Stratigraphy and facies development of the marine Late Devonian near the Boulongour Reservoir, northwest Xinjiang, China

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F14%3A61826" target="_blank" >RIV/60460709:41330/14:61826 - 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

Stratigraphy and facies development of the marine Late Devonian near the Boulongour Reservoir, northwest Xinjiang, China

Popis výsledku v původním jazyce

Late Devonian to Early Carboniferous stratigraphic units within the Zhulumute Formation, Hongguleleng Formation (stratotype), Hebukehe Formation and the Heishantou Formation near the Boulongour Reservoir in northwestern Xinjiang are fossil-rich. The Hongguleleng and Hebukehe formations are biostratigraphically well constrained by microfossils from the latest Frasnian linguiformis to mid-Famennian trachytera conodont biozones. The Hongguleleng Formation (96.8 m) is characterized by bioclastic argillaceous limestones and marls (the dominant facies) intercalated with green spiculitic calcareous shales. It yields abundant and highly diverse faunas of bryozoans, brachiopods and crinoids with subordinate solitary rugose corals, ostracods, trilobites, conodonts and other fish teeth. The succeeding Hebukeh Formation (95.7 m) consists of siltstones, mudstones, arenites and intervals of bioclastic limestone (e.g. Blastoid Hill) and cherts with radiolarians. A diverse ichnofauna, phacopid trilobi

Název v anglickém jazyce

Stratigraphy and facies development of the marine Late Devonian near the Boulongour Reservoir, northwest Xinjiang, China

Popis výsledku anglicky

Late Devonian to Early Carboniferous stratigraphic units within the Zhulumute Formation, Hongguleleng Formation (stratotype), Hebukehe Formation and the Heishantou Formation near the Boulongour Reservoir in northwestern Xinjiang are fossil-rich. The Hongguleleng and Hebukehe formations are biostratigraphically well constrained by microfossils from the latest Frasnian linguiformis to mid-Famennian trachytera conodont biozones. The Hongguleleng Formation (96.8 m) is characterized by bioclastic argillaceous limestones and marls (the dominant facies) intercalated with green spiculitic calcareous shales. It yields abundant and highly diverse faunas of bryozoans, brachiopods and crinoids with subordinate solitary rugose corals, ostracods, trilobites, conodonts and other fish teeth. The succeeding Hebukeh Formation (95.7 m) consists of siltstones, mudstones, arenites and intervals of bioclastic limestone (e.g. Blastoid Hill) and cherts with radiolarians. A diverse ichnofauna, phacopid trilobi

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

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

2014

Kód důvěrnosti údajů

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

Název periodika

JOURNAL OF ASIAN EARTH SCIENCES

ISSN

1367-9120

e-ISSN

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Svazek periodika

2014

Číslo periodika v rámci svazku

80

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

18

Strana od-do

101-118

Kód UT WoS článku

000331154800008

EID výsledku v databázi Scopus

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