全文获取类型
收费全文 | 32082篇 |
免费 | 425篇 |
国内免费 | 372篇 |
专业分类
测绘学 | 1221篇 |
大气科学 | 2437篇 |
地球物理 | 6214篇 |
地质学 | 11302篇 |
海洋学 | 2484篇 |
天文学 | 7640篇 |
综合类 | 143篇 |
自然地理 | 1438篇 |
出版年
2021年 | 279篇 |
2020年 | 276篇 |
2019年 | 324篇 |
2018年 | 816篇 |
2017年 | 778篇 |
2016年 | 1019篇 |
2015年 | 590篇 |
2014年 | 957篇 |
2013年 | 1688篇 |
2012年 | 1037篇 |
2011年 | 1278篇 |
2010年 | 1075篇 |
2009年 | 1387篇 |
2008年 | 1204篇 |
2007年 | 1160篇 |
2006年 | 1178篇 |
2005年 | 978篇 |
2004年 | 869篇 |
2003年 | 867篇 |
2002年 | 856篇 |
2001年 | 772篇 |
2000年 | 744篇 |
1999年 | 673篇 |
1998年 | 621篇 |
1997年 | 631篇 |
1996年 | 569篇 |
1995年 | 536篇 |
1994年 | 506篇 |
1993年 | 430篇 |
1992年 | 384篇 |
1991年 | 412篇 |
1990年 | 412篇 |
1989年 | 389篇 |
1988年 | 360篇 |
1987年 | 433篇 |
1986年 | 362篇 |
1985年 | 446篇 |
1984年 | 479篇 |
1983年 | 464篇 |
1982年 | 446篇 |
1981年 | 359篇 |
1980年 | 364篇 |
1979年 | 312篇 |
1978年 | 306篇 |
1977年 | 295篇 |
1976年 | 259篇 |
1975年 | 254篇 |
1974年 | 283篇 |
1973年 | 308篇 |
1972年 | 195篇 |
排序方式: 共有10000条查询结果,搜索用时 14 毫秒
991.
Abstract— Martian meteorites (MMs) have been launched from an estimated 5–9 sites on Mars within the last 20 Myr. Some 80–89% of these launch sites sampled igneous rock formations from only the last 29% of Martian time. We hypothesize that this imbalance arises not merely from poor statistics, but because the launch processes are dominated by two main phenomena: first, much of the older Martian surface is inefficient in launching rocks during impacts, and second, the volumetrically enormous reservoir of original cumulate crust enhances launch probability for 4.5 Gyr old rocks. There are four lines of evidence for the first point, not all of equal strength. First, impact theory implies that MM launch is favored by surface exposures of near‐surface coherent rock (≤102 m deep), whereas Noachian surfaces generally should have ≥102 m of loose or weakly cemented regolith with high ice content, reducing efficiency of rock launch. Second, similarly, both Mars Exploration Rovers found sedimentary strata, 1–2 orders of magnitude weaker than Martian igneous rocks, favoring low launch efficiency among some fluvial‐derived Hesperian and Noachian rocks. Even if launched, such rocks may be unrecognized as meteorites on Earth. Third, statistics of MM formation age versus cosmic‐ray exposure (CRE) age weakly suggest that older surfaces may need larger, deeper craters to launch rocks. Fourth, in direct confirmation, one of us (N. G. B.) has found that older surfaces need larger craters to produce secondary impact crater fields (cf. Barlow and Block 2004). In a survey of 200 craters, the smallest Noachian, Hesperian, and Amazonian craters with prominent fields of secondaries have diameters of ?45 km, ?19 km, and ?10 km, respectively. Because 40% of Mars is Noachian, and 74% is either Noachian or Hesperian, the subsurface geologic characteristics of the older areas probably affect statistics of recognized MMs and production rates of secondary crater populations, and the MM and secondary crater statistics may give us clues to those properties. 相似文献
992.
