全文获取类型
收费全文 | 79篇 |
免费 | 45篇 |
国内免费 | 33篇 |
专业分类
测绘学 | 9篇 |
大气科学 | 19篇 |
地球物理 | 69篇 |
地质学 | 26篇 |
海洋学 | 17篇 |
天文学 | 16篇 |
自然地理 | 1篇 |
出版年
2024年 | 3篇 |
2022年 | 1篇 |
2021年 | 1篇 |
2020年 | 3篇 |
2019年 | 4篇 |
2018年 | 1篇 |
2017年 | 2篇 |
2016年 | 2篇 |
2015年 | 1篇 |
2014年 | 4篇 |
2013年 | 8篇 |
2012年 | 7篇 |
2011年 | 6篇 |
2010年 | 9篇 |
2009年 | 8篇 |
2008年 | 6篇 |
2007年 | 7篇 |
2006年 | 7篇 |
2005年 | 3篇 |
2004年 | 3篇 |
2003年 | 1篇 |
2002年 | 9篇 |
2001年 | 6篇 |
2000年 | 4篇 |
1999年 | 5篇 |
1998年 | 3篇 |
1997年 | 4篇 |
1996年 | 2篇 |
1989年 | 2篇 |
1985年 | 4篇 |
1982年 | 2篇 |
1974年 | 4篇 |
1973年 | 2篇 |
1968年 | 1篇 |
1965年 | 2篇 |
1964年 | 2篇 |
1963年 | 1篇 |
1962年 | 1篇 |
1961年 | 2篇 |
1958年 | 1篇 |
1957年 | 1篇 |
1943年 | 4篇 |
1942年 | 2篇 |
1940年 | 1篇 |
1938年 | 1篇 |
1937年 | 4篇 |
排序方式: 共有157条查询结果,搜索用时 31 毫秒
71.
Selected Phase Relationships in the System Al-Mn-Fe-Si-O-H: A Model for Garnet Equilibria 总被引:1,自引:0,他引:1
The bulk compositions 3FeOx.Al2O3.3SiO2 $ excess H2O and 3MnO.Al2O3.3SiO2$ excess H2O were investigated employing conventional hydrothermaltechniques. Almandine and spessartine were synthesized and stabilityrelationships determined in terms of temperature, fluid pressure,and oxygen fugacity. Synthetic almandine has unit cell edge, a0 = 11.528 0.001 index of refraction, ND = 1.829 0.003. No systematic variationsof these values with respect to temperature, fluid pressure,and oxygen fugacity were observed. Spessartine, synthesizedat high temperatures, has average values of a0 = 11.614 0.001 and ND = 1.799 0.003. However, below about 600 C a0 graduallyincreases to 11.635 0.001 and ND decreases to 1.772 0.003with decreasing temperature, irrespective of fluid pressureand oxygen fugacity. These changes appear to reflect the productionof hydrospessartine below about 600 C. The stability of almandine strongly depends on the oxygen fugacity.It is stable up to the vicinity of oxygen fugacities definedby the fayalitemagnetite$quartz buffer; the low fo2,range has not been determined, but lies at oxygen fugacitiesless than those defined by the ironquartzfayalite buffer.The stability field of almandine$fluid is bounded by the followingPfluid-T values. At low oxidation states, the low temperature hydrous assemblageof equivalent composition consists of quartz$iron chlorite ($magnetite)$fluidand the high temperature equivalent assemblage consists of fayalite$ironcordierite$hercynite88$fluid. Where fO2 approximates or is inexcess of that defined by the fayalitemagnetite$quartzbuffer the low temperature hydrous assemblages consist of quartz$ironchlorite$magnetite$fluid, iron chlorite$pyrophyllite$magnetite$fluid,magnetite$mullite$pyrophyllite$fluid, and hematite$mullite$pyrophyllite$fluid;the anhydrous equivalent assemblages consist of quartz$hercynite88,$magnetite88$fluid, quartz$mullite$magnetite$fluid, and quartz$mullite$hematite$fluid,both in order of increasing oxygen fugacity. The stability of spessartine, in contrast to that of almandine,is essentially independent of oxygen fugacity at least up tothat defined by the magnetite-hematite buffer. Spessartine isstable up to the highest temperature, 930 C, employed in thisinvestigation at Pfluid = 500 bars. However, it decomposes toa hydrous assemblage consisting of quartz$manganese chlorite$fluidat the following Pfluid-T values: 414 5 C and 3000 bars;405 5C and 2000 bars; 386 10 C and 1000 bars; 3645C and 500 bars. Garnets are rare constituents of igneous rocks; those whichdo occur are predominantly spessartine-rich, and are virtuallyconfined to felsic magmas. Garnets are absent from mafic igneousrocks because the thermal stability ranges of iron-rich membersare below the solidus. The near absence of almandine in contactmetamorphosed pelitic rocks may reflect a relatively high oxidationstate in the aureoles rather than inappropriate P-T conditions.It is argued that the compositions of pyralspite garnets inpelitic schists are subject to various physical and chemicalfactors, including fO2. With appropriate provisions, the Mn/Feratios of garnet coexisting with chlorite and quartz might beused as a temperature indicator. The rarity of spessartine in igneous and metamorphic rocks apparentlystems from the departure of rock bulk composition from Mn-richvalues rather than from the absence of appropriate physicalconditions. 相似文献
72.
