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  • 1
    Monograph available for loan
    Monograph available for loan
    Mesozoic and Cenozoic Carbonate Systems of the Mediterranean and the Middle East : Stratigraphic and Diagenetic Reference Models (2010)
    London : The Geological Society
    Associated volumes
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    Call number: 9/M 07.0421(329)
    In: Geological Society special publication
    Description / Table of Contents: This volume contains a collection of stratigraphic and diagenetic case studies of Mesozoic and Cenozoic carbonate sequences from the Tethyan realm. High levels of industry and academic interest in the region have generated numerous multi-disciplinary studies of these sequences, a selection of which are presented in this volume. The studies presented are based on both comprehensive subsurface datasets from important hydrocarbon-bearing strata of the Middle East and the excellent surface exposures in the region of interest.The studies presented in this volume may serve as suitable starting points in the development of age and architecture specific carbonate reference models. Such models can form the basis of internally consistent models for carbonate deposition, sequence development and reservoir performance. Ideally such models, suitably scaled, will be equally applicable to academic studies, the exploration and development phases of the field life cycle and in the prediction of future reservoir performance.
    Type of Medium: Monograph available for loan
    Pages: vi, 422 S.
    ISBN: 9781862392922
    Series Statement: Geological Society special publication 329
    URL: http://sp.lyellcollection.org/content/vol329/issue1/
    Classification:
    Stratigraphy
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
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    Mesozoic and Cenozoic Carbonate Systems of the Mediterranean and the Middle East: Stratigraphic and Diagenetic Reference Models (2010)
    London : The Geological Society
    Details
    Description / Table of Contents: This volume contains a collection of stratigraphic and diagenetic case studies of Mesozoic and Cenozoic carbonate sequences from the Tethyan realm. High levels of industry and academic interest in the region have generated numerous multi-disciplinary studies of these sequences, a selection of which are presented in this volume. The studies presented are based on both comprehensive subsurface datasets from important hydrocarbon-bearing strata of the Middle East and the excellent surface exposures in the region of interest. The studies presented in this volume may serve as suitable starting points in the development of age and architecture specific carbonate reference models. Such models can form the basis of internally consistent models for carbonate deposition, sequence development and reservoir performance. Ideally such models, suitably scaled, will be equally applicable to academic studies, the exploration and development phases of the field life cycle and in the prediction of future reservoir performance.
    Pages: Online-Ressource (422 Seiten)
    ISBN: 9781862392922
    URL: http://sp.lyellcollection.org/content/vol329/issue1/
    Language: English
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  • 3
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    Mesozoic and Cenozoic carbonate systems of the Mediterranean and the Middle East: stratigraphic and diagenetic reference models - an introduction (2010)
    In:  Geological Society Special Publication 329: 1-7.
    Details
    Publication Date: 2010-04-01
    Description: The contributions in this volume originally formed a set of presentations at a conference on the same theme held in Mallorca, Spain in 2006. The goal of this conference was to investigate the potential to develop age or architecture specific reference models for carbonate systems and reservoirs similar to those successfully developed for siliciclastic systems. The conference focused on the Mesozoic and Cenozoic carbonate sequences of the Mediterranean and Middle East. These sequences were chosen for a number of reasons. Firstly, they represent sequence development in a variety of basin settings within a contiguous geographical entity, the former NeoTethys Ocean (Fig. 1). The sequences were also formed predominantly within tropical or sub-tropical climatic zones (cf. Schlager 2003). Finally, the high levels of industry and academic interest in the region have generated many excellent multidisciplinary studies of these sequences, based on both the comprehensive datasets of hydrocarbon-bearing strata and the excellent surface exposures in the region. In general, all Earth models underestimate the complexity of the subsurface and hence are intrinsically inaccurate. The value of developing such models, however, lies in the improved understanding of the processes controlling sequence development gained from their application (e.g. Ahr 1973; Read 1985; Burchette & Wright 1992; Handford & Loucks 1993; Pomar 2001; Bosence 2005). Extrapolating from data rich examples into areas where data coverage is poorer obliges us to distil out the generic from the specific and to propose appropriate subsurface analogues...
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  • 4
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    The influence of basin architecture and eustacy on the evolution of Tethyan Mesozoic and Cenozoic carbonate sequences (2010)
    In:  Geological Society Special Publication 329: 9-41.
