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  • 1
    Call number: 9/M 04.0316
    In: Geological Society special publication
    Description / Table of Contents: Content: Exhumation of the North Atlantic margin: introduction and background, A G Dore, J A Cartwright, M S Stoker, J P Turner and N White Present and past influence of the Iceland Plume on sedimentation, S M Jones, N White, B J Clarke, E Rowley and K Gallagher Timing and mechanisms of North Atlantic Cenozoic uplift: evidence for mantle upwelling, M Rohrman, P A Van Der Beek, R D Van Der Hilst and P Reemst Paleocene initiation of Cenozoic uplift in Norway, S B Nielsen, G E Paulsen, D L Hansen, L Gemmer, O R Clausen, B H Jacobsen, N Balling, M Huuse and K Gallagher A structural transect between the central North Sea Dome and the South Swedish Dome: Middle Jurassic-Quaternary uplift-subsidence reversal and exhumation across the eastern North Sea Basin, O Graversen Cenozoic inversion and uplift of southern Britain, D J Blundell Landforms and uplift in Scandinavia, K Lidmar-Bergstrom and J O Naslund Pattern and timing of the post-Caledonian denudation of northern Scandinavia constrained by apatite fission-track thermochronology, B W H Hendriks and P A M Andriessen Along-slope variation in the late Neogene evolution of the mid-Norwegian margin in response to uplift and tectonism, D Evans, S McGiveron, Z Harrison, P Bryn and K Berg Reconstructing the erosion history of glaciated passive margins: applications of in situ produced cosmogenic nuclide techniques, A P Stroeven, D Fabel, J Harbor, C Hattestrand and J Kleman The thermotectonic development of southern Sweden during Mesozoic and Cenozoic time, C Cederbom Neogene uplift and erosion of southern Scandinavia induced by the rise of the South Swedish Dome, P Japsen, T Bidstrup and K Lidmar-Bergstrom Cenozoic uplift and denudation of southern Norway: insights from the North Sea Basin, M Huuse Tectonic impact on sedimentary processes during Cenozoic evolution of the northern North Sea and surrounding areas, J I Faleide, R Kyrkjebo, T Kjennerud, R H Gabrielsen, H Jordt, S Fanavoll and M D Bjerke Scotland's denudational history: an integrated view of erosion and sedimentation at an uplifted passive margin, A Hall and P Bishop Cenozoic evolution of the Faroe Platform, comparing denudation and deposition, M S Andersen, A B Sorensen, L O Boldreel and T Nielsen Late Neogene development of the UK Atlantic margin, M S Stoker Quantifying exhumation from apatite fission-track analysis and vitrinite reflectance data: precision, accuracy and latest results from the Atlantic margin of NW Europe, P F Green, I R Duddy and K A Hegarty Sonic velocity analysis of the Tertiary denudation of the Irish Sea basin, P D Ware and J P Turner The Post-Variscan thermal and denudational history of Ireland, P A Allen, S D Bennett, M J M Cunningham, A Carter, K Gallagher, E Lazzaretti, J Galewsky, A L Densmore, W E A Phillips, D Naylor and C S Hach Prediction of the hydrocarbon system in exhumed basins, and application to the NW European margin, A G Dore, D V Corcoran and I C Scotchman Geological and geochemical consequences of basin exhumation, and commercial implications, L C Price Diagenesis and fluid flow in response to uplift and exhumation, J Parnell Uplift-related hydrocarbon accumulations: the release of natural gas from groundwater, B Cramer, S Schlomer and H S Poelchau Depressurization of hydrocarbon-bearing reservoirs in exhumed basin settings: evidence from Atlantic margin and borderland basins, D V Corcoran and A G Dore
    Type of Medium: Monograph available for loan
    Pages: 494 S. , Ill., graph. Darst., Kt.
