全文获取类型
收费全文 | 1361篇 |
免费 | 69篇 |
国内免费 | 327篇 |
专业分类
测绘学 | 74篇 |
大气科学 | 172篇 |
地球物理 | 613篇 |
地质学 | 505篇 |
海洋学 | 159篇 |
天文学 | 68篇 |
综合类 | 69篇 |
自然地理 | 97篇 |
出版年
2023年 | 15篇 |
2022年 | 13篇 |
2021年 | 25篇 |
2020年 | 8篇 |
2019年 | 12篇 |
2018年 | 16篇 |
2017年 | 6篇 |
2016年 | 18篇 |
2015年 | 13篇 |
2014年 | 28篇 |
2013年 | 25篇 |
2012年 | 64篇 |
2011年 | 107篇 |
2010年 | 28篇 |
2009年 | 28篇 |
2008年 | 69篇 |
2007年 | 65篇 |
2006年 | 72篇 |
2005年 | 81篇 |
2004年 | 64篇 |
2003年 | 54篇 |
2002年 | 58篇 |
2001年 | 44篇 |
2000年 | 73篇 |
1999年 | 36篇 |
1998年 | 32篇 |
1997年 | 41篇 |
1996年 | 40篇 |
1995年 | 54篇 |
1994年 | 40篇 |
1993年 | 55篇 |
1992年 | 64篇 |
1991年 | 74篇 |
1990年 | 53篇 |
1989年 | 44篇 |
1988年 | 31篇 |
1987年 | 36篇 |
1986年 | 23篇 |
1985年 | 23篇 |
1984年 | 19篇 |
1983年 | 18篇 |
1982年 | 14篇 |
1981年 | 8篇 |
1980年 | 16篇 |
1979年 | 4篇 |
1978年 | 4篇 |
1977年 | 3篇 |
1975年 | 3篇 |
1974年 | 4篇 |
1935年 | 5篇 |
排序方式: 共有1757条查询结果,搜索用时 15 毫秒
41.
42.
The uppermost part of the Upper Bathonian Sponge Limestone member, Patcham Formation, of the Jhura Dome of Kachchh Mainland is a thickening-and shallowing-upward succession topped by medium-to thick-bedded hummocky cross-stratified grainstones deposited by storm waves. Occasionally, thin, commonly lenticular, intraclastic-bioclastic silty marl intercalations between the grainstones are highly bioturbated, in contrast to the grainstones, in which, for the most part, trace fossils occur scattered. Large exposures of bedding planes of the grainstones allow the detailed investigation of ichnological features, whereas the high density of traces in the soft marls precludes the identification of any ichnotaxa. Eighteen ichnotaxa have been recorded including Ophiomorpha, Thalassinoides, Taenidium, Gyrophyllites, Chondrites, Dactyloidites, Teichichnus, Bolonia, and Ancorichnus. Except for Ophiomorpha nodosa and Thalassinoides, which generally indicate moderate to high energy conditions and are the dwelling burrows of suspension-feeding to omnivorous crustaceans, the ichnotaxa represent a deposit-feeding behaviour of their producers and thus are characteristic of low-energy environments. The trace fossils form three ichnoassemblages characterized by(1) Ophiomorpha nodosa and Thalassinoides suevicus,(2)?Thalassinoides isp. A, Taenidium, and Bolonia lata,and(3) Ancorichnus. The dominance of traces of deposit-feeders in rocks indicative of high-energy events is counterintuitive and points to their non-contemporaneity. The sediments were deposited during brief highenergy events, whereas the trace fossils were produced when, after waning of storms low-energy conditions prevailed. This time-averaging is particularly pronounced in trace fossils that extend vertically downwards and may reach strata deposited under distinctly different conditions. Thus, environmental interpretations based on trace fossils should refer to colonisation surfaces rather than to the sediment surrounding the trace fossils. In the latter case, interpretations may be erroneous, especially when erosion subsequently destroyed sedimentary evidence of their original environment. 相似文献
43.
