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52.
JASPER M. DALHUISEN CAROLINE A. RODENBURG HENRI L.F. DE GROOT PETER NIJKAMP 《European Planning Studies》2003,11(3):263-281
This article focuses on the identification of critical water policy instruments, and opportunities and barriers to transforming urban water use in a sustainable and efficient direction in Amsterdam (The Netherlands). The main lessons that can be inferred from past and current water policies and management practices in Amsterdam show (1) the relevance of common action for increasing the quality of or general control over water resources when shared interests of different actors using the same water resource are present; (2) that the effectiveness and applicability of water policy instruments are strongly conditional upon receiving the support of both water users and suppliers; (3) that the governance structure of water provision plays a crucial role in increasing the efficiency of water use. 相似文献
53.
NATURE AND MICROSTRUCTURE OF GALLIC IMITATIONS OF SIGILLATA SLIPS FROM THE LA GRAUFESENQUE WORKSHOP*
C. MIRGUET C. DEJOIE C. ROUCAU PH. DE PARSEVAL S. J. TEAT PH. SCIAU 《Archaeometry》2009,51(5):748-762
The red glaze (slip) that characterizes the Terra Sigillata potteries greatly contributed to their success during the Roman period. The colour of the slip can in fact be partially explained by the microstructure (crystalline phases, grain sizes) and the physico‐chemistry (composition) of the ceramics. However, the precise process and the diffusion of this technique are still not fully known. In particular, we do not know yet how the production of sigillata took place in the south of Gaul, and the role that was played by the production under Italian influence (pre‐sigillata) preceding the first local sigillata. In this work, a combination of transmission electron microscopy (TEM) and X‐ray synchrotron diffraction techniques was used to study the microstructure of pre‐sigillata slips from the main southern Gaul workshop (La Graufesenque), in order to compare their characteristics with those of high‐quality sigillata. These first results seem to indicate that the antique potters chose clays adapted to their firing conditions and to the type of coating that they wanted to make. These productions cannot be described as an initial phase for the later sigillata production and, rather, seem to correspond to the intention of developing a specific type of pottery only inspired by the famous Italian sigillata forms. 相似文献
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G. E. DE BENEDETTO P. ACQUAFREDDA M. MASIERI G. QUARTA L. SABBATINI P. G. ZAMBONIN M. TITE M. WALTON 《Archaeometry》2004,46(4):615-624
Five sherds of green glazed pottery excavated at Canosa (Apulia) in Italy have been analysed by scanning electron microscopy. The aim of the investigation was to determine the chemical composition of the glazes and thus obtain information on the methods used in their production. The glazes were all of the high‐lead type, coloured green by the addition of copper. Intermediate layers, observed at the interface between the glaze and body and giving the appearance of an applied white slip, were the result of the crystallization of lead feldspar from the molten glaze. Non‐calcareous clays were used in the production of the pottery bodies. Concentration profiles from the glaze exterior to the body suggested that the glazes were produced by applying a suspension consisting of lead oxide plus silica to the bodies. On the basis of the glaze and body compositions, it is suggested that the Canosa glazed pottery was produced locally. 相似文献
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A non‐destructive analytical method using wavelength‐dispersive X‐ray fluorescence (WDXRF) that allows the establishment of the provenance of archaeological obsidians was developed and a comparison with the classical XRF method on powders is discussed. Representative obsidian samples of all the geological outcrops of archaeological interest of the Mediterranean area (Lipari, Pantelleria, Sardinia, Palmarola and the Greek islands of Melos and Gyali), were analysed with the normal procedures used in rock analysis by XRF (crushing, powdering and pelletizing). The non‐destructive XRF analysis was instead conducted on splinters taken from the original geological pieces, with the shape deliberately worked to be similar to the refuse usually found at archaeological sites. Since the analysis was conducted on the raw geological fragment, intensity ratios of the suitably selected chemical elements were used, instead of their absolute concentrations, to avoid surface effects due to the irregular shape. The comparison between concentration ratios (obtained by traditional XRF methods) and the intensity ratios of the selected trace elements (obtained from the non‐destructive methodology) show that the different domains of the chemical composition, corresponding to the geological obsidians of the source areas, are perfectly equivalent. In the same way, together with the geological splinters, complete archaeological obsidians, from Neolithic sites, may be analysed and their provenance may be determined. The proposed non‐destructive method uses the XRF method. Due to its sensitivity, low cost and high speed, it is surely an extremely valid instrument for the attribution of the provenance of the archaeological obsidian from Neolithic sites. 相似文献
58.
