Magnetic Record in Cave Sediments: A Review

Kód výsledku v IS VaVaI

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Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Magnetic Record in Cave Sediments: A Review

Popis výsledku v původním jazyce

Dating cave sediments by the application of the magnetostratigraphy is a difficult task. The method is comparative in its principles and does not provide numerical ages. Dating of cave sediments is limited by the complex conditions occurring undergroundso that it is often necessary to combine it with other methods that offer supplementary ages. The sedimentary fills of a number of profiles are separated into individual sequences and cycles, divided by breaks in deposition (unconformities). The dynamiccharacter of cave fill deposition is reflected in the start or termination of individual magnetozones at unconformities in a number of profiles. The general character of cave depositional environments with their numbers of post-depositional changes, hiatuses, reworking and re-deposition does not allow precise calculation of the temporal duration of individual interpreted magnetozones. All these factors contribute to the fact that exact calibration of the geometric characteristics of the

Název v anglickém jazyce

Magnetic Record in Cave Sediments: A Review

Popis výsledku anglicky

Dating cave sediments by the application of the magnetostratigraphy is a difficult task. The method is comparative in its principles and does not provide numerical ages. Dating of cave sediments is limited by the complex conditions occurring undergroundso that it is often necessary to combine it with other methods that offer supplementary ages. The sedimentary fills of a number of profiles are separated into individual sequences and cycles, divided by breaks in deposition (unconformities). The dynamiccharacter of cave fill deposition is reflected in the start or termination of individual magnetozones at unconformities in a number of profiles. The general character of cave depositional environments with their numbers of post-depositional changes, hiatuses, reworking and re-deposition does not allow precise calculation of the temporal duration of individual interpreted magnetozones. All these factors contribute to the fact that exact calibration of the geometric characteristics of the

Druh

C - Kapitola v odborné knize

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2011

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název knihy nebo sborníku

The Earth's magnetic interior

ISBN

978-94-007-0322-3

Počet stran výsledku

18

Strana od-do

343-360

Počet stran knihy

445

Název nakladatele

Springer

Místo vydání

Dordrecht

Kód UT WoS kapitoly

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