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  • 1
    Call number: 9/M 10.0377
    In: Special publication ... of the International Association of Sedimentologists
    Description / Table of Contents: For several decades Peter Friend has been one of the leading figures in sedimentary geology and throughout that time he has helped scores of other people by supervising doctoral students, collaborating with colleagues, especially in developing countries, and selflessly sharing ideas with fellow geologists.
    Type of Medium: Monograph available for loan
    Pages: VI, 636 S.
    ISBN: 9781405179225
    Series Statement: Special publication ... of the International Association of Sedimentologists 38
    Classification:
    Sedimentology
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Blackwell Science
    Call number: AWI G1-99-0258
    Description / Table of Contents: The record of tectonic and climatic processes through geological time is held within sedimentary rocks along with evidence for the evolution of life on Earth. The study of the formation, transport and deposition of material to form sedimentary rocks and the temporal and spatial relationships between strata is a fundamental part of the Earth sciences. Sedimentology and Stratigraphy aims to provide students who are starting to study geology at university level with an introduction to the continuum of scales of observation and interpretation which lie between the formation of a grain of sand and a fill of a sedimentary basin. In the first section of this book, the author treats the formation and transport of sediment in a largely descriptive manner and introduces the concepts of environments and facies. The full spectrum of continental and marine sedimentary environments is then covered in a series of chapters which consider the depositional processes and products which may be considered to be characteristic for each setting. In the final part, the principles of stratigraphy and interpretation of the fill of sedimentary basins are considered. The text and illustrations are designed to be accessible to those completely new to the subject whilst at the same time the book covers the concepts and terminology used in more advanced work.
    Type of Medium: Monograph available for loan
    Pages: X, 355 Seiten , Illustrationen
    Edition: First published
    ISBN: 0632035781
    Language: English
    Note: Contents: Preface. - 1 Introduction: sedimentology and stratigraphy. - 1.1 Sedimentology and stratigraphy in Earth sciences. - 1.2 Stratigraphy and sedimentology. - 1.3 See the world in just one grain of sand. - 1.4 Processes and products. - 1.5 Sedimentary environments and facies. - 1.6 Modem and ancient sedimentary environments. - 1.7 Geographical distribution of environments and facies. - 1. 8 Changing environments and facies through time. - 1.9 The stratigraphic record and geological time. - 1.10 Earth history, global tectonics, climate and evolution. - 2 Terrigenous clastic sediments: gravel, sand and mud. - 2.1 The components of sediments and sedimentary rocks. - 2.2 Classification and nomenclature of terrigenous clastic sediments and sedimentary rocks. - 2.3 Gravel and conglomerate. - 2.4 Sand and sandstone. - 2.5 Clay, silt and mudrock. - 2.6 Description of the textures of terrigenous clastic sedimentary rocks. - 2.7 Granulometric and clast shape analysis. - 2.8 Maturity of terrigenous clastic material. - 2.9 Terrigenous clastic sediments: summary. - Further reading. - 3 Biogenic, chemical and volcanogenic sediments. - 3.1 Limestone. - 3.2 Volcanic and volcaniclastic rocks. - 3.3 Evaporite minerals. - 3.4 Cherts. - 3.5 Phosphates. - 3.6 Sedimentary ironstone. - 3.7 Carbonaceous (organic) deposits. - 3.8 The description of sedimentary rocks in hand specimen. - 3.9 Examination of sedimentary rocks under the microscope. - Further reading. - 4 Processes of transport and sedimentary structures. - 4.1 Transport media. - 4.2 The behaviour of fluids and particles in fluids. - 4.3 Flows, sediment and bedforms. - 4.4 Waves. - 4.5 Sedimentary structures in sand-mud mixtures. - 4.6 Mass flows. - 4.7 Mudcracks. - 4.8 Erosional sedimentary structures. - 4.9 Sedimentary structures and sedimentary environments. - Further reading. - 5 Environments and facies. - 5.1 Interpreting past depositional environments. - 5.2 The concept of 'facies'. - 5.3 Distribution of palaeoenvironments in time and space. - 5.4 Palaeocurrents. - 5.5 Provenance. - 5.6 Graphic sedimentary logs. - 5.7 Facies and environments: summary. - Further reading. - 6 Continents: sources of sediment and environments of deposition. - 6.1 From source of sediment to formation of strata. - 6.2 The formation of mountains and hills. - 6.3 Continental