3D Seismic Technology: Application to the Exploration of by R J Davies, J A Cartwright, S A Stewart, M Lappin and J R PDF

By R J Davies, J A Cartwright, S A Stewart, M Lappin and J R Underhill

ISBN-10: 1862391513

ISBN-13: 9781862391512

A 'new age' of subsurface geological mapping that's simply as a long way ranging in scope because the frontier floor geological mapping campaigns of the earlier centuries is rising. it's the direct results of the appearance of second, and consequently 3D, seismic facts paralleled via advances in seismic acquisition and processing during the last 3 a long time. Subsurface mapping is fuelled through the industrial force to discover and get better hydrocarbons yet unavoidably it's going to result in significant conceptual advances in Earth sciences, throughout a broader variety of disciplines than these made throughout the second seismic revolution of the Seventies. Now that 3D seismic info assurance has elevated and the know-how is largely to be had we're poised to mine the whole highbrow and monetary advantages. This ebook illustrates how 3D seismic expertise is getting used to appreciate depositional platforms and stratigraphy, structural and igneous geology, in constructing and generating from hydrocarbon reservoirs and in addition what fresh technological advances were made. This technological trip is a fast-moving one the place the remainder clinical power nonetheless some distance exceeds the scope of the advances made up to now. This e-book explores the breadth of the possibilities that lie forward in addition to the inevitable accompanying demanding situations. additionally to be had: the way forward for Geological Modelling in Hydrocarbon improvement - exact e-book no 309 - ISBN 1862392668 South Caspian to valuable Iran Basins - distinct e-book no 312 - ISBN 9781862392717 The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on the earth, and one of many biggest publishers within the Earth sciences.The Society publishes quite a lot of top of the range peer-reviewed titles for lecturers and execs operating within the geosciences, and enjoys an enviable overseas popularity for the standard of its work.The many parts within which we put up in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic reports and geochemistry-Remote sensing-History of geology-Regional geology publications

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Extra resources for 3D Seismic Technology: Application to the Exploration of Sedimentary Basins

Sample text

On slope-steps where the canyon is narrow and erodes deeply, the channel complexes and slope fans have low width:thickness ratios and small depositional areas because bypass processes dominate (Fig. 7). In slope mini-basins the canyon is broader and the width:thickness ratio and areal extent of depositional elements increases. In addition to variations in reservoir volume caused by changes of the slope gradient there is also a dramatic increase in volume from the slope to basin floor. Basin floor fans are an order of magnitude larger than slope channel complexes and fans (Fig.

2). 5 to 1 km in width and are interpreted as sand prone (Fig. 2). Fanlike bodies of sediment are not readily identifiable on the slope and toe-of-slope because of the complex, cross-cutting caused by prevalent channelization. Basin floor fans Basin floor fans in the study area are composed of medium- to high-amplitude reflectors that are dominantly continuous (Fig. 2). Individual reflections display convex upward and concave upward patterns. The latter are common and can be shown to comprise the distributary channel network of the fan complex.

A number of depositional elements have been recognized and characterized to aid interpretation of deepwater provinces: debrites, inter-canyon, slope channel complexes, passive channel fill, slope fans, basin floor fans, channellevee complexes and drape. Channel complexes and slope fans dominate the sand prone deposits on the slope. Slope channel complexes are often amalgamated and appear to have good connectivity both vertically and laterally, but may deteriorate towards the channel margins. Large fans and leveed-channel deposits characterize sand prone sediments on the basin floor.

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3D Seismic Technology: Application to the Exploration of Sedimentary Basins by R J Davies, J A Cartwright, S A Stewart, M Lappin and J R Underhill


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