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Seyed Hamidreza Azami

The course focus is on learning sedimentology in the field through practical experience. Students will learn to describe sedimentary structures and geometries in the field and link the new knowledge directly to the theory from the class room. Modern deposits from near-shore, fluvial and slope processes are investigated and used to discuss the influence of climatic zones on facies models and interpretation of e.

Well exposed outcrops of Mesozoic to Cenozoic rocks from fluvial to coastal and shallow shelf deposits allows for investigation and discussion of sedimentary processes and deposition patterns, facies models, geometries, heterogeneities, stacking patterns laterally and vertically. The link between modern and ancient deposits is a key part of methods development in sedimentology and is used actively in this course.

The course consists of alternating lectures, seminars and fieldwork. Lectures will provide background information for the current state of debate and students will be expected to critically assess published facies models and interpretations in seminars. The fieldwork will focus on gaining practical experience with description and interpretation of sedimentological data. The data collected in the field will be used to discuss published models and interpretations. Field excursions will be carried out partly as daytrips in the area near Longyearbyen and partly as overnight excursions to other areas in order to have access to the full range of sedimentary environments available.

Knowledge Upon completing the course, the students will: Have an advanced understanding of the origin, use and limitations of facies models used in sedimentological analyses. Skills Upon completing the course, the students will: Be able to identify and describe sedimentary characteristics for modern sedimentary environments and use the understanding of sedimentary processes, deposits and geometries to establish own facies models for sedimentary environments typical for the Arctic. Be able to analyse sedimentary facies and architecture in outcrops of any age and use theoretical knowledge to discuss alternative models.

Sedimentology & Stratigraphy

However, some beds coals are sufficiently organic-rich to be sources of biogenic and thermogenic methane discovered in numerous seeps. Reservoir-quality porosities and permeabilities are identified in a few delta front and turbidite sandstones of Sequences II and III, although zeolite, clay, and quartz diagenesis has destroyed most potential sandstone reservoirs.

The overall hydrocarbon potential of the basin is moderately low. Several requirements f or commercial accumulations of hydrocarbons, however, probably exist locally within and adjacent to the basin. Three speculative petroleum systems are identified. The first includes the southern part of the basin near the border with the Mesozoic Klamath Mountains and is related to a proposed subduction zone maturation mechanism along thrust faults. The second is centered in the northern part of the study area and may be associated with basin-center gas in an overpressured zone.

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The third occurs near the eastern border of the basin where maturation is related to local heating by sills and migration of hydrothermal fluids associated with mid- Tertiary volcanism in the Western Cascade arc. CVista PdfCompressor 4. Ryu, In-Chang. Laboratory studies of the development of an isotropic crystal structure and the flow properties of ice. Studies in devonian faunas Pt. The application of numerical models to the problems of meteorological analysis and prognosis over the Southern Hemisphere. The relationship between structure, gold mineralisation and intrusive events at Stawell, Victoria.

The tectonic and thermal evolution of the Murchison Basin, New Zealand: an apatite fission track study. Neoproterozoic oceans and climate change - Insights from interglacial carbonates, South Australia. Mineralogy, geochemistry and origin of the Kalgoorlie gold deposits, Western Australia [Download the full text from University of Melbourne ePrints Repository].

Geology of the Dookie district, Victoria. Mineralogy and geochemistry of the Mt Charlotte ore environment, Kalgoorlie. Evaporite sedimentology and sulphide mineralisation of the lower devonian Buchan Caves limestone of Buchan and Bindi, Eastern Victoria. The palaeoenvironmental and palaeoceanographical evolution of the Batesford region Victoria, and associated facies and biofacies transitions during the miocene. Stratigraphy and palaeoenvironmental evolution of Oligocene to Pliocene marine strata in the Murray Basin, Victoria, southeast Australia.

The geology of the area north of Mt Timbertop, Mansfield, Victoria. Geology of the Mt Camel range greenstone belt. Geology and mineralisation of three dykes in the Woods Point dyke swarm. The mapping of joints and fractures : an analysis of the jointing and mapping in the McKenzie Falls region and mapping fractures automatically using digital image analysis. The Stratigraphic, structural, alteration and rock magnetic variations across a basalt-high, Kewell, western Victoria.

