SEMINAL INSIGHTS CONCERNING THE VARIETY OF SIDERTIC STRUCTURES AND VARIABLE GENESIS AND OF SIDERITIC OCCURRENCES: AN UNEXPLORED SOURCE OF PALAEONTOLOGICAL INFORMATION (SYDNEY COALFIELD, MIDDLE PENNSYLVANIAN, CANADA)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00228745%3A_____%2F22%3AN0000006" target="_blank" >RIV/00228745:_____/22:N0000006 - isvavai.cz</a>
Výsledek na webu
<a href="https://folia.zcm.cz/images/pdf/56-4" target="_blank" >https://folia.zcm.cz/images/pdf/56-4</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.2478/fbgp-2022-0004" target="_blank" >10.2478/fbgp-2022-0004</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
SEMINAL INSIGHTS CONCERNING THE VARIETY OF SIDERTIC STRUCTURES AND VARIABLE GENESIS AND OF SIDERITIC OCCURRENCES: AN UNEXPLORED SOURCE OF PALAEONTOLOGICAL INFORMATION (SYDNEY COALFIELD, MIDDLE PENNSYLVANIAN, CANADA)
Popis výsledku v původním jazyce
Reported are descriptions of twelve samples representing a variety of sideritic structures, including nodules mostly from roof shale of the Middle Pennsylvanian Sydney Coalfield, Canada. The co-occurrence of fossiliferous nodules and compression fossils in the shaley roof rocks at Point Aconi enhance greatly palaeontological information. Newly discovered in a coal seam, and part of the sample, is a 40 mm thick continuous sheet-like layer of siderite with abundant permineralized-like-compressed small to micron-sized structures in a rather evenly-sized sideritic matrix, probably indicating a genetic origin different from that of the nodules. Methods include some thin-section, and two X-Ray analysis. However, large systematic sampling is a prerequisite to explore that situation, which additionally could provide faunal information for Euromerican correlation.
Název v anglickém jazyce
SEMINAL INSIGHTS CONCERNING THE VARIETY OF SIDERTIC STRUCTURES AND VARIABLE GENESIS AND OF SIDERITIC OCCURRENCES: AN UNEXPLORED SOURCE OF PALAEONTOLOGICAL INFORMATION (SYDNEY COALFIELD, MIDDLE PENNSYLVANIAN, CANADA)
Popis výsledku anglicky
Reported are descriptions of twelve samples representing a variety of sideritic structures, including nodules mostly from roof shale of the Middle Pennsylvanian Sydney Coalfield, Canada. The co-occurrence of fossiliferous nodules and compression fossils in the shaley roof rocks at Point Aconi enhance greatly palaeontological information. Newly discovered in a coal seam, and part of the sample, is a 40 mm thick continuous sheet-like layer of siderite with abundant permineralized-like-compressed small to micron-sized structures in a rather evenly-sized sideritic matrix, probably indicating a genetic origin different from that of the nodules. Methods include some thin-section, and two X-Ray analysis. However, large systematic sampling is a prerequisite to explore that situation, which additionally could provide faunal information for Euromerican correlation.
Klasifikace
Druh
J<sub>ost</sub> - Ostatní články v recenzovaných periodicích
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
—
Návaznosti
V - Vyzkumna aktivita podporovana z jinych verejnych zdroju
Ostatní
Rok uplatnění
2022
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Folia Musei rerum naturalium Bohemiae occidentalis - Geologica et Paleobiologica
ISSN
1805-2371
e-ISSN
—
Svazek periodika
56
Číslo periodika v rámci svazku
1-2
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
14
Strana od-do
43-56
Kód UT WoS článku
—
EID výsledku v databázi Scopus
—