    ISBN: 1862391122
    Series Statement: Geological Society special publication 196
    Classification:
    Deposits
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Description / Table of Contents: Northwest Europe has undergone repeated episodes of exhumation (the exposure of formerly buried rocks) due to such factors as post-orogenic unroofing, rift-shoulder uplift, hotspot activity, compressive tectonics, eustatic sea-level change, glaciation and isostatic readjustment. The main observational legacy of this exhumation around the North Atlantic is preserved in the comparatively young (Mesozoic and Cenozoic) geological record of this region. Despite a rapid increase in the understanding of the exhumation of this area, there are still many unknowns: the relative intensity of the various phases and their geographical variation; mechanisms of uplift; primary causes of exhumation. Tied to these problems is the larger-scale question of whether the circum-North Atlantic is unique or whether its behaviour is typical for passive margins. There have been several attempts in recent years to bring together researchers to address these questions, but these have often focused on one particular geographical area or one particular exhumation phase. Before an integrated story can emerge, disciplines that have traditionally remained apart need to come together: geomorphology and offshore seismic interpretation; Palaeogene and Neogene studies; Scandinavian and British-Irish research schools. This volume represents a first step in this direction by providing an inter-disciplinary set of studies over a wide latitudinal range of the NW European margin. The studies presented here are based on a variety of techniques that have been employed to address the main concerns of North Atlantic exhumation history, including timing, mechanisms and the sedimentary response of the continental margin. The 25 papers presented in this volume have
    Pages: Online-Ressource (494 Seiten)
    ISBN: 1862391122
    Language: English
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  • 3
    Publication Date: 2003-08-02
    Description: Reelin is an extracellular protein that is crucial for layer formation in the embryonic brain. Here, we demonstrate that Reelin functions postnatally to regulate the development of the neuromuscular junction. Reelin is required for motor end-plate maturation and proper nerve-muscle connectivity, and it directly promotes synapse elimination. Unlike layer formation, neuromuscular junction development requires a function of Reelin that is not mediated by Disabled1 or very-low-density lipoprotein receptors and apolipoprotein E receptor 2 receptors but by a distinct mechanism involving its protease activity.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Quattrocchi, Carlo C -- Huang, Cheng -- Niu, Sanyong -- Sheldon, Michael -- Benhayon, David -- Cartwright, Joiner Jr -- Mosier, Dennis R -- Keller, Flavio -- D'Arcangelo, Gabriella -- New York, N.Y. -- Science. 2003 Aug 1;301(5633):649-53.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉The Cain Foundation Laboratories, Houston, TX 77030, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/12893944" target="_blank"〉PubMed〈/a〉
    Keywords: Action Potentials ; Animals ; Axons/metabolism ; Cell Adhesion Molecules, Neuronal/genetics/metabolism/pharmacology/*physiology ; Culture Media, Conditioned ; Diaphragm/innervation ; Extracellular Matrix Proteins/genetics/metabolism/pharmacology/*physiology ; LDL-Receptor Related Proteins ; Mice ; Mice, Neurologic Mutants ; Microscopy, Confocal ; Microscopy, Electron ; Motor Endplate/ultrastructure ; Motor Neurons/metabolism ; Muscle, Skeletal/innervation ; Mutation ; Nerve Tissue Proteins/genetics/metabolism ; Neuromuscular Junction/*growth & ; development/metabolism/*physiology/ultrastructure ; Receptors, LDL/genetics/metabolism ; Receptors, Lipoprotein/genetics/metabolism ; Schwann Cells/metabolism ; Serine Endopeptidases ; Serine Proteinase Inhibitors/pharmacology ; Sulfones/pharmacology ; Synapses/*physiology/ultrastructure
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2004-03-27
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Quattrocchi, Carlo C -- Huang, Cheng -- Niu, Sanyong -- Sheldon, Michael -- Benhayon, David -- Cartwright, Joiner Jr -- Mosier, Dennis R -- Keller, Flavio -- D'Arcangelo, Gabriella -- New York, N.Y. -- Science. 2004 Mar 26;303(5666):1974.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/15044784" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 5
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    In:  Geological Society Special Publication 216: 323-334.
