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  • 2020-2024  (1)
  • 2015-2019  (9)
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  • 1
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    Fold and Thrust Belts: Structural Style, Evolution and Exploration (2020)
    London : The Geological Society
    Details
    Keywords: fold ; thrust ; belts ; reservoirs
    Description / Table of Contents: Introduction --- Fold and thrust belts: structural style, evolution and exploration – an introduction / James A. Hammerstein, Raffaele Di Cuia, Michael A. Cottam, Gonzalo Zamora and Robert W. H. Butler / Geological Society, London, Special Publications, 490, 1-8, 31 July 2020, https://doi.org/10.1144/SP490-2020-81 --- Modelling of fold & thrust belts and petroleum systems --- Henry Cadell's ‘Experimental researches in mountain building’: their lessons for interpreting thrust systems and fold–thrust structures / Robert W. H. Butler, Clare E. Bond and Mark A. Cooper / Geological Society, London, Special Publications, 490, 9-31, 5 March 2020, https://doi.org/10.1144/SP490-2019-142 --- Mechanical controls on structural styles in shortening environments: a discrete-element modelling approach / Amanda Hughes / Geological Society, London, Special Publications, 490, 33-55, 31 July 2020, https://doi.org/10.1144/SP490-2019-114 --- Syn-kinematic strata influence the structural evolution of emergent fold–thrust belts / Robert W. H. Butler / Geological Society, London, Special Publications, 490, 57-78, 1 October 2019, https://doi.org/10.1144/SP490-2019-14 --- Petroleum tectonic comparison of fold and thrust belts: the Zagros of Iraq and Iran, the Pyrenees of Spain, the Sevier of Western USA and the Beni Sub-Andean of Bolivia / Jerome Kendall, Jaume Vergés, Renas Koshnaw and Melanie Louterbach / Geological Society, London, Special Publications, 490, 79-103, 3 April 2019, https://doi.org/10.1144/SP490-2018-102 --- Modelling the evolution of seal integrity in deepwater toe thrust anticlines / Neil T. Grant / Geological Society, London, Special Publications, 490, 105-133, 14 May 2020, https://doi.org/10.1144/SP490-2018-54 --- Raman spectroscopy: an effective thermal marker in low temperature carbonaceous fold–thrust belts / D. K. Muirhead, C. E. Bond, H. Watkins, R. W. H. Butler, A. Schito, Z. Crawford and A. Marpino / Geological Society, London, Special Publications, 490, 135-151, 17 December 2019, https://doi.org/10.1144/SP490-2019-27 --- Europe --- The Môn–Deemster–Ribblesdale fold–thrust belt, central UK: a concealed Variscan inversion belt located on weak Caledonian crust / Tim Pharaoh, Richard Haslam, Ed Hough, Karen Kirk, Graham Leslie, Dave Schofield and Adrian Heafford / Geological Society, London, Special Publications, 490, 153-176, 28 August 2019, https://doi.org/10.1144/SP490-2018-109 --- Inversion of the north Iberian hyperextended margin: the role of exhumed mantle indentation during continental collision / Jesús García-Senz, Antonio Pedrera, Conxi Ayala, Ana Ruiz-Constán, Alejandro Robador and Luis Roberto Rodríguez-Fernández / Geological Society, London, Special Publications, 490, 177-198, 22 February 2019, https://doi.org/10.1144/SP490-2019-112 --- Along-strike variations in thin-skinned thrusting style controlled by pre-existing basement structure in the easternmost Jura Mountains (Northern Switzerland) / Alexander Malz, Herfried Madritsch, Peter Jordan, Beat Meier and Jonas Kley / Geological Society, London, Special Publications, 490, 199-220, 21 February 2019, https://doi.org/10.1144/SP490-2019-090 --- Revitalizing exploration and redevelopment of deep carbonate targets in the Southern Apennines thrust belt (southern Italy): reappraising vintage data with modern approaches / P. Pace, R. Di Cuia and V. Mascolo / Geological Society, London, Special Publications, 490, 221-240, 14 January 2020, https://doi.org/10.1144/SP490-2019-28 --- Latest fold and thrust tectonics conceals extensional structures inherited from Cretaceous syn-sedimentary deformation: insights for exploration in fold-and-thrust belts from the Maiella Mountain / Davide Casabianca, Antoine Auzemery, Andrea Barrier, Angelo Ricciato, Stefano Borello, Alice Lecardez and Raffaele Di Cuia / Geological Society, London, Special Publications, 490, 241-266, 6 March 2020, https://doi.org/10.1144/SP490-2019-9 --- Middle Miocene evolution and structural style of the Diapir Fold Zone, Eastern Carpathian Bend Zone, Romania: insights from scaled analogue modelling / Dan M. Tămaș, Zsolt Schléder, Alexandra Tămaș, Csaba Krézsek, Bianca Copoț and Sorin Filipescu / Geological Society, London, Special Publications, 490, 267-284, 21 February 2019, https://doi.org/10.1144/SP490-2019-091 --- Asia-Pacific --- Variation in syn-subduction sedimentation patterns from inner to outer portions of deep-water fold and thrust belts: examples from the Hikurangi subduction margin of New Zealand / A. D. McArthur, B. Claussmann, J. Bailleul, A. Clare and W. D. McCaffrey / Geological Society, London, Special Publications, 490, 285-310, 16 April 2019, https://doi.org/10.1144/SP490-2018-95 --- Interaction between the folded structures of the Western Papua New Guinea Highlands: an example of how surface observations can assist in subsurface understanding / Reinaldo Ollarves, Siyuan Zhao and Fleur Gilby / Geological