Vidzemes augstienes kēmu terasu morfoloģija un veidošanās paleoģeogrāfiskie apstākļi

6533b839fe1ef96bd12a5edd

RESEARCH PRODUCT

Vidzemes augstienes kēmu terasu morfoloģija un veidošanās paleoģeogrāfiskie apstākļi

Māris Dauškans

subject

description

Maģistra darbs veltīts par kēmu terašu pētījumiem Vidzemes augstienē. Kēmu terašu veidošanās apstākļu izzināšanā izmantoti šo reljefa formu morfoloģijas un iekšējās uzbūves pētījumi, kā arī nogulumu vecuma noteikšana, izmantojot OSL metodi, kā arī nesen veiktie laukakmeņu 10Be kosmogēnā vecuma datējumi. Veiktie kēmu terašu pētījumi liecina par to morfoloģisko un ģenētiso daudzveidību. Tie deva iespēju izveidot kēmu terašu klasifikāciju un nošķirt erozijas un akumulācijas tipa terases. Savukārt, iegūtie OSL datējumu rezultāti ir nozīmīgi, lai pilnveidotu kontinentālā segledāja izkušanas hronoloģiju Vidzemes augstienē un tai pieguļošajā teritorijā. Nogulumu datēšanas rezultāti liek secināt, ka Vidzemes augstienes dienvidaustrumu nogāzes kēmu terases augstākos līmeņus veido glaciofluviālie nogulumi, kas varēja uzkrāties pēdējā segledāja transgresijas etapā vēlā pleniglaciāla sākumposmā, bet kēmu terašu hipsometriski zemākie līmeņi veidojās pirms un pēc agrās lobveida deglaciācijas fāzes – Linkuvas ledāja malas oscilācijas. Tas apstiprina iepriekš izteikto hipotēzi, ka kēmu terases dažādus līmeņus veidojošie nogulumi ievērojami atšķiras pēc vecuma. Raksturvārdi: kēmu terases, glaciofluviālie nogulumi, glaciolimniskie nogulumi, glaciokarsts, OSL datējumi, morfoloģija, saguluma apstākļi, veidošanās apstākļi.

year	journal	country	edition	language
2008-01-01

https://dspace.lu.lv/dspace/handle/7/23988

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