ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Keywords: Wilson Cycle ; plate tectonics
    Description / Table of Contents: Introduction --- Fifty years of the Wilson Cycle concept in plate tectonics: an overview / R. W. Wilson, G. A. Houseman, S. J. H. Buiter, K. J. W. McCaffrey and A. G. Doré / Geological Society, London, Special Publications, 470, 1-17, 25 July 2019, https://doi.org/10.1144/SP470-2019-58 --- The Classic Wilson v. Supercontinent Cycles --- The classic Wilson cycle revisited / Ian W. D. Dalziel and John F. Dewey / Geological Society, London, Special Publications, 470, 19-38, 9 February 2018, https://doi.org/10.1144/SP470.1 --- Supercontinents: myths, mysteries, and milestones / Daniel Pastor-Galán, R. Damian Nance, J. Brendan Murphy and Christopher J. Spencer / Geological Society, London, Special Publications, 470, 39-64, 8 May 2018, https://doi.org/10.1144/SP470.16 --- Supercontinents and the case for Pannotia / R. Damian Nance and J. Brendan Murphy / Geological Society, London, Special Publications, 470, 65-86, 1 March 2018, https://doi.org/10.1144/SP470.5 --- Mantle Dynamics in the Wilson Cycle --- Mantle plumes and mantle dynamics in the Wilson cycle / Philip J. Heron / Geological Society, London, Special Publications, 470, 87-103, 19 November 2018, https://doi.org/10.1144/SP470-2018-97 --- Tectonic Inheritance in the Lithosphere --- Tectonic inheritance, structure reactivation and lithospheric strength: the relevance of geological history / A. M. C. Şengör, Nalan Lom and Nurbike G. Sağdıç / Geological Society, London, Special Publications, 470, 105-136, 15 March 2018, https://doi.org/10.1144/SP470.8 --- Exploring the theory of plate tectonics: the role of mantle lithosphere structure / Philip J. Heron, Russell N. Pysklywec and Randell Stephenson / Geological Society, London, Special Publications, 470, 137-155, 1 March 2018, https://doi.org/10.1144/SP470.7 --- Potential role of lithospheric mantle composition in the Wilson cycle: a North Atlantic perspective / Pauline Chenin, Suzanne Picazo, Suzon Jammes, Gianreto Manatschal, Othmar Müntener and Garry Karner / Geological Society, London, Special Publications, 470, 157-172, 6 March 2018, https://doi.org/10.1144/SP470.10 --- Rheological inheritance: lessons from the Death Valley region, US Basin and Range Province / Rodrigo D. Lima, Nicholas W. Hayman and Elena Miranda / Geological Society, London, Special Publications, 470, 173-204, 21 May 2018, https://doi.org/10.1144/SP470.14 --- Multi-phase reactivations and inversions of Paleozoic–Mesozoic extensional basins during the Wilson cycle: case studies from the North Sea (UK) and the Northern Apennines (Italy) / Vittorio Scisciani, Stefano Patruno, Enrico Tavarnelli, Fernando Calamita, Paolo Pace and David Iacopini / Geological Society, London, Special Publications, 470, 205-243, 3 May 2019, https://doi.org/10.1144/SP470-2017-232 --- Revisiting Tuzo's question on the Atlantic --- Examining the influence of tectonic inheritance on the evolution of the North Atlantic using a palinspastic deformable plate reconstruction / Bridget E. Ady and Richard C. Whittaker / Geological Society, London, Special Publications, 470, 245-264, 19 March 2018, https://doi.org/10.1144/SP470.9 --- Role of Avalonia in the development of tectonic paradigms / J. Brendan Murphy, R. Damian Nance, J. Duncan Keppie and Jaroslav Dostal / Geological Society, London, Special Publications, 470, 265-287, 23 March 2018, https://doi.org/10.1144/SP470.12 --- Diachronous Paleozoic accretion of peri-Gondwanan terranes at the Laurentian margin / John W. F. Waldron, David I. Schofield and J. Brendan Murphy / Geological Society, London, Special