Bassam A. ABUAMARAH Mokhles K. AZER Paul D. ASIMOW Habes GHREFAT Heba S. MUBARAK 《《地质学报》英文版》2021,95(2):459-480
The Abu Dabbab albite granite(ADAG), in the central Eastern Desert of Egypt, hosts the most significant rare metal ore deposit in the northern part of the Neoproterozoic Arabian-Nubian Shield. Here, we report detailed field,petrographic, mineralogical and geochemical investigation of the ADAG, an isolated stock-like granitic body with sharp intrusive contacts against metamorphic country rocks, probably emplaced at about 600 Ma. The fine-grained porphyritic upper unit is a preserved remnant of the shallowly-emplaced apex of the magma chamber, whereas the medium-grained lower unit crystallized at deeper levels under subvolcanic conditions. The peraluminous leucocratic ADAG shares common geochemical characteristics with post-collisional intraplate A-type magmas. In addition to the conspicuous enrichment in Na2 O, the ADAG is remarkable for its anomalous concentrations of Ta, Nb, Li, Hf, Ga, Sn, Zn and heavy rare-earth elements. Nb-Ta minerals in the ADAG are mixed with Fe-Mn oxides, forming black patches that increase in abundance toward of the base of the intrusion. Columbite-tantalite, cassiterite and wolframite are the most important ore minerals.Pronounced negative Eu anomalies(Eu/Eu* = 0.10–0.24) reflect extreme magmatic fractionation and perhaps the effects of late fluid-rock interaction. The ADAG was most likely generated by partial melting of the juvenile middle crust of the ANS as the geotherm was elevated by erosional uplift following lithospheric delamination and it was emplaced at the intersection of lineations of structural weakness. Although formation of the ADAG and its primary enrichment in rare metals are essentially due to magmatic processes, late-stage metasomatism caused limited redistribution of rare metals. Fluid-driven subsolidus modification was limited to the apex of the magma chamber and drove development of greisen, amazonite, and quartz veins along fracture systems. 相似文献
44.
Osama M. KASSEM Yousef A. ALAMRI Faisal K. ZAIDI Abdel Aziz M. AL BASSAM Mansour H. AL-HASHIM 《《地质学报》英文版》2021,95(3):750-760
The vorticity analysis technique was applied to measure the different lithological units,such as schist,metagranite and metavolcano-sedimentary rocks,which are present in the Halaban region.This work aims to interpret the relationship between the different lithologies and the tectonic setting,in order to elucidate the nature of kinematic analysis in the Halaban region.The kinematic analyses were applied to feldspar porphyroclasts,quartz and hornblende for twentysix samples.The kinematic vorticity number (W_m) for deformed rocks in the study area ranged from~0.6 to 0.9.The direction of the long axes for finite strain data (X axes) revealed a WNW trend with shallow dipping.The direction of the short axes for finite strain data (Z axes) were represented by vertical with associated horizontal foliation.The results of the kinematic vorticity and strain analyses are characterized by simple shear with different degrees of deformation in the Halaban region.Furthermore,our finite strain data shows no significant volume change during deformation.The subhorizontal foliation was synchronized with thrusting and deformation.Furthermore,throughout the overlying nappes,the same attitudes of tectonic contacts are observable,the nappes in the orogens being formed from simple shear deformation. 相似文献
45.
Ruth GEEN Marianne PIETSCHNIG Shubhi AGRAWAL Dipanjan DEY F.Hugo LAMBERT Geoffrey K.VALLIS 《大气科学进展》2023,(11):2029-2052
The East Asian Summer Monsoon(EASM) provides the majority of annual rainfall to countries in East Asia.Although state-of-the-art models broadly project increased EASM rainfall, the spread of projections is large and simulations of present-day rainfall show significant climatological biases. Systematic evapotranspiration biases occur locally over East Asia, and globally over land, in simulations both with and without a coupled ocean. This study explores the relationship between evapotranspiration... 相似文献
46.
50.
自1978年3月,在Fresmout谷(F谷)一口井中连续记录到水位资料.其靠近Garlock断裂带(G带)上的数条断层显示出有左旋位移和倾滑位移.水位差表明有断层从观测井和灌溉井间通过.4年间,记录到6次急剧的水位变化(脉冲),这些发生在2—4天以上的水位变化,幅度为15—30厘米,似断层蠕动的结果.在观测井南300米处的G带上可能有两种蠕动:(1)阶梯状的倾滑位移;(2)左旋位移.利用指数函数、反正切函数和斜余弦函数变化的位错模型分析了水位变化、压力分布和断层位移.结果表明,该断层上的单个蠕动事件的位移量在1厘米以内.1978—1982年期间,累计蠕变值为20-50毫米,这取决于使用模型的特殊性. 相似文献