The new Nb-P aplite at Reinhardsrieth: A keystone in the lateral and depth zonations of the Hagendorf-Pleystein Pegmatite Field, SE Germany

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F15%3A00087125" target="_blank" >RIV/00216224:14310/15:00087125 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.oregeorev.2015.04.015" target="_blank" >http://dx.doi.org/10.1016/j.oregeorev.2015.04.015</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.oregeorev.2015.04.015" target="_blank" >10.1016/j.oregeorev.2015.04.015</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The new Nb-P aplite at Reinhardsrieth: A keystone in the lateral and depth zonations of the Hagendorf-Pleystein Pegmatite Field, SE Germany

Popis výsledku v původním jazyce

The Hagendorf-Pleystein Pegmatite Field (HPPF) is the largest pegmatite concentration in Central-Europe, which has been intensively studied for its mineralogy, mainly at Hagendorf-South pegmatite stock. It was not until recently that the lateral and depth zonations of the HPPF could be clarified when the newly discovered tabular aplite at Reinhardsrieth aplite has been found at transition into the so-called barren zone devoid of rare metals. Thereby the theory of the derivation of the HPPF felsic mobilizates as a result of a successive differentiation of a pegmatitic melt from the Flossenburg Granite has to be discarded. From the structural and lithological point of view, stock-like, well zoned pegmatites, e.g. Hagendorf-South, developed in the hinge zone, whereas tabular aplites, such as Reinhardsrieth, evolved along the limb zone of strongly folded basement rocks.

Název v anglickém jazyce

The new Nb-P aplite at Reinhardsrieth: A keystone in the lateral and depth zonations of the Hagendorf-Pleystein Pegmatite Field, SE Germany

Popis výsledku anglicky

The Hagendorf-Pleystein Pegmatite Field (HPPF) is the largest pegmatite concentration in Central-Europe, which has been intensively studied for its mineralogy, mainly at Hagendorf-South pegmatite stock. It was not until recently that the lateral and depth zonations of the HPPF could be clarified when the newly discovered tabular aplite at Reinhardsrieth aplite has been found at transition into the so-called barren zone devoid of rare metals. Thereby the theory of the derivation of the HPPF felsic mobilizates as a result of a successive differentiation of a pegmatitic melt from the Flossenburg Granite has to be discarded. From the structural and lithological point of view, stock-like, well zoned pegmatites, e.g. Hagendorf-South, developed in the hinge zone, whereas tabular aplites, such as Reinhardsrieth, evolved along the limb zone of strongly folded basement rocks.

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

—

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

ORE GEOLOGY REVIEWS

ISSN

0169-1368

e-ISSN

—

Svazek periodika

70

Číslo periodika v rámci svazku

October

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

20

Strana od-do

208-227

Kód UT WoS článku

000356734500012

EID výsledku v databázi Scopus

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