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Thursday, July 30, 2020 | History

3 edition of Contributions to the interpretation of the Fennoscandian Border Zone found in the catalog.

Contributions to the interpretation of the Fennoscandian Border Zone

J. C. Baartman

Contributions to the interpretation of the Fennoscandian Border Zone

by J. C. Baartman

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  • 28 Currently reading

Published by I kommission hos C. A. Reitzel in København .
Written in English

    Places:
  • Denmark.,
  • Baltic Sea.
    • Subjects:
    • Geology -- Denmark.,
    • Geology -- Baltic Sea.

    • Edition Notes

      Statementby J. C. Baartman and Ole Bruun Christensen.
      Series[Skrifter] - Geological Survey of Denmark ; no. 102, Danmarks geologiske undersøgelse (Series)., nr. 102.
      ContributionsBruun Christensen, Ole, joint author.
      Classifications
      LC ClassificationsQE278 .D332 nr. 102
      The Physical Object
      Pagination47 p. :
      Number of Pages47
      ID Numbers
      Open LibraryOL4934067M
      ISBN 108742106400
      LC Control Number76361037

      Fennoscandian Lesser White-fronted Goose conservation project – Report – 5 T he Lesser White-fronted Goose (Anser erythropus, subsequently referred to as LWfG) is the most threatened arctic goose species of the Palearctic region, and the populations throughout the range from Fennoscandia to easternmost Siberia. Norway Sweden Denmark. Scandinavia is an ethno-linguistic area of north west Europe which contains the three kingdoms of Denmark, Norway and Sweden. The three countries are linked by an ethno-cultural heritage which originated in northern Germany. The three countries are also linked linguistically, by way of the ancient language known as, Old Norse, a Germanic language once spoken throughout.

        Naturally existing electromagnetic (EM) fields recorded at the surface of the Earth can be used to infer the electrical conductivity distribution of the subsurface. In the magnetovariational sounding (MVS) technique, the transient variations of orthogonal components of the Earth’s magnetic field are measured. In the frequency domain, the magnetic transfer function relates the vertical Cited by: 3. Sovremennye i pozdnegolotsenovye vertikal'nye dvizheniya zemnoj kory v Yugo-Vostochnoj Baltike--perehodnoj zone ot Fennoskandinavskogo shchita k Russkoj plite [Modern and late Holocene vertical earth crust movements in the South-Eastern Baltic as a transitional zone between the Fennoscandian shield and the Russian plate].

      Definition of Fennoscandian in the dictionary. Meaning of Fennoscandian. What does Fennoscandian mean? Information and translations of Fennoscandian in the most comprehensive dictionary definitions resource on the web. Weichselian glaciation refers to the last glacial period and its associated glaciation in northern parts of the Alpine region it corresponds to the Würm was characterized by a large ice sheet (the Fenno-Scandian ice sheet) that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, the March of Brandenburg and Northwest.


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Contributions to the interpretation of the Fennoscandian Border Zone by J. C. Baartman Download PDF EPUB FB2

The Fennoscandian Border Zone:a comparison of depositional environments and vegetation Henrik en,Lars n,Eva hus and Henning S.Sørensen Suitable climatic conditions for peat formation existed during Early–Middle Jurassic times in the Fennoscandian Border Zone.

Autochthonous peat and allochthonous organic matter were. The interpretation of newly released commercial 2-D reflection seismic data in the Kattegat area, Denmark, has provided a better understanding of the tectonic processes along the Tornquist strike-slip fault zone.

One of the major faults in this zone is the Børglum Fault, which has been active in several different periods since the Late by: 4. Fennoscandian Border Zone (Tornquist Line) An ancient Caledonian lineation separating the crystalline mass of Scandinavia and Russia from the fragmented crustal blocks of the remainder of north-western NW—SE trending structural feature complements the major Caledonian faults of northern Scotland (Great Glen Fault, Highland Boundary Fault, etc.).

During the Mesozoic, the Fennoscandian Border Zone was divided into two zones: the Sorgenfrei-Tornquist Zone to the west and the Skagerrak-Kattegat Platform to the east.

Tectonic activity during the Mesozoic can only be testified for the Sorgenfrei-Tornquist by: Map showing the structural outline of the Fennoscandian Border Zone and the location of Bornholm and the Øresund, Skagen-2 and Frederikshavn-3 wells. Modified from Liboriussen et al.

The new Khibiny National Park is located about kilometres from the Finnish border, in the central part of the Kola Peninsula. The national park belongs to the Green Belt of Fennoscandia that is composed of nature conservation areas in the border regions of Finland, Norway and Russia.

