Crustal structure of the southeastern margin of the Ordos Block |
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Authors: | Lu YiFeng Xu MingJie Wang LiangShu Mi Ning Li Hua Yu DaYong |
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Affiliation: | LU YiFeng*,XU MingJie*,WANG LiangShu,MI Ning,LI Hua & YU DaYong School of Earth Sciences and Engineering,Nanjing University,Nanjing 210093,China |
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Abstract: | We use a profile made up of teleseismic receiver functions to study the crustal thickness and structure of the southeastern
margin of the Ordos Block. The Mohorovičić discontinuity(Moho) has been identified beneath all stations. Its depth gradually
decreases towards the southeast, from about 43 km in the Ordos Block to ∼30 km near the northern margin of the Qinling Orogen.
Our results show clear lateral variations in the structure of the crust and the features of the Moho. Accordingly, the study
region can be divided into four parts: (1) Beneath the Ordos Block, the Moho is visible and flat at a depth of ∼40 km. The
crustal structure is best characterized by stable cratonic crust. (2) In the Weihe-Shanxi Graben, the Moho is uplifted by
about 3 km, which may be the result of upwelling of upper mantle materials. (3) Under the Xionger-Funiu Mountains, the Moho
is flat at a depth between 36 and 33 km, but becomes shallower towards the southeast. (4) In the Hehuai Basin, adjacent to
the northern margin of the Qinling Orogen, the Moho shows strong lateral variations with a mean depth of ∼31 km. The crustal
structure here is complex, which may indicate a complicated tectonic environment. Additionally, the Moho is clearly interrupted
at two locations (beneath stations st11 and st18) near major tectonic boundaries. These results suggest that the structure
of the deep crust along the southeastern margin of the Ordos Block has great lateral variability, which strongly affects the
complex geological features on the surface. Furthermore, these results can help us understand the interrelationships of different
parts of the southeastern margin of the Ordos Block. |
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Keywords: | receiver function crustal structure Moho H-κ stacking CCP migration |
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