Overwash processes along a gravel beach in south-east Ireland     

R. W. G. Carter  J. D. Orford 《地球表面变化过程与地形》1981,6(5):413-426

Recent overwashing, and to a more limited extent overtopping, has occurred on a gravel-dominated beach just west of Carnsore Point in south-east Ireland. At relatively low points swash excursions have breached the duneline and extensive gravel fans have formed on landward-facing slopes. Also, at interbreach positions, swash ramps have been built-up in front of previously eroding dune cliffs, allowing overtopping at heights of up to 5 m above MHWOST, spreading a veneer of sediment over the adjacent dune ridge. In both cases events appear to be preceded by erosion and backbeach sand and gravel deposition. Stratigraphic, textural and fabric analyses assist in identifying environmental conditions that prevailed during overwash throat and fan, and overtopping ramp, sedimentation.  相似文献   

Free and steady state vibration of non-linear structures using a finite element–non-linear eigenvalue technique     

L. Carter Wellford  G. M. Dib  W. Mindle 《地震工程与结构动力学》1980,8(2):97-115

The problem of free vibration of non-linear structures is considered initially. It is shown that this problem can be represented as a non-linear eigenvalue problem. Variational principles for non-linear eigenvalue problems are defined. These variational principles are implemented with finite element models to define numerical approximations for the free vibration problem. The solution of these approximate equations provides a set of non-linear modal vectors and natural frequencies which vary with the amplitude of the solution. The non-linear eigenvalue parameters can be used in modal expansion approximations for the non-linear transient or steady state response of structural systems. To demonstrate the proposed techniques the free vibration and steady state vibration characteristics of a geometrically non-linear circular plate are determined.  相似文献   

Fault-bounded blocks and their role in localising sedimentation and deformation adjacent to the alpine fault, southern New Zealand     

R.J. Norris  R.M. Carter 《Tectonophysics》1982,87(1-4)

Continental transform boundaries in detail consist of zones of fault-bounded blocks adjacent to the principal active transform fault(s). Relative movement of these blocks in response to plate boundary motions gives rise to differential vertical displacements of the earth's crust and hence exercises a degree of control on the tectonic evolution of sedimentary basins adjacent to the transform boundary. The Cenozoic sedimentary basins of southwest New Zealand have several features in common that may be attributed directly to the movement on the adjacent plate boundary. However, their location, detailed sedimentary evolution and tectonic development may best be understood in the context of the relative displacements of a number of fault-bounded blocks, in response to the plate motions. In particular, movements of the Fiordland block, bounded by the Alpine and Moonlight fault zones, exercised a large measure of influence on the development of the basins. The tectonic model presented is consistent with plate boundary motions inferred from marine magnetic anomalies while at the same time providing an explanation for many of the more detailed features of the basins.  相似文献   

Author's reply     

G.M. Thompson  D.N. Lumsden  R.L. Walker  J.A. Carter 《Geochimica et cosmochimica acta》1978,42(4):437-439

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Uranium series dating of stalagmites from Blanchard Springs Caverns,U.S.A.     

Glenn M. Thompson  David N. Lumsden  Raymond L. Walker  Joel A. Carter 《Geochimica et cosmochimica acta》1975,39(9):1211-1218

Because stalagmites are enriched in ²³⁴U beyond the equilibrium value at the time of deposition, they are potentially datable by measuring their progress toward equilibrium. Procedures for uranium-thorium and uranium disequilibrium dating of speleothems were developed, making use of alpha spectrometry for thorium determinations and mass spectrometry for uranium determinations. The stalagmites tested were generally beyond the age range of the U-Th age dating method and, as a result, ²³⁴U/²³⁸U ratios provided the most useful dating technique. The estimated age range for a stalagmite from Blanchard Springs is 135,000 to 785,000 years BP with an interval of slow or suspended growth from about 320,000 to 570,000 years BP.  相似文献   

