全文获取类型
收费全文 | 519篇 |
免费 | 10篇 |
国内免费 | 5篇 |
专业分类
测绘学 | 46篇 |
大气科学 | 20篇 |
地球物理 | 100篇 |
地质学 | 176篇 |
海洋学 | 22篇 |
天文学 | 155篇 |
自然地理 | 15篇 |
出版年
2022年 | 2篇 |
2021年 | 3篇 |
2020年 | 2篇 |
2019年 | 7篇 |
2018年 | 21篇 |
2017年 | 22篇 |
2016年 | 26篇 |
2015年 | 8篇 |
2014年 | 35篇 |
2013年 | 48篇 |
2012年 | 27篇 |
2011年 | 24篇 |
2010年 | 18篇 |
2009年 | 16篇 |
2008年 | 20篇 |
2007年 | 12篇 |
2006年 | 31篇 |
2005年 | 7篇 |
2004年 | 7篇 |
2003年 | 18篇 |
2002年 | 5篇 |
2001年 | 9篇 |
2000年 | 9篇 |
1999年 | 8篇 |
1998年 | 11篇 |
1997年 | 9篇 |
1996年 | 5篇 |
1995年 | 5篇 |
1994年 | 7篇 |
1993年 | 5篇 |
1992年 | 5篇 |
1991年 | 10篇 |
1990年 | 8篇 |
1989年 | 15篇 |
1988年 | 12篇 |
1987年 | 15篇 |
1986年 | 3篇 |
1985年 | 4篇 |
1984年 | 5篇 |
1983年 | 1篇 |
1982年 | 6篇 |
1981年 | 5篇 |
1980年 | 1篇 |
1979年 | 2篇 |
1977年 | 2篇 |
1976年 | 2篇 |
1975年 | 1篇 |
1973年 | 4篇 |
1971年 | 2篇 |
1970年 | 3篇 |
排序方式: 共有534条查询结果,搜索用时 15 毫秒
91.
92.
V. Chakravarthi B. Ramamma T. Venkat Reddy 《Journal of the Geological Society of India》2013,82(5):561-569
An automatic modeling scheme is developed in the space domain to interpret the gravity anomalies of sedimentary basins, among which the density contrast decreases exponentially with depth. Forward modeling is realized in the space domain using a combination of both analytical and numerical approaches. A collage of vertical prisms having equal widths, whose depths are to be estimated, describes the geometry of a sedimentary basin. Initial depths of a sedimentary basin are predicted using the Bouguer slab formula and subsequently updated, iteratively, based on the differences between the observed and theoretical gravity anomalies until the modeled gravity anomalies mimic the observed ones. The validity and applicability of the method is demonstrated with a synthetic and two real field gravity anomalies, one each over the Chintalpudi sub-basin in India and the other over the San Jacinto graben, California. In case of synthetic example, the assumed structure resembles a typical intracratonic rift basin formed by normal block faulting and filled with thick section of sediments. The proposed modeling technique yielded information that is consistent with the assumed parameters in the case of synthetic structure and with the available/drilling depths in case of field examples. 相似文献
93.
R. L. Naidu K. Dasu Naidu K. Shobhan Babu D. R. K. Reddy 《Astrophysics and Space Science》2013,347(1):197-201
In this paper, we have investigated a five dimensional Kaluza-Klein space-time in the frame work of Brans-Dicke (Phys. Rev. 124:925, 1961) scalar-tensor theory of gravitation when the source of energy momentum tensor is a bulk viscous fluid containing one dimensional cosmic strings. We have obtained a determinate solution of the field equations using the special law of variation for Hubble’s parameter proposed by Bermann (Nuovo Cimento B 74:182, 1983) We have also used a barotropic equation of state for the pressure and density. Some physical properties of the model are also discussed. 相似文献
94.
