Mineralogical and chemical composition of the Hagendorf-North Pegmatite, SE Germany - a monographic study

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F13%3A00072839" target="_blank" >RIV/00216224:14310/13:00072839 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1127/0077-7757/2013/0244" target="_blank" >http://dx.doi.org/10.1127/0077-7757/2013/0244</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1127/0077-7757/2013/0244" target="_blank" >10.1127/0077-7757/2013/0244</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Mineralogical and chemical composition of the Hagendorf-North Pegmatite, SE Germany - a monographic study

Popis výsledku v původním jazyce

Hagendorf-North is a zoned Li-Nb-P-feldspar-quartz pegmatite located W of the village of Hagendorf and about 0.5 km north of the renown Hagendorf-South deposit which once was the largest feldspar pegmatite in Central Europe. Hagendorf-North also known asMeixner Mine was much smaller in size and its minerals assemblage is less variegated than that recorded from its larger "brother". However it was the site where mining began in 1860. But already before the onset of World War II, the pegmatite has no longer been considered an economic target and the mine was shut down. The reason for that small size in the shadow of this huge Hagendorf-South pegmatite is due to its overall role as feeder system to the Hagendorf-type stocklike pegmatites, which was truncated by the Pliocene chemical weathering and Pleistocene erosion, which however was comparatively moderate when compared with the western part of the pegmatite province.

Název v anglickém jazyce

Mineralogical and chemical composition of the Hagendorf-North Pegmatite, SE Germany - a monographic study

Popis výsledku anglicky

Hagendorf-North is a zoned Li-Nb-P-feldspar-quartz pegmatite located W of the village of Hagendorf and about 0.5 km north of the renown Hagendorf-South deposit which once was the largest feldspar pegmatite in Central Europe. Hagendorf-North also known asMeixner Mine was much smaller in size and its minerals assemblage is less variegated than that recorded from its larger "brother". However it was the site where mining began in 1860. But already before the onset of World War II, the pegmatite has no longer been considered an economic target and the mine was shut down. The reason for that small size in the shadow of this huge Hagendorf-South pegmatite is due to its overall role as feeder system to the Hagendorf-type stocklike pegmatites, which was truncated by the Pliocene chemical weathering and Pleistocene erosion, which however was comparatively moderate when compared with the western part of the pegmatite province.

Druh

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

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Neues Jahrbuch fur Mineralogie, Abhandlungen

ISSN

0077-7757

e-ISSN

—

Svazek periodika

190

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

38

Strana od-do

281-318

Kód UT WoS článku

000322766800004

EID výsledku v databázi Scopus

—