全文获取类型
收费全文 | 1703篇 |
免费 | 342篇 |
国内免费 | 583篇 |
专业分类
测绘学 | 96篇 |
大气科学 | 455篇 |
地球物理 | 401篇 |
地质学 | 940篇 |
海洋学 | 231篇 |
天文学 | 130篇 |
综合类 | 153篇 |
自然地理 | 222篇 |
出版年
2024年 | 11篇 |
2023年 | 35篇 |
2022年 | 81篇 |
2021年 | 81篇 |
2020年 | 58篇 |
2019年 | 74篇 |
2018年 | 87篇 |
2017年 | 87篇 |
2016年 | 83篇 |
2015年 | 78篇 |
2014年 | 100篇 |
2013年 | 87篇 |
2012年 | 96篇 |
2011年 | 105篇 |
2010年 | 99篇 |
2009年 | 98篇 |
2008年 | 91篇 |
2007年 | 104篇 |
2006年 | 82篇 |
2005年 | 75篇 |
2004年 | 57篇 |
2003年 | 66篇 |
2002年 | 83篇 |
2001年 | 83篇 |
2000年 | 85篇 |
1999年 | 93篇 |
1998年 | 80篇 |
1997年 | 83篇 |
1996年 | 49篇 |
1995年 | 68篇 |
1994年 | 45篇 |
1993年 | 50篇 |
1992年 | 29篇 |
1991年 | 30篇 |
1990年 | 21篇 |
1989年 | 19篇 |
1988年 | 16篇 |
1987年 | 12篇 |
1986年 | 8篇 |
1985年 | 6篇 |
1984年 | 10篇 |
1983年 | 5篇 |
1982年 | 7篇 |
1981年 | 3篇 |
1978年 | 1篇 |
1977年 | 1篇 |
1975年 | 1篇 |
1973年 | 2篇 |
1971年 | 1篇 |
1958年 | 2篇 |
排序方式: 共有2628条查询结果,搜索用时 429 毫秒
21.
22.
Geochronological studies on the crust-derived Tianmenshan pluton were undertaken by SHRIMP zircon U-Pb dating and Ar-Ar dating of biotite, muscovite and K-feldspar, giving a petrogenetic age of 167 Ma. Owing to the closure systems in different minerals, the cooling history of the pluton can be determined with an age-temperature diagram. The late hydrothermal event has been recognized, which is related probably with mineralization. In terms of the comparative geochronological and petrologic records, it is concluded that there are some constrains on tectonic evolution and that the formation of the Tianmenshan pluton proceeded in a transition period from Indosinian post-orogeny extension to strong compressive tectonics. And the timing of the hydrothermal event matches the compressive climax of the Yanshanian orogeny. The temporal gap between granite emplacement and wolframite mineralization could last 10-20 Ma owing to the low cooling rate of the pluton. 相似文献
23.
本文介绍了全球稀土资源供需历史、现状和对未来的展望。从矿床成因视角切入,将稀土矿床分为内生和外生两大类型,其中内生稀土矿床包括碳酸岩型、碱性岩型、碱性岩型- 碳酸岩型、氧化铁铜金型、热液脉型,外生稀土矿床包括风化壳离子吸附型、沉积岩型、沉积矿产(煤矿、铝土矿和沉积磷矿)伴生型、砂矿和现代海洋底部含稀土的锰结核、结壳和软泥型。归纳总结了主要类型矿床的基本特点和时空分布;认为内生稀土矿床产出于四类构造环境,包括裂谷环境、碰撞后伸展环境、大陆碰撞环境和后俯冲伸展环境;从构造演化入手,探讨了在外生与内生地质过程中稀土元素的迁移和富集规律,建立了涵盖主要矿床类型的构造- 成矿模型。 相似文献
24.
The Ordovician radiation of marine life was among the most substantial pulses of diversification in Earth history and coincided in time with a major increase in the global level of orogenic activity. To investigate a possible causal link between these two patterns, the geographic distributions of 6576 individual appearances of Ordovician vician genera around the world were evaluated with respect to their proximity to probable centers of orogeny (foreland basins). Results indicate that these genera, which belonged to an array of higher taxa that diversified in the Middle and Late Ordovician (trilobites, brachiopods, bivalves, gastropods, monoplacophorans), were far more diverse in, and adjacent to, foreland basins than they were in areas farther removed from orogenic activity (carbonate platforms). This suggests an association of orogeny with diversification at that time. 相似文献
25.
26.
在Geolord-AT空三加密软件中对数码航片进行框标定向的前期处理,创建带有框标的数码航片或者直接创建内定向的*.kb文件,使数码航片顺利按要求通过内定向。 相似文献
27.
Distribution of the rare-earth elements (REE) in dacite has been studied so as to get a better understanding of the migration
behavior of REE during alteration. Both unaltered and altered samples were collected in an unpolluted area of Guangxi Zhuang
Autonomous Region, southwest China. The REE concentrations were analyzed by ICP-MS. It is concluded that the REE were enriched
during dacite alteration in varying degrees. The chondrite-normalized REE patterns of altered samples approximately maintain
the characteristics of unaltered samples. However, if we normalize the REE concentrations of altered samples with unaltered
dacite, fractionation of REE will appear. The LREE are more enriched than HREE in all altered samples with the LREE possibly
precipitated as carbonate minerals. Both positive and negative Eu anomalies exist. Enrichment, immobility and depletion are
noticed for the element Lu. Heavy mineral alteration, difference in stability constant between carbonate LREE and HREE complexes,
downward migration of weathering fluid and microenvironment change may be responsible for the fractionation of REE in the
altered dacite. 相似文献
28.
用现今小震推断洪洞、临汾两次历史大震的震源断层 总被引:5,自引:1,他引:5
山西临汾地区是一个历史强震多发区,1303年和1695年发生了洪洞(M=8)和临汾(M=73/4)两次特大地震,这两次地震所在区域至今仍在持续不断的小地震活动,具有明显的大震区地震长期活动特征,我们对临汾无线传输地震台网记录的1987-1999年期间发生的1670次中,小地震重新进行了震源定位,根据对这些地震震源位置三维空间分布特征和震源机解制的分析,认为洪洞地震的震源断层应是长80km,埋深5-26km的NNE走向,高倾角的右旋走滑型断层,而临汾地震的震源断层是长70km,埋深5-22km的NWW走向,高倾角的左旋走滑型断层。这与洪洞,临汾两次大震极震区的等震线及该地区应力场的构造环境是吻合的。 相似文献
29.
Introduction It is found that there are some relationships between the thermal structures of subduction zones and the deep seismicity, while the mechanism relates the thermal structure and the deep seismicity is still unsure (Helffrich, Brodholt, 1991; Furukawa, 1994; Kirby, et al, 1996). From 1980s, geoscientists have constituted a series of numerical simulations on the stress states of subduction slabs. Based on the kinetic computation of Sung and Burns (1976a, b), Goto, et al (1983, 1987… 相似文献
30.