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GODFREY BALDACCHINO 《Geographical review》2007,97(2):165-174
ABSTRACT. Being on the edge, being out of sight and so out of mind, exposes the weakness of mainstream ideas, orthodoxies, and paradigms and foments alternatives to the status quo. Islands are thus propelled as sites of innovative conceptualizations, whether of nature or human enterprise, whether virtual or real. They stand out as sites of novelty; they tend toward clairvoyance; they are disposed to act as advance indicators or extreme reproductions of what is present or future elsewhere. This article, which is essentially bibliographical, celebrates islands as the quintessential sites for experimentation, with reference to the physical sciences, the social sciences, and literature. 相似文献
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A type of iterative deconvolution that extracts the source waveform and reflectivity from a seismogram through the use of zero memory, non-linear estimators of reflection coefficient amplitnde is developed. Here, we present a theory for iterative deconvolution that is based upon the specification of a stochastic model describing reflectivity. The resulting parametric algorithm deconvolves the seismogram by forcing a filtered version of the seismogram to resemble an estimated reflection coefficient sequence. This latter time series is itself obtained from the filtered seismogram, and so a degree of iteration is required. Algorithms utilizing zero memory non-linearities (ZNLs) converge to a family of processes, which we call Bussgang, of which any colored Gaussian process and any independent process are members. The direction of convergence is controlled by the choice of ZNL used in the algorithm. Synthetic and real data show that, generally, five to ten iterations are required for acceptable deconvolutions. 相似文献
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LEE DER-CHUEN; HALLIDAY ALEX N.; DAVIES GARETH R.; ESSENE ERIC J.; FITTON J. GODFREY; TEMDJIM ROBERT 《Journal of Petrology》1996,37(2):415-441
Major element, trace element and Sr–Nd–Pb isotopiccompositions of ultramafic xenoliths and megacrysts from thecontinental Cameroon line provide evidence for metasomatismof the upper most lithospheric mantle by enriched melts duringthe Mesozoic The megacrysts probably crystallized within thelower continental crust from melts similar to the host magmas.All the xenoliths originated as depleted residues after theextraction of basaltic melts, but some indicate evidence ofinteraction with enriched partial melts before entrainment.The U–Pb isotopic data on garnet are consistent with coolingthrough >900C at >300 Ma. The Sm–Nd isotope systematicsin constituent phases appear to have been in equilibrium ona xenolith scale at the time of entrainment, indicating derivationfrom mantle that remained at temperatures >600C until eruption.Spinel therzolies that show simple light rare earth element(LREE) depletions are characterized by isotopic compositionsthat are comparable with, but slightly more depleted than AtlanticN-MORB, suggesting that the unmetasomatized sub-continentallithosphere of the Cameroon line may be isotopically similarto that of sub-oceanic lithosphere. The Nd-depleted mantle modelages of these xenoliths are consistent with late Proterozoicdepletion, similar in age to much of the overlying continentalcrust. In contrast, samples that have LREE-enriched clinopyr-oxenes(La/Yb =4.7–9.4) contain trace amounts of amphibole, areenriched in U and have more radiogenic Pb and Sr. These xenolithsyield U–Pb and Sm–Nd model ages consistent withMesozoic enrichment, in agreement with the age of enrichmentof the source regions of the basalts, as deduced from Pb isotopiccompositions. Clinopyroxenes record three orders of magnitudeenrichment in U and LREE accompanied by progressive K depletionassociated with the growth of trace amphibole, with K/U ratiosthat range from 12000 to 1. The ratios of the trace elementsthought to have similar bulk D in mantle melting, Ce/Pb, Ba/Rband Nd/Sr ratios, display regional variations related to thetime integrated history of enrichments indicated by Nd isotopiccompositions. Mass balance calculations suggest that the meltsresponsible for the most recent enrichment of the lithospherehad higher La/Yb and U/Pb than Cameroon line host magmas, andwere probably the product of small degrees of partial meltingassociated with the earliest stages of the breakup of Pangea. KEY WORDS: Cameroon line; mantle xenoliths; megacrysts; REE; isotopic composition; trace element 相似文献
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BRIAN J. GODFREY 《Geographical review》2002,92(1):127-139
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The North Atlantic igneous province offers an unrivalled opportunityto study mantle sources contributing to flood basalt magmatism,and melting dynamics associated with active and passive upwellingof hot mantle beneath the lithosphere. In this study, Palaeogenebasalts sampled at localities across the British Isles (fromthe Hebrides in the north to Lundy Island in the south) areshown to have concentrations of Nb, Zr and Y consistent withderivation from two mantle sources: ‘Icelandic’(plume) mantle and hot N-MORB-like mantle forming an outer envelopeto the plume. These sources were sampled over the period 61–58Ma (chrons 26R–26N). Values of 相似文献
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NICHOLSON HUGH; CONDOMINES MICHEL; FITTON J. GODFREY; FALLICK ANTHONY E.; GR?NVOLD KARL; ROGERS GRAEME 《Journal of Petrology》1991,32(5):1005-1020
The Krafla volcanic system consists of a central volcano andassociated fissure swarm in the NE axial rift zone of Iceland.Lavas spanning the whole of Krafla's exposed volcanic history(estimated to be 0-> 300 ka) have been analysed and rangein composition from olivine tholeiite to rhyolite. Major-elementcompositions suggest that fractional crystallization exertsthe main control over the differentiation process. However,K2O and the very incompatible trace elements, Rb, Th, and U,are all enriched beyond the extent expected by closed-systemfractional crystallization. Fractionation coupled with periodicreplenishment and tapping of the reservoir is unlikely to beresponsible for this enrichment, despite the geophysical evidencesuggesting a large number of inflations and deflations of ashallow magma reservoir (Tryggvason, 1986). Th- and O-isotope results confirm the work of previous authorsthat crustal assimilation is operating on a local scale beneathKrafla. A model is suggested, fitting both the Th- and O-isotopicdata, which involves the partial melting and incorporation ofa hydrothermally altered wall-rock contaminant during fractionalcrystallization (i. e., AFC processes). This process of partialmelting is likely to enhance the most highly incompatible elementconcentrations (e. g., increasing Rb/Zr) more than expectedby closed-system fractional crystallization. 相似文献
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BRIAN J. GODFREY 《Geographical review》1999,89(1):94-121
ABSTRACT. Contrasting models of urban development characterize the historical-geographical evolution of Brazil's two leading cities, viewed in an updating of the seminal 1933 article by Preston James. Native to Rio de Janeiro is a distinctive Luso-Brazilian style of irregular coastal urbanization, whereas SÃo Paulo displays a more uniform, modern type of inland commercial-industrial expansion. Even as Rio de Janeiro and SÃo Paulo sprawl today to form a virtual megalopolis in southeastern Brazil, they retain distinguishing roles in the national city system. Both metropolises are experiencing increasing functional decentralization and socioeconomic polarization, but in their own characteristic fashions. Generalized models of “Latin American city structure” are of limited value, unless they take into account such significant historical-geographical variations in urban form. 相似文献
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Pterosaur skulls were shaped by a host of selective pressures and because of the great number of variables they present a dizzying array of morphologies. These permutations present functional suites that can be analyzed allowing for a greater appreciation of pterosaur paleobiology. 相似文献