissolution (or precipitation) occurs neither when the fluid is vented nor when hydrothermal fluid entraining ambient seawater rises to form plume. From the ab- normal instance at E55 station, it is very possible that there might exist a new hydrothermal vent site. 相似文献