Publications, 470, 289-310, 29 March 2018, https://doi.org/10.1144/SP470.11 --- Inversion of Taconian extensional structures during Paleozoic orogenesis in western Newfoundland / Shawna E. White and John W. F. Waldron / Geological Society, London, Special Publications, 470, 311-336, 6 June 2018, https://doi.org/10.1144/SP470.17 --- Tectonic inheritance at multiple scales during more than two complete Wilson cycles recorded in eastern North America / William A. Thomas / Geological Society, London, Special Publications, 470, 337-352, 9 February 2018, https://doi.org/10.1144/SP470.4 --- Late Paleozoic extensional reactivation of the Rheic–Rhenohercynian suture zone in SW England, the English Channel and Western Approaches / Andrew C. Alexander, Robin K. Shail and Brian E. Leveridge / Geological Society, London, Special Publications, 470, 353-373, 4 January 2019, https://doi.org/10.1144/SP470.19 --- Opening and Closing of Oceans --- Non-Wilsonian break-up predisposed by transforms: examples from the North Atlantic and Arctic / E. R. Lundin and A. G. Doré / Geological Society, London, Special Publications, 470, 375-392, 21 February 2018, https://doi.org/10.1144/SP470.6 --- The Jan Mayen microplate complex and the Wilson cycle / Christian Schiffer, Alexander Peace, Jordan Phethean, Laurent Gernigon, Ken McCaffrey, Kenni D. Petersen and Gillian Foulger / Geological Society, London, Special Publications, 470, 393-414, 1 February 2018, https://doi.org/10.1144/SP470.2 --- The subduction initiation stage of the Wilson cycle / Robert Hall / Geological Society, London, Special Publications, 470, 415-437, 19 February 2018, https://doi.org/10.1144/SP470.3 --- 3D numerical modelling of the Wilson cycle: structural inheritance of alternating subduction polarity / Stéphane J. Beaussier, Taras V. Gerya and Jean-Pierre Burg / Geological Society, London, Special Publications, 470, 439-461, 2 May 2018, https://doi.org/10.1144/SP470.15 --- Cratonic Basins and their place in the Wilson Cycle --- Cratonic basins and the Wilson cycle: a perspective from the Parnaíba Basin, Brazil / M. C. Daly, B. Tozer and A. B. Watts / Geological Society, London, Special Publications, 470, 463-477, 3 May 2018, https://doi.org/10.1144/SP470.13
    Pages: Online-Ressource (VI, 490 Seiten) , Illustrationen, Diagramme
    ISBN: 9781786203830
    Language: English
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Description / Table of Contents: Recent advancements in the understanding of mountain belts have focused on vertical coupling of the lithospheric layers. This volume describes the extent to which observed or inferred sub-horizontal coupling or attachment zones provide vertical kinematic linkage between rheologically distinct layers in the continental lithosphere. A common theme is whether the deformation, which partitioned differently in each layer, is linked kinematically across attachment zones and driven by flow in the deeper crust and mantle lithosphere. The papers are divided into six sections. The first analyses the extent to which mantle flow controls deformation of the overlying layers. The Vertical axis block rotations section uses geological and palaeomagnetic data to constrain the role and magnitude of basal shear across mid-crustal attachment zones. The Lower crustal flow and topography section addresses the time-dependent development of orogenic plateaux and their role in the orogenic cycle. Multiple examples of the spatial and temporal development of lithospheric coupling are given in both the Orogenic examples and Subduction examples sections. Finally, rheological constraints of vertical coupling in the lithosphere are investigated.
