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581.
Purnima Srivastava 《Arabian Journal of Geosciences》2012,5(6):1411-1422
Fossils of the Vindhyan Supergroup exhibit extensive diversity and variable biologic affinities represented by: bacteria, cyanobacteria, algae, fungi, acritarchs, metaphytes and metazoans (including members of the Ediacaran Fauna) and ranging from less than a micron to almost a metre in size. Besides identified fossils, a number of bizarre morphologies (due to deviation of morphology from conventional structures), present in various stratigraphic horizons, have been observed. It is very difficult to identify and decide their biologic affinities. In thin sections of Lower Vindhyan cherts, microfossils resembling lichen-like or fungal forms in which a sac encompassing a coiled filament may possibly indicate a symbiotic relationship, a Volvox colony-like structure and a vase-shaped body without an opening are unique. Among the carbonaceous fossils, very unusual and interesting fossil is a transparent disc comprising numerous appendages of an unidentified mesoscopic insect-like organism. Megascopic branching and associated Grypania-like structure is another form preserved as impression on micritic limestone. Petrographic thin sections of chert belonging to the Sirbu Shale Formation, exhibit presence of microscopic bizarre forms. The assemblage includes acritarchs and acanthomorphs of variable morphology and a dividing cell-like structure interpreted to be of rhodophycean affinity or a cleaving embryo of an animal affinity. Other peculiar morphologies among the carbonaceous fossils are: branched filaments that have attached sporangia-like vesicles, Chuaria-like body comprising cluster of very small-sized spheroids resemble scale-like structure, a chrysophycean alga or a multicellular tissue of a metaphyte. Another carbonaceous fossil represents a possible metazoan exhibiting an elongate body and a mid-gut-like structure or a Vaucheriacean alga. Although the biologic affinities of these bizarre forms can be a matter of debate, their biogenic nature is almost undoubted. The presence of such forms in the Vindhyans indicates advancement in morphology and a gradual evolution of life during the Palaeoproterozoic–Neoproterozoic period. In addition, presence of Ediacaran fossils in Bhander Group and large-sized acritarchs especially Trachyhystrichosphaera sp. in petrographic thin section of chert from the Sirbu Shale Formation, Bhander Group, Upper Vindhyans, suggests Ediacaran age as an upper age limit of the Vindhyan Supergroup. 相似文献
582.
Kamlesh Verma Sanjeeb Bhattacharya A. M. Asim Ansari Prakash K. Srivastava Amit Dharwadkar 《Journal of the Geological Society of India》2014,83(5):532-534
Eleven glacial sediment samples collected from different elevation of Jutulsessen Nunatak, Gjelsvikfjella of East Antarctica were studied for the clay mineralogical analysis using X-ray diffraction technique. The result shows prominent peak at 10, and 3.34 Å suggesting the presence of biotite possibly derived from the catchment where biotite rich granite gneisses are exposed. The detailed investigation on the shape of biotite peak of certain samples shows the signs of alteration of biotite in to a mixed layer containing tri-octahedral smectite (low charge vermiculite). The presence of mixed layer along with the biotite is found to be associated with the samples of lower geomorphic level. The progressive alteration of clay sized biotite to form a mixed layer in the lower horizons of Jutulsessen Nunatak is probably due to the periodic accumulation of melt-water during the austral summer. 相似文献
583.
R. Sarvanan S. K. Srivastava T. S. Sunil Kumar S. Niranjan Kumar R. Mohanty P. V. Ramesh Babu 《Journal of the Geological Society of India》2014,83(2):142-146
Zoned Apatite crystals with intrinsic radioactivity are widespread in the S-type basement granite around Govardhanagiri-Chinnakolumulapalli-L.Banda areas of Kurnool District, A.P. The granite is overlain by Gulcheru quartzite and in turn by Vempalle dolostone of Papaghni Group belonging to the Cuddapah Supergroup. The area (4 km x 6 km) is characterized by conjugate fracture system comprising ENE-WSW and WNW-ESE of varying extents, of which, ENE-WSW is sympathetic to the major deep seated Gani Kalva fault. The apatite crystals are frequently zoned and vary in size from few microns to 1000 microns, occur mostly as veins or associated with pulverized matrix of granite cataclasite. Veins (upto 2 cm. thick) generally follow the major fracture-trend (ENE-WSW) in the area. The apatites are also found intimately associated with fluorite, tourmaline and sulphides, which suggest their derivation from pneumatolytic fluids. The intrinsic accessory uranium as scarce grains of uraninite and other labile phases of granite were remobilized consequent upon the deformation and locked up as ferroan-oxy/hydroxyl inclusions in slowly growing apatite crystals under very low temperature conditions. 相似文献
584.
J. Srivastava R. Naraian S. J. S. Kalra H. Chandra 《International Journal of Environmental Science and Technology》2014,11(6):1787-1800
Irrational and rapid global human societal development has culminated to a condition of environmental deterioration. Accidental leakage and deliberate use of organic and inorganic chemicals have contaminated the environment up to the level of ecosystem. Advancements have been made in the field of research on bioremediation of the hazardous contaminants especially in last three decades. Microbial bioremediation has been the most understood biotechnological process of environmental restoration. Bacteria and fungi because of their inherent ability to adapt and grow in extreme environments have been employed for either removal or degradation of the chemical contaminants. Researchers all over the world are getting breakthroughs in finding new bacterial strains having plasmid linked degradation/reduction ability. Molecular biology and genetic engineering helped in crafting the microbes for the desired results on environment. Despite having favorable conditions, microbial remediation largely depends on environmental factors and on the basic biological characters of microbes, especially bacteria being Gram-positive or Gram-negative. Metagenomic studies revealed the importance of microbial ecology as microbes work well in community, i.e., consortia. This review along with several other studies suggests the need of precision during microbial community identification, substrate specificity and the designing of microbes. 相似文献
585.
