Last edited by Judal
Tuesday, July 28, 2020 | History

4 edition of Deep-water traction curren deposits found in the catalog.

Deep-water traction curren deposits

a study of internal tides, internal waves, contour currents and their deposits

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  • 32 Currently reading

Published by VSP in Utrecht .
Written in English

    Subjects:
  • Oceanography

  • Edition Notes

    Co-publ. with Science Press, Beijing (ISBN 7030067045).

    StatementGao Zhenzhong ... [et al.].
    The Physical Object
    Paginationvi, 128 p. :
    Number of Pages128
    ID Numbers
    Open LibraryOL22496419M
    ISBN 109067642851

    Unless otherwise stated, in this book the term "deepwater systems" refers to marine-sediment gravity-flow processes, environments, and deposits. Other authors have used different terms for describing deepwater processes and deposits, such as "turbidite systems" (Mutti and Normark, , ), "turbidite system complexes" (Stelting et al., Book Editor(s): Dorrik A. V. Stow clastic and biogenic grains that are randomly oriented, suggestive of hemipelagic deposition. Facies IV (chaotic deposit) is characterized by the disruption of beds, the presence of isolated siltstone blocks (or balls) and large clasts in the muddy matrix, indicative of retrogressive rockfall and slide.

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Deep-water traction curren deposits Download PDF EPUB FB2

Get this from a library. Deep-water traction current deposits: a study of internal tides, internal waves, contour currents and their deposits. [Gao Zhenzhong].

: Deep-Water Traction Current Deposits: A Study of Internal Tides, Internal Waves, Contour Currents and Their Deposits (): Gao Zhenzhong, Kenneth A. Erikkson, He Youbin, Luo Shunshe, Guo Jianhua: BooksCited by: Buy Deep-water Traction Current Deposits: A Study of Internal Tides, Internal Waves, Contour Currents and Their Deposits by Zhenzhong, Gao, etc.

(ISBN: ) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Hardcover. Sedimentary structures of bottom-current deposits occur in discrete units.

Selected examples of studies that dealt with tidal processes and their deposits in modern and ancient deep-water environments are also reviewed. Traction features interpreted as indicative of deep-water bottom current reworking are also diagrammatically by: A wealth of literature is available in documenting the link between traction structures and bottomcurrent reworking in deep-water environments (Hsü, Hsü, Hubert, ; Hollister, Antidunes and traction-carpet deposits in deep-water channel sandstones, Cretaceous, British Columbia, Canada Koji Yagishita.

Koji Yagishita Related Book Content. Stratigraphy and structural setting of the mid-Cretaceous Olvidada Formation, Baja California Norte, Mexico.

But bidirectional cross-laminae have been documented in deep-water traction deposits associated with wind-driven Loop Current in the Gulf of Mexico (Shanmugam et al., a, b, c Shanmugam et al., a Shanmugam et al., b Shanmugam et al., c).

The Loop Current generates eddies that can create complex current orientations. Bouma and Coleman () considered these submarine deposits to be analogous to fluvial point-bar deposits in subaerial environments. The problems in interpret- ing deep-water deposits using fluvial point-bar analogy are discussed in Chapter 7.

An inversely graded gravel layer underlies the sigmoidal cross bedding of Unit 11 (Fig. 40). Traction-dominated deep-water sand deposits in the Gulf of Mexico that show very good potential as reservoirs (high porosities and high permeability values) have been interpreted as sandy contourites by Shanmugam et al.

(b). The observed process in the flume study explains remarkably well some formerly enigmatic sandy deposits shown in Fig.

4C and D. Units of structureless coarse-tail graded beds in association with flame structures truncating traction carpet deposits of the upper flow regime indicate the location of the hydraulic jump of a 2-phase flow. PDF | On Jan 1,G. Shanmugam published Chinese translation of Book in Deep-water processes and facies models: Implications for sandstone petroleum reservoirs | Find, read and cite.

Deep Water Deposition SEPM Deepwater Research Group Annual Meeting Report - ‘Supercritical flows, bedforms, and deposits’ Organizers: Fabien Laugier (Chevron) Lilian Navarro (U Ottawa) Emma Morris (U College Dublin) Panelists: Tim Demko (ExxonMobil) Andrea Fildani (Equinor) Sophie Hage (National Oceanographic.

These deposits, which accumulated in synclinal lows, tend to have an external channel-like morphology but do not necessarily exhibit facies associations commonly ascribed to channels in fan models. Deep-water sediments from Yowlumne Field, Tule Elk Field, and some of the production Elk Hills Field are best explained by the “confinement” model.

Deep Water Traction Current Deposits A Study Of Internal Deep water traction current deposits a study of internal tides inte. Book lovers, when you need a new book to read, find the book here. Never worry not to find what you need. deposits (MTDs) and bottom-current-reworked sands (Shanmugam, a, a).

Thus, a plethora of confusing concepts and Thus, a plethora of confusing concepts and classifications exist. Resedimentation of the liquefied portions of such flows may be responsible for the deposition of the A‐subdivision of many turbidites and many thick, structureless ‘proximal turbidites’ or ‘fluxoturbidites’.

Similar units can originate by liquefaction of the traction deposits of normal turbidity currents. The deposits that Lowe, illustrates above as being deposited from high density turbidity currents match the Mulder & Alexander's () concentrated density flow deposits explained below.

Concentrated density flow These flows are defined on the basis of the turbulent fluid motion of the flow that supported from 10% to 25% sand sized particles. the fi elds of deep-water gravity-fl ow deposits. of repeated collapse of near-bed traction carpets be- dens ity turbi dity curren t deposit s.

Traction structures in deep-marine, bottom-current-reworked sands in the Pliocene and Pleistocene, Gulf of Mexico Article (PDF Available) in Geology 21(10) October with Reads.

Bryan T. Cronin, Mark A. Jones, "Facies Classification and Facies Association of Deep-water Depositional Systems: Application to the Prediction of Slope and Fan Architecture in the Upper Jurassic Thelma Field Area, South Viking Graben, North Sea", Rift-Related Coarse-Grained Submarine Fan Reservoirs; the Brae Play, South Viking Graben, North Sea, Colin C.

Turner, Bryan T. Cronin. The distinction between turbidites, contourites and hemipelagites in modern and ancient deep-water systems has long been a matter of controversy. This is partly because the processes themselves show a degree of overlap as part of a continuum, so that the deposit characteristics also overlap.

In addition, the three facies types commonly occur within interbedded sequences of continental margin.In striving to enrich the lives of all readers, TeachingBooks supports the First Amendment and celebrates the right to read.Deepwater Drilling: Well Planning, Design, Engineering, Operations, and Technology Application presents necessary coverage on drilling engineering and well construction through the entire lifecycle process of deepwater wells.

Authored by an expert with real-world experience, this book delivers illustrations and practical examples throughout to keep engineers up-to-speed and relevant in today.