Groundwater targeting in a hard-rock terrain using fracture-pattern modeling, Niva River basin, Andhra Pradesh, India 总被引:1,自引:0,他引:1
In hard-rock terrain, due to the lack of primary porosity in the bedrock, joints, fault zones, and weathered zones are the
sources for groundwater occurrence and movement. To study the groundwater potential in the hard-rock terrain and drought-prone
area in the Niva River basin, southern Andhra Pradesh state, India, Landsat 5 photographic data were used to prepare an integrated
hydrogeomorphology map. Larsson's integrated deformation model was applied to identify the various fracture systems, to pinpoint
those younger tensile fracture sets that are the main groundwater reservoirs, and to understand the importance of fracture
density in groundwater prospecting. N35°–55°E fractures were identified as tensile and N35°–55°W fractures as both tensile
and shear in the study area. Apparently, these fractures are the youngest open fractures. Wherever N35°–55°E and N35°–55°W
fracture densities are high, weathered-zone thickness is greater, water-table fluctuations are small, and well yields are
high. Groundwater-potential zones were delineated and classified as very good, good to very good, moderate to good, and poor.
Electronic Publication 相似文献
95.
Non-existence of higher dimensional anisotropic cosmological model in bimetric theory of gravitation
A Five dimensional spherically symmetric space-time model in Rosen's (1973) bimetric theory of gravitation is considered.
It is shown that, in this theory, the geometry of the five dimensional space-time does not admit perfect fluid source. Hence
a vacuum model is presented and studied. It is observed that in the case of stiff fluid we again get the vacuum model.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
96.
Hydrometallurgical processing and recovery of molybdenum trioxide from spent catalyst 总被引:5,自引:0,他引:5
Kyung Ho Park B. Ramachandra Reddy D. Mohapatra Chul-Woo Nam 《International Journal of Mineral Processing》2006,80(2-4):261-265
Hydrometallurgical processing of spent hydrodesulphurisation (HDS) catalyst for the recovery of molybdenum using sodium carbonate and hydrogen peroxide mixtures was investigated. The results indicated that the recovery of molybdenum was largely dependent on the concentrations of Na2CO3 and H2O2 in the reaction medium, which controls the acidity of the leach liquor and carry over of impurities such as Al, Ni, P, Si and V. Leaching process was exothermic and leaching efficiency of molybdenum decreased with increasing solid to liquid ratio. Large scale leaching of spent catalyst, under optimum conditions: 20% pulp density, 85 g/L Na2CO3, 10 vol.% H2O2 and 1 h reaction, resulted a leaching efficiency of 84% Mo. The obtained leach liquor contained (g/L): Mo — 22.0, Ni — 0.015 and Al — 0.82, P — 1.1, Si — 0.094 and minor quantities of V — 8 mg/L, As and Co — < 1 mg/L. Recovery of Mo from leach solution as MoO3 of 97.30% purity was achieved by ammonium molybdate precipitation method. 相似文献
97.
T.E. Johnson C.L. Kirkland D.R. Viete S. Fischer S.M. Reddy N.J. Evans B.J. McDonald 《地学前缘(英文版)》2017,8(6):1469-1478
The type locality for high-temperature,low-pressure regional metamorphism,the Buchan Block in NE Scotland,exhibits profound differences to the rest of the Grampian Terrane.These differences have led some to regard the Buchan Block as an exotic crustal fragment comprising Precambrian basement gneisses and cover rocks thrust into their current position during Grampian orogenesis.Although rocks of the Buchan Block are now generally correlated with Dalradian strata elsewhere,the origin of the gneisses and the cause of the high heat flow and associated magmatism is debated.We report SIMS U-Pb and LA-ICPMS Hf isotopic data in zircon from high-grade rocks from the northeast(Inzie Head Gneiss)and northwest(Portsoy)corners of the Buchan Block.Around Inzie Head,upper amphibolite to granulite facies metasedimentary gneisses coexist with diorite sheets that were emplaced contemporaneously with partial melting of their host rocks,at least locally.U-Pb geochronology indicates a crystallisation age for the diorite of 486±9 Ma.Highly-deformed diorites within the Portsoy Gabbro have a crystallisation age of 493±8 Ma.Ages of ca.490 Ma for magmatism and high-grade metamorphism,which are broadly contemporaneous with ophiolite obduction and the onset of orogenesis,are significantly older than the established peak of Grampian metamorphism(ca.470 Ma).We propose a new model for the Grampian Orogeny involving punctuated tectonothermal activity due to tectonic switching during accretionary orogenesis.Rollback of a NW-dipping subduction zone at ca.490 Ma produced a back-arc environment(the Buchan Block)with associated arc magmatism and high dT/dP metamorphism.Arrival of an outboard arc resulted in shortening(the initial phase of the Grampian Orogeny)at ca.488 Ma.Rollback of a NW-dipping subduction zone to the SE of the ca.488 Ma suture began at 473 Ma and led to lithospheric-scale extension,decompression melting and advective heating of the middle crust,producing the widespread ca.470 Ma Grampian(classic Barrovian and Buchan)regional metamorphism.Resumed hinge advance and the final phase of shortening cut off the heat supply at ca.465 Ma,marking the end of the Grampian Orogeny. 相似文献
98.
