4 edition of Neotectonics and Quaternary Fault-reactivation in Europe"s Intraplate Lithosphere found in the catalog.
August 4, 2005 by Elsevier Science .
Written in English
|Contributions||S.A.P.L. Cloetingh (Editor), T.G.M. Cornu (Editor)|
|The Physical Object|
|Number of Pages||280|
Hampel et al.[, hereinafter Ha15] recently commented on our study [Steffen et al., a], which investigates the effect of stress and fault parameters on fault slip magnitude and activation time during a glacial cycle using a newly developed two‐dimensional glacial isostatic adjustment (GIA)‐fault model [Steffen et al., b].In summary, Ha15 criticize the following parts of our Cited by: 2. The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben (German: Oberrheinische Tiefebene, Oberrheinisches Tiefland or Oberrheingraben, French: Vallée du Rhin) is a major rift, about kilometre-long ( mi) and on average kilometre-wide (31 mi), between Basel in the south and the cities of Frankfurt/Wiesbaden in the north. Its southern section straddles the border between France. a theory in geology: the lithosphere of the earth is divided into a small number of plates which float on and travel independently over the mantle and much of the earth's seismic activity occurs at the boundaries of these plates. Divergent Boundary. n plate tectonics, a divergent boundary or divergent plate boundary (also known as a.
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Buy Neotectonics and Quaternary Fault-reactivation in Europe's Intraplate Lithosphere: NHBS - Edited By: SAPL Cloetingh and TGM Cornu, Elsevier. TY - BOOK. T1 - Neotectonics and Quaternary fault-reactivation in Europe's intraplate lithosphere. AU - Cloetingh, S.A.P.L.
AU - Cornu, T. PY - Y1 - M3 - Book. BT - Neotectonics and Quaternary fault-reactivation in Europe's intraplate lithosphere. PB - Elsevier.
CY - Vrije Universiteit, Dept. of Tectonics, Amsterdam. ER -Cited by: 5. Neotectonics and Quaternary fault-reactivation in Europe's intraplate lithosphere. Amsterdam ; Boston: Elsevier, (OCoLC) Document Type: Book: Neotectonics and Quaternary Fault-reactivation in Europes Intraplate Lithosphere book Authors / Contributors: Sierd Cloetingh; T M G Cornu.
Late Quaternary evolution of the Feldbiss Fault (Roer Valley Rift System, the Netherlands) based Neotectonics and Quaternary Fault-reactivation in Europes Intraplate Lithosphere book trenching, and its potential relation to glacial unloading.
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The type of intraplate magmatism appears to be related to Neotectonics and Quaternary Fault-reactivation in Europes Intraplate Lithosphere book thickness of the lithosphere.
Unlike oceanic transform faults where large horizontal movements have occurred, reactivated zones of weakness in continents usually appear to have been the sites of only relatively small displacement.
over, if a previous fault pattern is present, fault reactivation rather than formation of new faults is frequently observed, even if the consecutive deformation episodes are not coaxial, in. Lateral variations in the properties of the downgoing plates largely control the collision mode in the Carpathians and the post-collisional evolution of the entire system.
the Iberian lithosphere during the Alpine deformations. The seismogenic thickness bounds the seismic activity in the upper–middle crust, and the decreasing crustal strength from the Duero Basin towards the Madrid Basin is related to a parallel increase in Plio–Quaternary deformations and seismicity.
Rock deformation caused by the structure of the earth (e.g., folds, faults, joints, cleavage) is often the only kind of tectonic deformation considered by geological manuals, giving the impression that areas devoid of such type of deformation are “tectonically stable.”.
neotectonics Download neotectonics or read online here in PDF or EPUB. Neotectonics And Quaternary Fault Reactivation In Europe S Intraplate Lithosphere. Author by: Sierd Cloetingh Environmental Tectonics research program ENTEC has led to new insights into the strength distribution of Europe's intraplate lithosphere, and its.