The precambrian of north-western Queensland,Australia     

E. K. Carter 《International Journal of Earth Sciences》1959,47(2):510-522

Precambrian rocks, ranging in age from probable Archaean to Upper Proterozoic, crop out over an area of 25,000 square miles in north-western Queensland. They fall into four large divisions, separated by major unconformities. Little is known of the history of the Archaean rocks, which are believed to include altered acid lavas, schists, gneisses and migmatite. The Lower Proterozoic strata form part of an orogenic belt. The Lower Proterozoic lower sequence is rich in altered acid and basic lavas. It has a maximum thickness of not less than 40,000 feet and was strongly deformed by east-west pressure and probably intruded by granite before the Lower Proterozoic upper sequence was deposited. Sediments form the bulk of the Lower Proterozoic upper sequence; these accumulated most thickly to the west and north-west of the core of lower sequence belt, but overlie lower sequence strata. The greatest thickness of sediments is at least 40,000 feet. The sequence was deformed by a renewal of east-west compressive stresses, accompanied by granite emplacement. Folding is strong to moderate, but lacks well-defined linearity in the west of the outcrop area.Upper Proterozoic sediments and lavas accumulated mainly in the west and north-west of the region. They are gently to moderately folded on west to north-west axes.The Precambrian in north-western Queensland, excluding the Camooweal Dolomite, crops out over about 25,000 square miles. Systematic field work was started by joint teams of the Commonwealth Bureau of Mineral Resources and the Geological Survey of Queensland in 1950.Reconnaissance mapping of the region was completed in 1954 but check work and more detailed mapping of areas of economic interest are still in progress. Maps are being prepared at a scale of 1 inch to 4 miles (1: 253,440) and a report on the area is being written (Carter andBrooks, in preparation). The Camooweal Dolomite, of Upper Proterozoic or Lower Cambrian age, is not included. Its stratigraphic and palaeographic position is discussed byNoakes (1956).The reconstruction of the geological history of the region presented below is an interpretation of the data obtained. The evidence is not sufficiently complete to enable a unique interpretation to be made of all aspects of the region's history. In particular the history of granite intrusion has not yet been completely unravelled.Paper published by permission of the Secretary, Department of National Development.  相似文献   

Seasonal and spatial distribution of planktonic crustacea in the lower Saint John River,a multibasin estuary in New Brunswick,Canada     

J. C. H. Carter  M. J. Dadswell 《Estuaries and Coasts》1983,6(2):142-153

Five stations on the lower Saint John River, a complex multibasin estuary, were sampled semiquantitatively for zooplankton at biweekly intervals for one year, and qualitatively over a 4-year period. Planktonic Crustacea were dominated by the true estuarine copepods,Acartia tonsa andEurytemora affinis and the euryhaline marine copepodsOithona similis andPseudocalanus minutus. Atypical estuarine forms, confined to a lower fiord-like basin with salinity of 20‰, were the amphipod,Parathemisto abyssorum and the mysidErythrops erythrophthalma. River flows were highly variable from year to year. Certain basins function as lakes in some years and estuaries in other years, causing extreme zooplankton community fluctuations, and succession patterns dependent on salinity rather than season. On occasion freshwater zooplankters maintained viable populations at unusually high salinities (ca. 5‰). Vertical and horizontal distributions of zooplankters indicate that the estuary in fact comprises two systems: a true estuary in the upper reaches and the surface waters at the lower end, and a fiord in a subsidiary basin in the lower end.  相似文献   

Habitat requirements for submerged aquatic vegetation in Chesapeake Bay: Water quality, light regime, and physical-chemical factors   总被引：1，自引：0，他引：1  

W. Michael Kemp  Richard Batleson  Peter Bergstrom  Virginia Carter  Charles L. Gallegos  William Hunley  Lee Karrh  Evamaria W. Koch  Jurate M. Landwehr  Kenneth A. Moore  Laura Murray  Michael Naylor  Nancy B. Rybicki  J. Court Stevenson  David J. Wilcox 《Estuaries and Coasts》2004,27(3):363-377

