全文获取类型
收费全文 | 1615篇 |
免费 | 76篇 |
国内免费 | 29篇 |
专业分类
测绘学 | 39篇 |
大气科学 | 176篇 |
地球物理 | 361篇 |
地质学 | 601篇 |
海洋学 | 131篇 |
天文学 | 251篇 |
综合类 | 4篇 |
自然地理 | 157篇 |
出版年
2023年 | 5篇 |
2022年 | 9篇 |
2021年 | 31篇 |
2020年 | 33篇 |
2019年 | 22篇 |
2018年 | 48篇 |
2017年 | 40篇 |
2016年 | 74篇 |
2015年 | 45篇 |
2014年 | 65篇 |
2013年 | 109篇 |
2012年 | 54篇 |
2011年 | 98篇 |
2010年 | 83篇 |
2009年 | 91篇 |
2008年 | 90篇 |
2007年 | 93篇 |
2006年 | 94篇 |
2005年 | 61篇 |
2004年 | 63篇 |
2003年 | 47篇 |
2002年 | 47篇 |
2001年 | 39篇 |
2000年 | 31篇 |
1999年 | 36篇 |
1998年 | 23篇 |
1997年 | 19篇 |
1996年 | 19篇 |
1995年 | 16篇 |
1994年 | 12篇 |
1993年 | 17篇 |
1992年 | 7篇 |
1991年 | 17篇 |
1990年 | 15篇 |
1989年 | 17篇 |
1987年 | 13篇 |
1986年 | 17篇 |
1985年 | 9篇 |
1984年 | 5篇 |
1983年 | 14篇 |
1982年 | 12篇 |
1981年 | 14篇 |
1980年 | 12篇 |
1979年 | 6篇 |
1978年 | 6篇 |
1977年 | 6篇 |
1976年 | 6篇 |
1975年 | 4篇 |
1974年 | 7篇 |
1973年 | 5篇 |
排序方式: 共有1720条查询结果,搜索用时 15 毫秒
441.
The insoluble organic material in the Orgueil (Cl) chondrite was analyzed by combined high vacuum pyrolysis-gas chromatography-mass spectrometry. Stepwise pyrolyses at 150, 300, 450 and 600°C of Orgueil meteorite powder which had been exhaustively extracted with solvents yielded a series of alkenes and alkanes to C8, an extensive series of alkylbenzene isomers, thiophene, alkylthiophenes, and benzothiophene, together with the nitrogen- and oxygen-containing breakdown products, acetonitrile, acrylonitrile, benzonitrile, acetone and phenol. The Orgueil polymer fragmentation products are very similar both qualitatively and quantitatively to pyrolysis products of solvent-extracted Pueblito de Allende (C3) chondrite described in the literature.Changes in the relative abundances of polymer degradation products between 150 and 600°C imply the preferential loss of aliphatic and certain heteroatomic portions of the polymer at lower temperatures to leave highly condensed aromatic and heteroaromatic portions of the polymer which begin to fragment only at 450–600°C. The Orgueil polymer-like matter thus appears to be a complex mixture of polymerized materials having different thermal stabilities. Similarities between vacuum pyrolyzates of the Orgueil polymer and terrestrial kerogen suggest the possibility that meteorite organic matter may have been subjected on the meteorite parent bodies to diagenetic processes similar to those by which terrestrial kerogen is formed. 相似文献
442.
443.
Steven R. Bohlen Arthur L. Boettcher Wayne A. Dollase Eric J. Essene 《Earth and Planetary Science Letters》1980,47(1):11-20
The effect of manganese on the stability of ferrosilite relative to fayalite + quartz has been experimentally determined to assess its importance to orthopyroxene barometry. Reaction reversals in a piston-cylinder apparatus were obtained to within 0.1-kbar intervals indicating instability of Fs95Rh5 below 10.3, 10.9, 11.4, 12.2, 12.9, 13.7 kbar and Fs90Rh10 below 9.8, 10.4, 10.9, 11.6, 12.4 and 13.2 kbar at 750, 800, 850, 900, 950 and 1000°C, respectively. Each mole % MnSiO3 extends the pyroxene stability by approximately 0.12 kbar relative to FeSiO3. Electron microprobe analyses of run products indicate a small preference of Mn for pyroxene over olivine withKDMn-Feopx-oliv = 1.2?1.5, similar to values observed for natural pairs. Mössbauer spectra are consistent with a random distribution of Mn between the M1 and M2 sites in the orthopyroxene. These experimental data allow downward revision of pressure estimates based on the orthopyroxene barometer in areas where Mn is a significant component in orthopyroxene. 相似文献
444.