The lithosphere of the Pannonian Basin is a particularly sensitive recorder of changes in lithospheric stress induced by near-field intraplate and far-field plate boundary processes.
response to. The NW European lithosphere has undergone a polyphase evolution with an intensive interplay of upper mantle thermal perturbations and stress-induced intraplate deformation. A number of recent findings point to an important role of lithospheric folding in thermally weakened lithosphere of the northwestern European by: Quantifying the links between lithosphere dynamics, neotectonics and surface and climatic processes is a key target, through the development of numerical models, making use of datasets that cover different aspects of these phenomena at a wide range of by: We focus on lithosphere memory and neotectonics with special attention to the thermo-mechanical structure of the lithosphere, mechanisms of large-scale intraplate deformation, Late-Neogene anomalies in subsidence and uplift, and links with surface processes and topography by: Research, incorporating iterative data interactive modelling, focuses on the lithosphere memory and neotectonics, with special attention on the thermo-mechanical structure of the lithosphere, mechanisms controlling large-scale plate boundary and intraplate deformations, anomalous subsidence and uplift, and links with surface processes and topography : S.
Cloetingh, P. Ziegler. Interplay of lithosphere folding and plume impingement on the continental intraplate lithosphere occurred probably almost simultaneously in late Neogene times in the Northwestern European foreland.
The Hellenic orogen that extends into the Aegean area and Turkey is a composite of three orogenic Cimmerian orogenic belt, which includes the Rhodope, Serbomacedonian, Circum Rhodope, Axios, and Pelagonian zones in Greece and the Sakarya, Kirklareli, Sinop, and Bayburt zones in Turkey (Şengör et al., ; Okay et al., ), represents an internal orogenic belt created in pre.
Neotectonics and quaternary fault-reactivation in Europe's intraplate lithosphere () Plio-Quaternary Volcanism in Italy () Late quaternary environmental change (). Abstract. Thanks to a continuous effort for unravelling geological records since the early days of coal and petroleum exploration and water management, the architecture and chrono-litho-stratigraphy of most sedimentary basins has been accurately described by means of conventional geological and geophysical studies, using both surface (outcrops) and subsurface (exploration wells Cited by: Unfortunately, this book can't be printed from the OpenBook.
If you need to print pages from this book, we recommend downloading it as a PDF. Visit to get more information about this book, to buy it in print, or to download it as a free PDF. Neotectonics and quaternary fault-reactivation in Europe's intraplate lithosphere, S.
Fault reactivation in brittle-viscous wrench systems - dynamically scaled analogue models and application to the Rhine-Bresse Transfer Zone, in: Neotectonics and Quaternary Fault-reactivation in Europe's Intraplate Lithosphere (eds.
Cloetingh and T. Cornu), pp.Elsevier, Amsterdam. Ustaszewski, K., M.E. Schumacher, and S.M. Schmid, The controls on seismicity and fault reactivation in stable intraplate crust located far from active plate boundaries are poorly understood.
The southern Australian continental margin has been undergoing mild levels of deformation over the past ~10Myr, manifested today by high levels of seismicity for a stable intraplate region. Widespread magmatism developed in the Mediterranean and surrounding regions during the Neogene to Quaternary (Wilson and Downes, ; Wilson and Bianchini, ; Lustrino, ; Wilson and Patterson, ; Harangi et al., ).A large variation of magmatic rocks was produced that can be roughly divided into orogenic (calc-alkaline, potassic, and ultrapotassic) and anorogenic (alkaline sodic.
In: Cloetingh SAPL, Cornu TGM (eds) Neotectonics and Quaternary fault-reactivation in Europe’s intraplate lithosphere: Oxford, Pergamon, Oxford, pp – Google Scholar Michon L, Van Balen RT, Merle O, Pagnier HJM () The Cenozoic evolution of the Roer Valley Rift System integrated at a European by: Due to its low rigidity and the intraplate compression concentrated in the thin elastic core of the crust, the area exhibits large-scale bending manifested in Quaternary subsidence and uplift anomalies that control the morphology within the basin system (Horváth and Cloetingh, ).
