Trace elements in Upper Devonian rocks of the Andoma Hill zone of fold-and-fault dislocations (southeastern Onega region) as indicators of source areas
The paper reports the results of lithogeochemical studies of the Upper Devonian rocks from the Andoma Hill zone of fold-and-fault dislocations (SE Onega region). The rocks are characterized by the negative Eu anomaly (from 0.4 to 0.65) that maks them different from modern sediments of the White Sea....
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| Veröffentlicht in: | Lithology and Mineral Resources 2017-07, Vol.52 (4), p.319-333 |
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| container_title | Lithology and Mineral Resources |
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| creator | Terekhov, E. N. Baluev, A. S. Kolodyazhnyi, S. Yu Belokrys, M. A. |
| description | The paper reports the results of lithogeochemical studies of the Upper Devonian rocks from the Andoma Hill zone of fold-and-fault dislocations (SE Onega region). The rocks are characterized by the negative Eu anomaly (from 0.4 to 0.65) that maks them different from modern sediments of the White Sea. The latter can be regarded as the average composition of mainly Archean (Karelian–Kola) part of the Baltic Shield. In terms of the contents of some trace elements, they also differ from the Vendian rocks of the Zimnii Bereg area. Since the considered rocks are geochemically similar to the Svecofennian metamorphic rocks and Paleoproterozoic granite rapakivi, they could be formed by the erosion of these complexes. The clastic material was transported via a channel confined to the Baltic Shield and Russian Platform junction known as the Polkanov geoflexure. |
| doi_str_mv | 10.1134/S0024490217040071 |
| format | Article |
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Since the considered rocks are geochemically similar to the Svecofennian metamorphic rocks and Paleoproterozoic granite rapakivi, they could be formed by the erosion of these complexes. The clastic material was transported via a channel confined to the Baltic Shield and Russian Platform junction known as the Polkanov geoflexure.</description><subject>Baltic Shield (Europe)</subject><subject>Composition</subject><subject>Devonian</subject><subject>Dislocations</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Erosion</subject><subject>Fault lines</subject><subject>Geochemistry</subject><subject>Granite</subject><subject>Indicators</subject><subject>Isotopes</subject><subject>Metamorphic rocks</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Plate tectonics</subject><subject>Rock</subject><subject>Sediment</subject><subject>Sedimentology</subject><subject>Sediments</subject><subject>Trace elements</subject><issn>0024-4902</issn><issn>1608-3229</issn><issn>1573-8892</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kMtOwzAQRS0EEqXwAewssYFFwI8kjpdVeUqVugDW0TQel0BqFztFgh_hd3EoCyTEajRzz507GkKOOTvnXOYX94yJPNdMcMVyxhTfISNesiqTQuhdMhrkbND3yUGMzyz1SvMR-XwI0CDFDlfo-khbRx_Xawz0Et-8a8HR4JuXSL2l_RPSiTN-BfS27Tr64R0Oc-s7k4EzmYVN11PTxs430LfeRXoa_Sb5IPYYHJ07XAINuEzaGYUhzbQJ9eE7ILEh3QIh8Ydkz0IX8einjsnj9dXD9DabzW_uppNZBlLqPisrYxcSF1Y1ALbiqIpSaLlQAvPC2sJIzjUrQZQFNFItlMkbDcKawuqqsFKOycl27zr41w3Gvn5OV7gUWXPNVSVEUQ4U31JN8DEGtPU6tCsI7zVn9fD_-s__k0dsPTGxbonh1-Z_TV_Hvokg</recordid><startdate>20170701</startdate><enddate>20170701</enddate><creator>Terekhov, E. 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The latter can be regarded as the average composition of mainly Archean (Karelian–Kola) part of the Baltic Shield. In terms of the contents of some trace elements, they also differ from the Vendian rocks of the Zimnii Bereg area. Since the considered rocks are geochemically similar to the Svecofennian metamorphic rocks and Paleoproterozoic granite rapakivi, they could be formed by the erosion of these complexes. The clastic material was transported via a channel confined to the Baltic Shield and Russian Platform junction known as the Polkanov geoflexure.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0024490217040071</doi><tpages>15</tpages></addata></record> |
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| subjects | Baltic Shield (Europe) Composition Devonian Dislocations Earth and Environmental Science Earth Sciences Erosion Fault lines Geochemistry Granite Indicators Isotopes Metamorphic rocks Mineral Resources Mineralogy Plate tectonics Rock Sediment Sedimentology Sediments Trace elements |
| title | Trace elements in Upper Devonian rocks of the Andoma Hill zone of fold-and-fault dislocations (southeastern Onega region) as indicators of source areas |
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