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Rui Gao

Researcher at Sun Yat-sen University

Publications -  39
Citations -  743

Rui Gao is an academic researcher from Sun Yat-sen University. The author has contributed to research in topics: Crust & Subduction. The author has an hindex of 12, co-authored 36 publications receiving 372 citations. Previous affiliations of Rui Gao include Ministry of Land and Resources of the People's Republic of China & Jilin University.

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A possible buried Paleoproterozoic collisional orogen beneath central South China: Evidence from seismic-reflection profiling

TL;DR: In this article, a 400 km-long high-resolution seismic reflection profile across the purported suture between the Yangtze and Cathaysia blocks was presented, revealing folded and thrust-imbricated seismic reflectors which were interpreted to represent the relics of the collisional orogen.
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Mantle influx compensates crustal thinning beneath the Cathaysia Block, South China: Evidence from SINOPROBE reflection profiling

TL;DR: In this article, the authors analyzed the whole crustal architecture of the Cathaysia Block, South China, through a ∼300 km-long SINOPROBE deep seismic reflection profile.
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Crustal thickness and Poisson's ratios of South China revealed from joint inversion of receiver function and gravity data

TL;DR: In this article, the authors improved the technique of the joint inversion of receiver function and gravity data and utilized it to improve the estimates of crustal thickness and Poisson's ratio in South China.
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SINOPROBE deep reflection profile reveals a Neo-Proterozoic subduction zone beneath Sichuan Basin

TL;DR: In this paper, a multichannel seismic reflection profile collected across the Sichuan Basin in southern China by SINOPROBE images prominent reflectors that originate within the lower crust and penetrate well into the underlying mantle.
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New images of the crustal structure beneath eastern Tibet from a high-density seismic array

TL;DR: In this paper, an east-west trending, high-density seismic array was deployed along the eastern margin of the Tibetan Plateau to investigate its eastward expansion, and the array included 330 short-period seismographs spaced at 500 m intervals, which recorded teleseismic 3-component waveforms over a one month period.