Numerical analysis of the morphological features of plkeistocene podocopida from the Port Fairy calcarenite. The observation of fault gouge in laboratory see-through experiments and natural conditions in Wattle Gully mine, Chewton, Victoria.



Sedimentology, stratigraphy and structure of the Grampians group in the Northwestern Black Range. The geology of the Rokewood-Dereel area, and the application of Landsat TM data to groundwater investigations in the newer volcanics province of Western Victoria. Petrology of the Panton and McIntosh layered intrusions, Western Australia, with particular reference to the genesis of the Panton Chromite deposits.

Structural and metamorphic evolution of two proterozoic terrains: southeastern Anmatjira Range central Australia and Jetty Peninsula east Antarctica. Geologic and geomorphic applications of aster satellite imagery, Northern Flinders Ranges, South Australia. Structural analysis of the Mallacoota beds Pt.

Experimental deformation of ice-mica multilayers. An investigation into the current detectability of tropical cyclone TC trends in the Australian region. Geology of the central Howqua River region. Controls on high-grade mineralisation associated with the Hangingwall Reefs, Stawell, western Victoria.

A climatology of south eastern Australian frontal structures, developed with the use of compositing techniques. The geology of the central Howqua region. Genesis of gold-sulphide mineralisation in metaboninitic rocks.

The petrology and platinum-group element geochemistry of the Munni Munni and Mount Sholl layered mafic-ultramafic intrusions of the west Pilbara Block, Western Australia 2 vols. The sedimentology, stratigraphy and structure of the Grampians group, Mount Arapiles, Western Victoria. The sand-box modelling of accretionary wedges. The weather and climate of Australia at the last glacial maximum. Physical and chemical influences of tidal activity on groundwater in a coastal aquifer: implications for major ion and trace metal behavior.

Biogeochemical arsenic cycling in the hypothermal acid-sulfide springs at Waiotapu, New Zealnd: Implications for the evolution of arsenic resistance. The geochemistry of sulphur, selenium, tellurium, mercury, thallium and bismuth- their determination by thermal neutron activation analysis and their geochemical significance.

The structural geology of the ordovicaian rocks of the Southern Brisbane Ranges, Victoria, Australia. The late proterozoic iron formations and glaciogenic sediments of the Cornish Well area, Olary, South Australia.

Technicien supérieur Géologue Propecteur

Lead zinc mineralisation of the Wonawinta deposit, Central N. The geology and petrology of the lower Devonian Buchan group, Victoria. Text and appendices. Characterising the Zonally asymmetric features of the Southern Hemisphere extratropical circulation and their influence on regional climate variability. Experimental investigations of the flow of ice Jahnke, F. Structural geology of the Morrison area.

Application of digital computers to weather analysis and forecasting and to problems of the Antarctic water budget. A spectral study of the transient atmospheric structure : a comparison of observational and model generated statistics. The use of biogeochemistry to reflect the position of mineralisation in the auriferous slate belt in central Victoria. Investigation of magnetite origin and distribution in the Broken Hill area, with a view to aeromagnetic interpretation. Hydrothermal alteration and lithogeochemistry of the Kewell and Wallup prospects and their comparison with the Magdala gold, Stawell, Victoria.

The volcano-sedimentary and structural evolution of the Wildwood prospect, Western Lachlan Orogen.

The Eocene to Oligocene palaeoenvironmental and palaeoceanographic evolution of the Gippsland basin: Through foraminiferal analysis. Aspects of the metamorphism, structure and geochronology of high-temperature granulite-facies terranes, with emphasis on the Rauer Group, east Antarctica.

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  • Sedimentology and stratigraphy of the Carboniferous Donegal Basin.

Mineralisation and diagenesis of upper devonian carbonates on the Barbwire Terrace, Canning Basin, W. Some patterns of southern hemisphere cyclogenesis, cyclone tracks and cyclolysis and their relations to climatic variables and Victorian rainfall. Metamorphic and tectonic studies of granulite facies rocks from the Bunger Hills, East Antarctica.

Insights into the nanoscale formation of fission tracks in solids and low temperature thermochronology study of the Archaean Slave Province, Northwest Territories, Canada. The geology of the Murray River in the Hattah Lakes area and relationship to river patterns and soil development. Hydrothermal alteration at Bronzewing Gold Mine and equilibrium thermodynamic modelling of alteration.