Present-day crustal uplift and dynamic process of the Tibetan Plateau from multiple geodetic observations

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This preprint studied present-day vertical land motion and crustal uplift on the Tibetan Plateau using geodetic observations, combining GNSS and precise leveling with a hydrological load deformation model that integrates GRACE/GFO satellite gravity and a surface hydrological fusion model. After correcting for surface elastic deformation and accounting for geocentric motion (-0.1 to -0.2 mm yr−1) and glacial isostatic adjustment (0.3 to 0.4 mm yr−1), the authors report significant uplift in the southern and northeastern plateau (up to 2 mm yr−1), attributing it primarily to plate compression, while the north and southeast show more complex vertical tectonic behavior possibly linked to block extrusion and mid-lower crustal flow. A major caveat is that the work is a Research Square preprint that has not been peer reviewed. The paper does not explicitly discuss endometriosis or adenomyosis; it was included in the corpus via a keyword match in the upstream search index.

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Abstract Vertical land motion (VLM) on the Tibetan Plateau (TP) is influenced by various geophysical factors, including surface fluid mass variations and tectonic deformation. In this study, we investigate the present-day crustal uplift in the TP using geodetic observations, including Global Navigation Satellite System (GNSS) and precise leveling. A hydrological load deformation model is formulated by integrating the Gravity Recovery and Climate Experiment and Follow-On (GRACE/GFO) satellite gravity with a surface hydrological fusion model. Tectonic-induced VLM is calculated after correcting for surface elastic deformation, geocentric motion (-0.1 to -0.2 mm yr-1) and glacial isostatic adjustment (0.3 to 0.4 mm yr− 1). The comprehensive VLM imaging and dynamic tomography reveal significant crustal uplift in the southern and northeastern TP, with uplift rates up to 2 mm yr-1, primarily attributed to plate compression. The northern and southeastern TP exhibit complex vertical tectonic movements, potentially influenced by block extrusion and mid-lower crustal flow.
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Present-day crustal uplift and dynamic process of the Tibetan Plateau from multiple geodetic observations | Research Square window.SnipcartSettings = { analytics: { enabled: false } }; (function() { var accessVector = localStorage.getItem('access_vector') || ''; window.dataLayer = window.dataLayer || []; if (accessVector) { window.dataLayer.push({ user: { profile: { profileInfo: { snid: accessVector } } } }); } })(); (function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start':new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0],j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src='https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f);})(window,document,'script','dataLayer','GTM-K279D39R'); Browse Preprints In Review Journals COVID-19 Preprints AJE Video Bytes Research Tools Research Promotion AJE Professional Editing AJE Rubriq About Preprint Platform In Review Editorial Policies Our Team Advisory Board Help Center Sign In Submit a Preprint Cite Share Download PDF Article Present-day crustal uplift and dynamic process of the Tibetan Plateau from multiple geodetic observations Yuanjin Pan, Zhenhong Li, Jiashuang Jiao, Meilin He, Jiangtao Li, and 2 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-4816952/v1 This work is licensed under a CC BY 4.0 License Status: Posted Version 1 posted You are reading this latest preprint version Abstract Vertical land motion (VLM) on the Tibetan Plateau (TP) is influenced by various geophysical factors, including surface fluid mass variations and tectonic deformation. In this study, we investigate the present-day crustal uplift in the TP using geodetic observations, including Global Navigation Satellite System (GNSS) and precise leveling. A hydrological load deformation model is formulated by integrating the Gravity Recovery and Climate Experiment and Follow-On (GRACE/GFO) satellite gravity with a surface hydrological fusion model. Tectonic-induced VLM is calculated after correcting for surface elastic deformation, geocentric motion (-0.1 to -0.2 mm yr-1) and glacial isostatic adjustment (0.3 to 0.4 mm yr − 1 ). The comprehensive VLM imaging and dynamic tomography reveal significant crustal uplift in the southern and northeastern TP, with uplift rates up to 2 mm yr-1, primarily attributed to plate compression. The northern and southeastern TP exhibit complex vertical tectonic movements, potentially influenced by block extrusion and mid-lower crustal flow. Earth and environmental sciences/Solid Earth sciences/Geophysics Earth and environmental sciences/Solid Earth sciences/Tectonics GNSS and leveling measurements Elastic deformation induced by hydrological load Nonlinear fluctuations within the GNSS Imaged vertical crustal deformation of Tibetan Plateau Coupling between crustal uplift and tectonic dynamics Full Text Additional Declarations There is NO Competing Interest. Cite Share Download PDF Status: Posted Version 1 posted You are reading this latest preprint version Research Square lets you share your work early, gain feedback from the community, and start making changes to your manuscript prior to peer review in a journal. As a division of Research Square Company, we’re committed to making research communication faster, fairer, and more useful. We do this by developing innovative software and high quality services for the global research community. Our growing team is made up of researchers and industry professionals working together to solve the most critical problems facing scientific publishing. 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