A comparative fluid inclusion study of the Waterville and Sangerville (Vassalboro) Formations,south-central Maine     

Sakiko N. Olsen  John M. Ferry 《Contributions to Mineralogy and Petrology》1995,118(4):396-413

 Petrologic and oxygen isotope data indicate that water-rich fluids infiltrated metasedimentary rocks of the Waterville and Sangerville (formally Vassalboro) Formations, south-central Maine, during peak metamorphism, and depleted Sangerville rocks in alkalis but not equivalent Waterville rocks. Fluid inclusion data from two outcrops, ∼1 km apart, one of the Waterville and the other of the Sangerville Formations, suggest a cause for the geochemical difference between the two units. Postulated peak metamorphic inclusions, the texturally earliest of aqueous inclusions in the metasediments, approximate the water-rich compositions of peak fluids predicted by mineral-fluid equilibria, and have average salinity in the Sangerville Formation ∼ three times that of equivalent Waterville inclusions. The higher salinity in the Sangerville fluids could explain the greater alkali depletion in these rocks. Probable pre-peak or prograde inclusions are preserved in metasediments as the texturally earliest carbonic inclusions which contain CO₂, CH₄, N₂±H₂O, as determined by microthermometry and Raman spectrometry. They may have formed by breakdown of organic matter. Probable retrograde inclusions occur as texturally late aqueous inclusions in healed fractures with salinity ranges indistinguishable between the two formations. Synmetamorphic granitic dikes present in the two outcrops were ruled out as a source for fluids in metasediments because composition and density ranges of inclusions in dikes and metasediments are fundamentally different, and because there is no correlation between the abundance or composition of inclusions in a sample and proximity to dikes. Isochores for many of the inclusions in both metasediments and dikes are not consistent with the inferred P−T conditions of their trapping, but intersect at ∼300° to 400° C and 1 to 2 kbar. The intersections probably resulted because inclusion densities continued to equilibrate during uplift and cooling until quartz became rigid. The present densities are those at the last equilibration, not the time of trapping. In contrast, the clear distinctions in inclusion compositions between dikes and between dike and country rock show that the original compositional differences generally have been preserved. Received: 4 February 1994 / Accepted: 22 June 1994  相似文献   

Reservoir Characterization Applying High-Resolution Seismic Profiling, Rabis Creek, Denmark   总被引：1，自引：0，他引：1  

Henrik Olsen  Garsten Ploug  Uffe Nielsen  Kurt Sorensen 《Ground water》1993,31(1):84-90

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Isotropic and deviatoric characterization of the Coalora nuclear explosion in Yucca Flats     

Brian W. Stump  Robert E. Reinke  Kenneth H. Olsen  Lane R. Johnson 《Geophysical Journal International》1994,116(3):538-552

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岩土钻探工程大口径钻头设计与应用          下载免费PDF全文

卢予北 《探矿工程》1994,(3):25-27

分析对比了多种岩土钻探工程大口径钻头的优缺点，设计了适应不同地层的大口径钻头。  相似文献   

Integration of European habitat monitoring based on plant life form composition as an indicator of environmental change and change in biodiversity     

Margit Bloch-Petersen  Jesper Brandt  Martin Olsen 《Geografisk tidskrift / udgivet af Bestyrelsen for Det Kongelige danske geografiske selskab》2013,113(2):61-74

Geografisk Tidsskrift, Danish Journal of Geography 106(2): 61–74, 2006

During the last 25 years a number of European countries have developed general landscape monitoring systems. In the agricultural landscapes of Denmark the Small Biotope Monitoring Program (SBMP). which focuses on the dynamics of small biotopes and their relation to changes in agricultural technology and structural characteristics, has been developed since 1981. Erom 2007, the SBMP will continue as part of the Danish nature monitoring program, NOVANA.

In Europe, during the last 10 years, several national landscape surveys have cooperated to develop a European platform for consistent landscape related habitat monitoring. This has been through the BioHab Concerted Action Framework Programme of the EU (2002–2005), and the resulting publication of a handbook for recording and monitoring habitats (Bunce et al., 2005). The focus on environmentally conditioned habitat changes at a landscape level has led to the re-introduction of Raunkiaer's plant life form concept. This approach enables the indication of changes in biodiversity based on alterations in general habitat composition and quality.

Although the objectives of the SBMP and the BioHab projects have been somewhat different, the methodologies have much in common. In this paper the background and perspectives of the two approaches are discussed, and a test of the BioHab field methodology in an area previously monitored by the SBMP is presented. It was found not to be difficult to integrate the BioHab field recording methodology with the existing SBMP methods, thus permitting the SBMP to deliver an additional European perspective, with relatively little additional effort.  相似文献   

Timing and maximum flood level of the Early Holocene glacial lake Nedre Glomsjø outburst flood,Norway     

Fredrik Høgaas  Louise Hansen  Ivar Berthling  Martin Klug  Oddvar Longva  Helle Daling Nannestad  Lars Olsen  Anders Romundset 《Boreas: An International Journal of Quaternary Research》2023,52(3):295-313

