Sedimentation tectonics eustasy (6 résultats)
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Vendeur : -OnTimeBooks-, Phoenix, AZ, Etats-Unis-OnTimeBooks-
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EUR 19,10
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Etat : good. A copy that has been read, remains in good condition. All pages are intact, and the cover is intact. The spine and cover show signs of wear. Pages can include notes and highlighting and show signs of wear, and the copy can include "From the library of" labels or previous owner inscriptions. 100% GUARANTEE! Shipped w…ith delivery confirmation, if you're not satisfied with purchase please return item! Ships via media mail.
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Vendeur : Zubal-Books, Since 1961, Cleveland, OH, Etats-UnisZubal-Books, Since 1961
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EUR 15,90
EUR 3,89 expéditionExpédition nationale : Etats-UnisQuantité disponible : 1 disponible(s)
Etat : Good. 518 pp., paperback, ex library, else text clean and binding tight. - If you are reading this, this item is actually (physically) in our stock and ready for shipment once ordered. We are not bookjackers. Buyer is responsible for any additional duties, taxes, or fees required by recipient's country.
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Vendeur : Anybook.com, Lincoln, Royaume-UniAnybook.com
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EUR 10,82
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Etat : Poor. Volume 12. This is an ex-library book and may have the usual library/used-book markings inside.This book has soft covers. In poor condition, suitable as a reading copy. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,1350grams, ISBN:9780632030170.
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Vendeur : Anybook.com, Lincoln, Royaume-UniAnybook.com
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EUR 12,04
EUR 18,37 expéditionExpédition depuis Royaume-Uni vers Etats-UnisQuantité disponible : 1 disponible(s)
Etat : Good. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. Clean from markings. In good all round condition. No dust jacket. Re-bound by library. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,1500grams, I…SBN:9780632030170.
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Vendeur : Phatpocket Limited, Waltham Abbey, HERTS, Royaume-UniPhatpocket Limited
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EUR 21,15
EUR 12,40 expéditionExpédition depuis Royaume-Uni vers Etats-UnisQuantité disponible : 1 disponible(s)
Etat : Good. Your purchase helps support Sri Lankan Children's Charity 'The Rainbow Centre'. Ex-library, so some stamps and wear, but in good overall condition. Our donations to The Rainbow Centre have helped provide an education and a safe haven to hundreds of children who live in appalling conditions.
Vendeur : ConchBooks, Harxheim, AllemagneConchBooks
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EUR 10,35
EUR 24,00 expéditionExpédition depuis Allemagne vers Etats-UnisQuantité disponible : 1 disponible(s)
Ajouter au panierSequence-stratigraphic models conceptualize the deposition of genetically related sediment packages along continental margins as a response to various phases of the cycle of relative change of sea level. Regional tectonics (subsidence/uplift), eustasy, and rate of sediment supply interact to produce the measure of relative chang…e of sea level. During a complete cycle of sea-level change, characteristic stratal patterns resulting within siliciclastic systems comprise: a basal, basinward prograding wedge of lowstand (or shelf-margin) systems tract; an intermediate, retrogradational landward back-stepping, transgressive systems tract; and an upper, aggrading to prograding, highstand systems tract. In siliciclastic systems most of the terrigenous material is delivered to the basin during the lowstand. Stratal patterns in carbonate systems are comparable to those in the siliciclastic systems; much of the carbonate is transferred to the basin during lowstand progradation. However, carbonate can also be exported off-bank during late highstand, when productivity on the bank top is high while accommodation is reduced. Both lowstand and late highstand progradation contribute to lateral growth of the platform. In hybrid siliciclasticcarbonate systems, lowstands may be dominated by clastic deposition, while carbonate accumulation may occur both during lowstand and highstand times. The history of the development of the basic conceptual framework of sequence stratigraphy, and the efforts that led to the documentation of sea-level variations deciphered from sequence analysis of subsurface and outcrop data, is outlined. The resulting history of sea-level change and its relationship to the sedimentary patterns of the deep sea are also discussed. A climatic feedback model of an alternating erosive/corrosive response to sea-level fall and rise is offered. Erosion on the sea floor is dominant during low sea-stands, and canyon incision on the margins during major falls of sea level. Carbonate dissolution on the sea floor is enhanced during times of maximum flooding of the shelves and during early highstand when carbonate is conserved on the inner shelves and nearshore. During the late highstand phase, following reduced accommodation on the banks, carbonate is again exported to the basins, abating the corrosive cycle. Distinction between early and late highstand phases, and between late highstand and lowstand progradation is, therefore, critical to understanding the response of the carbonate system and deep-sea sedimentary patterns to sea-level change along continental margins. 37 pp. 16 figs, 1 tab., gr. 8.