73.
HSU Weibiao 《《地质学报》英文版》2004,78(5)
Coupled with a petrographical study, I carried out an ion probe study of rare earth element microdistributions in mineral phases of silicate inclusions from the Colomera ⅡE iron meteorite. Most mineral grains have homogeneous REEs, but show considerable inter-grain variations by a factor of 2 to 100. The whole rock REE abundances for Colomera, estimated by combining REE data with modal abundances, are relatively LREE-enriched with REEs of -10'CI, which suggest that Colomera silicates were highly differentiated and might represent a low degree partial melt (-10%) of a chondritic source. REE geochemistry of Colomera silicate inclusions points to an origin that involves differentiation, dynamic mixing, remelting, reduction, recrystallization, and subsequent rapid cooling near the surface of a planetary body. 相似文献
74.
Surface deformation and gravity changes caused by dilatancy in a layered elastic-vis-coelastic half space 总被引:1,自引:0,他引:1
Surfacedeformationandgravitychangescausedbydilatancyinalayeredelastic┐vis┐coelastichalfspaceYONGWANG(王勇)HOUTSEHSU(许厚泽)Instit... 相似文献
75.
曼桂陨石是新近(2018年6月1日)陨落在云南西双版纳地区的目击球粒陨石,其中的主要矿物为橄榄石(Fa_(24.3±0.6))、斜方辉石(Fs_(20.6±0.5)Wo_(0.4±0.2))、长石(An_(11-12)Or_(2-4))、铁镍金属和陨硫铁,次要矿物为铬铁矿、白磷钙矿等.橄榄石和辉石的化学成分表明曼桂陨石属于L型普通球粒陨石.陨石中球粒很少且轮廓不清晰,基质矿物普遍经历过重结晶,重结晶矿物颗粒粒径较大,高钙辉石粒径25–30μm,长石颗粒大多超过50μm,说明该陨石属于6型岩石类型.橄榄石和辉石颗粒中发育有波状消光、嵌晶块状消光现象、平面裂隙和面状变形构造,长石熔长石化并不完全,陨石中观察到宽度不等且纵横交错的冲击熔融脉,表明曼桂普通球粒陨石受到的冲击变质作用可以达到S5级以上.通过熔融脉中的矿物组合推断出熔融脉中矿物经历的压力在15–16 GPa左右. 相似文献
76.
En-Tian LIN Chih-Tsung HSU Keh-Chia YEH 《国际泥沙研究》2006,21(4):281-293
1 INTRODUCTION The study of sediment transport in alluvial river is one of the most important fields in hydraulic engineering. Sediment transport has direct influence on the evolution of riverbeds, estuaries and coastlines, and, in turn, affects decision-making of flood control, operating rule of reservoir, design of hydraulic structure and many other aspects. Models with different orders of dimensions were presented in the literature, and most of them had common basis that they were formu… 相似文献
77.
78.
基于新型残余星间速度法(RIRM)反演了120阶GRACE Follow-On地球重力场. 第一,由于GPS定轨精度相对较低,通过将激光干涉测距仪的高精度残余星间速度(测量精度10-7 m·s-1)引入残余轨道速度差分矢量的视线分量构建了新型RIRM观测方程. 第二,基于2点、4点、6点和8点RIRM公式对比论证了最优的插值点数. 如果相关系数和采样间隔一定,随着插值点数的增加,卫星观测值的信号量被有效加强,而卫星观测值的误差量也同时增加. 因此,6点RIRM公式是提高下一代地球重力场精度的较优选择. 第三,相关系数对地球重力场精度的影响在不同频段表现为不同特性. 随着相关系数的逐渐增大,地球长波重力场精度逐渐降低,而地球中长波重力场精度逐渐升高. 第四,基于6点RIRM公式,通过30天观测数据和采样间隔5 s,分别利用星间速度和残余星间速度观测值,在120阶次处反演下一代GRACE Follow-On累计大地水准面精度为1.638×10-3 m和1.396×10-3 m. 研究结果表明:(1)残余星间速度观测量较星间速度对地球重力场反演精度更敏感;(2)GRACE Follow-On地球重力场精度较GRACE至少高10倍. 相似文献
79.
In this paper a series of numerical simulations are performed to investigate the vortex shedding mechanism for a solitary wave propagating over a submerged breakwater by use of Reynolds averaged Navier-Stokes (RANS) model combined with a k-ε model. Flows of different Reynolds numbers up to Re=1.4×105 corresponding to varying incident wave heights are considered in which the characteristic fluid velocity is represented by the maximum horizontal velocity above the submerged breakwater. For the verification of... 相似文献
80.
Based on the reforecast data(1999–2010) of three operational models [the China Meteorological Administration(CMA), the National Centers for Environmental Prediction of the U.S.(NCEP) and the European Centre for MediumRange Weather Forecasts(ECMWF)] that participated in the Subseasonal to Seasonal Prediction(S2S) project, we identified the major sources of subseasonal prediction skill for heatwaves over the Yangtze River basin(YRB). The three models show limited prediction skills in terms of the ... 相似文献