2016
DOI: 10.21638/11701/spbu07.2016.208
|View full text |Cite
|
Sign up to set email alerts
|

Rural settlement recreational space

Abstract: 85 УДК 911.53,911.373 Ж. Б. Соломина, Г. Н. Шастина РЕКРЕАЦИОННОЕ ПРОСТРАНСТВО СЕЛЬСКИХ ПОСЕЛЕНИЙ Санкт-Петербургский государственный университет, Российская Федерация, 199034, Санкт-Петербург, Университетская наб., 7-9 В статье исследовано рекреационное пространство сельских населенных пунктов. Выяв-лена его зональная структура. Дана оценка трансформации местного рекреационного про-странства под влиянием «неместной» рекреации (организованной, дачной, самодеятельной). Выявлены самостоятельные рекреацио… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2018
2018
2024
2024

Publication Types

Select...
3

Relationship

0
3

Authors

Journals

citations
Cited by 3 publications
(1 citation statement)
references
References 0 publications
0
1
0
Order By: Relevance
“…The water edge (brine) in the lake is 21 m below the level of the Caspian Sea. Lake Baskunchak arose in the western part of the Caspian lowland as a result of salt dome tectonics -as a compensatory depression (mulda) located between salt domes and having a thickness of lake sediments of Quaternary age over 270 m [1]. The salt domes of this area have a similar structure and are represented by a thickness of halite (according to geophysical data, their thickness exceeds 800 m), covered in the roof with gypsum deposits with a thickness from the first tens to 80 m. The depth of the "plaster hat" varies from 0 to 50 m [1].…”
Section: Introductionmentioning
confidence: 99%
“…The water edge (brine) in the lake is 21 m below the level of the Caspian Sea. Lake Baskunchak arose in the western part of the Caspian lowland as a result of salt dome tectonics -as a compensatory depression (mulda) located between salt domes and having a thickness of lake sediments of Quaternary age over 270 m [1]. The salt domes of this area have a similar structure and are represented by a thickness of halite (according to geophysical data, their thickness exceeds 800 m), covered in the roof with gypsum deposits with a thickness from the first tens to 80 m. The depth of the "plaster hat" varies from 0 to 50 m [1].…”
Section: Introductionmentioning
confidence: 99%