R. Nagendra P. Sathiyamoorthy A. N. Reddy Harry Gilbert B. C. Jaiprakash 《Arabian Journal of Geosciences》2014,7(10):4133-4144
Grey shale Member of the Dalmiapuram Formation, Ariyalur Group, Cauvery Basin, India was studied for its stratigraphic position, age, and paleobathymetry with a re-look into the lithological relationship and foraminifer assemblages in the deepened limestone mine excavations at M/s Dalmia Cements, Dalmiapuram. Twenty grey shale samples from Kovandankurchchi (pit-4) and Kallakkudi mines yielded diversified calcareous, benthic, and rare index planktic foraminifera. The foraminiferal assemblages suggest a latest Albian age and middle neritic depositional conditions. The abundance of kaolinite and smectite clay minerals relate to warm/humid climate which corroborate with rising relative sea level during grey shale deposition. The grey shale occurs in patches within the marl bedded limestone member which exhibits cyclic deposition of limestone and marl. The limestone mine sections demonstrate that the grey shale forms part of basal marl bedded limestone, directly overlying the coral algal limestone. The present study demonstrates that the grey shale outcrops in Dalmiapuram Formation should be placed stratigraphically as part of marl bedded limestone. The member status for grey shale which is current usage stands discounted. 相似文献
99.
D. Lu L. White R. S. Reddy P. J. Croft J. M. Medlin 《Meteorology and Atmospheric Physics》2006,94(1-4):153-165
Summary A numerical mesoscale model (COAMPS) is used to study some of the features associated with the evolution of the kinematic,
thermodynamic, and physical structure of the Alabama sea and bay breeze circulations and convections in weak shear environments
based on five cases from Medlin and Croft (1998). The general and expected features and evolution of sea and bay breeze circulations
are captured by the model simulations, including horizontal and vertical wind shifts, thermal contrast between land and water
surface, vertical stability over water and land, return currents and moisture increase. The relationship of the circulations
to specific synoptic flow regimes and local physiographic features was investigated. The sea breeze triggered convective cells
are confirmed to have a preferred location according to the flow regime and local conditions. This result can assist the forecasters
in understanding the anticipated convective cell initiation and development on a given day as related to sea and bay breeze
cells as well as improve the short-term forecast accuracy of the location of thunderstorm initiation based on routine observations
and subsequent convective activity. If local NWS office model a selective subset of cases then they can better visualize and
forecast those cases operationally. 相似文献
100.
Jaya Naithani H. N. Dutta P. K. Pasricha B. M. Reddy K. M. Aggarwal 《Boundary-Layer Meteorology》1995,74(1-2):195-208
Turbulent fluxes have been evaluated for clear sunny days over the Indian Antarctic station, Maitri, using the basic meteorological data recorded at four levels of a 28 m tower. The data are supplemented with radiation data. The surface layer over Maitri remains thermally stratified during the hours of minimum solar insolation, the so-called nighttime period. The surface winds during this period are generally very strong resulting in high momentum fluxes. In particular, for high winds (>12 m s–1), the temperature gradient is found to be less positive than for moderate winds (4 to 7 m s–1). Solar insolation provided the daytime heating necessary for the diurnal variation of atmospheric stability, and hence, for the turbulent fluxes. Thus, on clear days daytime conditions are marked by upward transport of heat with reduced momentum flux, while stable nighttime conditions are marked by a downward heat flux with increased momentum fluxes. 相似文献