Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications
Vinogradov, V. I. ; Murav'ev, V. I. ; Bujakaite, M. I. ; Golovin, D. I. ; Gorozhanin, V. M. ; Veis, A. F.
Springer
Published 2000
Springer
Published 2000
| ISSN: |
1608-3229
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|---|---|
| Source: |
Springer Online Journal Archives 1860-2000
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| Topics: |
Geosciences
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| Notes: |
Abstract The Rb–Sr and K–Ar characteristics of whole-rock argillite samples from the Middle Riphean Yurmatinian Group have been studied. The timing of final rock alteration was estimated at 525 ± 30 Ma by the Rb–Sr geochronometer. In the section near the Bol'shoi Avzhyan Settlement, the rocks experienced alteration up to the stage of deep epigenesis. The K–Ar data indicate that rock alterations continued after the Rb–Sr system conservation and was accompanied by a gradual gain of K. The great temporal gap between alterations of Middle and Lower Riphean rocks was established in the southern Urals. This gap may be explained either by the affiliation of sampled rocks to different tectonic units or by principal errors in stratigraphic correlations.
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| Type of Medium: |
Electronic Resource
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| URL: |
| _version_ | 1798297319686275072 |
|---|---|
| autor | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. |
| autorsonst | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. |
| book_url | http://dx.doi.org/10.1023/A:1026601616053 |
| datenlieferant | nat_lic_papers |
| hauptsatz | hsatz_simple |
| identnr | NLM198718063 |
| issn | 1608-3229 |
| journal_name | Lithology and mineral resources |
| materialart | 1 |
| notes | Abstract The Rb–Sr and K–Ar characteristics of whole-rock argillite samples from the Middle Riphean Yurmatinian Group have been studied. The timing of final rock alteration was estimated at 525 ± 30 Ma by the Rb–Sr geochronometer. In the section near the Bol'shoi Avzhyan Settlement, the rocks experienced alteration up to the stage of deep epigenesis. The K–Ar data indicate that rock alterations continued after the Rb–Sr system conservation and was accompanied by a gradual gain of K. The great temporal gap between alterations of Middle and Lower Riphean rocks was established in the southern Urals. This gap may be explained either by the affiliation of sampled rocks to different tectonic units or by principal errors in stratigraphic correlations. |
| package_name | Springer |
| publikationsjahr_anzeige | 2000 |
| publikationsjahr_facette | 2000 |
| publikationsjahr_intervall | 7999:2000-2004 |
| publikationsjahr_sort | 2000 |
| publisher | Springer |
| reference | 35 (2000), S. 571-582 |
| search_space | articles |
| shingle_author_1 | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. |
| shingle_author_2 | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. |
| shingle_author_3 | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. |
| shingle_author_4 | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. |
| shingle_catch_all_1 | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications Abstract The Rb–Sr and K–Ar characteristics of whole-rock argillite samples from the Middle Riphean Yurmatinian Group have been studied. The timing of final rock alteration was estimated at 525 ± 30 Ma by the Rb–Sr geochronometer. In the section near the Bol'shoi Avzhyan Settlement, the rocks experienced alteration up to the stage of deep epigenesis. The K–Ar data indicate that rock alterations continued after the Rb–Sr system conservation and was accompanied by a gradual gain of K. The great temporal gap between alterations of Middle and Lower Riphean rocks was established in the southern Urals. This gap may be explained either by the affiliation of sampled rocks to different tectonic units or by principal errors in stratigraphic correlations. 1608-3229 16083229 Springer |
| shingle_catch_all_2 | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications Abstract The Rb–Sr and K–Ar characteristics of whole-rock argillite samples from the Middle Riphean Yurmatinian Group have been studied. The timing of final rock alteration was estimated at 525 ± 30 Ma by the Rb–Sr geochronometer. In the section near the Bol'shoi Avzhyan Settlement, the rocks experienced alteration up to the stage of deep epigenesis. The K–Ar data indicate that rock alterations continued after the Rb–Sr system conservation and was accompanied by a gradual gain of K. The great temporal gap between alterations of Middle and Lower Riphean rocks was established in the southern Urals. This gap may be explained either by the affiliation of sampled rocks to different tectonic units or by principal errors in stratigraphic correlations. 1608-3229 16083229 Springer |
| shingle_catch_all_3 | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications Abstract The Rb–Sr and K–Ar characteristics of whole-rock argillite samples from the Middle Riphean Yurmatinian Group have been studied. The timing of final rock alteration was estimated at 525 ± 30 Ma by the Rb–Sr geochronometer. In the section near the Bol'shoi Avzhyan Settlement, the rocks experienced alteration up to the stage of deep epigenesis. The K–Ar data indicate that rock alterations continued after the Rb–Sr system conservation and was accompanied by a gradual gain of K. The great temporal gap between alterations of Middle and Lower Riphean rocks was established in the southern Urals. This gap may be explained either by the affiliation of sampled rocks to different tectonic units or by principal errors in stratigraphic correlations. 1608-3229 16083229 Springer |
| shingle_catch_all_4 | Vinogradov, V. I. Murav'ev, V. I. Bujakaite, M. I. Golovin, D. I. Gorozhanin, V. M. Veis, A. F. Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications Abstract The Rb–Sr and K–Ar characteristics of whole-rock argillite samples from the Middle Riphean Yurmatinian Group have been studied. The timing of final rock alteration was estimated at 525 ± 30 Ma by the Rb–Sr geochronometer. In the section near the Bol'shoi Avzhyan Settlement, the rocks experienced alteration up to the stage of deep epigenesis. The K–Ar data indicate that rock alterations continued after the Rb–Sr system conservation and was accompanied by a gradual gain of K. The great temporal gap between alterations of Middle and Lower Riphean rocks was established in the southern Urals. This gap may be explained either by the affiliation of sampled rocks to different tectonic units or by principal errors in stratigraphic correlations. 1608-3229 16083229 Springer |
| shingle_title_1 | Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications |
| shingle_title_2 | Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications |
| shingle_title_3 | Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications |
| shingle_title_4 | Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications |
| sigel_instance_filter | dkfz geomar wilbert ipn albert fhp |
| source_archive | Springer Online Journal Archives 1860-2000 |
| timestamp | 2024-05-06T10:06:06.943Z |
| titel | Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications |
| titel_suche | Epigenesis of Middle Riphean Rocks in the Bashkir Meganticlinorium, Southern Urals: Timing of Alterations and Geological Implications |
| topic | TE-TZ |
| uid | nat_lic_papers_NLM198718063 |