Thesis (doctoral)--Karolinska Universitet, Stockholm, 1987. / Added t.p. with thesis statement inserted. Includes bibliographical references.

Thesis (doctoral)--Karolinska Universitet, Stockholm, 1987. / Added t.p. with thesis statement inserted. Includes bibliographical references.

名古屋大学年代測定総合研究センターシンポジウム報告

第23回名古屋大学年代測定総合研究センターシンポジウム平成22(2010)年度報告

No description available.

No description available.

Thesis (Ph. D.)--Pennsylvania State University. / Includes bibliographical references (p. 118-124).

The Palmer Zone of Transpression (PZoT) in the Bronson Hill zone of central Massachusetts is an expression of late Paleozoic oblique convergence between Avalonia and Laurentia. The steeply W-dipping, N-S trending PZoT is defined by bounding high strain zones (Mt. Dumplin on west, Central Maine and Conant Brook on east) of opposing shear sense enclosing the Monson orthogneiss. Research was designed to establish the timing of deformation to test the hypothesis that strain in transpressional systems occurs contemporaneously. An understanding of the timing of deformation in this zone could elucidate the mechanisms that formed the zone and contribute to a greater overall understanding of fabric evolution in transpressional systems. U-Pb SIMS ages of zircon in deformed pegmatites in Monson orthogneiss and Paxton and Rangeley paragneisses are 369 to 364 Ma. Plutons that contain all fabrics associated with progressive transpression – lineations ranging from subhorizontal (initial) to steeply-plunging parallel to dip (final) – mark the maximum age of deformation. Ages range from 360-355 Ma in the Hardwick tonalite, Wachusett tonalite, West Warren diorite, Walker Mountain orthogneiss, and Nichewaug diorite, and indicate transpression in the PZoT initiated after ca. 355 Ma. Monazite from Rangeley paragneisses and schists selected in the context of petrofabrics and syn-deformational mineral assemblages yield U-Th-Pb EPMA chemical ages that indicate dextral transpression occurred continuously from 355 to 315 Ma. Monazite chemical ages also indicate that sinistral lateral displacement in the west-bounding Mt. Dumplin high strain zone initiated ca. 325 Ma and lasted for roughly 45 m.y., ending around 280 Ma. The data for the Central Maine zone, Conant Brook shear zone, and Greenwich syncline support the idea of contemporaneous deformation across the compartmentalized zones of a transpressive system (355-315 Ma), while the ages for the Mt. Dumplin high strain zone indicate sinistral lateral displacement overlapped dextral transpression by about 10 m.y. but generally continued later in time (325-280 Ma).

Aluminium is increasingly being used in the automotive industry to reduce the weight of vehicles. It is the additions of transition elements such as Mn and Cr that can be picked up during recycling, that can form dispersoid particles during homogenisation. Dispersoids play a significant role in the recrystallization and texture development for wrought Al-Mg-Si alloys by inhibiting grain boundary motion. It is therefore important to understand the precipitation kinetics of such particles. The Mn+Cr dispersoid phases are currently thought to nucleate on β'-Mg1.8Si particles via an intermediate semi-coherent precipitate denoted the u-phase. In this study, Al-Mg-Si alloys with additions of Fe and varying levels of Cr were cast to study the effect of different homogenisation regimes on the dispersoid precipitation mechanisms and final characteristics. Electron Probe Micro Analysis (EPMA) was conducted to study the inhomogeneity of elements in the cast structure and through heating to the homogenisation temperature. It was found that Mg, Si and Fe segregate towards the dendrite edges during solidification while Cr segregates towards the dendrite centre. During heating, the matrix composition of both Mg and Si decrease and increase due to precipitation of Mg+Si phases. Cr and Fe stay segregated during the heating process due to the slower diffusion rates in the face centred cubic Al matrix. Dispersoid free regions have also been observed in the microstructure correlating to the elemental segregation in the as-cast condition. Optical, scanning and transmission electron microscopy was utilised in order to study the change in dispersoid characteristics with varying homogenisation regimes and as a function of distance through a grain. With an increase in homogenisation temperature, the mean size of dispersoids increased but number density decreased. For a longer dwell time, the dispersoids remained approximately the same size but increased in volume fraction and density. Increasing the heating rate did not significantly change the dispersoid size, volume fraction or density. The dispersoids size and number density was also studied as a function of distance through a number of grains with the interplay of nucleation, growth and coarsening discussed. Both α-Al(FeCr)Si and α'-AlCrSi dispersoids were found to exist with a variety of morphologies while the α'-AlCrSi dispersoids were found to have a larger effective diameter.

Cement-based materials are of importance in the construction of geothermal wells and high-temperature oil and gas wells. These materials fill the annulus between the well casing and the rock forming a protective layer, known as sealant, which is used primarily to secure and support the casing inside the well. In addition it prevents entry of unwanted fluids into the well and communication between formation fluids at different levels. These cement based sealants need to perform for many years at high temperatures and in severe chemical environments; conditions which can cause the material of the well-casing to degrade resulting in reduced strength and increased permeability. The aim of this study is to develop new materials which will have the potential properties (high strength and low permeability) for use as sealants in geothermal and deep, hot oil wells. In order to do this special cement slurries, based on the CaO−Al2O3−SiO2−H2O (CASH) hydroceramic system, have been synthesised over the temperature range 200 to 350 °C (i.e. the typical working temperature of these wells). The additives used in these cement slurries are silica flour and alumina. A detailed description of a suite of novel hydroceramic compositions over the temperature range 200 to 350 °C is given. X-ray diffraction has been used to determine the mineralogical composition and Rietveld refinement to quantify the known phases present at different temperatures. In addition the chemistry of some of the major phases present has been examined using electron probe microanalysis. Scanning electron microprobe and simulation software have been employed to study the crystal shape of these major minerals. The engineering properties of the hydroceramic materials are very important. A study of the compressive strength and permeability has been carried out over a range of temperature (200 to 350 °C). In addition permeability has been calculated using simulation software and the results compared with experimental values. Hydroceramic formulations with excellent strength and permeability measurements have been found. Some of these formulations have been tested for durability under simulated well conditions. These materials have been immersed into different brines for a certain period of time at temperatures between 200 to 300 °C. Some preliminary results regarding the changes in mineralogy in these samples are presented in this thesis. These experiments have been carried out at the Synchrotron Radiation Source (SRS) using tomographic energy-dispersive diffraction imaging (TEDII).