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Tracing Tectonic Deformation Using the Sedimentary Record.


Tracing Tectonic Deformation Using the Sedimentary Record

Edited by Tom McCann and Aline Saintot The Geological Society of London The Geological Society of London is a learned society based in the United Kingdom with the aim of "investigating the mineral structure of the Earth". It is the oldest national geological society in the world and the largest in Europe with over 9000 Fellows entitled to the  (UK), Special Publication No. 208, 2003, 364 p. ISBN ISBN
abbr.
International Standard Book Number


ISBN International Standard Book Number

ISBN n abbr (= International Standard Book Number) → ISBN m 
 1-86239-129-7, Hardback, $142.00 US (list price); $71.00 US (GSL GSL - Grenoble System Language. M. Berthaud, IBM, Grenoble. "GSL Language Reference Manual", M. Berthaud et al, March 1973. "A MOL-Based Software Construction System", M. Berthaud et al, in Machine Oriented Higher Level Languages, W. van der Poel, N-H 1974, pp.151-157.  member price); $85.00 US (AAPG/SEPM/GSA member price).

This volume reflects the outcome of a technical session titled "Tectonics tectonics

Scientific study of the deformation of the rocks that make up the Earth's crust and the forces that produce such deformation. It deals with the folding and faulting associated with mountain building; the large-scale, gradual, upward and downward movements of the
 and Sedimentation sedimentation

In geology, the process of deposition of a solid material from a state of suspension or solution in a fluid (usually air or water). Broadly defined it also includes deposits from glacial ice and materials collected under the effect of gravity alone, as in talus
", which was held at the European Union European Union (EU), name given since the ratification (Nov., 1993) of the Treaty of European Union, or Maastricht Treaty, to the

European Community
 of Geosciences meeting in Strasburg in April 2001. It consists of a collection of sixteen papers, including an overview on the broad topic of linked tectonics and sedimentation, followed by fifteen field-based case studies.

The topic approached in this Special Publication is relevant to the study of any type of sedimentary basin The term sedimentary basin is used to refer to any geographical feature exhibiting subsidence and consequent infilling by sedimentation. As the sediments are buried, they are subjected to increasing pressure and begin the process of lithification. . Processes of sedimentation are dependent on the tectonic controls on the formation and evolution of basins and, as a result, subsidence subsidence, lowering of a portion of the earth's crust. The subsidence of land areas over time has resulted in submergence by shallow seas (see oceans). Land subsidence can occur naturally or through human activity.  histories may be interpreted based on the nature and stacking patterns of basin fills. The structural and sedimentological aspects of basin analysis are often approached separately in field studies. The message of this volume is that integration of the linked tectonic--sedimentological systems leads to far better results and to a more comprehensive understanding of the complex evolution of sedimentary basins. The related themes of tectonics and sedimentation require the application of many different theoretical, experimental and empirical resources provided by structural geology structural geology

Scientific discipline concerned with rock deformation on both small and large scales. Its scope ranges from submicroscopic lattice defects in crystals to fault structures and fold systems of the Earth's crust.
, sedimentology sedimentology

Scientific discipline concerned with the physical and chemical properties of sedimentary rocks and the processes involved in their formation, including transportation, deposition, and lithification of sediments.
, geochemistry geochemistry, study of the chemical changes on the earth. More specifically, it is the study of the absolute and relative abundances of chemical elements in the minerals, soils, ores, rocks, water, and atmosphere of the earth and the distribution and movement of , geophysics, or numerical modeling. Following this philosophy, this volume provides a fine example of interdisciplinary research, which is proven once again as the modern scientific approach that has the edge over the individual application of conventional disciplines.

Because of the complex nature of its objective, a volume like this is bound to be both useful and limited. It is useful because of the theoretical discussions and practical examples of how the structural and sedimentological aspects of basin analysis can be integrated in field studies, but it is limited in the sense that relatively few basin types are exemplified with case studies. Out of the fifteen research papers, five deal with fold-thrust belts and associated intramontane or piggyback piggyback

1. A broker trading in his or her personal account after trading in the same security for a customer. The broker may believe the customer has access to privileged information that will cause the transaction to be profitable.

