Wavefield Reconstruction of Teleseismic Receiver Function with the Stretching‐and‐Squeezing Interpolation Method

2018 ◽  
Vol 90 (2A) ◽  
pp. 716-726 ◽  
Author(s):  
Shaoqian Hu ◽  
Xiaohuan Jiang ◽  
Lupei Zhu ◽  
Huajian Yao
Keyword(s):  
Interpolation Method ◽  
Receiver Function ◽  
Teleseismic Receiver Function

scholarly journals Wavefield reconstruction of teleseismic receiver function with the stretching‐and‐squeezing interpolation method

2019 ◽  
Vol 93 (S1) ◽  
pp. 321-321
Author(s):  
Shaoqian Hu ◽  
Lupei Zhu ◽  
Huajian Yao
Keyword(s):  
Interpolation Method ◽  
Receiver Function ◽  
Teleseismic Receiver Function

Crustal Structure Beneath the Indo-Burma Ranges from the Teleseismic Receiver Function and Its Implications for Dehydration of the Subducting Indian Slab

2021 ◽  
Author(s):  
Dipok K. Bora ◽  
A. P. Singh ◽  
Kajaljyoti Borah ◽  
Aakash Anand ◽  
Rajib Biswas ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Receiver Function ◽  
Teleseismic Receiver Function

Sediment Thickness and Moho Depth Beneath Western Indonesian Region From Teleseismic Receiver Function

2021 ◽  
Author(s):  
Syaiful Bahri ◽  
Wiwit Suryanto ◽  
Drajat Ngadmanto
Keyword(s):  
Shear Wave ◽  
Shear Wave Velocity ◽  
Receiver Function ◽  
Velocity Model ◽  
Moho Depth ◽  
Sediment Layer ◽  
The North ◽  
East Kalimantan ◽  
Crust Layer ◽  
Teleseismic Receiver Function

Abstract The Earth's crust layer and sediment in Western Indonesia has been studied using the inversion of teleseismic receiver function from BMKG’s seismic network. Earthquake events were analyzed in this study with a moment magnitude greater than 6.0 with epicentral distances of 30° to 90°. A total of 60 earthquake events were observed and recorded by 91 stations around the study area. Furthermore, an inversion process was carried out using the initial velocity model from the modification of the AK135f velocity model to obtain the shear wave velocity structure below each stations. The velocity model from the azimuthally stacked vertical receiver function showed that the sediment layer had a relatively medium shear wave velocity value with an average of 2.1 km/s, while the crust layer had 4.60 km/s. The sedimentary layer thickness in this region also varies between 2 km to 10 km. A relatively thick sediment layer of about 8 km to 10 km was observed in two locations, in East Kalimantan associated with the Kutai Basin and Northern part of Sumatera in the North Sumatera Basin, a two major oil producer basinal area in Indonesia. The Moho discontinuity was also found at depths that vary between 16 km to 50 km. In addition, the most shallow Moho depth is 16 km below the North Kalimantan and North part of West Java, while the deeper Moho depth of 50 km is located below East Kalimantan, Central Kalimantan, North Sumatera and South Sumatera.

Nature of crust beneath Sri Lanka using teleseismic receiver function

2020 ◽  
Vol 187 ◽  
pp. 104096 ◽  
Author(s):  
Pousali Mukherjee ◽  
Kajaljyoti Borah ◽  
Dipok K. Bora
Keyword(s):  
Sri Lanka ◽  
Receiver Function ◽  
Teleseismic Receiver Function

scholarly journals Predictive models for the deep geometry of a thick-skinned thrust matched to crustal structure: Wind River Range, western USA

Lithosphere ◽  
2019 ◽  
Vol 11 (4) ◽  
pp. 448-464
Author(s):  
Richard H. Groshong ◽  
Ryan Porter
Keyword(s):  
Crustal Structure ◽  
Receiver Function ◽  
Function Analysis ◽  
Trailing Edge ◽  
Circular Arc ◽  
Wind River Range ◽  
Arc Model ◽  
Receiver Function Analysis ◽  
Kinematic Models ◽  
Teleseismic Receiver Function

Abstract The ability of models designed to use near-surface structural information to predict the deep geometry of a faulted block is tested for a thick-skinned thrust by matching the surface geometry to the crustal structure beneath the Wind River Range, Wyoming, USA. The Wind River Range is an ∼100-km-wide, thick-skinned rotated basement block bounded on one side by a high-angle reverse fault. The availability of a deep seismic-reflection profile and a detailed crustal impedance profile based on teleseismic receiver-function analysis makes this location ideal for testing techniques used to predict the deep fault geometry from shallow data. The techniques applied are the kinematic models for a circular-arc fault, oblique simple-shear fault, shear fault-bend fold, and model-independent excess area balancing. All the kinematic models imply that the deformation cannot be exclusively rigid-body rotation but rather require distributed deformation throughout some or all of the basement. Both the circular-arc model and the oblique-shear models give nearly the same best fit to the master fault geometry. The predicted lower detachment matches a potential crustal detachment zone at 31 km subsea. The thrust ramp is located close to where this zone dies out to the southwest. The circular-arc model implies that the penetrative deformation could be focused at the trailing edge of the basement block rather than being distributed uniformly throughout and thus helps to explain the line of second-order anticlines along the trailing edge of the Wind River block. Key points: (1) The circular-arc fault model and the oblique-shear model predict a lower detachment for the Wind River rotated block to be ∼31 km subsea, consistent with the crustal structure as defined by teleseismic receiver-function analysis. The thrust ramp starts where this zone dies out. (2) The kinematic models require distributed internal deformation within the basement block, probably concentrated at the trailing edge. (3) The uplift at the trailing edge of the rotated block is explained by the circular-arc kinematic model as a requirement to maintain area balance of a mostly rigid block above a horizontal detachment; the oblique-shear model can explain the uplift as caused by displacement on a dipping detachment.

scholarly journals Crustal structure and deformation beneath the NE margin of the Tibetan plateau constrained by teleseismic receiver function data

2015 ◽  
Vol 204 (1) ◽  
pp. 167-179 ◽  
Author(s):  
Qiong Wang ◽  
Fenglin Niu ◽  
Yuan Gao ◽  
Yuntai Chen
Keyword(s):  
Tibetan Plateau ◽  
Crustal Structure ◽  
Receiver Function ◽  
The Tibetan Plateau ◽  
Function Data ◽  
Teleseismic Receiver Function

scholarly journals Seismic imaging of crust beneath the Dharwar Craton, India, from ambient noise and teleseismic receiver function modelling

2014 ◽  
Vol 197 (2) ◽  
pp. 748-767 ◽  
Author(s):  
Kajaljyoti Borah ◽  
S. S. Rai ◽  
K. S. Prakasam ◽  
Sandeep Gupta ◽  
Keith Priestley ◽  
...  
Keyword(s):  
Ambient Noise ◽  
Seismic Imaging ◽  
Receiver Function ◽  
Dharwar Craton ◽  
Function Modelling ◽  
Teleseismic Receiver Function

A study on deep structure using teleseismic receiver function in Western Yunnan

2004 ◽  
Vol 17 (3) ◽  
pp. 262-271 ◽  
Author(s):  
Chuan-song He ◽  
Chun-yong Wang ◽  
Jian-ping Wu
Keyword(s):  
Deep Structure ◽  
Receiver Function ◽  
Western Yunnan ◽  
Teleseismic Receiver Function
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