Sir Eric Smith 《Marine pollution bulletin》1982,13(2):71-72
445.
Young-of-the-year alewife, American shad, blueback herring, and striped bass were analyzed for Kepone contamination. Samples were collected from the Potomac, Rappahannock, Pamunkey, Mattaponi, Chickahominy, and James rivers during the period 1977–79. Concentrations of Kepone ≥0.3 ppm occurred in all four species collected in the James River nursery zone between km 65 and 120, and in the lower Chickahominy River. Concentrations of Kepone <0.3, ppm were also present in samples from the Mattaponi and Pamunkey rivers. Four possible explanations, for the occurrence of Kepone in these samples from the upper York River system (Mattaponi and Pamunkey rivers) were, evaluated. Kepone was not detectable in samples from the Rappahannock and Potomac rivers. 相似文献
446.
447.
Philip Brown Eric J. Essene Donald R. Peacor 《Contributions to Mineralogy and Petrology》1978,67(3):227-232
Manganese-rich metamorphic rocks containing violan from St. Marcel, Piedmont, Italy formed under blueschist facies conditions,
yielding an unusual suite of minerals including omphacite-albite-quartz, braunite, microcline, hollandite, piedmontite, and
strontian calcite. Violan, a violet-colored pyroxene, is shown to be a manganoan omphacite having a primitive unit cell, and
is found in the same sample as diopside, possibly indicating a solvus relation. A manganoan phlogopite and a celadonitic muscovite
coexist in one sample with microcline. The occurrence of celadonite and phlogopite is the first from the blueschist facies
and the celadonite component in the dioctahedral mica is buffered at a maximum by coexistence with phlogopite, microcline,
and quartz. Various phase relations are used to establish the P and T of equilibration at 8±1 kbar and 300±50 °C, respectively, while the oxygen fugacity is shown to have been very high, for
these temperatures, as consistent with braunite+quartz and the presence of piedmontite.
Contribution No. 343, from the Mineralogical Laboratory, Department of Geology and Mineralogy, The University of Michigan,
Ann Arbor, MI 48109, USA 相似文献
448.
The U---Pb age on pooled data of zircnos from the postorogenic Svecokarelian Mosshaga granite is 1788 ± 11 Ma (2 σ). The corresponding Rb---Sr whole rock age is 1742 ± 34 Ma (2 σ). The Mosshaga granite intrudes a synorogenic granodiorite, which has a U---Pb zircon age of 1889 ± 10 Ma and a Rb---Sr whole rock age of 1850 ± 28 Ma. The age differences between the U---Pb zircon ages and Rb---Sr whole rock ages are concluded to be geologically significant. It is shown that the Mosshaga pluton cooled rapidly and as a consequence the Rb---Sr isotopic system closed at a time very close to the crystallization of the zircons. A commonly observed feldspar and biotite alteration in Svecokarelian granitoids indicates migration of Rb and Sr isotopes in the whole rock system which may lead to apparently younger Rb---Sr ages. 相似文献
449.
450.
Katja?Freitag Alan?P.?BoyleEmail author Eric?Nelson Murray?Hitzman James?Churchill Magda?Lopez-Pedrosa 《Mineralium Deposita》2004,39(1):103-113
The Greens Creek polymetallic massive sulphide deposit is hosted in a typical polyphase deformed lower greenschist facies orogenic setting. The structure of the host rocks is well constrained, exhibiting a series of three superimposed ductile deformations followed by two brittle episodes. The ore is found both in fold hinges where early-formed depositional features are preserved and in fold limbs where primary features are typically strongly modified or obliterated. Samples from both settings have been investigated using electron backscatter diffraction (EBSD) coupled with forescatter orientation contrast (OC) imaging in order to observe the effects of deformation and lower greenschist facies metamorphism on pyrite. Results suggest that colloform pyrite may preserve information relevant to palaeoenvironment, that apparently simple textures are generally more complex, and that pyrite can deform plastically by dislocation glide and creep processes at lower temperatures and/or strain rates than generally accepted. This analysis indicates that EBSD and OC imaging provide powerful tools for observing textural relationships in pyrite that are not shown by more traditional methods. They should become routine tools for pyrite texture analysis.Editorial handling: D. Lentz 相似文献