{"title":"河流捕获加强了珠穆朗玛峰的隆起","authors":"","doi":"10.1038/s41561-024-01557-4","DOIUrl":null,"url":null,"abstract":"Modelling of the evolution of the Kosi drainage basin near Chomolungma suggests that a river capture event occurred approximately 89 ka ago. Isostatic rebound due to this capture event could contribute 10–50% of the total rock uplift rate in the Chomolungma region and might partly explain Chomolungma’s renewed uplift rate and anomalous elevation.","PeriodicalId":19053,"journal":{"name":"Nature Geoscience","volume":"17 10","pages":"961-962"},"PeriodicalIF":15.7000,"publicationDate":"2024-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"River capture enhances the uplift of Chomolungma\",\"authors\":\"\",\"doi\":\"10.1038/s41561-024-01557-4\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Modelling of the evolution of the Kosi drainage basin near Chomolungma suggests that a river capture event occurred approximately 89 ka ago. Isostatic rebound due to this capture event could contribute 10–50% of the total rock uplift rate in the Chomolungma region and might partly explain Chomolungma’s renewed uplift rate and anomalous elevation.\",\"PeriodicalId\":19053,\"journal\":{\"name\":\"Nature Geoscience\",\"volume\":\"17 10\",\"pages\":\"961-962\"},\"PeriodicalIF\":15.7000,\"publicationDate\":\"2024-09-30\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Nature Geoscience\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.nature.com/articles/s41561-024-01557-4\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Nature Geoscience","FirstCategoryId":"89","ListUrlMain":"https://www.nature.com/articles/s41561-024-01557-4","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Modelling of the evolution of the Kosi drainage basin near Chomolungma suggests that a river capture event occurred approximately 89 ka ago. Isostatic rebound due to this capture event could contribute 10–50% of the total rock uplift rate in the Chomolungma region and might partly explain Chomolungma’s renewed uplift rate and anomalous elevation.
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Nature Geoscience is a monthly interdisciplinary journal that gathers top-tier research spanning Earth Sciences and related fields.
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Topics include atmospheric science, biogeochemistry, climate science, geobiology, geochemistry, geoinformatics, remote sensing, geology, geomagnetism, paleomagnetism, geomorphology, geophysics, glaciology, hydrology, limnology, mineralogy, oceanography, paleontology, paleoclimatology, paleoceanography, petrology, planetary science, seismology, space physics, tectonics, and volcanology.
Nature Geoscience upholds its commitment to publishing significant, high-quality Earth Sciences research through fair, rapid, and rigorous peer review, overseen by a team of full-time professional editors.
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