    Details
    Publication Date: 2010-04-01
    Description: During the Mesozoic and Cenozoic Eras, regional tectonic processes, eustatic variations and the volume and distribution of non-carbonate sediment controlled the progressive expansion and rapid reduction of the accommodation space available for the deposition of carbonate sequences, in the area that is now the Mediterranean and Middle East. We present a simplified super-regional tectonostratigraphic history of this area from earliest Triassic time to the present day, to demonstrate the influence of these large-scale processes on the evolution of major Tethyan Mesozoic and Cenozoic carbonate sequences. The time period is divided into 11 tectonostratigraphic phases (TSP) two of which (1 and 11) are incomplete. Each TSP commenced with major changes in basin architecture in response to regional tectonic processes. Subsequent pulses of transgression and regression generated sequence stratigraphic hierarchies. These stratigraphic hierarchies reflect the interaction between regional and local tectonics, eustatic variations, carbonate growth processes, climate and non-carbonate sediment supply. A map is presented of a major second-order transgressive sequence (TST) within each TSP to illustrate the maximum extent of marine onlap. These maps also include the main plate configurations; active regional tectonic features and the resultant time averaged carbonate gross depositional systems that developed during the transgression. The sequence of maps illustrate that the volume of available accommodation space during the Mesozoic and Cenozoic Eras reached a maximum during the Late Cretaceous and has been progressively reduced during the Cenozoic Era to the present day minimum.
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  • 5
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    Professor David Gwyn Roberts - a Life in Geoscience (2018)
    Geological Society of London
    Details
    Publication Date: 2018
    Description: 〈p〉This conference was held to celebrate the outstanding career of a remarkable man. Professor David Gwyn Roberts was one of the most creative, productive and influential geoscientists of his generation. The range of his achievements and the scope of his influence on the world of geoscience are remarkable. He had a profound impact on geological thinking and understanding that serves as his lasting legacy. His Life in Geoscience commenced as a marine geoscientist at the Institute of Oceanographic Sciences, where he rapidly developed a global reputation for innovative research; this was followed by a highly influential spell as an explorer, technical expert and mentor in BP, and culminated in a successful career as a globally respected consultant, professor, teacher and author. He also edited numerous journals, founded the publication 〈i〉Marine and Petroleum Geology〈/i〉 and held high office in a number of professional organizations. Through his lectures, workshops and courses he served as an inspiration to hundreds of geoscientists around the world. Any phase of his career would identify David Gwyn Roberts as an outstanding geoscientist. The fact that these achievements were the work of one man mark Professor Roberts's life and contribution to the geosciences as truly remarkable.〈/p〉
    Print ISSN: 0375-6440
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Published by Geological Society of London
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  • 6
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    Professor David Gwyn Roberts - a Life in Geoscience (2018)
    Geological Society (of London)
    Details
    Publication Date: 2018-03-06
    Description: This conference was held to celebrate the outstanding career of a remarkable man. Professor David Gwyn Roberts was one of the most creative, productive and influential geoscientists of his generation. The range of his achievements and the scope of his influence on the world of geoscience are remarkable. He had a profound impact on geological thinking and understanding that serves as his lasting legacy. His Life in Geoscience commenced as a marine geoscientist at the Institute of Oceanographic Sciences, where he rapidly developed a global reputation for innovative research; this was followed by a highly influential spell as an explorer, technical expert and mentor in BP, and culminated in a successful career as a globally respected consultant, professor, teacher and author. He also edited numerous journals, founded the publication Marine and Petroleum Geology and held high office in a number of professional organizations. Through his lectures, workshops and courses he served as an inspiration to hundreds of geoscientists around the world. Any phase of his career would identify David Gwyn Roberts as an outstanding geoscientist. The fact that these achievements were the work of one man mark Professor Roberts's life and contribution to the geosciences as truly remarkable.
    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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    Mesozoic and Cenozoic carbonate systems of the Mediterranean and the Middle East: stratigraphic and diagenetic reference models – an introduction (2010)
    Geological Society of London
    Details
    Publication Date: 2010-01-01
    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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    The influence of basin architecture and eustacy on the evolution of Tethyan Mesozoic and Cenozoic carbonate sequences (2010)
    Geological Society of London
    Details
    Publication Date: 2010-01-01
    Description: During the Mesozoic and Cenozoic Eras, regional tectonic processes, eustatic variations and the volume and distribution of non-carbonate sediment controlled the progressive expansion and rapid reduction of the accommodation space available for the deposition of carbonate sequences, in the area that is now the Mediterranean and Middle East.We present a simplified super-regional tectonostratigraphic history of this area from earliest Triassic time to the present day, to demonstrate the influence of these large-scale processes on the evolution of major Tethyan Mesozoic and Cenozoic carbonate sequences. The time period is divided into 11 tectonostratigraphic phases (TSP) two of which (1 and 11) are incomplete. Each TSP commenced with major changes in basin architecture in response to regional tectonic processes. Subsequent pulses of transgression and regression generated sequence stratigraphic hierarchies. These stratigraphic hierarchies reflect the interaction between regional and local tectonics, eustatic variations, carbonate growth processes, climate and non-carbonate sediment supply. A map is presented of a major second-order transgressive sequence (TST) within each TSP to illustrate the maximum extent of marine onlap. These maps also include the main plate configurations; active regional tectonic features and the resultant time averaged carbonate gross depositional systems that developed during the transgression.The sequence of maps illustrate that the volume of available accommodation space during the Mesozoic and Cenozoic Eras reached a maximum during the Late Cretaceous and has been progressively reduced during the Cenozoic Era to the present day minimum.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Published by Geological Society of London
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