Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Avo Miidel"'
Publikováno v:
Estonian Journal of Earth Sciences, Vol 62, Iss 3, Pp 160-170 (2013)
The distribution, structure and origin of the hill range of Vaivara Sinimäed and bedrock folds are discussed. Many narrow (150–500 m), east- to northeast-trending folds with 1–10 km long axes are found in the studied area. Anticlines resulting f
Externí odkaz:
https://doaj.org/article/5eed485f0a2d4344b4da3cf55a76e566
Publikováno v:
Estonian Journal of Earth Sciences, Vol 62, Iss 3, Pp 160-170 (2013)
The distribution, structure and origin of the hill range of Vaivara Sinimäed and bedrock folds are discussed. Many narrow (150–500 m), east- to northeast-trending folds with 1–10 km long axes are found in the studied area. Anticlines resulting f
Publikováno v:
Boreas. 36:211-221
This paper describes a Geographical Information System (GIS)-based palaeogeographic reconstruction of the development of proglacial lakes formed during deglaciation in Estonia, and examines their common features and relations with the Baltic Ice Lake
Publikováno v:
GFF. 123:15-22
Seismic reflection profiling in the western part of Lake Peipsi, eastern Estonia, revealed two major units in the sedimentary bedrock, namely Devonian terrigenous rocks on top of Ordovician carbonate rocks. In the Ordovician sequence several subhoriz
Publikováno v:
GFF. 120:47-52
Shallow marine seismic reflection profiling in the western part of Lake Peipsi, eastern Estonia, has revealed new information about thickness, structure and distribution of the Quaternary deposits. Additional data from numerous drillings in the area
Publikováno v:
Estonian Journal of Earth Sciences, Vol 59, Iss 1, Pp 37-48 (2010)
The distribution, morphology, fillings, and origin of buried valleys are discussed. The direction of the valleys varies from NW to NE. Within the Viru-Harju Plateau the valleys have a more or less symmetric profile, but asymmetric profiles are domina
NEW DATA ON THE DISTRIBUTION AND STRATIGRAPHY OF THE BOTTOM DEPOSITS OF LAKE PEIPSI, EASTERN ESTONIA
Publikováno v:
Proceedings of the Estonian Academy of Sciences. Geology. 50:233
The bottom sediments of Lake Peipsi, eastern Estonia, were investigated. Earlier obtained continuous seismic reflection profiling data is compared with the coring data. Generally good accordance is found, with minor discrepancies in the southern part