M. J. Lehner C. Alcock T. Axelrod F. Bianco Y.‐I. Byun W.‐P. Chen K. H. Cook R. Dave I. de Pater J. Giammarco S.‐K. King T. Lee J. Lissauer S. L. Marshall S. Mondal T. Nihei J. Rice M. Schwamb A. Wang S.‐Y. Wang C.‐Y. Wen Z.‐W. Zhang 《Astronomische Nachrichten》2006,327(8):814-817
The Taiwanese‐American Occultation Survey (TAOS) seeks to determine the number and size spectrum for small (∼3 km) bodies in the Kuiper Belt. This will be accomplished by searching for the brief occultations of bright stars (R ∼ 14) by these objects. We have designed and built a special purpose photometric monitoring system for this purpose. TAOS comprises four 50 cm telescopes, each equipped with a 2048 × 2048 pixel CCD camera, in a compact array located in the central highlands of Taiwan. TAOS will monitor up to 2 000 stars at 5 Hz. The system went into scientific operation in the autumn of 2005. (© 2006 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim) 相似文献
993.
Solar Physics - We study a quiet-Sun blowout jet which was observed on 2014 May 16 by the instruments on board the Solar Dynamics Observatory (SDO). We find the twin CME as jet-like and bubble-like... 相似文献
994.
Jos C. Aponte Hannah K. Woodward Neyda M. Abreu Jamie E. Elsila Jason P. Dworkin 《Meteoritics & planetary science》2019,54(2):415-430
The water‐soluble organic compounds in carbonaceous chondrite meteorites constitute a record of the synthetic reactions occurring at the birth of the solar system and those taking place during parent body alteration and may have been important for the later origins and development of life on Earth. In this present work, we have developed a novel methodology for the simultaneous analysis of the molecular distribution, compound‐specific δ13C, and enantiomeric compositions of aliphatic monocarboxylic acids (MCA) extracted from the hot‐water extracts of 16 carbonaceous chondrites from CM, CR, CO, CV, and CK groups. We observed high concentrations of meteoritic MCAs, with total carbon weight percentages which in some cases approached those of carbonates and insoluble organic matter. Moreover, we found that the concentration of MCAs in CR chondrites is higher than in the other meteorite groups, with acetic acid exhibiting the highest concentration in all samples. The abundance of MCAs decreased with increasing molecular weight and with increasing aqueous and/or thermal alteration experienced by the meteorite sample. The δ13C isotopic values of MCAs ranged from ?52 to +27‰, and aside from an inverse relationship between δ13C value and carbon straight‐chain length for C3–C6 MCAs in Murchison, the 13C‐isotopic values did not correlate with the number of carbon atoms per molecule. We also observed racemic compositions of 2‐methylbutanoic acid in CM and CR chondrites. We used this novel analytical protocol and collective data to shed new light on the prebiotic origins of chondritic MCAs. 相似文献
995.
R. L. C. Starling M. J. Page G. Branduardi-Raymont A. A. Breeveld R. Soria K. Wu 《Monthly notices of the Royal Astronomical Society》2005,356(2):727-733
We present an XMM–Newton observation of the Seyfert–LINER (low-ionization nuclear emission-line region) galaxy NGC 7213. The RGS soft X-ray spectrum is well fitted with a power law plus soft X-ray collisionally ionized thermal plasma ( kT = 0.18+0.03 −0.01 keV) . We confirm the presence of Fe i , Fe xxv and Fe xxvi Kα emission in the EPIC spectrum and set tighter constraints on their equivalent widths of 82+10 −13 , 24+9 −11 and 24+10 −13 eV, respectively. We compare the observed properties together with the inferred mass accretion rate of NGC 7213 with those of other Seyfert and LINER galaxies. We find that NGC 7213 has intermediate X-ray spectral properties lying between those of the weak active galactic nucleus found in the LINER M81 and higher-luminosity Seyfert galaxies. There appears to be a continuous sequence of X-ray properties from the Galactic Centre through LINER galaxies to Seyferts, probably determined by the amount of material available for accretion in the central regions. 相似文献
996.