We developed an algorithm for calculating habitat suitability for seagrasses and related submerged aquatic vegetation (SAV) at coastal sites where monitoring data are available for five water quality variables that govern light availability at the leaf surface. We developed independent estimates of the minimum light required for SAV survival both as a percentage of surface light passing though the water column to the depth of SAV growth (PLW _min) and as a percentage of light reaching reaching leaves through the epiphyte layer (PLL _min). Value were computed by applying, as inputs to this algorithm, statistically dervived values for water quality variables that correspond to thresholds for SAV presence in Chesapeake Bay. These estimates ofPLW _min andPLL _min compared well with the values established from a literature review. Calcultations account for tidal range, and total light attenuation is partitioned into water column and epiphyte contributions. Water column attenuation is further partitioned into effects of chlorophylla (chla), total suspended solids (TSS) and other substances. We used this algorithm to predict potential SAV presence throughout the Bay where calculated light available at plant leaves exceededPLL _min. Predictions closely matched results of aerial photographic monitoring surveys of SAV distribution. Correspondence between predictions and observations was particularly strong in the mesohaline and polythaline regions, which contain 75–80% of all potential SAV sites in this estuary. The method also allows for independent assessment of effects of physical and chemical factors other than light in limiting SAV growth and survival. Although this algorithm was developed with data from Chesapeake Bay, its general structure allows it to be calibrated and used as a quantitative tool for applying water quality data to define suitability of specific sites as habitats for SAV survival in diverse coastal environments worldwide.  相似文献   

Mid-Cretaceous uplift and erosion on the northern margin of the Ligurian Tethys deduced from thermal history reconstruction     

Jean-Baptiste Peyaud  Jocelyn Barbarand  Andy Carter  Maurice Pagel 《International Journal of Earth Sciences》2005,94(3):462-474

The paleogeography during Early Cretaceous of the northern margin of the Ligurian Tethys is poorly constrained because of deformation and erosion during Pyrenean and Alpine orogenic phases. The present-day limit between Lower Cretaceous sediments in the South–East basin, located at the northwestern margin of the Ligurian Tethys, and basement rocks is the consequence of a protracted erosion history. Lower Cretaceous sediments observed today in the basin, even close to the present-day outcropping border, are characteristic of pelagic environments. A larger extent of a Lower Cretaceous cover on the basement must then be considered. This study focuses on the western part of this margin (the Causses basin), in the South of the Massif Central (France), using several thermochronometers and geothermometers to decipher the former extent of the sedimentary cover. Apatite fission track thermochronology on basement rocks surrounding the Causses basin suggests that these rocks cooled from temperatures higher than 110°C during the mid-Cretaceous. Average fluid inclusion homogenisation temperatures between 94°C and 108°C are recorded in calcite veins from outcropping Toarcian and Aalenian shales. In the shales, Tmax values, temperature obtained by Rock–Eval pyrolysis of organic matter, are in agreement with these elevated temperatures. Different explanations for these relatively high temperatures, which cannot be explained by the present-day sedimentary serie in the basin, have been tested using a 1D thermal modelling procedure (Genex). For a 95±10-mW/m² paleoflux, thick sedimentary deposits (2.5±0.3 km) including 1.3±0.3 km of Lower Cretaceous sediments cover the South of the Massif Central; these formations have been subsequently eroded from mid-Cretaceous time onwards. This study confirms that the South of the Massif Central was a site of marine sedimentation during the Early Cretaceous where a thick sedimentary sequence was once deposited.  相似文献   

Rural diversification in Bulgaria     

F.W. Carter  D. Kaneff 《GeoJournal》1998,46(3):183-191

Agriculture has always been very important for the Bulgarian economy, but during the socialist period there was considerable progress made in the diversification of employment opportunities in rural areas. While many people commuted to non-agricultural jobs in the townships (and there was a large permanent transfer from rural to urban areas), there were additional opportunities in small factories and local services in the villages themselves. The transition has seen these opportunities much reduced, at precisely the time when full-time paid work in agriculture has declined due to market restructuring while complex problems have emerged associated with liquidating the state-run cooperatives and establishing a viable alternative. The paper discusses the general issues and presents a case study from the north-central part of the country. The rebuilding of a cooperative farming system (along with other forms of consolidation) is a positive trend which could increase spending power in the villages and help in the growth of employment in rural industries and services. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献