Society, London, Special Publications, 490, 311-327, 30 May 2019, https://doi.org/10.1144/SP490-2018-124 --- Geological development of the Timor Orogen / Pedro Martinez Duran, Peter Baillie, Eduardo Carrillo and Gregor Duval / Geological Society, London, Special Publications, 490, 329-349, 18 November 2019, https://doi.org/10.1144/SP490-2018-120 --- Broadband seismic imaging around the Banda Arc: changes in the anatomy of offshore fold-and-thrust belts / Peter Baillie, Myra Keep, Pedro Martinez Duran, Eduardo Carrillo and Gregor Duval / Geological Society, London, Special Publications, 490, 351-360, 21 February 2020, https://doi.org/10.1144/SP490-2018-141 --- Middle east --- Structure and kinematics of the Central Sivas Basin (Turkey): salt deposition and tectonics in an evolving fold-and-thrust belt / Etienne Legeay, Jean-Claude Ringenbach, Charlie Kergaravat, Alexandre Pichat, Geoffroy Mohn, Jaume Vergés, Kaan Sevki Kavak and Jean-Paul Callot / Geological Society, London, Special Publications, 490, 361-396, 20 June 2019, https://doi.org/10.1144/SP490-2019-92 --- Quantifying vertical movements in fold and thrust belts: subsidence, uplift and erosion in Kurdistan, northern Iraq / Richard S. J. Tozer, Michael Hertle, Henrik I. Petersen and Kim Zinck-Jørgensen / Geological Society, London, Special Publications, 490, 397-415, 8 March 2019, https://doi.org/10.1144/SP490-2019-118 --- Remote sensing applications in the Fars Region of the Zagros Mountains of Iran / Jorge Ginés, Rowan Edwards, Tina Lohr, Hayley Larkin and Rachel Holley / Geological Society, London, Special Publications, 490, 417-444, 20 March 2019, https://doi.org/10.1144/SP490-201
    Pages: Online-Ressource (VII, 454 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786204479
    URL: https://sp.lyellcollection.org/content/490/1
    Language: English
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  • 2
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    Tracking sand-fairways through a deformed turbidite system: the Numidian (Miocene) of Central Sicily, Italy (2017)
    Wiley
    Details
    Publication Date: 2017-09-20
    Description: Understanding ancient deep-water sedimentary systems that accumulated at complex plate boundaries requires confronting the stratigraphic record of deformed sedimentary successions by tracking sand-fairways and identifying original relationships in later deformed sequences. Here, we investigate the Numidian turbidite system (early to mid-Miocene) of Central-East Sicily to explore a deep-water sedimentary system deposited at an active thrust belt on the Central Mediterranean. Turbidites include multi-metre thick-bedded, ultra-mature quartz sandstones that were sourced from North Africa and are now deformed and dismembered within the Apennine-Maghrebian orogen. To date, much research has focused on the little-deformed sections that sample discrete parts of the original turbidite pathways. Yet the bulk of these systems are represented by deformed successions and these have attracted little modern sedimentological and stratigraphic investigation. We present new data based on field mapping, sedimentological/structural fieldwork, and biostratigraphy (planktonic foraminifera and nannofossils) that focus on the Numidian turbidites of Central-East Sicily. Thickness and facies variations, together with evidence of large-scale sediment bypass and local substrate reworking, characterize the Numidian turbidites of the study area, consistent with a partially confined turbidite system. Our work demonstrates that the Numidian turbidite system accumulated across active structures and these provided tortuous, evolving corridors through which turbidity currents were routed, transporting coarse sand over many hundreds of km. These results provide insight on structurally confined turbidites in analogous tectonic settings and demonstrate the need to seek sedimentological and stratigraphic data from deformed and dismembered parts of deep-water systems. © 2017 The Authors. Basin Research © 2017 John Wiley & Sons Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists
    Print ISSN: 0950-091X
    Electronic ISSN: 1365-2117
    Topics: Geosciences
    Published by Wiley
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  • 3
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    Discussion on ‘A reassessment of the proposed ‘Lairg impact structure’ and its potential implications for the deep structure of northern Scotland’ Journal of the Geological Society, London, 176, 817-829 (2019)
    Geological Society of London
    Details
    Publication Date: 2019-11-28
    Print ISSN: 0016-7649
    Topics: Geosciences
    Published by Geological Society of London
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  • 4
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    Interpreting syndepositional sediment remobilization and deformation beneath submarine gravity flows; a kinematic boundary layer approach (2015)
    Geological Society of London
    Details
    Publication Date: 2015-09-22
    Print ISSN: 0016-7649
    Topics: Geosciences
    Published by Geological Society of London
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  • 5
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    Geikie's field researches and their geological controversies (2018)
