Granitoids of the Mauthausen type in the Czech part of the Moldanubian Batholith

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F23%3A10136160" target="_blank" >RIV/00023272:_____/23:10136160 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.intechopen.com/chapters/88068" target="_blank" >https://www.intechopen.com/chapters/88068</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.5772/intechopen.113101" target="_blank" >10.5772/intechopen.113101</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Granitoids of the Mauthausen type in the Czech part of the Moldanubian Batholith

Popis výsledku v původním jazyce

The Modanubian (or South Bohemian batholith) is the largest Variscan magmatic complex in the Bohemian Massif, which is part of the Central European Hercynian belt. In northern part of the Moldanubian batholith occur relatively small bodies of granitoids which could be correlated with biotite granodiorites of the Mauthausen type which occur in the Austrian part of this batholithic complex. The first body is formed by biotite-muscovite granite of the Pavlov type. The second occurrence of granitoids of the Mauthausen type is formed by two, relatively small bodies of the biotite granodiorites of the Pohled type. The granites of the Pavlov type contain quartz, K-feldspar, plagioclase (An22-37), biotite (annite) and muscovite. This granite is slightly peraluminous (A/CNK 1.15-1.22). The biotite granodiorites of the Pohled type contain quartz, plagioclase (An16-45), K-feldspar and biotite (annite). This granodiorite is also slightly peraluminous(A/CNK 1.05- 1.15).

Název v anglickém jazyce

Granitoids of the Mauthausen type in the Czech part of the Moldanubian Batholith

Popis výsledku anglicky

The Modanubian (or South Bohemian batholith) is the largest Variscan magmatic complex in the Bohemian Massif, which is part of the Central European Hercynian belt. In northern part of the Moldanubian batholith occur relatively small bodies of granitoids which could be correlated with biotite granodiorites of the Mauthausen type which occur in the Austrian part of this batholithic complex. The first body is formed by biotite-muscovite granite of the Pavlov type. The second occurrence of granitoids of the Mauthausen type is formed by two, relatively small bodies of the biotite granodiorites of the Pohled type. The granites of the Pavlov type contain quartz, K-feldspar, plagioclase (An22-37), biotite (annite) and muscovite. This granite is slightly peraluminous (A/CNK 1.15-1.22). The biotite granodiorites of the Pohled type contain quartz, plagioclase (An16-45), K-feldspar and biotite (annite). This granodiorite is also slightly peraluminous(A/CNK 1.05- 1.15).

Druh

C - Kapitola v odborné knize

CEP obor

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OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2023

Kód důvěrnosti údajů

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

Název knihy nebo sborníku

Recent Advances in Mineralogy

ISBN

978-1-83768-980-4

Počet stran výsledku

19

Strana od-do

11-29

Počet stran knihy

153

Název nakladatele

IntechOpen Ltd.

Místo vydání

London

Kód UT WoS kapitoly

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