Crustal structure and upper mantle anisotropy of the Afar triple junction
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F21%3A00546491" target="_blank" >RIV/67985530:_____/21:00546491 - isvavai.cz</a>
Result on the web
<a href="https://earth-planets-space.springeropen.com/articles/10.1186/s40623-021-01495-0" target="_blank" >https://earth-planets-space.springeropen.com/articles/10.1186/s40623-021-01495-0</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1186/s40623-021-01495-0" target="_blank" >10.1186/s40623-021-01495-0</a>
Alternative languages
Result language
angličtina
Original language name
Crustal structure and upper mantle anisotropy of the Afar triple junction
Original language description
The Afar region is a tectonically distinct area useful for studying continental break-up and rifting. Various conflicting models have been suggested to explain the lateral variations of the anisotropy in this region. To address this issue, we investigated the tectonics of the Afar region using receiver function and shear-wave splitting measurements based on broadband seismic data from 227 stations in the region. Further, the receiver function results were inverted to obtain the crustal thickness and V-p/V-s ratio of the region. Our results reveal a thick African crust (thicker than 40 km) with typical V-p/V-s values for the continental crust, elongated down to 21 km along the rift system with very high V-p/V-s values near the fractured zones, suggesting crustal thinning near the fractured zones. Our shear-wave splitting measurements indicate a general fast axis orientation of N030E. However, substantial disparities in the fast anisotropy direction exist in the triple junction region, with some stations displaying a direction of N120E, which is perpendicular to the fast directions measured at the surrounding stations. In addition, many stations located close to the rifts and within the Arabian Plate provide mostly null measurements, indicating the presence of fluids or isotropic media. This study uses several methodologies to unravel the structure and evolution of the Afar region, providing valuable insight into the Afar, a tectonically distinct region, which will be useful for elucidating the mechanisms and characteristics of a continental break-up and the rifting process.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10507 - Volcanology
Result continuities
Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2021
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Earth, Planets and Space
ISSN
1880-5981
e-ISSN
1880-5981
Volume of the periodical
73
Issue of the periodical within the volume
1
Country of publishing house
DE - GERMANY
Number of pages
17
Pages from-to
166
UT code for WoS article
000688564300003
EID of the result in the Scopus database
2-s2.0-85113283441