Determining clast and magnetic fabric of a subaqueous lahar deposit as a tool for reconstructing paleoflow directions and emplacement processes.

Flow-related fabric of a subaqueously emplaced laharic deposit (Rám Hill Pumiceous Sandstone) were investigated around the middle Miocene Keserűs Hill lava dome group (northern Hungary). A twofold methodology, consisting of image analyis on rock surfaces and low-field anisotropy of magnetic suscepti...

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Xehetasun bibliografikoak

Argitaratua izan da:	Repository of the Academy's Library (Library of the Hungarian Academy of Sciences)
Egile nagusia:	Tamás Bíró
Beste egile batzuk:	Dávid Karátson, Emő Márton, Sándor Józsa
Formatua:	Artikulua
Hizkuntza:	ingelesa
Argitaratua:	Library and Information Centre of the Hungarian Academy of Sciences 2014
Gaiak:	Geological formations and processes Geomagnetism and Paleomagnetism Studies Landslides and related hazards lahar deposits magnetic fabric clast fabric anisotropy of magnetic susceptibility paleoflow direction shear direction aggradation Miocene volcanism
Sarrera elektronikoa:	http://real.mtak.hu/20623/1/Biro_etal_ESSEWECA2014_abstract.pdf
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