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SOURCES OF MAGNETIC ANOMALIES IN THE PRE-TERTIARY BASEMENT OF EASTERN SLOVAKIA (CZECHO-SLOVAKIA)

In: Geologica Carpathica, vol. 42, no. 3
Ivan Gnojek - Dusan Hovorka - Lubomil Pospisil
Detaily:
Rok, strany: 1991, 169 - 180
Jazyk: eng
O článku:
Quantitative interpretation of magnetic anomalies,the sources of which lie in the Inner Carpathian subjacent rocks in eastern Slovakia, have made it possible to determine probable locations of these sources in a geological section. Derived aeromagnetic maps have provided information on areal distribution of these specific rocks partly underlying near-surface neovolcanic complexes. Petrophysical studies of rock drillcore samples have shown that the magnetic anomalies are caused by variously serpentinized (lizardite, chrysotile) peridotites resembling highly serpentinized spinel peridotites present in a number of tectonically confined bodies of the Meliata Group. The above-mentioned common characteristics make us assume mutual genetic relationships between these rocks, and their common spatial as well as temp oral origin during the formation of the "Meliata-Vardar" oceanic crust.
Ako citovať:
ISO 690:
Gnojek, I., Hovorka, D., Pospisil, L. 1991. SOURCES OF MAGNETIC ANOMALIES IN THE PRE-TERTIARY BASEMENT OF EASTERN SLOVAKIA (CZECHO-SLOVAKIA). In Geologica Carpathica, vol. 42, no.3, pp. 169-180. 1335-0552.

APA:
Gnojek, I., Hovorka, D., Pospisil, L. (1991). SOURCES OF MAGNETIC ANOMALIES IN THE PRE-TERTIARY BASEMENT OF EASTERN SLOVAKIA (CZECHO-SLOVAKIA). Geologica Carpathica, 42(3), 169-180. 1335-0552.