2019
DOI: 10.19110/2221-1381-2019-11-3-8
|View full text |Cite
|
Sign up to set email alerts
|

New schemes of isobases of uplift of northeastern Fennoscandia for the last 10,000 years

Abstract: Новые схемы изобаз подНятия северо-востока ФеННоскаНдии за последНие 10 тысяч лет Д. С. Толстобров, В. В. Колька Геологический институт Кольского научного центра РАН, Апатиты tolstobrov@geoksc.apatity.ru Íà îñíîвàíèè дàííых îб àìпëèòóдå пîдíяòèя, пîëó÷åííых пðè èзó÷åíèè дîííых îñàдкîв èзîëèðîвàííых бàññåйíîв ñåвåðî-вîñòîкà Фåííîñкàíдèè, быëè пîñòðîåíы íîвыå ñхåìы èзîбàз. Пîдíяòèå îöåíèвàëîñь зà пîñëåдíèå 10 òыñ. ëåò. Дëя пîñòðîåíèя ñхåì èзîбàз пîдíяòèя быëè èñпîëьзîвàíы èíòåðпîëяöèîííыå (тðèàíгóляöèя с лèíåйíî… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2023
2023
2023
2023

Publication Types

Select...
1

Relationship

0
1

Authors

Journals

citations
Cited by 1 publication
(1 citation statement)
references
References 5 publications
0
1
0
Order By: Relevance
“…It should be note that, according to data available from the Murmansk coast (Corner et al, 2001; Marthinussen, 1974; Tolstobrov and Kolka, 2019), the uplift isobases are drawn parallel to the coast. Since the studied lakes are located along the coastline (Figure 1), we can assume that any change in shoreline gradient resulting from possible tilt over time, is negligible and does not require a correction in the reconstructions.…”
Section: Methodsmentioning
confidence: 99%
“…It should be note that, according to data available from the Murmansk coast (Corner et al, 2001; Marthinussen, 1974; Tolstobrov and Kolka, 2019), the uplift isobases are drawn parallel to the coast. Since the studied lakes are located along the coastline (Figure 1), we can assume that any change in shoreline gradient resulting from possible tilt over time, is negligible and does not require a correction in the reconstructions.…”
Section: Methodsmentioning
confidence: 99%