Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F12%3A00188578" target="_blank" >RIV/68407700:21110/12:00188578 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11310/12:10128650 RIV/00025798:_____/12:00000098

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.jsg.2011.12.011" target="_blank" >http://dx.doi.org/10.1016/j.jsg.2011.12.011</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.jsg.2011.12.011" target="_blank" >10.1016/j.jsg.2011.12.011</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif

Popis výsledku v původním jazyce

The w354e336 Ma Central Bohemian Plutonic Complex is a Variscan magmatic arc that developed in the central Bohemian Massif in response to subduction of the Saxothuringian lithosphere beneath the Teplá eBarrandian microplate. Magmatic to solid state fabrics in the most voluminous portion of this arc (the w346 Ma Blatná pluton) record two superposed orogenic events: dextral transpression associated with arc-parallel stretching and arc-perpendicular shortening, and normal shearing associated with exhumation of the high-grade core of the orogen (Moldanubian unit). This kinematic switch is an important landmark in the evolution of this segment of the Variscan belt for it marks the cessation of subduction-related compressive forces in the upper crust givingway to gravity-driven normal move- ments of the TepláeBarrandian hanging wall block relative to the high-grade Moldanubian footwall. We use thermal modeling to demonstrate that the emplacement of huge volumes of arc magmas and their slow

Název v anglickém jazyce

Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif

Popis výsledku anglicky

The w354e336 Ma Central Bohemian Plutonic Complex is a Variscan magmatic arc that developed in the central Bohemian Massif in response to subduction of the Saxothuringian lithosphere beneath the Teplá eBarrandian microplate. Magmatic to solid state fabrics in the most voluminous portion of this arc (the w346 Ma Blatná pluton) record two superposed orogenic events: dextral transpression associated with arc-parallel stretching and arc-perpendicular shortening, and normal shearing associated with exhumation of the high-grade core of the orogen (Moldanubian unit). This kinematic switch is an important landmark in the evolution of this segment of the Variscan belt for it marks the cessation of subduction-related compressive forces in the upper crust givingway to gravity-driven normal move- ments of the TepláeBarrandian hanging wall block relative to the high-grade Moldanubian footwall. We use thermal modeling to demonstrate that the emplacement of huge volumes of arc magmas and their slow

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

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

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2012

Kód důvěrnosti údajů

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

Název periodika

Journal of Structural Geology

ISSN

0191-8141

e-ISSN

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Svazek periodika

36

Číslo periodika v rámci svazku

March

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

16

Strana od-do

27-42

Kód UT WoS článku

000301630600004

EID výsledku v databázi Scopus

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