K. Iwasawa D. B. Sanders A. S. Evans N. Trentham G. Miniutti H. W. W. Spoon 《Monthly notices of the Royal Astronomical Society》2005,357(2):565-571
Prominent Fe Kα line emission is detected in the XMM–Newton spectrum of the ultraluminous infrared galaxy Arp 220. The centroid of the line is found at an energy of 6.7 keV and the equivalent width of the line is EW ∼ 1.9 keV (at 3.5σ significance). A few other spectral features are found at various degrees of significance in the lower energy range on a hard 2.5–10 keV continuum (Γ∼ 1) . The large EW of the Fe K line poses a problem with interpreting the hard X-ray emission as integrated X-ray binary emission. A thermal emission spectrum with a temperature of kT ∼ 7 keV modified by absorption of N H ≃ 3 × 1022 cm−2 , can describe the 2.5–10 keV continuum shape and the Fe K emission. A hot bubble that is shocked internally in a starburst region would have a similar temperature and gives a good explanation for the observed X-ray properties with a high star formation rate. An ensemble of radio supernovae in a dense environment, as suggested from VLBI imaging, could be another possibility, if such powerful supernovae are produced continuously at a high rate. However, the apparent lack of emission from X-ray binaries is incompatible with the high supernova rate (∼2 SNe yr−1 ) required by both interpretations. Highly photoionized, low-density gas illuminated by a hidden Compton-thick active galactic nucleus is a possible alternative for the hard X-ray emission, which can be tested by examining whether radiative recombination continua from highly ionized Ca and Fe are present in better quality data from a forthcoming observation. 相似文献
997.
Contribution to diffuse gamma-rays in the Galactic Centre region from unresolved millisecond pulsars
W. Wang Z. J. Jiang K. S. Cheng 《Monthly notices of the Royal Astronomical Society》2005,358(1):263-269
Diffuse gamma-rays in the Galactic Centre region have been studied. We propose that there exists a population of millisecond pulsars in the Galactic Centre, which emit GeV gamma-rays through synchrotron-curvature radiation as predicted by outer gap models. These GeV gamma-rays from unresolved millisecond pulsars probably contribute to the diffuse gamma-ray spectrum detected by EGRET which displays a break at a few GeV. We have used a Monte Carlo method to obtain simulated samples of millisecond pulsars in the Galactic Centre region covered by EGRET (∼ 15) according to the different period and magnetic field distributions from observed millisecond pulsars in the Galactic field and globular clusters, and superposed their synchrotron-curvature spectra to derive the total GeV flux. Our simulated results suggest that there probably exist about 6000 unresolved millisecond pulsars in the region of angular resolution of EGRET, the emissions of which could contribute significantly to the observed diffuse gamma-rays in the Galactic Centre. 相似文献
998.
999.
1000.
Jörg M. Colberg Ravi K. Sheth Antonaldo Diaferio Liang Gao Naoki Yoshida 《Monthly notices of the Royal Astronomical Society》2005,360(1):216-226
We study the formation and evolution of voids in the dark matter distribution using various simulations of the popular Λ cold dark matter cosmogony. We identify voids by requiring them to be regions of space with a mean overdensity of −0.8 or less – roughly the equivalent of using a spherical overdensity group finder for haloes. Each of the simulations contains thousands of voids. The distribution of void sizes in the different simulations shows good agreement when differences in particle and grid resolution are accounted for. Voids very clearly correspond to minima in the smoothed initial density field. Apart from a very weak dependence on the mass resolution, the rescaled mass profiles of voids in the different simulations agree remarkably well. We find a universal void mass profile of the form ρ(< r )/ρ( r eff ) ∝ exp[( r / r eff )α ] , where r eff is the effective radius of a void and α∼ 2 . The mass function of haloes in voids is steeper than that of haloes that populate denser regions. In addition, the abundances of void haloes seem to evolve somewhat more strongly between redshifts ∼1 and 0 than the global abundances of haloes. 相似文献