Crustal characteristics beneath the Tien Shan belt, Central Asia, using the seismic receiver function
The crustal structure beneath Tien Shan belt was evaluated using teleseismic waveforms from 20 broadband stations and gravity modeling as well. The crustal thickness varies from 36 km to 68 km where the crust thickens due north and the southwest of Tien Shan, while the central part has a thin crust....
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| Published in | Journal of King Saud University. Science Vol. 32; no. 3; pp. 2157 - 2162 |
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| Main Author | |
| Format | Journal Article |
| Language | English |
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Elsevier B.V
01.04.2020
Elsevier |
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| Abstract | The crustal structure beneath Tien Shan belt was evaluated using teleseismic waveforms from 20 broadband stations and gravity modeling as well. The crustal thickness varies from 36 km to 68 km where the crust thickens due north and the southwest of Tien Shan, while the central part has a thin crust. The area of interest has Vp/Vs ratio of 1.81 ± 0.025, indicating a mafic crust, detached by Moho from the mantle. Additionally, collision zone between Tien Shan and the Tarim Basin has the thickest crust and highest Φ values. The average Moho sharpness, R (0.17), is comparable to that of the typical crust and decreases due northwest. Stations east of the Talas-Fergana strike-slip fault show low Vp/Vs ratios and anomalously thin crust of about 42 km, probably suggesting delamination of the lower crust. The average Bouguer anomalies are large and negative, particularly near the stations in the southern part of Tien Shan where the elevations are the highest. The study suggests these large negative values beneath Tien Shan are a result of thickening of the lithosphere. |
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| AbstractList | The crustal structure beneath Tien Shan belt was evaluated using teleseismic waveforms from 20 broadband stations and gravity modeling as well. The crustal thickness varies from 36 km to 68 km where the crust thickens due north and the southwest of Tien Shan, while the central part has a thin crust. The area of interest has Vp/Vs ratio of 1.81 ± 0.025, indicating a mafic crust, detached by Moho from the mantle. Additionally, collision zone between Tien Shan and the Tarim Basin has the thickest crust and highest Φ values. The average Moho sharpness, R (0.17), is comparable to that of the typical crust and decreases due northwest. Stations east of the Talas-Fergana strike-slip fault show low Vp/Vs ratios and anomalously thin crust of about 42 km, probably suggesting delamination of the lower crust. The average Bouguer anomalies are large and negative, particularly near the stations in the southern part of Tien Shan where the elevations are the highest. The study suggests these large negative values beneath Tien Shan are a result of thickening of the lithosphere. The crustal structure beneath Tien Shan belt was evaluated using teleseismic waveforms from 20 broadband stations and gravity modeling as well. The crustal thickness varies from 36 km to 68 km where the crust thickens due north and the southwest of Tien Shan, while the central part has a thin crust. The area of interest has Vp/Vs ratio of 1.81 ± 0.025, indicating a mafic crust, detached by Moho from the mantle. Additionally, collision zone between Tien Shan and the Tarim Basin has the thickest crust and highest Φ values. The average Moho sharpness, R (0.17), is comparable to that of the typical crust and decreases due northwest. Stations east of the Talas-Fergana strike-slip fault show low Vp/Vs ratios and anomalously thin crust of about 42 km, probably suggesting delamination of the lower crust. The average Bouguer anomalies are large and negative, particularly near the stations in the southern part of Tien Shan where the elevations are the highest. The study suggests these large negative values beneath Tien Shan are a result of thickening of the lithosphere. Keywords: Crustal structure, Moho, Vp/Vs ratio, Receiver function, Tien Shan |
| Author | Almadani, Sattam A. |
| Author_xml | – sequence: 1 givenname: Sattam A. surname: Almadani fullname: Almadani, Sattam A. email: salmadani@ksu.edu.sa organization: Department of Geology and Geophysics, College of Science, King Saud University, Riyadh, Saudi Arabia |
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| CitedBy_id | crossref_primary_10_1016_j_tecto_2022_229677 |
| Cites_doi | 10.1029/JB095iB10p15303 10.1130/0016-7606(1996)108<1004:LCSOTT>2.3.CO;2 10.1029/JB089iB07p06203 10.1016/0012-821X(74)90052-1 10.1144/GSL.SP.1988.037.01.09 10.1029/JB084iB07p03425 10.1134/S1069351306080027 10.1214/ss/1177013815 10.1029/2005JB003802 10.1126/science.189.4201.419 10.1016/j.tecto.2008.10.010 10.1029/92JB01963 10.1029/1999JB900322 10.1016/j.tecto.2009.05.007 10.1038/384450a0 10.1029/97TC03140 10.3126/hjs.v2i4.817 10.1016/0012-821X(90)90013-N 10.1029/97GL01434 10.1016/j.epsl.2004.04.015 10.1007/BF02910304 10.1016/j.epsl.2004.05.039 10.1029/2001GL014588 10.1029/98GL00516 10.1029/95JB02158 |
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| Issue | 3 |
| Keywords | Tien Shan Vp/Vs ratio Receiver function Crustal structure Moho |
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| Title | Crustal characteristics beneath the Tien Shan belt, Central Asia, using the seismic receiver function |
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