Fennoscandian Mineral Deposits Download the database Disclaimer Explanation book for metallogenic map ( MB) FODD Explanation Book ( kB) Disclaimer Explanation book for metallogenic map ( MB) FODD Explanation Book ( kB).

National working group of Fennoscandian Green Belt in the 5th of Febryary The working period the group will be from th 6th of February to the 31th of December of The task of working group is develop cooperation in Fennoscandian green belt according.

In the shield part of the profiles northeast of the Sorgenfrei-Tornquist Zone, crustal reflectivity is observed at all levels and its termination in depth coincides largely with the crust-mantle boundary.

the wide-angle data indicate a three-layer crust with velocities of –, circaand – km s −1. the Moho is found between.

Digging deeper in Fennoscandian ancestry II This is a continuation of the previous analysis was run through Finestructures clustering processing but it was unable to differentiate the remaining Scandinavians meaning it appeared by the software to be one population.

However in the PCA plot it was possible to infer structure. the Fennoscandian Shield underlying Norway, Sweden, Finland, and Northern Denmark; Baltic Shield. (culture) the culture group comprising the Finnic, Sami, and Scandinavian cultures. Usage notes. Unlike the term ‘Nordic countries’, Fennoscandia does not include Iceland, Greenland, or other geographically disconnected overseas areas.

The interpretation of the new 2D seismic data and the resulting revision of the structural model influence the further plans for data collection, drilling planning and injection : Lars Henrik Nielsen.

Fennoscandia or Fenno-Scandinavia is the region including the Scandinavian Peninsula, Finland, Karelia, and the Kola Peninsula. The term usually covers the countries Finland, Norway, and Sweden in their entireties. It also includes a part of name comes from the Latin words Fennia (which means Finland) and Scandia (which means Scandinavia).

Protected Areas in Northern Fennoscandia Finland is situated on the western margin of the large coniferous forest – the taiga – that extends across the whole of northern Russia. The western parts of the taiga belt are relatively intact on the Russian side of the border, with a diverse tree species composition and a high diversity of animals.

The logical approach to unravel the mystery of the Fennoscandian history is to look at it rationally, in a sequence of events in the history of the Fennoscandia with a timeline, the gradual process how and where the peoples traveled, settled left rock art and cave paintings and other antiquities and at some places later grew into larger community.

I think that it would be interesting to compare our Fennoscandian component scores from the Eurogenes K36 test at GEDmatch. I have been in contact recently with David about this and he told me that even though we know about ancient components these days such as ANE, WHG and EEF the other components from his other tests such as this one are still useful for working out more recent.

Fennoscandia is a term that represent geographically and geologically regions that comprise Norway, Sweden Finland and the the land of the Nomadic Sami It is located in the northern Europe region of the Fennoscandian. According to archeological study and evidence the area was settled around BC in the era of the stone age where by the.

The bedrock of Skåne, the southernmost province of Sweden, has been targeted for geothermal feasibility studies since the late s. An exploration project concerning the geothermal potential in the Romeleåsen Fault Zone was launched outside the town of Lund in Besides geophysical imaging of the thrust fault zone, the investigations included drilling and investigations of a Cited by: 1.

Lithological formation classification of the basin units (from Michelsen, ) and the seismic layer subdivision as used in the starting model for the ray tracing interpretation. Typical sonic log interval velocities are given. SEISMIC MODELLING OF THE NORWEGIAN-DANISH BASIN 40 60 tance from SP 10 (km) Fig.

by: 2. The Vihanti-Pyhäsalmi district is located at the border zone between the Archaean craton in the northeast and the Palaeoproterozoic Svecofennian domain Cited by: 2. Fennoscandian Border Zone (Gravesen et al. ; Jørgart & Nielsen ). Several publications deal with the stratigraphy and facies of the Arnager Limestone For-mation (Bromley ; Christensen ; Tröger & Chris-tensen ), and the first palaeoecological interpretation of the sponge-rich limestone was given by Noe-Nygaard.As we can see the different models appear to give different results and its due to that in geneology the La Braña 1 closest to Basque, Sardinians and Western Europeans but in ancient ancestry closest to Finns and clustering in geneology with Basque, Sardinians and Western Europeans in the linked model make sense as the La Braña 1 individual was found in today northern Spain.

Geologic interpretation of gravity and magnetic data over the central part of the Duluth Complex, northeastern Minnesota. Economic Geology Crossref, Google Scholar. Chandler, V.W., and Lively, R.S. Cited by: 7.