P?T?t?d evolution of orogenic middle crust of the Roc de Frausa Massif (Eastern Pyrenees): A result of horizontal crustal flow and Carboniferous doming?

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F15%3A00000183" target="_blank" >RIV/00025798:_____/15:00000183 - isvavai.cz</a>

Výsledek na webu

<a href="http://onlinelibrary.wiley.com/doi/10.1111/jmg.12120/abstract" target="_blank" >http://onlinelibrary.wiley.com/doi/10.1111/jmg.12120/abstract</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1111/jmg.12120" target="_blank" >10.1111/jmg.12120</a>

Jazyk výsledku

angličtina

Název v původním jazyce

P?T?t?d evolution of orogenic middle crust of the Roc de Frausa Massif (Eastern Pyrenees): A result of horizontal crustal flow and Carboniferous doming?

Popis výsledku v původním jazyce

In the Roc de Frausa Massif in the Eastern Pyrenees, the pre-Variscan lithological succession is the Upper, Intermediate and Lower series by two orthogneiss sheets and intruded by Variscan igneous rocks. Two phases of Variscan deformation. D1 are markedby flat-lying foliation (S1) that affects the whole crustal section, D2 structures are characterized by tight upright folds facing to the NW with steep NE?SW axial planes, D2 leads to an almost complete transposition into a sub-vertical foliation (S2) inthe high-grade metamorphic domain. In the Upper series, and-sill grew during the S1 indicating heating from 580 to 640°C associated with an increase in pressure. Static growth of cordierite points to post-D1 decompression. In the Intermediate series, asill?bi?mu-bearing assemblage parallel to the S1 is statically overgrown by crd-ksp. This points to ~1 kbar of post-D1 decompression at 630?650°C. The Intermediate series intruded by a gabbro?diorite has a aureole where, the migmatitic S1

Název v anglickém jazyce

P?T?t?d evolution of orogenic middle crust of the Roc de Frausa Massif (Eastern Pyrenees): A result of horizontal crustal flow and Carboniferous doming?

Popis výsledku anglicky

In the Roc de Frausa Massif in the Eastern Pyrenees, the pre-Variscan lithological succession is the Upper, Intermediate and Lower series by two orthogneiss sheets and intruded by Variscan igneous rocks. Two phases of Variscan deformation. D1 are markedby flat-lying foliation (S1) that affects the whole crustal section, D2 structures are characterized by tight upright folds facing to the NW with steep NE?SW axial planes, D2 leads to an almost complete transposition into a sub-vertical foliation (S2) inthe high-grade metamorphic domain. In the Upper series, and-sill grew during the S1 indicating heating from 580 to 640°C associated with an increase in pressure. Static growth of cordierite points to post-D1 decompression. In the Intermediate series, asill?bi?mu-bearing assemblage parallel to the S1 is statically overgrown by crd-ksp. This points to ~1 kbar of post-D1 decompression at 630?650°C. The Intermediate series intruded by a gabbro?diorite has a aureole where, the migmatitic S1

Druh

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

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

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

Návaznosti

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

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

Journal of Metamorphic Geology

ISSN

0263-4929

e-ISSN

—

Svazek periodika

33

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

22

Strana od-do

273-294

Kód UT WoS článku

000351210400003

EID výsledku v databázi Scopus

—