Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Anne Põldvere"'
Autor:
Yukio Isozaki, Anne Põldvere, Heikki Bauert, Hiroki Nakahata, Kazumasa Aoki, Shuhei Sakata, Takafumi Hirata
Publikováno v:
Estonian Journal of Earth Sciences, Vol 63, Iss 4, Pp 251-256 (2014)
In order to clarify the tectono-sedimentary history of Paleozoic Baltica, age spectra of detrital zircon grains from the Ediacaran (Kotlin Regional Stage) and Lower Cambrian sandstones (lowermost Lontova and Lükati formations) in western Estonia in
Externí odkaz:
https://doaj.org/article/38774cbe12764d5bb548751e738d7eb1
Publikováno v:
Estonian Journal of Earth Sciences, Vol 63, Iss 1, Pp 1-17 (2014)
A gap corresponding to several conodont and chitinozoan zones occurs in the Llandovery–Wenlock boundary interval in some sections in the western coastal region of Estonia and on islands in the Muhu Strait. New data from the Suigu (S-3) core section
Externí odkaz:
https://doaj.org/article/8b8ffb95787047bdb67f20ab9db8ff17
Autor:
Anne Kleesment, Kristjan Urtson, Tarmo Kiipli, Tõnu Martma, Anne Põldvere, Toivo Kallaste, Alla Shogenova, Kazbulat Shogenov
Publikováno v:
Estonian Journal of Earth Sciences, Vol 62, Iss 3, Pp 139-159 (2013)
The Upper Devonian Plavinas Regional Stage in southern Estonia and northern Latvia is represented by dolostones containing interlayers of dolomitic marlstones and limestones. Petrographic, cathodoluminescence, electron microprobe and isotope techniqu
Externí odkaz:
https://doaj.org/article/b701b5af38cd4895a45ad6342592cecb
Autor:
Elga Mark-Kurik, Anne Põldvere
Publikováno v:
Estonian Journal of Earth Sciences, Vol 61, Iss 1, Pp 33-47 (2012)
An updated version of the Devonian stratigraphical chart of Estonia with comments is presented. Estonian regional stratigraphical units are correlated with the standard conodont zonation and miospore zonation, used in the western part of the East Eur
Externí odkaz:
https://doaj.org/article/9d5e6af7e0a3460184f59457f7db45a2
Publikováno v:
GFF. 136:100-104
The Viki drill core is one of the reference sections for the Estonian bedrock succession, characterizing strata of Mid Ordovician through early Silurian age in the eastern part of the Baltoscandian basin. In this article, we present the hitherto miss
Autor:
Heikki Bauert, Shuhei Sakata, Kazumasa Aoki, Takafumi Hirata, Anne Põldvere, Juho Kirs, Yukio Isozaki
Publikováno v:
GFF. 136:214-217
Detrital zircon U–Pb ages of Lower Cambrian and Middle Devonian have been determined for sandstone in Estonia through LA-ICP-MS (Nu instruments, Wrexham, UK). Both sandstones have a similar zircon age spectrum with distinct age clusters that reflec
Autor:
Toivo Kallaste, Alla Shogenova, Kazbulat Shogenov, Anne Põldvere, Tõnu Martma, Tarmo Kiipli, K Urtson, A. Kleesment
Publikováno v:
Estonian Journal of Earth Sciences, Vol 62, Iss 3, Pp 139-159 (2013)
The Upper Devonian Plavinas Regional Stage in southern Estonia and northern Latvia is represented by dolostones containing interlayers of dolomitic marlstones and limestones. Petrographic, cathodoluminescence, electron microprobe and isotope techniqu
Autor:
Anne Põldvere, Elga Mark-Kurik
Publikováno v:
Estonian Journal of Earth Sciences, Vol 61, Iss 1, Pp 33-47 (2012)
An updated version of the Devonian stratigraphical chart of Estonia with comments is presented. Estonian regional stratigraphical units are correlated with the standard conodont zonation and miospore zonation, used in the western part of the East Eur
Autor:
Takafumi Hirata, Heikki Bauert, Shuhei Sakata, Hiroki Nakahata, Anne Põldvere, Kazumasa Aoki, Yukio Isozaki
Publikováno v:
Estonian Journal of Earth Sciences. 63:251
In order to clarify the tectono-sedimentary history of Paleozoic Baltica, age spectra of detrital zircon grains from the Ediacaran (Kotlin Regional Stage) and Lower Cambrian sandstones (lowermost Lontova and Lukati formations) in western Estonia in c
Publikováno v:
Estonian Journal of Earth Sciences, Vol 63, Iss 1, Pp 1-17 (2014)
A gap corresponding to several conodont and chitinozoan zones occurs in the Llandovery-Wenlock boundary interval in some sections in the western coastal region of Estonia and on islands in the Muhu Strait. New data from the Suigu (S-3) core section d