Manika Gupta Prashant K. Srivastava Tanvir Islam Asnor Muizan Bin Ishak 《Environmental Earth Sciences》2014,71(10):4421-4431
The Tropical Rainfall Measuring Mission (TRMM) is a joint space mission between NASA and the Japan Aerospace Exploration Agency (JAXA) designed to monitor and study tropical rainfall. In this study, the daily rainfall from TRMM has been utilized to simulate the soil moisture content up to 30 cm vertical soil profile of at an interval depth of 15 cm by using the HYDRUS 1D numerical model for the three plots. The simulated soil moisture content using ground-based rainfall and TRMM-derived rainfall measurements indicate an agreeable goodness of fit between the both. The Nash–Sutcliffe efficiency using ground-based and TRMM-derived rainfall was found in the range of 0.90–0.68 and 0.70–0.40, respectively. The input data sensitivity analysis of precipitation combined with different irrigation treatment indicates a high dependency of soil moisture content with rainfall input. The overall analysis reveals that TRMM rainfall is promising for soil moisture prediction in absence of ground-based measurements of soil moisture. 相似文献
586.
MCT Zone of Alakhnanda valley is a major ductile shear zone in Garhwal Himalaya, which is characterised by different types
of mylonite rocks. On the basis of grain size and the percentage of matrix in the rock, zones comprising protomylonite, augen
mylonite, mylonite and ultramylonite have been identified. The study of microstructures, grain size and crystallographic preferred
orientation of quartz c-axis fabric reveals that the rocks of the MCT zone were deformed by a combination of intracrystalline creep (power law creep)
and grain boundary migration (sliding super plasticity). 相似文献
587.
One dimensional numerical model has been developed to predict the production of space charge and variations in other electrical
parameters within the low level stratiform type of cloud having very weak vertical motion. Non-linear coupled differential
equations which govern ion concentrations, charged and neutral droplet concentrations and electric field were used. Symmetry
has been observed in all the electrical parameters within the cloud. The magnitude of average positive ion concentrations
was observed to be high as compared to the negative ion concentrations, which is due to low scavenging rate of positive ions
than the negative ions, highly attributed to their mobilities. The rate of scavenging of ions affects the concentration of
charged droplets, which eventually influence the electric field and thus the space charge density within the cloud. Maximum
electric field (E
max) was observed at middle of the cloud whereas minimum was observed at both the edges of the cloud. Minimum electric field
(E
min) was found to be equal and constant (∼27 Vm−1) for any drop concentration. Net positive and negative space charges were observed at the top and bottom of the cloud, respectively.
The simulated results show some discrepancies to the natural condition, which are due to simulations made under some basic
assumptions and limitations and that will be incorporated in the future studies for natural cloud condition. 相似文献
588.
In this study, an attempt has been made to estimate land surface temperatures (LST) and spectral emissivities over a hard
rock terrain using multi-sensor satellite data. The study area, of about 6000 km2, is a part of Singhbhum-Orissa craton situated in the eastern part of India. TIR data from ASTER, MODIS and Landsat ETM+
have been used in the present study. Telatemp Model AG-42D Portable Infrared Thermometer was used for ground measurements
to validate the results derived from satellite (MODIS/ASTER) data. LSTs derived using Landsat ETM+ data of two different dates
have been compared with the satellite data (ASTER and MODIS) of those two dates. Various techniques, viz., temperature and
emissivity separation (TES) algorithm, gray body adjustment approach in TES algorithm, Split-Window algorithms and Single
Channel algorithm along with NDVI based emissivity approach have been used. LSTs derived from bands 31 and 32 of MODIS data
using Split-Window algorithms with higher viewing angle (50°) (LST1 and LST2) are found to have closer agreement with ground
temperature measurements (ground LST) over waterbody, Dalma forest and Simlipal forest, than that derived from ASTER data
(TES with AST 13). However, over agriculture land, there is some uncertainty and difference between the measured and the estimated
LSTs for both validation dates for all the derived LSTs. LST obtained using Single Channel algorithm with NDVI based emissivity
method in channel 13 of ASTER data has yielded closer agreement with ground measurements recorded over vegetation and mixed
lands of low spectral contrast. LST results obtained with TIR band 6 of Landsat ETM+ using Single Channel algorithm show close
agreement over Dalma forest, Simlipal forest and waterbody with LSTs obtained using MODIS and ASTER data for a different date.
Comparison of LSTs shows good agreement with ground measurements in thermally homogeneous area. However, results in agriculture
area with less homogeneity show difference of LST up to 2°C. The results of the present study indicate that continuous monitoring
of LST and emissivity can be undertaken with the aid of multi-sensor satellite data over a thermally homogeneous region. 相似文献