climatic regimes. - 6.4 Surface processes. - 6.5 Weathering processes. - 6.6 Erosion and transport. - 6.7 Factors which influence erosion rates. - 6.8 Continental environments of deposition. - 6.9 Continental environments: summary. - Further reading. - 7 Glaciers and ice caps. - 7.1 Formation of glaciers. - 7.2 Erosion by glaciers. - 7.3 Glacial deposits. - 7.4 Distribution of glacial deposits. - 7.5 Recognition of glacial deposits: summary. - Further reading. - 8 Arid continental depositional environments. - 8.1 Deserts. - 8.2 Wind in deserts. - 8.3 Water in a desert. - 8.4 Alluvial fans. - 8.5 Playa lakes. - 8.6 Life in the desert. - 8.7 Characteristics of the deposits of arid continental environments: summary. - Further reading. - 9 Rivers: the fluvial environment. - 9.1 River forms and patterns. - 9.2 Modern rivers. - 9.3 Floodplains. - 9.4 Ancient fluvial deposits. - 9.5 Palaeocurrents in fluvial systems. - 9.6 Fossils in fluvial environments. - 9.7 Soils and palaeosols. - 9.8 Recognition of fluvial deposits: summary. - Further reading. - 10 Lacustrine environments: fresh and saline lakes. - 10.1 Modern lakes. - 10.2 Morphology and processes in lakes. - 10.3 Lacustrine sediments and facies. - 10.4 Saline lakes. - 10.5 Life in lakes. - 10.6 Lake environments: summary. - Further reading. - 11 The marine realm: morphology and processes. - 11.1 Marine environments. - 11.2 Tides. - 11.3 Wave and storm processes. - 11.4 Thermo-haline currents. - 11.5 Divisions of the marine realm. - 11.6 Chemical and biochemical sedimentation in oceans. - 11.7 Ecology of the seas. - 11.8 Marine environments: summary. - Further reading. - 12 Deltas and estuaries. - 12.1 Deltas. - 12.2 Controls on deltas. - 12.3 Coarse-grained deltas. - 12.4 Delta 'cycles'. - 12.5 Post- and syndepositional effects on deltas. - 12.6 Recognition of deltaic deposits: summary. - 12.7 Estuaries. - 12.8 Recognition of estuarine deposits: summary. - Further reading. - 13 Coastlines: beaches, barriers and lagoons. - 13.1 Coastal environments. - 13.2 Morphological features of coastlines. - 13.3 Clastic coastlines. - 13.4 Carbonate coastlines. - 13.5 Arid coastlines. - 13.6 Recognition of coastal deposits: summary. - Further reading. - 14 Shallow seas. - 14.1 Sediment supply to shallow seas. - 14.2 Shallow marine clastic environments. - 14.3 Storm-dominated shallow clastic seas. - 14.4 Tide-dominated shallow clastic seas. - 14.5 Shallow marine carbonate environments. - 14.6 Carbonate ramps. - 14.7 Rimmed carbonate shelves. - 14.8 Epeiric, drowned and isolated carbonate platforms. - 14.9 Barred basins and saline giants. - 14.10 Criteria for the recognition of shelf sediments. - Further reading. - 15 Deep marine environments. - 15.1 Modem and ancient oceans. - 15.2 Deep marine mass flows. - 15.3 Submarine fans. - 15.4 Contourites. - 15.5 Pelagic and hemipelagic sedimentation. - 15.6 Other features of deep ocean sediments. - 15.7 Fossils in deep ocean sediments. - 15.8 Ancient deep ocean deposits. - 15.9 Recognition of deep ocean deposits: summary. - Further reading. - 16 Volcanic environments. - 16.1 Volcanic and volcaniclastic rocks. - 16.2 Lavas. - 16.3 Volcaniclastic rocks. - 16.4 Environments of deposition. - 16.5 Recognition of volcanigenic deposits: summary. - 16.6 Volcanic rocks in stratigraphy: flows, dykes and sills. - Further reading. - 17 Sediments into rocks: postdepositional processes. - 17.1 Post-depositional modification of sedimentary layers. - 17.2 Post-depositional physical and chemical processes. - 17.3 Nodules and concretions. - 17.4 Clastic diagenesis. - 17.5 Carbonate diagenesis. - 17.6 Post-depositional changes to evaporites. - 17.7 Diagenesis of volcaniclastic sedirnents. - 17.8 Formation of coal and hydrocarbons. - 17.9 Diagenetic processes: summary. - Further reading. - 18 Stratigraphy: concepts and lithostratigraphy. - 18.1 Stratigraphy and geological time. - 18.2 Chronostratigraphy. - 18.3 Physical stratigraphy. - 18.4 Lithostratigraphy. - 18.5 Lithostratigraphic nomenclature. - 18.6 Lithostratigraphy and environments. - 18.7 Lithostratigraphy and geological maps. - 18.8 Lithostratigraphy and correlation. - Further reading. - 19 Biostratigraphy. - 19.1 Strata and fossils. - 19.2 Fossils in stratigraphy. - 19.3 Taxa used in biostratigraphy. - 19.4 Correlating different environments. - 19.5 Biostratigraphic nomenclature. - 19.6 Biostratigraphy and chronostratigraphy. - Further reading. - 20 Dating and correlation techniques. - 20.1 Radiometric dating. - 20.2 Magnetostratigraphy. - 20.3 Other dating methods. - 20.4 Dating in the Quaternary. - 20.5 Correlation. - Further reading. - 21 Sequence stratigraphy and sea level changes. - 21.1 Introduction. - 21.2 Depositional sequences and systems