Application of the Material Balance Method in Paleoelevation Recovery: A Case Study of the Longmen Mountains Foreland Basin on the Eastern Margin of the Tibetan Plateau
Yan Zhaokun1,2; Li Yong1,2; Li Haibing3; Dong Shunli4; Zhao Guohua1,2; Li Jingbo1,2; Li Fensheng1,2; Yan Liang1,2; Zheng Lilong1,2
刊名ACTA GEOLOGICA SINICA-ENGLISH EDITION
2015-04-01
卷号89期号:2页码:598-609
关键词Longmen Mountains foreland basin material balance method paleoelevation recovery the eastern margin of the Tibetan Plateau
DOI10.1111/1755-6724.12450
文献子类Article
英文摘要We applied the material balance principle of the denudation volume and sedimentary flux to study the denudation-accumulation system between the Longmen Mountains (Mts.) and the foreland basin. The amount of sediment in each sedimentation stage of the basin was estimated to obtain the denudation volume, erosion thickness and deposit thickness since the Late Triassic Epoch, to enable us to recover the paleoelevation of the provenance and the sedimentary area. The results show the following: (1) Since the Late Triassic Epoch, the elevation of the surface of the Longmen Mts. has uplifted from 0 m to 2751 m, and the crust of the Longmen Mts. has uplifted by 9.8 km. Approximately 72% of the materials introduced have been denuded from the mountains. (2) It is difficult to recover the paleoelevation of each stage of the Longmen Mts. foreland basin quantitatively by the present-day techniques and data. (3) The formation of the Longmen Mts. foreland basin consisted of three stages of thrust belt tectonic load and three stages of thrust belt erosional unload. During tectonic loading stages (Late Triassic Epoch, Late Jurassic-Early Cretaceous, Late Cretaceous-Miocene), the average elevation of Longmen Mts. was lower (approximately 700-1700 m). During erosional unloading stages (Early and Middle Jurassic, Middle Cretaceous and Jiaguan, Late Cenozoic), the average elevation of Longmen Mts. was high at approximately 2000-2800m.
WOS关键词WENCHUAN EARTHQUAKE ; SEDIMENT ; SECTION ; UPLIFT ; FAULT ; SHAN
WOS研究方向Geology
语种英语
WOS记录号WOS:000353982500023
资助机构National Natural Science Foudation of China(41372114 ; National Natural Science Foudation of China(41372114 ; 41340005 ; 41340005 ; 41172162 ; 41172162 ; 40972083) ; 40972083) ; National Natural Science Foudation of China(41372114 ; National Natural Science Foudation of China(41372114 ; 41340005 ; 41340005 ; 41172162 ; 41172162 ; 40972083) ; 40972083)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/62527]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
作者单位1.Chengdu Univ Technol, Inst Sedimentray Geol, Chengdu 610059, Sichuan, Peoples R China
2.State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Sichuan, Peoples R China
3.Chinese Acad Geol Sci, Inst Geol, State Key Lab Continental Tecton & Dynam, Beijing 100037, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Yan Zhaokun,Li Yong,Li Haibing,et al. Application of the Material Balance Method in Paleoelevation Recovery: A Case Study of the Longmen Mountains Foreland Basin on the Eastern Margin of the Tibetan Plateau[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2015,89(2):598-609.
APA Yan Zhaokun.,Li Yong.,Li Haibing.,Dong Shunli.,Zhao Guohua.,...&Zheng Lilong.(2015).Application of the Material Balance Method in Paleoelevation Recovery: A Case Study of the Longmen Mountains Foreland Basin on the Eastern Margin of the Tibetan Plateau.ACTA GEOLOGICA SINICA-ENGLISH EDITION,89(2),598-609.
MLA Yan Zhaokun,et al."Application of the Material Balance Method in Paleoelevation Recovery: A Case Study of the Longmen Mountains Foreland Basin on the Eastern Margin of the Tibetan Plateau".ACTA GEOLOGICA SINICA-ENGLISH EDITION 89.2(2015):598-609.
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