Growth of the Qaidam Basin during Cenozoic exhumation in the northern Tibetan Plateau: Inferences from depositional patterns and multiproxy detrital provenance signatures-Reference-Cited by-同舟云学术

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Growth of the Qaidam Basin during Cenozoic exhumation in the northern Tibetan Plateau: Inferences from depositional patterns and multiproxy detrital provenance signatures

Published:2015-12-07 Issue:1 Volume:8 Page:58-82
ISSN:1941-8264
Container-title:Lithosphere
language:en
Short-container-title:Lithosphere

Author:

Bush Meredith A.,Saylor Joel E.,Horton Brian K.,Nie Junsheng

Publisher

GeoScienceWorld

Subject

Geology

Cited by 142 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Detrital muscovite 40Ar/39Ar geochronology and provenance of Cenozoic deposits in the Qaidam basin, northern Tibetan Plateau and comparison with detrital zircon and apatite records;Marine and Petroleum Geology;2024-11

2. Fracture stratigraphy in oil-rich shale of the Upper Xiaganchaigou Formation (upper Eocene), western Qaidam Basin;Marine and Petroleum Geology;2024-09

3. Grain textural bias in detrital single-mineral provenance studies;Sedimentary Geology;2024-09

4. Variability in interseismic strain accumulation rate and style along the Altyn Tagh Fault;Nature Communications;2024-08-11

5. June insolation gradient and ice sheet forcing on Qaidam precipitation during the middle Piacenzian warm period;Palaeogeography, Palaeoclimatology, Palaeoecology;2024-08

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