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Lopolit Bibliografia | Zobacz też | Menu nawigacyjne830183626

Multi tool use
Multi tool use

PlutonizmWulkanizmStruktury geologiczne


intruzjasoczewkiżyłamagmyogniska magmowegolakkolitu












Lopolit




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Lopolit – duża intruzja o kształcie odwróconego bochenka albo soczewki płasko-wypukłej lub wklęsło-wypukłej, odwróconej wypukłością ku dołowi. Zaburza warstwy leżące poniżej, pozostawiając bez zmian warstwy nadległe. Od spodu zazwyczaj dochodzi żyła, stanowiąca pozostałość po dopływie magmy z ogniska magmowego. Jest więc jakby odwrotnością lakkolitu.


Przypuszcza się, że opisany wyżej kształt lopolitu, o wypukłości skierowanej ku dołowi, jest spowodowany zapadaniem się nadkładu niżej leżącego ogniska magmowego w miarę wydobywania się z niego materiału wypełniającego intruzję.



Bibliografia |



  • WojciechW. Jaroszewski WojciechW., LeszekL. Marks LeszekL., AndrzejA. Radomski AndrzejA., Słownik geologii dynamicznej, Warszawa: Wydawnictwa Geologiczne, 1985, ISBN 83-220-0196-7, OCLC 830183626 .;


Zobacz też |


  • lakkolit

  • batolit




Źródło: „https://pl.wikipedia.org/w/index.php?title=Lopolit&oldid=53929886”










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