tracts. - 21.3 Facies patterns in depositional sequences. - 21.4 Sequences in carbonate depositional environments. - 21.5 Subdivision of depositional sequences and systems tracts: parasequences. - 21.6 Sequence stratigraphy and depositional environments. - 21.7 Practical sequence stratigraphy. - 21.8 Causes of sea level fluctuations. - Further reading. - 22 Subsurface stratigraphy. - 22.1 Seismic reflection profiles. - 22.2 Interpreting seismic reflections. - 22.3 Structural features on seismic profiles. - 22.4 Seismic facies. - 22.5 Relating seismic profiles to geological cross-sections. - 22.6 Borehole stratigraphy and sedimentology. - 22.7 Subsurface facies analysis. - 22.8 Use of borehole data. - Further reading. - 23 Sedimentary basins. - 23.1 Tectonics of sedimentary basins. - 23.2 Basins related to crustal extension. - 23.3 Basins related to subduction. - 23.4 Basins related to continen
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 3
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Analytical chemistry 45 (1973), S. 1973-1975 
    ISSN: 1520-6882
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 39 (1992), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Evidence from fusain deposits in Lower Carboniferous rocks of western Ireland indicates that a catastrophic wildfire destroyed thousands of square kilometres of Carboniferous ‘forest’. In addition to yielding large quantities of charcoal, this wildfire event resulted in increased surface water runoff which affected sedimentation in an adjacent estuarine environment where the fusain is now preserved. This is the oldest documented evidence for a catastrophic palaeowildfire and a clear example of the sedimentological effects of large-scale fires.The Lower Carboniferous (Visean) rocks in the Largymore Syncline of western Donegal, Ireland, are shallow marine sandstones, mudstones and limestones. The Upper Shalwy Beds are mudstones and cross-bedded sandstones which show bi-polar cross-stratification and mud drapes on cross-bed foresets indicating deposition in a tidal environment, probably a large estuary. In three coastal exposures a bed containing up to 20% fusain is found at the same stratigraphic horizon. The fusain is interpreted as fossil charcoal produced by palaeowildfire in a land area to the north-west. The volume of fusain present in the unit can be estimated and by comparison with charcoal production in modern wildfires it has been calculated that around 95 000 km2 (more than the present land area of Ireland) was burnt.Along with the fusain, other effects of the wildfire can be seen in the deposits, which are poorly sorted compared to the rest of the Upper Shalwy Beds and are characterized by inclined heterolithic stratification produced by the draping of underlying bedforms. These features are considered to be due to a considerably increased sediment load in the estuary, resulting from enhanced surface runoff and soil erosion due to the wildfire.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Sedimentology 52 (2005), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Climate and tectonics play important roles in controlling processes of transport and deposition on alluvial fans, but the bedrock lithology in the fan catchment area is also a significant, independent factor. Adjacent Oligo-Miocene alluvial fan deposits on the northern margin of the Ebro Basin display contrasting depositional characteristics with one dominated by the deposits of debris flows and the other by deposition from flows of water. A difference in clast compositions indicates that the two studied fans (the Nueno and San Julián fans) had contrasting bedrock lithology in their drainage basins. The proximal facies of the Nueno fan body contains matrix-supported conglomerate beds with up to 80% pebble clasts of gypsum in a matrix of gypsiferous sand, interbedded with gypsarenite beds. The drainage basin of this fan was dominated by Triassic bedrock consisting of beds of gypsum, marl and micritic limestone. The San Julián fan body comprises clast-supported, polymict conglomerate beds containing pebbles from Triassic, Cretaceous and Palaeogene limestone units that are exposed in the adjacent part of the basin margin. The interfingering of the deposits of these two fans demonstrates that they were contemporaneous. Given the consistent climate, the differences in fan depositional processes must therefore be attributed to the contrasting bedrock lithology in their drainage basins. A drainage basin consisting mainly of marl and gypsum bedrock provided sufficient fine-grained material to generate debris flows, whereas more dilute, water-lain processes dominated where the drainage basin was largely limestone strata.
