The structure of the lithosphere of the Cameroon fault zone according to deep seismic sounding
Two models of the lithosphere structure are being compared corresponding to two variants of interpretation of DSS wave fields registered on the intersection of the Angola-Brazil geotraverse with Cameroon fracture zone in the area of transition between the east flank of middle ridge and the Angola ba...
Збережено в:
| Дата: | 2012 |
|---|---|
| Автори: | , , |
| Формат: | Стаття |
| Мова: | Російська |
| Опубліковано: |
S. Subbotin Institute of Geophysics of the NAS of Ukraine
2012
|
| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/116587 |
| Теги: |
Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|
| Назва журналу: | Geofizicheskiy Zhurnal |
Репозитарії
Geofizicheskiy Zhurnal| _version_ | 1856543247093989376 |
|---|---|
| author | Tulina, Yu. V. Burmin, V. Yu. Shemeleva, I. B. |
| author_facet | Tulina, Yu. V. Burmin, V. Yu. Shemeleva, I. B. |
| author_sort | Tulina, Yu. V. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T12:02:45Z |
| description | Two models of the lithosphere structure are being compared corresponding to two variants of interpretation of DSS wave fields registered on the intersection of the Angola-Brazil geotraverse with Cameroon fracture zone in the area of transition between the east flank of middle ridge and the Angola basin. Special features of the fields have been revealed and interpreted by the authors, which prove the model with subvertical low-velocities intrusions into high-velocity layered mantle with really reached depth of seismic waves penetration about 40 km opposite the previously published model with the alternation of the high-velocity and low-velocity subhorizontal layers with relatively increased and decreased velocities and the depth of the lighting the section up to 80 km. |
| first_indexed | 2025-07-17T11:07:02Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-116587 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:07:02Z |
| publishDate | 2012 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1165872020-10-07T12:02:45Z The structure of the lithosphere of the Cameroon fault zone according to deep seismic sounding Tulina, Yu. V. Burmin, V. Yu. Shemeleva, I. B. Two models of the lithosphere structure are being compared corresponding to two variants of interpretation of DSS wave fields registered on the intersection of the Angola-Brazil geotraverse with Cameroon fracture zone in the area of transition between the east flank of middle ridge and the Angola basin. Special features of the fields have been revealed and interpreted by the authors, which prove the model with subvertical low-velocities intrusions into high-velocity layered mantle with really reached depth of seismic waves penetration about 40 km opposite the previously published model with the alternation of the high-velocity and low-velocity subhorizontal layers with relatively increased and decreased velocities and the depth of the lighting the section up to 80 km. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116587 10.24028/gzh.0203-3100.v34i1.2012.116587 Geofizicheskiy Zhurnal; Vol. 34 No. 1 (2012); 63-77 Геофизический журнал; Том 34 № 1 (2012); 63-77 Геофізичний журнал; Том 34 № 1 (2012); 63-77 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116587/110614 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | Tulina, Yu. V. Burmin, V. Yu. Shemeleva, I. B. The structure of the lithosphere of the Cameroon fault zone according to deep seismic sounding |
| title | The structure of the lithosphere of the Cameroon fault zone according to deep seismic sounding |
| title_full | The structure of the lithosphere of the Cameroon fault zone according to deep seismic sounding |
| title_fullStr | The structure of the lithosphere of the Cameroon fault zone according to deep seismic sounding |
| title_full_unstemmed | The structure of the lithosphere of the Cameroon fault zone according to deep seismic sounding |
| title_short | The structure of the lithosphere of the Cameroon fault zone according to deep seismic sounding |
| title_sort | structure of the lithosphere of the cameroon fault zone according to deep seismic sounding |
| url | https://journals.uran.ua/geofizicheskiy/article/view/116587 |
| work_keys_str_mv | AT tulinayuv thestructureofthelithosphereofthecameroonfaultzoneaccordingtodeepseismicsounding AT burminvyu thestructureofthelithosphereofthecameroonfaultzoneaccordingtodeepseismicsounding AT shemelevaib thestructureofthelithosphereofthecameroonfaultzoneaccordingtodeepseismicsounding AT tulinayuv structureofthelithosphereofthecameroonfaultzoneaccordingtodeepseismicsounding AT burminvyu structureofthelithosphereofthecameroonfaultzoneaccordingtodeepseismicsounding AT shemelevaib structureofthelithosphereofthecameroonfaultzoneaccordingtodeepseismicsounding |