R
Renqi Lu
Researcher at China Earthquake Administration
Publications - 29
Citations - 756
Renqi Lu is an academic researcher from China Earthquake Administration. The author has contributed to research in topics: Fault (geology) & Geology. The author has an hindex of 11, co-authored 23 publications receiving 512 citations. Previous affiliations of Renqi Lu include National Taiwan University.
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Philippine Sea and East Asian plate tectonics since 52 Ma constrained by new subducted slab reconstruction methods
TL;DR: The authors reconstructed the Philippine Sea and East Asian plate tectonics from 28 slabs mapped in 3D from global tomography, with a subducted area of ~25% of present-day global oceanic lithosphere.
Journal Article
Philippine Sea and East Asian plate tectonics since 52 Ma constrained by new subducted slab reconstruction methods
TL;DR: This article reconstructed the Philippine Sea and East Asian plate tectonics from 28 slabs mapped in 3D from global tomography, with a subducted area of ~25% of present-day global oceanic lithosphere.
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Late Cenozoic thrusting of major faults along the central segment of Longmen Shan, eastern Tibet: Evidence from low-temperature thermochronology
TL;DR: In this paper, the authors collected 22 samples from vertical profiles in the Xuelongbao Massif and the range frontal area located at the hanging walls of the Wenchuan-Maoxian Fault and Jiangyou-Guanxian Fault respectively, and conduct apatite and zircon fission track analyses.
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Parallelism between the maximum exhumation belt and the Moho ramp along the eastern Tibetan Plateau margin: Coincidence or consequence?
TL;DR: In this paper, the authors evaluate the timing and rate of uplift on the principle crustal faults in the central Longmen Shan along the eastern Tibetan Plateau margin, including mid-crustal channel flow, upper crustal shortening, and whole crust shearing.
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Sedimentary provenance constraints on the Jurassic to Cretaceous paleogeography of Sichuan Basin, SW China
TL;DR: The provenance of Jurassic to Cretaceous sediments in the Sichuan Basin is constrained by sandstone petrology and detrital zircon U-Pb geochronology as discussed by the authors.