Articles | Volume 10, issue 3
https://doi.org/10.5194/se-10-647-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-10-647-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
16 May 2019
Research article |
| 16 May 2019
| 16 May 2019
Regional Pliocene exhumation of the Lesser Himalaya in the Indus drainage
Department of Geology and Geophysics, Louisiana State University, Baton
Rouge, LA 70803, USA
Research Center for Earth System Science. Yunnan University, Kunming, Yunnan
Province, 650091, China
Peng Zhou
Department of Geology and Geophysics, Louisiana State University, Baton
Rouge, LA 70803, USA
Daniel F. Stockli
Department of Geological Sciences, Jackson School of Geosciences, University
of Texas, Austin, TX 78712-1722, USA
Jerzy Blusztajn
Department of Geology and Geophysics, Woods Hole Oceanographic Institution,
Woods Hole, MA 02540, USA
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Cited
28 citations as recorded by crossref.
- Quantifying the Link Between the Detrital Zircon Record and Tectonic Settings D. Jian et al. 10.1029/2022JB024606
- Modern-like deep water circulation in Indian Ocean caused by Central American Seaway closure P. Prabhat et al. 10.1038/s41467-022-35145-0
- Monsoon controls on sediment generation and transport: Mass budget and provenance constraints from the Indus River catchment, delta and submarine fan over tectonic and multimillennial timescales P. Clift & T. Jonell 10.1016/j.earscirev.2021.103682
- Erosion of the Himalaya-Karakoram recorded by Indus Fan deposits since the Oligocene H. Feng et al. 10.1130/G48445.1
- Phased evolution and variation of the South Asian monsoon, and resulting weathering and surface erosion in the Himalaya–Karakoram Mountains, since late Pliocene time using data from Arabian Sea core H. Lu et al. 10.1017/S0016756820000291
- Palaeoredox reconstruction in the eastern Arabian Sea since the late Miocene: Insights from trace elements and stable isotopes of molybdenum (δ98/95Mo) and tungsten (δ186/184W) at IODP Site U1457 of Laxmi Basin M. Alam et al. 10.1016/j.palaeo.2021.110790
- The major uplift in Himalayas was no earlier than the Miocene: Evidence from marine sediment record in the Bay of Bengal Z. Song et al. 10.1016/j.palaeo.2024.112275
- Dust sources in Westernmost Asia have a different geochemical fingerprint to those in the Sahara T. Kunkelova et al. 10.1016/j.quascirev.2022.107717
- Provenance of Thal Desert sand: Focused erosion in the western Himalayan syntaxis and foreland-basin deposition driven by latest Quaternary climate change E. Garzanti et al. 10.1016/j.earscirev.2020.103220
- Neogene Kinematic Evolution and Exhumation of the NW India Himalaya: Zircon Geo‐ and Thermochronometric Insights From the Fold‐Thrust Belt and Foreland Basin C. Colleps et al. 10.1029/2018TC005304
- Variations in aridity across the Asia–Australia region during the Neogene and their impact on vegetation P. Clift 10.1144/SP549-2023-58
- Marine sedimentary records of chemical weathering evolution in the western Himalaya since 17 Ma P. Zhou et al. 10.1130/GES02211.1
- Chemical weathering and erosion responses to changing monsoon climate in the Late Miocene of Southwest Asia P. Clift et al. 10.1017/S0016756819000608
- Zircon U‐Pb Age Constraints on NW Himalayan Exhumation From the Laxmi Basin, Arabian Sea P. Zhou et al. 10.1029/2021GC010158
- Climate–tectonic interactions in the eastern Arabian Sea P. Clift et al. 10.1017/S0016756820000461
- Late Miocene changes in C3, C4 and aquatic plant vegetation in the Indus River basin: evidence from leaf wax δ13C from Indus Fan sediments K. Suzuki et al. 10.1017/S0016756819001109
- Persistent Provenance of South Asian Monsoon‐Induced Silicate Weathering Over the Past 27 Million Years S. Ali et al. 10.1029/2020PA003909
- U(‐Th)–Pb age and petrogenesis of Shigar leucogranites, Karakoram Metamorphic Complex, North Pakistan M. Awais et al. 10.1002/gj.4527
- Landform evolution in Asia during the Cenozoic revealed by formation of drainages of Wei River and Indus River H. Lu et al. 10.1016/j.palaeo.2023.111516
- Himalayan‐Tibetan Erosion Is Not the Cause of Neogene Global Cooling P. Clift & T. Jonell 10.1029/2020GL087742
- The impact of Himalayan-Tibetan erosion on silicate weathering and organic carbon burial P. Clift et al. 10.1016/j.chemgeo.2024.122106
- Slowing rates of regional exhumation in the western Himalaya: fission track evidence from the Indus Fan P. Zhou et al. 10.1017/S001675681900092X
- Clay-fraction strontium and neodymium isotopes in the Indus Fan: implications for sediment transport and provenance S. Carter et al. 10.1017/S0016756820000394
- When did the Indus River of South-Central Asia take on its “modern” drainage configuration? Y. Najman et al. 10.1130/B36596.1
- Seismic stratigraphy and the sedimentation history in the Laxmi Basin of the eastern Arabian Sea: Constraints from IODP Expedition 355 N. Nair et al. 10.1016/j.gsf.2020.11.008
- Cretaceous forearc basin remnant sediments in the eastern Yarlung Zangbo suture zone, near the eastern Himalaya syntaxis Z. Wei et al. 10.1016/j.palaeo.2021.110620
- Hydroclimatic conditions and sediment provenance in the northeastern Arabian Sea since the late Miocene: insights from geochemical and environmental magnetic records at IODP Site U1457 of the Laxmi Basin M. Alam et al. 10.1017/S0016756822001273
- Provenance, weathering, and paleoclimatic records of the Pliocene-Pleistocene sequences of the Himalayan foreland basin, NW Himalaya S. Ali et al. 10.1007/s12517-021-06461-4
27 citations as recorded by crossref.
