scholarly journals The crustal structure of south central Mongolia using receiver functions

Tectonics ◽  
2016 ◽  
Vol 35 (6) ◽  
pp. 1392-1403 ◽  
Author(s):  
Jing He ◽  
Qingju Wu ◽  
Eric Sandvol ◽  
James Ni ◽  
Andrea Gallegos ◽  
...  
2020 ◽  
Author(s):  
Mohammed Bello ◽  
David G. Cornwell ◽  
Nicholas Rawlinson ◽  
Anya M. Reading ◽  
Othaniel K. Likkason

Abstract. In an effort to improve our understanding of southeast Australia’s enigmatic tectonic evolution, we analyse teleseismic earthquakes recorded by 24 temporary and 8 permanent broadband stations using the receiver function method. Crustal thickness, bulk seismic velocity and internal crustal structure of the southern Tasmanides – an assemblage of Palaeozoic accretionary orogens that occupy eastern Australia – are constrained by our new results which point to: (1) a 39.0 ± 0.5 km thick crust, a relatively high Poisson’s ratio (0.262 ± 0.014) and a broad (> 10 km) crust-mantle transition beneath the Lachlan Fold Belt. This is interpreted to represent magmatic underplating of mafic materials at the base of the crust; (2) a complex crustal structure beneath VanDieland, a postulated Precambrian continental fragment embedded in the southernmost Tasmanides, where the crust thickens (37.5 ± 1.2 km) towards the northern tip of the microcontinent as it enters south central Victoria but thins south into Bass Strait (30.5 ± 2.1 km), before once again becoming thicker beneath western Tasmania (33.5 ± 1.9 km). The thinner crust beneath Bass Strait can be attributed to lithospheric stretching that resulted from the break-up of Antarctica and Australia and the opening of the Tasman Sea; (3) stations located in the East Tasmania Terrane and eastern Bass Strait (ETT+EB) collectively indicate crust of uniform thickness (∼ 33 km) and a slightly broad Moho transition that reflect a possible underplating event associated with a Palaeozoic subduction system. The relative uniformity of Vp/Vs and Poisson’s ratio in VanDieland – suggesting uniformity in composition – could be used in support of the VanDieland microcontinental model that explains the tectonic evolution of southeast Australia.


2010 ◽  
Vol 11 (8) ◽  
pp. n/a-n/a ◽  
Author(s):  
Y. Dzierma ◽  
M. M. Thorwart ◽  
W. Rabbel ◽  
E. R. Flueh ◽  
G. E. Alvarado ◽  
...  

2014 ◽  
Vol 96 ◽  
pp. 237-254 ◽  
Author(s):  
Sumer Chopra ◽  
Tao-Ming Chang ◽  
Sowrav Saikia ◽  
R.B.S. Yadav ◽  
Pallabee Choudhury ◽  
...  

2016 ◽  
Vol 64 (6) ◽  
pp. 2020-2049 ◽  
Author(s):  
Syuhada Syuhada ◽  
Nugroho Dwi Hananto ◽  
Chalid I. Abdullah ◽  
Nanang T. Puspito ◽  
Titi Anggono ◽  
...  

2019 ◽  
Vol 751 ◽  
pp. 41-53 ◽  
Author(s):  
Carolina Buffoni ◽  
Martin Schimmel ◽  
Nora Cristina Sabbione ◽  
María Laura Rosa ◽  
Gerardo Connon

2017 ◽  
Vol 122 (10) ◽  
pp. 7839-7859 ◽  
Author(s):  
Arun Singh ◽  
M. Ravi Kumar ◽  
Debasis D. Mohanty ◽  
Chandrani Singh ◽  
Rahul Biswas ◽  
...  

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