    Pages: Online-Ressource (344 Seiten)
    ISBN: 1862391599
    Language: English
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Description / Table of Contents: Faults and their deeper level equivalents, shear zones, are localized regions of intense deformation within the Earth. They are recognized at all scales from micro to plate boundary, and are important examples of the nature of heterogeneous deformation in natural rocks. Faults and shear zones are significant as they profoundly influence the location, architecture and evolution of a broad range of geological phenomenao The topography and bathymetry of the Earth’s surface is marked by mountain belts and sedimentary basins that are controlled by faults and shear zoneso In addition, faults and shear zones control fluid migration and transport including hydrothermal and hydrocarbon systems. Once faults and shear zones are established, they are often long-lived features prone to multiple reactivation over very large time-scales. This collection of papers addresses lithospheric deformation and the rheology of shear zones, together with processes of partitioning and the unravelling of fault and shear zone histories.
    Pages: Online-Ressource (379 Seiten)
    ISBN: 186239153X
    Language: English
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2021-11-09
    Description: Rapidly developing methods of digital acquisition, visualization and analysis allow highly detailed outcrop models to be constructed, and used as analogues to provide quantitative information about sedimentological and structural architectures from reservoir to subseismic scales of observation. Terrestrial laser-scanning (lidar) and high precision Real-Time Kinematic GPS are key survey technologies for data acquisition. 3D visualization facilities are used when analysing the outcrop data. Analysis of laser-scan data involves picking of the point-cloud to derive interpolated stratigraphic and structural surfaces. The resultant data can be used as input for object-based models, or can be cellularized and upscaled for use in grid-based reservoir modelling. Outcrop data can also be used to calibrate numerical models of geological processes such as the development and growth of folds, and the initiation and propagation of fractures.
    Description: Published
    Description: 87–98
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: N/A or not JCR
    Description: reserved
    Keywords: Laser-Scanning ; Outcrop analogues ; Reservoirs ; 04. Solid Earth::04.04. Geology::04.04.09. Structural geology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2021-11-09
    Description: Terrestrial laser scanning is used to capture the geometry of three single folded bedding surfaces. The resulting light detection and ranging (LIDAR) point clouds are filtered and smoothed to enable meshing and calculation of principal curvatures. Fracture traces, picked from the LIDAR data, are used to calculate fracture densities. The rich data sets produced by this method provide statistically robust estimates of spatial variations in fracture density across the fold surface. The digital nature of the data also allows resampling to derive fracture parameters that are more traditionally measured manually from outcrops (e.g., one-dimensional line transects of fracture spacing). The fracture statistics derived from the LIDAR data are compared with the calculated principal and Gaussian curvatures of the surface to assess whether areas of extreme curvature correlate with high-fracture density. For the folds studied, all the fracture spacing distributions showed an exponential distribution, and no significant correlation between fracture density and surface curvature was observed. This questions the validity of using curvature as a proxy for high brittle strains and highlights the need for a complete understanding of fold and fracture mechanics that include considerations of other factors including lithology, strain rate, and confining pressure, not just finite strain. The three case studies also illustrate how terrestrial laser scanning can be used to gather detailed quantitative data sets on fracture and fold distributions from outcrop analogs.
    Description: Published
    Description: 771-794
    Description: JCR Journal
    Description: restricted
    Keywords: laser scanning tecnique ; 04. Solid Earth::04.03. Geodesy::04.03.09. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2022-08-25
    Description: We present a 1:25,000 scale map of the coseismic surface ruptures following the 30 October 2016 M-w 6.5 Norcia normal-faulting earthquake, central Italy. Detailed rupture mapping is based on almost 11,000 oblique photographs taken from helicopter flights, that has been verified and integrated with field data (〉7000 measurements). Thanks to the common efforts of the Open EMERGEO Working Group (130 people, 25 research institutions and universities from Europe), we were able to document a complex surface faulting pattern with a dominant strike of N135 degrees-160 degrees (SW-dipping) and a subordinate strike of N320 degrees-345 degrees (NE-dipping) along about 28km of the active Mt. Vettore-Mt. Bove fault system. Geometric and kinematic characteristics of the rupture were observed and recorded along closely spaced, parallel or subparallel, overlapping or step-like synthetic and antithetic fault splays of the activated fault systems, comprising a total surface rupture length of approximately 46km when all ruptures were considered.