ANNA DE JONG 《Geographical Research》2015,53(2):211-223
Geographers have long been alert to the ways space matters to knowledge production and the stories participants choose to share. Despite such understandings, however, geographers remain surprisingly absent from discussions regarding the ways these concerns play out across online spaces. This article reflects on the employment of one online space, Facebook, as a site for storytelling in research exploring return journeys to two Australian festivals – the Big Day Out and Mardi Gras Parade. This article argues that insight over longer temporalities and shifting spatialities afforded through Facebook facilitates heightened understandings of the nuances, repetitions, differences and paradoxes of identities, encounters, and politics. Facebook, therefore, has the potential to allow for different ways of knowing that cannot be ascertained in more orthodox research spaces. Moreover, the slipperiness of conceptualisations of privacy and consent in this space draws attention to the necessity of understanding consent as fluid and ongoing, rather than antecedent to fieldwork commencement. Crucially, however, reconceptualisations of privacy and consent in this space expose potential obstacles university ethics committees may meet in responding to research moving online. 相似文献
59.
DAVID SANTAMARÍA JAVIER FORTEA MARCO DE LA RASILLA LUCÍA MARTÍNEZ ENRIQUE MARTÍNEZ JUAN CARLOS CA
AVERAS SERGIO SNCHEZ‐MORAL ANTONIO ROSAS ALMUDENA ESTALRRICH ANTONIO GARCÍA‐TABERNERO CARLES LALUEZA‐FOX 《Oxford Journal of Archaeology》2010,29(2):119-148
This paper presents the first detailed analysis of the lithic industry from El Sidrón Cave. Previously we have published other works concerning Anthropology and Palaeogenetics. The lithic assemblage contains 415 artefacts coming from both unofficial and official excavations and is largely flake‐based. The raw material derives from the immediate cave environment, and is mostly chert, with quartzite in a lesser proportion. To date, 67 artefacts have been refitted, including some tools and cores. The spatial distribution of the refitted lithic artefacts confirms, on the one hand, the unity of the assemblage and, on the other, its secondary context. 相似文献
60.
J. M. PARÉS A. PÉREZ‐GONZÁLEZ J. L. ARSUAGA J. M. BERMÚDEZ DE CASTRO E. CARBONELL A. I. ORTEGA 《Archaeometry》2010,52(5):882-898
We use a combination of rock magnetism (anisotropy of magnetic susceptibility, AMS) and magnetic polarity to characterize cave deposits and as a proxy for sedimentary fabric. In three localities at the Atapuerca archaeological site (Galeria, Gran Dolina and Sala de los Cíclopes), magnetic foliation (Kmax/Kint) is always greater than lineation (Kint/Kmin), consistent with a primary, depositional, sedimentary fabric. Our results, although preliminary, reveal a higher degree of anisotropy in autochtonous deposits compared to allochthonous deposits, possibly indicative of a higher hydrodynamic regime in the former. At two localities the magnetic lineation (Kmax) defines a cluster, which is thought to be antipodal to the palaeocurrent direction. Hence we are able to retrieve palaeoflow directions in deposits that otherwise lack any other sedimentary structure. We conclude that AMS is a powerful tool for determining the hydrodynamic character of depositional environments in cave sediments at the Atapuerca archaeological site. A better understanding of the depositional environment and how sedimentation occurred allows reconstruction of the karst evolution and ultimately a better definition of human interaction with the environment. 相似文献