    Publication Date: 2003-01-01
    Description: New multi-beam sonar and seismic data collected in Lake Superior document the wide-spread development of lake-floor rings in fine-grained lake-floor sediments. The multi-beam images reveal that the rings develop as connected clusters and that individual rings have an irregular polygonal appearance. High-resolution seismic data collected with a 28 kHz echo sounder reveal extensive fracturing and faulting in the glacio-lacustrine sediments below the lake-floor. Displacement on the faults is typically normal with throws of less than 50 cm. Three styles of faulting are recognized: (a) monoclinal flexure; (b) graben-like; and (c) conjugate. Zones of acoustic blanking below the faults may be associated with de-watering and mobilization of the sediments. Lateral thickness variation in some horizons suggests that fault and fracture development is linked with lateral movement of sediment. Piston cores collected near lake-floor rings show well-developed fractures and micro-faults, suggesting that fracturing and faulting occurs on a wide range of scales. The seismic and lithological characteristics of the glacio-lacustrine section are similar to those of sediments in which Polygonal Fault Systems (PFS) have been described. This suggests that the rings in Lake Superior may be the surface expression of PFS in the near-surface sediments.
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  • 6
    Publication Date: 2003-01-01
    Description: This paper documents normal fault sets observed in chalks exposed in widely separated localities in the UK and France. These faults are characterized by having a wide range of strikes at any one locality, are developed entirely within the chalk succession and do not seem to interconnect to deeper or shallower structures. These structures may result from two different mechanisms: (1) complex polyphase deformational histories involving contrasting stress states; or (2) a single deformational phase in which the faults develop to accommodate compactional strains. Evidence is presented from microstructural and petrographic data to support the latter interpretation. In particular, the association of calcite and marcasite mineralizations with fracture surfaces and fault zones and textural observations relating flint occurrence to early fault formation point towards fault propagation at a very early stage of burial and compaction of the chalky sediments. An analogy is drawn between these outcrop-scale structures and polygonal fault systems at a larger scale recognised from seismic observations of chalk sequences deposited at passive continental margins. The origin of these structures may be related to syneresis at an early stage of deformation followed by pressure solution phenomena that may reactivate this early-inherited polygonal fault pattern until the present day.
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  • 7
    Publication Date: 2002-01-01
    Description: Since consolidation during the Caledonian and Variscan orogenies, NW Europe has undergone repeated episodes of exhumation (the exposure of formerly buried rocks) as a result of such factors as post-orogenic unroofing, rift-shoulder uplift, hotspot activity, compressive tectonics, eustatic sea-level change, glaciation and isostatic readjustment. Modern measurement techniques, such as apatite fission-track analysis, have helped to establish useful denudation chronologies for this entire time span. However, the main observational legacy of exhumation around the North Atlantic is preserved in the comparatively young (Mesozoic and Cenozoic) geological record of this region. This is clearly reflected by the unifying theme of this volume, which documents evidence for the widespread uplift and emergence of large sections of the North Atlantic margin in Cenozoic time. All students of NW European geology are aware of the compelling palaeogeographical evidence for the transition at the end of the Cretaceous from shelf seas and low-relief landmasses to an area dominated by highlands and newly emergent landmasses, flanked by shelves dominated by rejuvenated clastic deposition. Similarly, it is also widely known that the highlands of Norway and Scotland do not represent the original Caledonian mountain range but must be instead a product of late emergence or uplift. The Cenozoic uplift of Fennoscandia in particular has a long history of study. It is arguably one of the oldest debates in the history of systematic geology and featured prominently in Lyell's Principles of Geology (Lyell 1830-1875). All of this early work was, of course, based on onshore observations. By the late ... This 250-word extract was created in the absence of an abstract.
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  • 8
    Publication Date: 2001-04-24
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 9
    Publication Date: 2004-04-26
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 10
    Publication Date: 2002-09-01
    Print ISSN: 0938-0108
    Electronic ISSN: 1875-0494
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Natural Sciences in General , Technology
    Published by Springer
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