- Quantifying the Link Between the Detrital Zircon Record and Tectonic Settings D. Jian et al. 10.1029/2022JB024606
- Modern-like deep water circulation in Indian Ocean caused by Central American Seaway closure P. Prabhat et al. 10.1038/s41467-022-35145-0
- Monsoon controls on sediment generation and transport: Mass budget and provenance constraints from the Indus River catchment, delta and submarine fan over tectonic and multimillennial timescales P. Clift & T. Jonell 10.1016/j.earscirev.2021.103682
- Erosion of the Himalaya-Karakoram recorded by Indus Fan deposits since the Oligocene H. Feng et al. 10.1130/G48445.1
- Phased evolution and variation of the South Asian monsoon, and resulting weathering and surface erosion in the Himalaya–Karakoram Mountains, since late Pliocene time using data from Arabian Sea core H. Lu et al. 10.1017/S0016756820000291
- Palaeoredox reconstruction in the eastern Arabian Sea since the late Miocene: Insights from trace elements and stable isotopes of molybdenum (δ98/95Mo) and tungsten (δ186/184W) at IODP Site U1457 of Laxmi Basin M. Alam et al. 10.1016/j.palaeo.2021.110790
- The major uplift in Himalayas was no earlier than the Miocene: Evidence from marine sediment record in the Bay of Bengal Z. Song et al. 10.1016/j.palaeo.2024.112275
- Dust sources in Westernmost Asia have a different geochemical fingerprint to those in the Sahara T. Kunkelova et al. 10.1016/j.quascirev.2022.107717
- Provenance of Thal Desert sand: Focused erosion in the western Himalayan syntaxis and foreland-basin deposition driven by latest Quaternary climate change E. Garzanti et al. 10.1016/j.earscirev.2020.103220
- Neogene Kinematic Evolution and Exhumation of the NW India Himalaya: Zircon Geo‐ and Thermochronometric Insights From the Fold‐Thrust Belt and Foreland Basin C. Colleps et al. 10.1029/2018TC005304
- Variations in aridity across the Asia–Australia region during the Neogene and their impact on vegetation P. Clift 10.1144/SP549-2023-58
- Marine sedimentary records of chemical weathering evolution in the western Himalaya since 17 Ma P. Zhou et al. 10.1130/GES02211.1
- Chemical weathering and erosion responses to changing monsoon climate in the Late Miocene of Southwest Asia P. Clift et al. 10.1017/S0016756819000608
- Zircon U‐Pb Age Constraints on NW Himalayan Exhumation From the Laxmi Basin, Arabian Sea P. Zhou et al. 10.1029/2021GC010158
- Climate–tectonic interactions in the eastern Arabian Sea P. Clift et al. 10.1017/S0016756820000461
- Late Miocene changes in C3, C4 and aquatic plant vegetation in the Indus River basin: evidence from leaf wax δ13C from Indus Fan sediments K. Suzuki et al. 10.1017/S0016756819001109
- Persistent Provenance of South Asian Monsoon‐Induced Silicate Weathering Over the Past 27 Million Years S. Ali et al. 10.1029/2020PA003909
- U(‐Th)–Pb age and petrogenesis of Shigar leucogranites, Karakoram Metamorphic Complex, North Pakistan M. Awais et al. 10.1002/gj.4527
- Landform evolution in Asia during the Cenozoic revealed by formation of drainages of Wei River and Indus River H. Lu et al. 10.1016/j.palaeo.2023.111516
- Himalayan‐Tibetan Erosion Is Not the Cause of Neogene Global Cooling P. Clift & T. Jonell 10.1029/2020GL087742
- The impact of Himalayan-Tibetan erosion on silicate weathering and organic carbon burial P. Clift et al. 10.1016/j.chemgeo.2024.122106
- Slowing rates of regional exhumation in the western Himalaya: fission track evidence from the Indus Fan P. Zhou et al. 10.1017/S001675681900092X
- Clay-fraction strontium and neodymium isotopes in the Indus Fan: implications for sediment transport and provenance S. Carter et al. 10.1017/S0016756820000394
- When did the Indus River of South-Central Asia take on its “modern” drainage configuration? Y. Najman et al. 10.1130/B36596.1
- Seismic stratigraphy and the sedimentation history in the Laxmi Basin of the eastern Arabian Sea: Constraints from IODP Expedition 355 N. Nair et al. 10.1016/j.gsf.2020.11.008
- Cretaceous forearc basin remnant sediments in the eastern Yarlung Zangbo suture zone, near the eastern Himalaya syntaxis Z. Wei et al. 10.1016/j.palaeo.2021.110620
- Hydroclimatic conditions and sediment provenance in the northeastern Arabian Sea since the late Miocene: insights from geochemical and environmental magnetic records at IODP Site U1457 of the Laxmi Basin M. Alam et al. 10.1017/S0016756822001273
Discussed (preprint)
Latest update: 14 Dec 2024
Short summary
Surface processes driven by climate have been linked to the tectonic evolution of mountain belts, with the Himalaya and Asian monsoon being classic examples. Sediments from the Arabian Sea show an increase in erosion from the Karakoram between 17 and 9.5 Ma, followed by an increase in the relative flux from the Himalaya after 5.7 Ma and especially from the Lesser Himalaya after 1.9 Ma. Lack of correlation with climate histories suggests that tectonic forces dominate control over erosion.
Surface processes driven by climate have been linked to the tectonic evolution of mountain...
