全文获取类型
收费全文 | 8123篇 |
免费 | 1975篇 |
国内免费 | 3004篇 |
专业分类
测绘学 | 1251篇 |
大气科学 | 1213篇 |
地球物理 | 1603篇 |
地质学 | 5557篇 |
海洋学 | 1405篇 |
天文学 | 159篇 |
综合类 | 777篇 |
自然地理 | 1137篇 |
出版年
2024年 | 81篇 |
2023年 | 179篇 |
2022年 | 515篇 |
2021年 | 619篇 |
2020年 | 463篇 |
2019年 | 568篇 |
2018年 | 505篇 |
2017年 | 453篇 |
2016年 | 495篇 |
2015年 | 566篇 |
2014年 | 537篇 |
2013年 | 622篇 |
2012年 | 711篇 |
2011年 | 764篇 |
2010年 | 682篇 |
2009年 | 677篇 |
2008年 | 618篇 |
2007年 | 694篇 |
2006年 | 583篇 |
2005年 | 475篇 |
2004年 | 351篇 |
2003年 | 245篇 |
2002年 | 261篇 |
2001年 | 260篇 |
2000年 | 216篇 |
1999年 | 174篇 |
1998年 | 89篇 |
1997年 | 123篇 |
1996年 | 95篇 |
1995年 | 63篇 |
1994年 | 60篇 |
1993年 | 82篇 |
1992年 | 55篇 |
1991年 | 43篇 |
1990年 | 29篇 |
1989年 | 19篇 |
1988年 | 18篇 |
1987年 | 19篇 |
1986年 | 17篇 |
1985年 | 9篇 |
1984年 | 16篇 |
1983年 | 6篇 |
1982年 | 5篇 |
1981年 | 8篇 |
1979年 | 3篇 |
1975年 | 3篇 |
1973年 | 3篇 |
1959年 | 2篇 |
1957年 | 3篇 |
1954年 | 9篇 |
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
771.
华南晚古生代礁硅岩套的组成和分类及地质涵义 总被引:4,自引:0,他引:4
礁硅岩套是一种重要的含矿岩石组合,它是由生物礁相碳酸盐岩、热水沉积岩(矿)、细碎屑岩和泥灰岩、同怪位或相邻地区地层中的火山质岩或潜火山岩,以较为固定的时空有序的状态组合而成。根据生物礁的形成环境和热水沉积作用的产出方式,礁硅岩套可分为盆地型、台地型和过渡型三类。它是在特征地质背景下,在盆地演化的一定阶段内,由盆地正常沉积作物、盆地中的生物作用、盆下源的热水沉积作用和岩石圈深部岩浆作用综合形成的产物 相似文献
772.
浙江景宁鹤溪群斜长角闪岩变质新生锆石特征、离子探针(SHRIMP)U-Pb年龄及地质意义 总被引:10,自引:0,他引:10
景宁鹤溪群斜长角闪岩变质新生锆石特征是粒度均匀(约70μm),晶体结晶和透明度极好,色调一致的淡粉红色,呈金刚光泽.未见裂隙、表面熔蚀、环带和核心构造。离子探针质谱GHRIMPⅡ)的206Pb/238U、207Pb/235U两组年龄在误差范围内基本谐和,206Pb/238U年龄的加权平均值(252±5Ma)为变质新生铁石的结晶年龄。锆石的精确定年(252±5Ma)为丽水—余姚断裂以东地区呈“天窗式”零星出露于中生代火山岩系中的鹤溪群提供了一个变质作用的确切年龄,也为印支运动在丽水—余姚断裂以东地区的存在提供了重要的年代学佐证。 相似文献
773.
774.
LIU Dequan TANG Yanling ZHOU RuhongXinjiang Bureau of Geology Mineral Exploration Development No. W. Karamay Rd. Urumqi Xinjiang 《《地质学报》英文版》1998,72(4):339-349
The great majority of the Palaeozoic orogenjc belts of Central Asia are of the intercontinental type, whose evolution always follows a five-stage model, i.e. the basal continental crust-extensional transitional crust-oceanic crust-convergent transitional crust-new continental crust model. The stage for the extensional transitional crust is a pretty long, independent and inevitable phase. The dismembering mechanism of the basal continental crust becoming an extensional continental crust is delineated by the simple shear model put forward by Wernike (1981). The continental margins on the sides of a gently dipping detachment zone and moving along it are asymmetric: one side is of the nonmagmatic type and the other of the magmatic type with a typical bimodal volcanic formation. In the latter case, however, they were often confused with island arcs. This paper discusses the five-stage process of the crustal evolution of some typical orogenic belts in Xinjiang. 相似文献
775.
