DOI: 10.1016/j.epsl.2017.12.030
Scopus记录号: 2-s2.0-85040583686
论文题名: Lithospheric thickness under the Dinarides
作者: Belinić T. ; Stipčević J. ; Živčić M.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2018
卷: 484 起始页码: 229
结束页码: 240
语种: 英语
英文关键词: Dinarides
; lithoshpere–asthenosphere boundary
; receiver functions
Scopus关键词: Laboratories
; Tectonics
; Tomography
; Central Mediterranean
; Dinarides
; High degree of variability
; Lithosphere-asthenosphere boundary
; Lithospheric thickness
; Receiver functions
; S-receiver functions
; Upper mantle structure
; Structural geology
; asthenosphere
; geological mapping
; lithospheric structure
; plate tectonics
; seismicity
; slab
; tectonic plate
; tomography
; upper mantle
; Adriatic Sea
; Alps
; Dinaric Alps
; Eastern Alps
; Mediterranean Sea
; Pannonian Basin
英文摘要: The nature of the interaction between Adriatic and Euroasian lithospheric plates in the Dinarides is important for understanding the complex tectonic history of the central Mediterranean. Using the data from permanent and temporary seismic stations in the wider Dinaric region, we imaged the lithospheric and upper mantle structure under this area. Specifically, we focused on mapping the lithosphere asthenosphere boundary (LAB) using the S receiver functions in order to establish boundaries between different tectonic domains present in this region. The lithospheric thickness in the investigated area varies between ∼50 and ∼160 km with high degree of variability between adjacent tectonic realms. Below northwestern Dinarides the LAB depth varies between 100 and 120 km thinning towards Adriatic sea and Pannonian basin, to 90 and 70 km respectively. In the central Dinaric region (Lika region) we find anomalously thin lithosphere with thickness varying between 50 and 70 km and weak velocity gradient defining the LAB. Further south the signal from the LAB is more pronounced with lithosphere getting thicker again with average depths around 90 km. The intriguing observation of thinned lithosphere under central part of the Dinarides coincides with the zone of lower seismicity and with the tomographic images showing the slab gap in this area. © 2017 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/110067
Appears in Collections: 影响、适应和脆弱性 气候变化事实与影响
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作者单位: Department of Geophysics, Faculty of Science, University of Zagreb, Horvatovac 95, Zagreb, 10000, Croatia; Slovenian Environment Agency, Vojkova 1b, Ljubljana, SI-1000, Slovenia
Recommended Citation:
Belinić T.,Stipčević J.,Živčić M.. Lithospheric thickness under the Dinarides[J]. Earth and Planetary Science Letters,2018-01-01,484