<abstract xml:lang="en" xmlns="http://www.w3.org/1999/xhtml"><p>The study of the evolution of the river network in the Great Hungarian Plain has been based on sedimentological, neotectonical, morphological investigations, heavy mineral analysis and complementary OSL dating. The study area extends from the Körös sub-basin into the Ér and Berettyó river valleys which are situated northeast from the subsiding basin and northwest from the uplifting Apuseni Mountains.</p><p>The OSL ages provide evidence that a large river run in the Ér-valley at least from 46±4 to 39±4 ka. It deposited garnet and magnetite-ilmenite-rich sediments, similar to the recent Berettyó, Ér and Sebes- Körös rivers and less intensive the modern Tisza river. These sediments originated from the nearly located metamorphic and Neogene volcanic rocks and contain some reworked older clastic sedimentary rocks from the northern part of the Apuseni Mountains. These OSL ages fit the active tectonic phase of the Érmellék depression. Loess is 49-47, 44, 39 and 25 ka old and aeolian sands 10 to 9 ka were dated. Their heavy mineral composition and that of fluvial sands is similar.</p></abstract>

The study of the evolution of the river network in the Great Hungarian Plain has been based on sedimentological, neotectonical, morphological investigations, heavy mineral analysis and complementary OSL dating. The study area extends from the Körös sub-basin into the Ér and Berettyó river valleys which are situated northeast from the subsiding basin and northwest from the uplifting Apuseni Mountains.The OSL ages provide evidence that a large river run in the Ér-valley at least from 46±4 to 39±4 ka. It deposited garnet and magnetite-ilmenite-rich sediments, similar to the recent Berettyó, Ér and Sebes- Körös rivers and less intensive the modern Tisza river. These sediments originated from the nearly located metamorphic and Neogene volcanic rocks and contain some reworked older clastic sedimentary rocks from the northern part of the Apuseni Mountains. These OSL ages fit the active tectonic phase of the Érmellék depression. Loess is 49-47, 44, 39 and 25 ka old and aeolian sands 10 to 9 ka were dated. Their heavy mineral composition and that of fluvial sands is similar.

Osl Dates and Heavy Mineral Analysis of Upper Quaternary Sediments from the Valleys of the Ér and Berettyó Rivers

Geological Institute of Hungary, Stefánia út 14, 1143 Budapest, Hungary

Eötvös Loránd Geophysical Institute of Hungary, Homonna utca 1, 1118 Budapest, Hungary

Geochronometria

The study of the evolution of the river network in the Great Hungarian Plain has been based on sedimentological, neotectonical, morphological investigations,...

Osl Dates and Heavy Mineral Analysis of Upper Quaternary Sediments from the Valleys of the Ér and Berettyó Rivers

Pubblicato online: 29 ott 2007

Pagine: 17 - 23

DOI: https://doi.org/10.2478/v10003-007-0026-x

Parole chiave
OSL dating on quartz, heavy mineral analysis, river network, Érmellék, Great Hungarian Plain

This content is open access.

Osl Dates and Heavy Mineral Analysis of Upper Quaternary Sediments from the Valleys of the Ér and Berettyó Rivers

Pubblicato online: 29 ott 2007

Pagine: 17 - 23

DOI: https://doi.org/10.2478/v10003-007-0026-x

Parole chiaveOSL dating on quartz, heavy mineral analysis, river network, Érmellék, Great Hungarian Plain

This content is open access.

Parole chiave
OSL dating on quartz, heavy mineral analysis, river network, Érmellék, Great Hungarian Plain