Mineralogy of Burning-Coal Waste Piles in Collieries of the Czech Republic : (chapter 5)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F15%3A00443048" target="_blank" >RIV/67985831:_____/15:00443048 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/B978-0-444-59509-6.00005-3" target="_blank" >http://dx.doi.org/10.1016/B978-0-444-59509-6.00005-3</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/B978-0-444-59509-6.00005-3" target="_blank" >10.1016/B978-0-444-59509-6.00005-3</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Mineralogy of Burning-Coal Waste Piles in Collieries of the Czech Republic : (chapter 5)

Popis výsledku v původním jazyce

Due to long-lasting tradition of coal mining and industrial history on the territory of Czech Republic, significant amount of waste piles of various ages and scales occur. Many of them, along with scarce occurrences of naturally burned coal measures, spontaneously ignited and subsequently, served as a source of diverse assemblage of newly formed minerals – products of pyrometamorphism, alteration, and sublimation. Several new minerals associated with combustion metamorphism were first described from the Czech Republic: tschermigite (1853), rosickýite (1931), letovicite (1932), kratochvílite (1937), kladnoite (1942), koktaite (1948), and rostite (1979). This chapter mainly focuses on two most famous localities, both situated to the Carboniferous sedimentary basins: Kladno Coal District in Central Bohemia near the capital Prague and Radvanice at Trutnov in Eastern Bohemia, close to border with Poland. These two localities, which were studied in detail, provided nearly 100 recently formed minerals and unnamed compounds.

Název v anglickém jazyce

Mineralogy of Burning-Coal Waste Piles in Collieries of the Czech Republic : (chapter 5)

Popis výsledku anglicky

Due to long-lasting tradition of coal mining and industrial history on the territory of Czech Republic, significant amount of waste piles of various ages and scales occur. Many of them, along with scarce occurrences of naturally burned coal measures, spontaneously ignited and subsequently, served as a source of diverse assemblage of newly formed minerals – products of pyrometamorphism, alteration, and sublimation. Several new minerals associated with combustion metamorphism were first described from the Czech Republic: tschermigite (1853), rosickýite (1931), letovicite (1932), kratochvílite (1937), kladnoite (1942), koktaite (1948), and rostite (1979). This chapter mainly focuses on two most famous localities, both situated to the Carboniferous sedimentary basins: Kladno Coal District in Central Bohemia near the capital Prague and Radvanice at Trutnov in Eastern Bohemia, close to border with Poland. These two localities, which were studied in detail, provided nearly 100 recently formed minerals and unnamed compounds.

Druh

C - Kapitola v odborné knize

CEP obor

—

OECD FORD obor

10504 - Mineralogy

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název knihy nebo sborníku

Coal and Peat Fires: a Global Perspective

ISBN

978-0-444-59509-6

Počet stran výsledku

61

Strana od-do

110-159

Počet stran knihy

817

Název nakladatele

Elsevier

Místo vydání

Amsterdam

Kód UT WoS kapitoly

000410545500008