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  • 6
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    In:  Geological Society Special Publication 251: 187-206.
    Publication Date: 2007-10-08
    Description: Tertiary alluvial fan deposits along the margin of the Ebro foreland basin north of Huesca, Spain, are remarkable for the range of sedimentological and tectonic features preserved within them. The fan deposits formed after the southern Pyrenean thrust front (the Guarga Thrust) was established in this area, forming steep topography at the basin margin in the mid-Oligocene. Some shortening continued during deposition of the earliest fans resulting in synsedimentary faults, folds and unconformities. Clast compositions in the fan conglomerate beds record unroofing of the thrust front and also reveal differences in bedrock provenance between adjacent, coeval fan deposits. Bedrock provenance also influenced processes of deposition, with fans built up of detritus derived from areas rich in gypsum and mudrock showing more evidence of debris-flow processes. Deposition by debris flows also dominated the smallest fan body, but the majority of the fans were the products of sedimentation from unconfined or poorly confined traction currents. These resulted in sheets of conglomerate in the more proximal areas. Within individual fan bodies the proportion of sandstone increases over a distance of up to 5 km to where the distal fan facies are seen as thin sandstone and mudstone beds. The fringes of the fan bodies interfinger with lacustrine and fluvial facies, which indicate a temperate-semi-aric palaeoclimate. Vertical aggradation of the fan deposits due to rising base level in the Ebro Basin in the Oligocene and early Miocene was followed by deep incision following a late Miocene base level-fall. This led to the partial erosion of the fan deposits and their spectacular exposure in the modern landscape.
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  • 7
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    In:  Geological Society Special Publication 191: 5-22.
    Publication Date: 2002-01-01
    Description: The volume of sediment deposited in the basins around Borneo indicates that at least 6 km of crust has been removed by erosion during the Neogene. The amount of tectonic uplift implied by this is not reflected in a large area of high mountains on the island, which has an average elevation much lower than that of the Alps or Himalayas. High weathering and erosion rates in the tropical climate of SE Asia are likely to have been an important factor governing the formation of relief in Borneo, and consequently, controlled the structural development of the orogenic belt. Very rapid removal of material by erosion prevented tectonic denudation by fauling: around Borneo there was no lithospheric flexure due to thrust loading and no true foreland basins were developed. The sediment was deposited adjacent to the orogenic belt in older, deep oceanic basins. In terms of sediment yield, the Borneo mountains are comparable in importance to mountain ranges such as the Alps or Himalayas. However, the differences in elevation and structural style suggest that mountain belts formed in regions of high erosion rates may be different from those formed in other settings and the effects of climate need to be considered to understand orogenic evolution.
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  • 8
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    In:  Geological Society Special Publication 210: 89-108.
    Publication Date: 2003-01-01
    Description: Northern Thailand is located in a structurally complex area between three major tectonic regimes, a region of extensional tectonics to the south and two major strike-slip zones, the Sagaing fault zone to the west and the Red River fault zone to the northeast. Cenozoic tectonics in northern Thailand resulted from the collision between the Indian plate and Eurasia. The continued indentation of the Indian plate into Eurasia caused polyphase extrusion of Sundaland and the movement of major strike-slip faults. The movement of these faults accompanying the regional east-west extension during Late Oligocene to Early Miocene initiated the formation of the Tertiary basins. Thirty-six major faults and forty-two intra-cratonic depositional basins in northern Thailand have been recognized and delineated using Landsat TM images. More than 70% of these basins are related to strike-slip tectonics. Five basin types have been recognized on the basis of geometric and kinematic considerations. These are fault-tip basins, pull-apart basins, fault-wedge basins, fault zone basins, and extensional basins. The opening and development of these basins was influenced by the movement of NW-trending dextral faults and NE-trending sinistral faults associated with north-south shortening and east-west extension.
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  • 9
  • 10
    Publication Date: 1991-10-01
    Print ISSN: 0743-9547
    Electronic ISSN: 1879-1832
    Topics: Geosciences
    Published by Elsevier
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