Thermomechanical models demonstrate that this important transition in the mode and distribution of intraplate deformation can be explained by a strength reversal resulting from the combined effects of changes in Moho depth due to the transition from rifting to inversion and heating by mantle by: Neotectonics and Quaternary Fault-reactivation in Europe's Intraplate Lithosphere eBook Well eBook Mission theology: An introduction (Studia Instituti Missiologici Societatis Verbi Divini) eBook.
Toutes les informations de la Bibliothèque Nationale de France sur: Failles (géologie). The study of Quaternary fluvial erosion through a new method for measuring incision shows that the drainage basins of the HEDs record greater amounts of base level fall during Quaternary times.
This implies that differential uplift is responsible for the large‐scale relief development of the Armorican Massif during the Quaternary. The Caucasus Mountain System (Fig.
1) is the part of the largest Alpine-Himalayan collision zone, stretching out kilometers across Eurasia from the Western Mediterranean to the Western geological terms, it is represented by huge area of the Trans-Eurasian Belt (TEB) of Late Cenozoic activation, which was formed after the closure of the Mesozoic-Early Cenozoic ocean Cited by: 1.
Introduction  The nature of intraplate stress fields in continental lithosphere and its relationship to plate tectonic driving forces has been subject to a large number of observational [e.g., Zoback, ; Van der Pluim et al., ] and modeling studies [e.g., Richardson et al., ; Cloetingh and Wortel, ; Bada et al., ; Golke and Coblentz, ].Cited by: Nowadays, the Armorican Massif is an intraplate domain of the western European lithosphere, which corresponds to the extended foreland of the Pyrenees and the Alps [Ziegler et al., ].
The western European lithosphere is currently under compression, with a roughly constant horizontal maximumCited by: We present a neotectonic model of ongoing lithosphere deformation and a corresponding estimate of long‐term shallow seismicity across the Africa‐Eurasia plate boundary, including the eastern Atlantic, Mediterranean region, and continental Europe.
GPS and stress data are absent or inadequate for the part of the study area covered by by: Water is not only important in causing the rheological contrast between the lithosphere and the asthenosphere in intraplate settings, but it also has a significant role at convergent margins.
Abstract. The isostatic adjustment of the solid Earth to the glacial loading (GIA, Glacial Isostatic Adjustment) with its temporal signature offers a great opportunity to retrieve information of Earth’s upper mantle to the changing mass of glaciers and ice sheets, which in turn is driven by variations in Quaternary by: Quaternary deformation in SE Sicily: Insights into the life and cycles of forebulge fault systems Cenozoic deformation Europe Pleistocene geomorphology ground water Hyblean Plateau faults Italy tectonics Quaternary neotectonics Southern Europe Syracuse Italy Cited by: 8.
A lithosphere (Ancient Greek: λίθος [lithos] for "rocky", and σφαίρα [sphaira] for "sphere") is the rigid, outermost shell of a terrestrial-type planet, or natural satellite, that is defined by its rigid mechanical Earth, it is composed of the crust and the portion of the upper mantle that behaves elastically on time scales of thousands of years or greater.
Smith, R. B.,Structural Style and Deformation Pdf Intraplate Tectonics of the Basin-Range: Inferences for Thermal and Mechanical Properties of an Extending Lithosphere, International Un.
of Geodesy and Geophysics (IUGG), XVIII General Assembly, ICL Inter-Un. Commission on the Lithosphere, Program and Abstracts, Buy Developments and Interactions of the Precambrian Atmosphere, Lithosphere and Biosphere on FREE SHIPPING on qualified orders.ebook In addition to being caused by deep Earth phenomena, Dr Brandes and his colleagues are uniquely ebook with the load that ice-sheets apply to continental plates, and how the melting of the ice can trigger earthquakes.
Although it is well-known that the climate is warming due to human influences, causing ice to melt in cold regions, the.