This study discusses the timing and maximum flood level of the Nedre Glomsjø outburst flood, Norway, based on sediment records retrieved from 15 bog and lake basins located close to the purported maximum flooded level. The sediment records in 12 of the basins consist of a distinct light-coloured silty bed that is correlated to the outburst-flood-deposited ‘Romerike Silt Bed’ identified elsewhere in the region. The silt bed is recorded in basins up to a certain elevation and is absent above this level. The new maximum flood level inferred from the basin sediment records exceeds the established landform-induced palaeostage indicators by 5–10 m. The data indicate a higher maximum flood level and larger inundation area than previously suggested and highlight the importance of acquiring a wide range of geological data when reconstructing palaeofloods. Radiocarbon dates of terrestrial macrofossils found stratigraphically above and below the Romerike Silt Bed suggest that the glacial lake Nedre Glomsjø outburst flood occurred between 10.5 and 10.3 cal. ka BP. The new and well-constrained timing of the outburst flood is beneficial for reconstructing regional deglaciation and provides a precise age for the Romerike Silt Bed chronostratigraphical marker, which is of value for studies in SE Norway and adjacent regions.  相似文献   

AgCam传感器平场校正     

窦长勇  张晓东  Doug Olsen  贺明霞 《中国海洋大学学报(自然科学版)》2010,40(9)

平场校正对获得高质量的遥感图像起着非常关键的作用。针对利用商业相机开发的传感器需要进行平场校正的问题,提出对Agriculture Camera(AgCam)传感器的平场校正方法。应用AgCam的定标实验数据分别得到传感器CCD阵列的暗电流(Dark Current),渐晕效应(Vegnitting Effect)和光电响应(Quantum Efficiency)的校正系数。AgCam的定标实验数据和实际拍摄图像处理结果表明,该方法能够有效地对AgCam的平场效应进行校正。  相似文献   

Characterizing solute transport in undisturbed soil cores using electrical and X‐ray tomographic methods     

P. A. Olsen  A. Binley  S. Henry‐Poulter  W. Tych 《水文研究》1999,13(2):211-221

Solute transport in undisturbed soil is a complex process and detailed information on the transport characteristics is needed to provide fundamental understanding of the processes involved. X‐ray computer tomography (CT) and electrical resistivity tomography (ERT) have been used to gain information on the transport characteristics. Both methods are non‐intrusive and do not disturb the soil, in contrast to other methods. CT provides high resolution information on bulk density and macropores, while ERT provides a three‐dimensional image of the internal resistivity structure. By adding a suitable solute under steady‐state flow, the internal resistivity changes can be interpreted as a change in resident concentrations. In our experiment two cores from different field sites were investigated. The ERT measurements revealed two transport modes (one fast and one slow) in one of the cores and only one mode in the other. This was consistent with the results of transfer function modelling on the independently measured breakthrough curves (BTCs). The fast transport mode is perhaps a result of many connected macropores, detected by CT, but this could not be verified with the ERT measurements because of the coarser resolution. However, with ERT in both cases we were able to explain the observed BTC qualitatively. Copyright © 1999 John Wiley & Sons, Ltd.  相似文献   

The measurement of sand transport in two inlets of Venice lagoon,Italy     

C.L. Amos  M. Villatoro  R. Helsby  C.E.L. Thompson  L. Zaggia  G. Umgiesser  V. Venturini  D. Are  T.F. Sutherland  A. Mazzoldi  F. Rizzetto 《Estuarine, Coastal and Shelf Science》2010

Sand transport in Lido and Chioggia inlets was measured using modified Helley–Smith sand traps equipped with 60-micron nets. The traps had an efficiency of about 4% only but provided enough material for analysis. Very fine sand (0.07 < d < 0.11 mm) only was collected in the traps. Transport of sand was greatest in the bottom 10% of the water column and followed a Rouse profile. Sand extended to a height of about 4 m above the bed during peak flows corresponding to the estimated thickness of the boundary layer; and observed in synoptic ADCP profiles. The sand in the benthic boundary layer was largely inorganic (>95%); above this layer, organic content varied widely and was greatest near the surface. The movability number Ws/U_∗$W_s/U_{\ast }$ showed a linear relationship to dimensionless grain diameter (D_*): (Ws/U_∗)=(D_∗/10)$\left(W_s/U_{\ast }\right)=\left(D_{\ast }/10\right)$; D_* < 10. Sand concentration in suspension was simulated by a mean Rouse parameter of −2.01 ± 0.66 (Lido inlet) and −0.82 ± 0.27 (Chioggia inlet). The β parameter ( Hill et al., 1988) was correlated with D_* and movability number in the form: β=2.07−2.03D_∗+59(Ws/U_∗)²$\beta =2.07-2.03D_{\ast }+59{\left(W_s/U_{\ast }\right)}^2$ (r² = 0.42). Von Karman's constant was back-calculated from a Law of the Wall relationship as a test on the accuracy of U_* estimates; a mean value of 0.37 ± 0.1 (compared to the accepted value of 0.41) suggest U_* was accurate to within 10%. The constant of proportionality (γ = 3.54 × 10⁻⁴) between reference concentration (C_a) and normalized excess bed shear stress was in line with the published literature.  相似文献   

Minor planet observations 1984-1990     

H. J. Fogh Olsen 《Astronomische Nachrichten》1993,314(1):47-48

An overview of the minor planet search performed in the period 1984–1990 at Brorfelde Observatory is presented. All basic information about the observations is given but the positions are not presented because they are already published in Minor Planet Circulars. 1973 positions have been measured on 413 plates. 303 positions belong to unknown minor planets. At the end of 1992, 42 of these are numbered, having got enough observations to calculate a reliable orbit.  相似文献