Shallow-water platform carbonates at the Devonian/Carboniferous boundary - an interdisciplinary study in Ertocoun and Nanbiancun sections (Southern China)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F13%3A00073638" target="_blank" >RIV/00216224:14310/13:00073638 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Shallow-water platform carbonates at the Devonian/Carboniferous boundary - an interdisciplinary study in Ertocoun and Nanbiancun sections (Southern China)

Popis výsledku v původním jazyce

The Nanbiancun and Ertocoun sections, located in the vicinity of the city of Guilin, represent Devonian/Carboniferous boundary intervals of shallow-water platform carbonates. In the Ertocoun section platform interior to platform margin facies are exposedwith a deepening upward trend from microbial mounds into the talus microfacies being replaced by an upward shallowing succession higher in the section. Marginal slope facies exposed at the Nanbiancun section show different trends. At the base, a thick talus layer is exposed and overlain by a upward thinning succession of tempestite beds, which is interpreted as a deepening trend. Field gamma-ray spectrometry (GRS) as well as low-field magnetic susceptibility (XLF) measurements were performed in both sections. In addition, laboratory rock magnetic analyses have been applied in order to determine the nature of magnetic components in these sections.

Název v anglickém jazyce

Shallow-water platform carbonates at the Devonian/Carboniferous boundary - an interdisciplinary study in Ertocoun and Nanbiancun sections (Southern China)

Popis výsledku anglicky

The Nanbiancun and Ertocoun sections, located in the vicinity of the city of Guilin, represent Devonian/Carboniferous boundary intervals of shallow-water platform carbonates. In the Ertocoun section platform interior to platform margin facies are exposedwith a deepening upward trend from microbial mounds into the talus microfacies being replaced by an upward shallowing succession higher in the section. Marginal slope facies exposed at the Nanbiancun section show different trends. At the base, a thick talus layer is exposed and overlain by a upward thinning succession of tempestite beds, which is interpreted as a deepening trend. Field gamma-ray spectrometry (GRS) as well as low-field magnetic susceptibility (XLF) measurements were performed in both sections. In addition, laboratory rock magnetic analyses have been applied in order to determine the nature of magnetic components in these sections.

Druh

O - Ostatní výsledky

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GAP210%2F11%2F1891" target="_blank" >GAP210/11/1891: Hranice devonu a karbonu v Evropě - multidisciplinární přístup</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2013

Kód důvěrnosti údajů

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