2.
 basins, three papers focus on foreland basins, three on rift and/or graben/half-graben basins, two concentrate on intracratonic basins, one presents the case study of a divergent continental margin, and one other deals with a fore-arc basin. The case studies presented in the volume thus only cover about half of the range of basin types. This is in part due to space limitations imposed on a Special Publication such as this, but is also a consequence of the fact that the volume is the full-length extension of the papers presented in a conference technical session, where the selection of papers is partly a function of submissions rather than the conveners' own choice. Nevertheless, the research papers included in this volume exemplify most of the basic tectonic settings, including extensional, intraplate, and compressional.

Another consequence of this volume being the offspring of a European Union of Geosciences meeting is that the case studies are heavily based on European basins (twelve out of fifteen papers), with additional examples from Australia (one fore-arc basin), Chile (a divergent continental margin), and Asia (one intracratonic basin). This may hamper the interest of the North American North American

named after North America.


North American blastomycosis
see North American blastomycosis.

North American cattle tick
see boophilusannulatus.
 readership, even though the presented material does have value in providing analogues and examples of practical methodologies "at work".

The opening paper by McCann and Saintot provides a useful overview of the process-response relationship between tectonic activity that may operate over a wide range of scales, and its effects on the sedimentary record. This review brings the purpose of the volume into focus, and represents a good introduction to the fifteen research papers that follow. After examining the basin-forming mechanisms in extensional and compressional settings, the paper provides useful summaries of the models of sedimentation that are currently available in various plate tectonic settings, from local to continental scales. These models account for the complex interplay of differential subsidence, sediment supply, basin physiography, climate, and sea-level changes, and emphasize the importance of three-dimensional models, which consider both along-dip and along-strike variations in structural style and deposition, over the two-dimensional ones. A good point is also made: that stratigraphic stra·tig·ra·phy  
n.
The study of rock strata, especially the distribution, deposition, and age of sedimentary rocks.



strat
 models of basin fill architecture are better constrained for certain types of basins, such as divergent continental margins, foreland basins, or rift basins, but are less developed for most other basin types as a result of the lack of studies and/or economic interest. The final section of this review is also interesting, suggesting a series of possible new research directions, almost exclusively interdisciplinary, which would help to improve existing models of interlinked sediment--tectonics systems.

One third of the research papers in this volume focus on fold-thrust belts and the related areas of sediment accumulation. These papers deal with reconstructions of plate-tectonic configurations (Golonka et al.), palinspastic restorations (Lamarche et al.,), subsidence analysis (Carrapa et al.), provenance of piggy-back basin fills (Cibin et al.), and synkinematic sedimentation (Nalpas et al.). The sedimentation styles of graben to rift systems are exemplified by the work of Fernandez et al., Derer et al., and McCann et al. Three case studies of foreland systems focus on the sequence stratigraphy Sequence stratigraphy is a relatively new branch of geology that attempts to link prehistoric relative sea-level changes to sedimentary deposits. The essence of the method is mapping of strata based on identification of time lines (e.g.  (Lazauskiene et al.), basin migration (Christophoul et al.), and thermal history of related orogens in such settings. Two intracratonic basins are examined in terms of facies facies /fa·ci·es/ (fa´she-ez) pl. fa´cies   [L.]
1. the face.

2. surface; the outer aspect of a body part or organ.

3. expression (1).
 distribution and paleogeography paleogeography
 or palaeogeography

Geography of selected portions of the Earth's surface at specific times in the geologic past. The simplest kind of paleogeography is a map showing the locations of ancient lands and seas, but paleogeographic maps may also
 (Rieke et al.), and subsidence rates and mechanisms (Artyushkov and Chekhovich). Papers revealing the subsurface geometry and tectonic development of a fore-arc basin using geophysical data (Wartenberg et al.,), and the tectonic setting of a divergent margin based on a combination of provenance, geochemical and isotope studies (Augustsson and Bahlburg) complete the collection of case studies in this volume.

All papers are well illustrated with high-quality black-and-white diagrams, and the presentation of the volume in general is very good. I can conclude that in spite of unavoidable limitations, as argued above, this Special Publication is yet another fine product of the Geological Society of London, which captures the insight of one of the most significant topics in the modern research of sedimentary basins--the issue of linked tectonics and sedimentation. The volume should be of interest to a wide range of readership, from sedimentologists and structural geologists to geochemists, geophysicists and computer modelers.

Octavian Catuneanu

Dept of Earth and Atmospheric Sciences

University of Alberta

1-26 Earth Sciences Building Edmonton, Alberta, T6G 2E3

octavian@ualberta.ca
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Author:Catuneanu, Octavian
Publication:Geoscience Canada
Article Type:Book Review
Date:Jun 1, 2004
Words:1060
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