XY Leo (BD+18° 2307, p = 0d .28) was observed each season from 1992 through 1995 at Yunnan Observatory with the 1 m telescope
and 37 new heliocentric times of minimum light were determined. The newly expanded database of the minimum times,including
these new epochs, definitely confirm the sine-like variation of its O–C values. Observations and analyses strongly supported
the viewpoint that the variation of the O–C values of the minimum times is mainly caused by the light- time effect. Based
on this newly expanded database, new light elements for the eclipsing system XY Leo and new light-time orbit for this complex
system have been obtained with much better accuracy than before by means of the least squares fitting to the light-time equation.
It's also noted that the additional period variation for XY Leo probably may not be ruled out besides the light-time effect.
The method of analysis and the discussion of the results are presented in this paper.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
776.
运动质点的多普勒效应使它们散射的雷达信号呈现为一种随机过程,对这随机过程的统计特性进行分析就能够推断云和降水的微物理或运动学的状况。本文由这种观点讨论了雷达气象的几种测量原理,它能够比较清楚地阐明每种方法的实质,也便于对各种方法的优缺点进行对比。文中还讨论了脉冲波列的谱分析问题,涉及了如何根据雷达测量结果去推断云和降水的微物理或运动学状况的问题。 相似文献
777.
人类活动与地理环境 总被引:5,自引:0,他引:5
潘玉君 《云南地理环境研究》1990,2(2):19-28
本文从如下几个方面论述了人类活动与(自然)地理环境之间的关系问题:1、人类活动与地理环境关系主要学说的考察;2、人类活动与地理环境相互作用的历史分析;3、地理环境对人类活动的影响;4,人类活动对地理环境的反作用;5、人类与地理环境的共生。 相似文献
778.
T. N. Krishnamurti John Molinari Hua-Lu Pan Vince Wong 《Pure and Applied Geophysics》1977,115(5-6):1357-1372
In this short paper we have identified some of the modelling groups that have the capability of simulating or carrying out short range numerical weather prediction over the monsoon belt. We have next outlined some of the important and desirable ingredients for a multilevel primitive equation model over the tropics, with most of the emphasis on the present version of Florida State University's Tropical Prediction Model. Finally, we present briefly some important results based on the present version of our prediction models that relate to the NWP efforts over the monsoon belt. Here we have identified the importance of mountains, convection, the radiative heating balance of the earth's surface, and the planetary boundary layer over the Arabian Sea. 相似文献
779.
780.
R.-X. CHEN Y.-F. ZHENG Z.-F. ZHAO J. TANG F.-Y. WU X. M. LIU 《Journal of Metamorphic Geology》2007,25(8):873-894
A combined study of zircon morphology, U–Pb ages and Hf isotopes as well as whole‐rock major and trace elements was carried out for ultrahigh‐pressure (UHP) eclogite and felsic gneiss from the main hole (MH) of the Chinese Continental Scientific Drilling (CCSD) project in the Sulu orogen. The results show contrasting Hf isotope compositions for bimodal UHP metaigneous rocks, pointing to contrasting origins for their protoliths (thus dual‐bimodal compositions). The samples of interest were from two continuous core segments from CCSD MH at depths of 734.21–737.16 m (I) and 929.67–932.86 m (II) respectively. Zircon U–Pb dating for four samples from the two core segments yields two groups of ages at 784 ± 17 and 222 ± 3 Ma, respectively, corresponding to protolith formation during supercontinental rifting and metamorphic growth during continental collision. Although the Triassic UHP metamorphism significantly reset the zircon U–Pb system of UHP rocks, the Hf isotope compositions of igneous zircon can be used to trace their protolith origin. Contrasting types of initial Hf isotope ratios are, respectively, correlated with segments I and II, regardless of their lithochemistry. The first type shows positive ?Hf(t) values of 7.8 ± 3.1 to 6.0 ± 3.0, with young Hf model age of 1.03 and 1.11 Ga. The second type exhibits negative ?Hf(t) values of ?6.9 ± 1.6 to ?9.1 ± 1.1, with old Hf model ages of 2.11 and 2.25 Ga. It appears that the UHP rocks from the two segments have protoliths of contrasting origin. Consistent results are also obtained from their trace element compositions suggesting that mid‐Neoproterozoic protoliths of bimodal UHP metaigneous rocks formed during supercontinental rifting at the northern margin of the South China Block. Thus, the first type of bimodal magmatism formed by rapid reworking of juvenile crust, whereas the second type of bimodal magmatism was principally generated by rift anatexis of Paleoproterozoic crust. Melting of orogenic lithosphere has potential to bring about bimodal magmatism with contrasting origins. Because arc–continent collision zones are the best place to accumulate both juvenile and ancient crusts, the contrasting types of bimodal magmatism are proposed to occur in an arc–continent collision orogen during the supercontinental rifting, in response to the attempted breakup of the supercontinent Rodinia at c. 780 Ma. 相似文献