    Geological Society of London
    Details
    Publication Date: 2018-04-18
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Published by Geological Society of London
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  • 6
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    Tectonic evolution of the Himalayan syntaxes: the view from Nanga Parbat (2018)
    Geological Society of London
    Details
    Publication Date: 2018-08-30
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Published by Geological Society of London
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  • 7
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    Fold–thrust structures – where have all the buckles gone? (2019)
    Geological Society of London
    Details
    Publication Date: 2019-02-20
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Published by Geological Society of London
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  • 8
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    Inversion structures in a foreland domain: Seismic examples from the Italian Adriatic Sea (2015)
    Society of Exploration Geophysicists
    Details
    Publication Date: 2015-11-01
    Description: Positive structural inversion within foreland domains ahead of thrust belts can create structures with significant hydrocarbon potential in mature and underexplored areas. Within this context, the Adriatic region represents a well-established hydrocarbon province constituting a foreland domain bounded by the Apennines, Southern Alps, and Dinaric fold-and-thrust belts. Newly reprocessed regional 2D seismic data and a renewed exploration interest in the area motivate a reappraisal of the regional structure and stratigraphy of the deformed Central Adriatic region of Italy (i.e., the Mid-Adriatic Ridge). Here, we developed and discussed examples of inversion structures that have different structural styles. The structural interpretations displayed on time-to-depth converted profiles had been validated by 2D structural-kinematic balancing and forward modeling. Our aim was to better define the geometry, style, and timing of the analyzed inversion-related folds. Positive inversion structures appeared locally as asymmetric harpoon-shaped anticlines riding over high-angle blind thrusts. More commonly, inversion structures were symmetric anticlines formed above conjugate faults. Retrodeformed cross sections showed that positive inversion involved symmetric graben and asymmetric half-graben that originated during the Triassic and Jurassic. That these inversion structures developed during basement-involved thrusting, as suggested for the Adriatic in general, was consistent with forward modeling. Regionally, the contractional structures belonging to the Mid-Adriatic Ridge can be explained in terms of intraplate deformation that chiefly acted through reactivation of Mesozoic normal faults.
    Print ISSN: 2324-8858
    Electronic ISSN: 2324-8866
    Topics: Geosciences
    Published by Society of Exploration Geophysicists
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  • 9
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    Platform-basin transitions and their role in Alpine-style collision systems: a comparative approach (2017)
    Springer
    Details
    Publication Date: 2017-01-10
    Print ISSN: 1661-8726
    Electronic ISSN: 1661-8734
    Topics: Geosciences
    Published by Springer
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  • 10
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    Syn-kinematic strata influence the structural evolution of emergent fold–thrust belts (2019)
    Geological Society of London
    Details
    Publication Date: 2019-08-14
    Description: Whether thrusts are ramp-dominated and form imbricate fans or run out onto the syn-orogenic surface, forming ‘thrust-allochthons’, is governed by the activity of secondary ‘upper’ detachments along the syn-orogenic surface, activations of which are inhibited by syn-kinematic sedimentation at the thrust front. In the northern Apennines, where thrust systems are ramp-dominated and form an emergent imbricate fan, syn-kinematic sedimentation was abundant and accumulated ahead and above each thrust. In the southern Apennines, the far-travelled Lagronegro allochthon achieved its high displacements (〉65 km) while the foredeep basin received little sediment. The imbricate fan at the front of the main Himalayan arc developed within a foredeep that experienced high rates of syn-kinematic sedimentation. In contrast, further west, the Salt Range Thrust emerged into a distal, weakly developed foredeep with significantly reduced rates of sediment accumulation. Displacements were strongly localized onto this thrust (c. 25 km displacement) which activated an upper detachment along the syn-orogenic surface. It is an arrested thrust-allochthon. Lateral variations into the adjacent, ramp-dominated but still salt-detached, Jhelum fold-belt are marked by increases in syn-kinematic sedimentation. As sedimentation styles can vary in space and time, individual thrusts and thrust systems can evolve from being allochthon prone to imbricate dominated.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Published by Geological Society of London
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