    Description: Published
    Description: 151-160
    Description: 2T. Deformazione crostale attiva
    Description: 6T. Studi di pericolosità sismica e da maremoto
    Description: 2SR TERREMOTI - Gestione delle emergenze sismiche e da maremoto
    Description: 4IT. Banche dati
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2022-08-25
    Description: We provide a database of the coseismic geological surface effects following the Mw 6.5 Norcia earthquake that hit central Italy on 30 October 2016. This was one of the strongest seismic events to occur in Europe in the past thirty years, causing complex surface ruptures over an area of 〉400 km2. The database originated from the collaboration of several European teams (Open EMERGEO Working Group; about 130 researchers) coordinated by the Istituto Nazionale di Geofisica e Vulcanologia. The observations were collected by performing detailed field surveys in the epicentral region in order to describe the geometry and kinematics of surface faulting, and subsequently of landslides and other secondary coseismic effects. The resulting database consists of homogeneous georeferenced records identifying 7323 observation points, each of which contains 18 numeric and string fields of relevant information. This database will impact future earthquake studies focused on modelling of the seismic processes in active extensional settings, updating probabilistic estimates of slip distribution, and assessing the hazard of surface faulting.
    Description: Published
    Description: id 180049
    Description: 1T. Struttura della Terra
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 31 (1996), S. 52-58 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Quantitative description and prediction of vein hosted deposits using fractal statistics have been tested using data collected from the Curraghinalt gold deposit, Sperrin Mountains, County Tyrone, N. Ireland. Goldbearing quartz veins are hosted by Neo-Proterozoic Dalradian (Southern Highland Group) age psammites, pelitic schists and graphitic schists. Veins trend E to ESE and cross-cut regional structures. Vein thickness (z) distributions closely approximate a power-law distribution of the form N(⩾ z) = cz -D ,with an exponent (D) of 0.76 over three orders of magnitude. Vein spacing data approximate a log normal distribution with a mean of 2.92m. Numerical analysis indicates that the veins are more clustered than expected from a random distribution. Regions of high percentage extension and high vein density define vein clusters. The vein clustering relationship may be combined with the power-law thickness distribution and used in a predictive manner. The data may be used to constrain the probability of intersecting veins of potentially mineable dimension.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 408 (2000), S. 669-673 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The origin of granites was once a question solely for petrologists and geochemists. But in recent years a consensus has emerged that recognizes the essential role of deformation in the segregation, transport and emplacement of silica-rich melts in the continental crust. Accepted petrological ...
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2007-10-08
    Description: Subhorizontal attachment zones provide coupling between lithospheric layers in orogenic belts. A mid-crustal attachment zone is exposed in the Palaeoproterozoic Ketilidian orogen, south Greenland, which formed as a result of north-directed oblique convergence at a cordilleran-type margin. Rifting (c. 2.1 Ga) and compressional deformation and magmatism (〉 1850 Ma) on the continental margin was followed by an extended sinistral transpression from 1850 to 1730 Ma now separated into three episodes or peaks of activity. The first episode was focused on the back-arc region and was followed by the main arc construction phase during which transpression was partitioned into strike-slip and contraction components. Despite the longevity of this active margin system, individual tectonic events took place rapidly, e.g. development of fore-arc D1-D3 and accompanying high-temperature, low-pressure metamorphism took place over c. 12 Ma. We explain the fore-arc and batholith evolution by the upward migration of an underlying attachment structure through the upper crustal partitioned blocks. This migration may be attributed to an increase in the geothermal gradient accompanied by, or followed by, exhumation of the mid-crust. The partially molten, hence weak, attachment zone solidified and strengthened during cooling before emplacement of the post-orogenic rapakivi suite during the third distinct phase of mild sinistral transpression.
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...