Thermal overprint in Paleozoic sediments of the Moravo-Silesian zone, Bohemian Massif: a record of late Variscan orogen-parallel extension

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F05%3A00009999" target="_blank" >RIV/61989592:15310/05:00009999 - isvavai.cz</a>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

Thermal overprint in Paleozoic sediments of the Moravo-Silesian zone, Bohemian Massif: a record of late Variscan orogen-parallel extension

Popis výsledku v původním jazyce

Moravo-Silesian Zone (MSZ) constitutes the eastern periphery of the Variscan orogene in Europe. Devonian and Lower Carboniferous sedimentary and volcanic rocks of the MSZ (eastern part of the Czech Republic and the Cracow-Silesia region of southern Poland) show a general trend in increasing thermal maturity from the foreland located to the E to the Variscan orogene located to the W. In the eastern, Polish part of the MSZ thermal overprint is relatively low and related mainly to intrusions of small intrusive bodies. In the western, Moravian and Silesian part, however, the thermal maturity is much higher and it shows some peculiarities that, so far, have not been sufficiently explained. Principal characteristics of the thermal maturity field in the western part of the MSZ as revealed from combined vitrinite reflectance (Rr), conodont colour alteration index (CAI) and illite crystallinity (IC) data-base are as follows: (i) thermal maturity ranges from anchimetamorphic conditions (Rr = 3.5

Název v anglickém jazyce

Thermal overprint in Paleozoic sediments of the Moravo-Silesian zone, Bohemian Massif: a record of late Variscan orogen-parallel extension

Popis výsledku anglicky

Moravo-Silesian Zone (MSZ) constitutes the eastern periphery of the Variscan orogene in Europe. Devonian and Lower Carboniferous sedimentary and volcanic rocks of the MSZ (eastern part of the Czech Republic and the Cracow-Silesia region of southern Poland) show a general trend in increasing thermal maturity from the foreland located to the E to the Variscan orogene located to the W. In the eastern, Polish part of the MSZ thermal overprint is relatively low and related mainly to intrusions of small intrusive bodies. In the western, Moravian and Silesian part, however, the thermal maturity is much higher and it shows some peculiarities that, so far, have not been sufficiently explained. Principal characteristics of the thermal maturity field in the western part of the MSZ as revealed from combined vitrinite reflectance (Rr), conodont colour alteration index (CAI) and illite crystallinity (IC) data-base are as follows: (i) thermal maturity ranges from anchimetamorphic conditions (Rr = 3.5

Druh

D - Stať ve sborníku

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2005

Kód důvěrnosti údajů

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

Název statě ve sborníku

Geolines

ISBN

—

ISSN

1210-9606

e-ISSN

—

Počet stran výsledku

161

Strana od-do

—

Název nakladatele

Geologický ústav AV ČR

Místo vydání

Praha

Místo konání akce

—

Datum konání akce

—

Typ akce podle státní příslušnosti

—

Kód UT WoS článku

—